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Climate Change Driven Variations in the Wave Climate along the Coast of Vietnam Rev.5
March 2014
Authors :
Supott Thammasittirong (AIT) Sutat Weesakul (AIT)
Ali Dastgheib (UNESCO-IHE) Roshanka Ranasinghe (UNESCO-IHE)
i
Executive Summary
Introduction
This report presents the results of the study of the Climate Change Driven Variations
in the Wave Climate along the Coast of Vietnam. This project was funded by Ministry
of environment and infrastructure of the Netherlands.
Vietnam has been identified by the International Panel on Climate Change (IPCC,
2007, 2014) as one of the countries that might be most affected by climate change. In
particular the Mekong and the Red River deltas, with their extremely high population
density in low lying areas, are severely threatened by sea level rise and anticipated
increases in the frequency and intensity of typhoons and storms. The coastline of
Vietnam is presently severely eroded and mangrove forests are reduced in area and
density by severe storms and sea level rise.
Changes in regional wave climate, in response to climate change driven variations of
atmospheric circulation, are of interest from many different perspectives, particularly
in the coastal zone. Significant change in wave climate due to climate change in turn
will affect the coastal morphology, coastline position and orientation and the efficacy
of coastal structures.
To this date, no study has been carried out to determine the effect of climate change on
the offshore wave climate along this coast. The present study was undertaken to
address this knowledge gap.
Objective
The main objective of this study is to determine the effect of climate change on the
offshore wave climate along the entire coastline of Vietnam.
Methodology
In this study, a third generation numerical wave model forced with future projected
wind data from selected Global Circulation Models (GCMs) is used to simulate the
future offshore wave climate along Vietnam coast.
A MIKE21 model was setup for the South China Sea and the Gulf of Thailand. Results
were subjected to detailed analysis at 14 locations along the coast of Vietnam (Figure
E-1).
The model is forced by NCEP/CFSR winds (benchmark simulation) and climate
model derived winds with 2 GCMs (GFDL CM 2.1 and ECHAM5), that had been
downscaled by CSIRO’s Cubic Conformal Atmospheric Model (CCAM) at 0.5° x 0.5°
resolution. The model is validated by running hindcast simulations for the1981 to
2000 time slice (i.e. present condition) and comparing model results with wave data
from the ship observations at two locations, Hon Dau and Hon Ngu and with ERA-40
wave data at three locations, Point B, Point E and Point K (Figure E-1). The mean
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significant wave height, wave period and wave direction from simulations with
NCEP/CFSR, ECHAM and GFDL wind input for the 1981 - 2000 time slice showed
very small differences. Thus the model was considered sufficiently validated.
Subsequently, the model was used to simulate the future time slices 2041 - 2060 and
2081 - 2100 forced with downscaled winds from GFDL CM 2.1 and ECHAM5 for the
high end A2 climate change scenario (comparable to RCP 8.5 in IPCC 2013).
Figure E-1. Offshore locations along the Vietnam coast at which the effect of climate change
on the wave climate was analysed (shown by red tick sysmbols).
Summary Results
Future mean significant wave height under the effect of climate change along the
North coast of Vietnam is projected to be smaller by about 8 cm (compared to the
present) with slightly longer wave periods (increase of 0.20 s), while future wave
direction is projected to shift towards the south (clockwise) by less than 4 degrees.
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Along the central coast, future mean significant wave height is projected to slightly
increase by 5 cm, wave period to increase by less than 0.08 s and wave direction is
projected to shift to the south (clockwise) by less than 6 degrees. Along the South
coast of Vietnam, the future mean significant wave height is projected to slightly
increase by 7 cm with longer wave period (increase of 0.16 s) and future wave
direction is projected to shift towards the north (counter-clockwise) by less than 8
degrees.
The spatial distribution of the future mean significant wave height showed decreases
of wave height along the North coast (Stations Hon Dau, Hon Ngu, A and B) of less
than 8 cm and increases of wave height along the South coast (Station G, G1, K, L, L1
and O) of less than 4 cm. The spatial distribution of future mean wave period showed
increases of less than 0.20 s along the North coast and less than 0.20 s along the South
coast. The spatial distribution of future wave direction showed a clockwise rotation of
wave direction (rotation towards the south) of less than 8 degrees along the North
coast (Station Hon Dau, Hon Ngu, A and B) and the Central coast (Station C, C1, E
and E1). On the other hand, future wave direction is projected to rotate counter
clockwise (rotation towards the north) along the south coast (Station G, G1, K, L, L1
and O) by less than 8 degrees.
The most significant future potential change in the mean wave climate along the
Vietnam coast is therefore the projected changes in wave directions, leading to a zone
of wave direction divergence in the vicinity of Danang. This could result in longshore
currents and sediment transports that diverge in this area, potentially leading to
unprecedented rates of coastal erosion and coastline recession in the vicinity of
Danang.
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TABLE OF CONTENTS
Executive Summary i
Table of Contents iv
List of Figures vi
List of Tables viii
1. Introduction 1
1.1 Background 1
1.2 Statement of Problems 2
1.3 Objectives of the Study 2
1.4 Scope of the Study 3
1.5 Limitations 3
2 Literature Review 5
2.1 Numerical Wind-Wave Models 5
2.1.1 Third Generation Spectral Wave Models 6
2.1.2 Wave Model Processes and Scales 7
2.1.3 Modeling Spectral Wind-Wave with MIKE21 SW Models 8
2.2 Changing of Wave Climate from Climate Variability 9
2.3 Coastal Study and Climate Change in Vietnam 12
3 Theoretical Considerations 14
3.1 Spectral Wind-Wave Model 14
3.1.1 Governing Equations and Formulations 14
3.1.2 Source Term Functions 14
3.2 Energy Transfer 19
3.3 Initial and Boundary Conditions 19
3.4 Model Outputs 19
15
4 Methodology and Data Collection 20
4.1 Methodology 20
4.2 Data Collection 20
5 Results and Discussion 29
5.1 Model Calibration 29
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5.2 Modeling Result of Present Wave Climate 37
5.3 Modeling Result of Future Wave Climate 47
5.3.1 Monthly and Annual Mean Wave Climate 47
5.3.2 Probability Distribution 53
5.3.3 Spatial Distribution 59
6 Conclusion 63
References 66
Appendix A Performance Measurement 69
Appendix B Result of Present Wave Climate 72
Appendix C Result of Monthly Mean Future Wave Climate 91
Appendix D Result of Probability Wave Climate 135
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LIST OF FIGURES
FIGURE PAGE
1.1 Main cities in Vietnam 4
2.1 Scales of wave processes 8
2.2 Layout of the forcing and output data sets: combinations of control
(C) and emission scenarios (A refers to A2; B refers to B2) and
GCMs (H denotes HadAM3H; E denotes ECHAM4/OPYC3) used
as driving data for the regional climate model (R, RCAO), and six
WAM (W) output data sets named with respect to the six driving
data sets derived from the RCAO model (Grabemann, 2008)
10
4.1 Research framework of this present study 21
4.2 Conceptual of modeling study 22
4.3 Bathymetric map of the computational domain 24
4.4 CCAM and representation of wind components (McGregor, 2005) 25
4.5 Locations of ERA-40 and ship observation 27
5.1-1 Locations of wave data for model calibration 30
5.1-2 Result of model calibration at Hon Dau 32
5.1-3 Scatter plot of wave height at Hon Dau 32
5.1-4 Result of model calibration at Hon Ngu 33
5.1-5 Scatter plot of wave height at Hon Ngu 33
5.1-6 Result of model calibration at Point B 34
5.1-7 Scatter plot of wave height at Point B 34
5.1-8 Result of model calibration at Point E 35
5.1-9 Scatter plot of wave height at Point E 35
5.1-10 Result of model calibration at Point K 36
5.1-11 Scatter plot of wave height at Point K 36
5.2-1 Locations of wave climate output from modeling 38
5.2-2 Present wave parameter at Hon Dau 39
5.2-3 Present wave parameter at Point G 40
5.2-4 Monthly mean significant wave height (Hm0) 41
5.2-5 Summary of mean wave parameters and their differences 46
5.3.1-1 Change of monthly mean wave parameters at Hon Dau 50
5.3.1-2 Change of monthly mean wave parameters at Point G 51
5.3.1-3 Change of annual wave parameters 52
5.3.2-1 Probability distribution of present and future wave climate at Hon
Dau 54
5.3.2-2 Probability distribution of present and future wave climate at Point
G 55
5.3.2-3 Change of probability distribution at Hon Dau 56
5.3.2-4 Change of probability distribution at Point G 57
5.3.2-5 Probability change of significant wave height and wave period 58
5.3.3-1 Time averaged mean significant wave height difference between
future and present period (Source: Mori et al., 2010)
59
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5.3.3-2 Spatial distribution of average ECHAM and GFDL mean
significant wave height in 1981-2000, 2041-2060, 2081-2100 and
its difference between 2081-2100 and 1981-2000
60
5.3.3-3 Spatial distribution of average ECHAM and GFDL mean wave
period in 1981-2000, 2041-2060, 2081-2100 and its difference
between 2081-2100 and 1981-2000
61
5.3.3-4 Spatial distribution of average ECHAM and GFDL mean wave
direction in 1981-2000, 2041-2060, 2081-2100 and its difference
between 2081-2100 and 1981-2000
62
6.1 Changes of future wave direction in north (Hon Ngu), central
(Station C1) and south (Station O) coast of Vietnam in year 2041-
2060 and 2081-2100
65
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LIST OF TABLES
TABLE PAGE
2.1 Relative importance of various wave model process in different
regions of the ocean: 1-Negligible; 2-Minor importance; 3-
Significant; 4-Dominant (Battjes, 1994 and Young, 1999)
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4.1 Types of data and sources 20
4.2.1 Summary of wave data 28
5.1-1 Summary of statistics performance of modeling result at Hon Dau,
Hon Ngu, Point B, E and K
31
5.2-1 Summary of depths and distances from shoreline at 14locations 37
5.3-1 Summary of depths and distances from shoreline at 14locations 47
5.3.1-1 Differences of average significant wave height, wave period and
wave direction between 2041 to 2060 and 1981 to 2000 and 2081
to 2100 and 1981 to 2000 at ten locations
49
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CHAPTER 1
INTRODUCTION
1.1 Background
The coastline of Vietnam is 3,260 km long, extended through the territories of 24
provinces and cities, which include 127 rural and urban districts, 6 main cities and 21
towns. Coastal cities along Vietnam coast have been successively developed with different
activities. Da Nang is a major port city and the largest city of central Vietnam. Qui Nhon is
a fishing city which is shifted towards service industries and tourism. Nha Trang, located
in the south central coast, is well known for its beach, scuba diving and the world’s most
beautiful bay which is now a popular destination for international tourists. In addition, the
unique nature of Ha long bay in the north having 1,600 islands forms a spectacular
seascape of limestone pillars. Its outstanding scenic beauty is complemented by great
biological interest. Figure 1.1 shows main cities in Vietnam. The landforms of the coastal
zone of Vietnam are multiform and diverse. In many areas the landforms are strongly
dissected, giving the coast many beauty bays and spots. The coastal zone of Vietnam also
receives many natural calamities, causing multidirectional impacts on the nature and socio-
economic conditions. Coastal erosion occurs in a number of locations in the Vietnam
shoreline. Erosion occurs in most lithological types of coasts; gravel sand, clayey muds
with the highest rate in sandy coast which is more than ninety percent. It causes difficulties
for the life of populations. Medium to severe erosion rates occur in convex shapes of
shoreline facing strong wave action. The wave driven by wind is one of the main natural
factors that govern the coastal condition effect to activities, function of those cities and
significantly coastal erosion.
The wind patterns in Vietnam are influenced by two monsoon systems and their
transitions. Winds in northeast monsoon season are mostly northeasterly and easterly
direction, starting from November-February. Winds in the transition period are
southeasterly direction and stormily, starting from March-April and September-October.
Winds in southwest monsoon season are southerly and southwesterly directions, starting
from May-August. Occurrences of tropical storms and storm surges can generate such
wave forces acting on the coasts during northeast monsoon season and transition period
from October-December.
The northeast waves in South China Sea coming to Vietnam are more severe due to
stronger northeast winds and much longer fetch lengths. Under the effect of climate
change, offshore wave conditions in Vietnam can be affected by changes due to wind
systems and dramatically impacts from sea-level rise, whereas those subsidence and
erosion problems already exist. Furthermore, changing wind systems may have the effect
of altering the surface ocean wave energy and increasing threat to coastal sustainability.
Therefore, it is necessary to investigate changes in offshore wave climate in response to
climate change driven wind variations.
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Wave climate is an essential accessory for wave analysis i.e. hindcasting and forecasting. It
is a long-term statistical characterization of the behavior of waves in the sea and the ocean.
Numerical wave models have been used to assess potential changes to the wave climate,
currents and sedimentation transport, recently. They aim to provide efficient solutions to
complex problems in coastal environment and they are essential for predicting the
dynamics in coastal engineering works. Furthermore, they are increasingly being used as a
tool to transfer offshore wave information to nearshore location as well as to simulate the
hydrodynamic of various coastal characteristics and the governing physical processes such
as waves, currents and sediment transport.
MIKE21, a commonly used numerical wave model, has been developed by Danish
Hydraulic Institute (DHI), Denmark. Several models in MIKE21 are introduced to this
study. They can be used as a tool to assist in performing the numerous calculations
involved in defining wave climate, often applied to the studies of wave disturbances in
coastal areas and capable for simulating a wide range of hydrodynamic and related wave
phenomena.
1.2 Statement of the Problems
Variations of offshore wave climate in the Lower Gulf of Thailand, which is close to
Vietnam, were analyzed by Weerasinghe (2010) using numerical wave model, MIKE21
SW. The offshore wave climate in the far future represented that the mean of northeast
monsoon wave was slightly increased and wave direction was changed towards the East.
Therefore, this may result in changing of nearshore wave climate and associated wave-
induced current, wave-current induced sediment transport in this region.
Variability of future offshore wave climate and their plausible changes in response to
climate change in Vietnam will increase the severity of coastal problems. Wave is an
important factor governing coastal processes in the nearshore zone. Changing of wave
direction will alter the sediment transport in the surf zone and provide permanent shoreline
change to approach a new equilibrium platform. Sediment budget can be in unbalanced
condition due to changing of wave-induced sediment transport. The shoreline can be more
eroded and it can occur at the area where this problem has never been faced before.
Shifting of extreme conditions such as design waves will cause damage to coastal
protection, fishing ports and harbor structures. Therefore the study of changing of offshore
wave climate is basically important and required in order to obtain the future wave
condition and use for preparedness for its impact to coastal area in Vietnam.
1.3 Objectives of the Study
The main objective of this study is to analyze present and future offshore wave climate
along the coast of Vietnam using a numerical wave model.
Specific objectives of this study are as follows:
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a) To simulate the present and future wave condition along the coast of Vietnam
using a third generation wave model (MIKE21 SW).
1) To examine the variation of the computed results of wave climate from
different sources of wind fields.
2) To determine temporal and spatial variability of future wave climate.
1.4 Scope of the Study
In order to achieve the objectives, the scope of study can be defined as follows:
1) Present and future nearshore and offshore wave climate are derived from
numerical wave model, MIKE21 Spectral Wave (SW) model.
2) Present wave climate is driven by analytical global wind field, National Centers
for Environment Prediction and Climate Forecast System Reanalysis
(NCEP/CFSR).
3) Present and future wave climate are driven by Global Climate Models (GCMs)
derived wind with A2 scenario, ECHAM5 and GFDL CM2.1 downscaled from
Cubic Conformal Atmospheric Model (CCAM), developed by Commonwealth
Scientific and Industrial Research Organization (CSIRO).
4) Future wave climate is defined for 2 durations which are 2041-2060 and 2081-
2100 while present wave climate is defined in the period from 1981 to 2000.
5) The location of wave computation will be in 10 locations along the coast of
Vietnam.
1.5 Limitations
There are limitations presented in this study:
1) The computational domain including wind field from CCAM is between 98° to
120° E and 2° S to 25° N. Swells generated from the sources outside this area
cannot be computed and included in the present study.
2) Analysis work will focus on the change of monthly, spatial and probabilistic
distribution of mean monthly significant wave height, wave period and wave
directions.
4
Figure 1.1 Main cites in Vietnam (Source: Wikipedia)
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CHAPTER 2
LITERATURE REVIEW
This chapter reviews the numerical wave models, which are a significant tool to use for
future wave computation. Past studies of climate change related to wave climate are also
reviewed. It shows study locations in the North Sea in northern Europe, Mediterranean
Sea, east coast of Australia, Thailand and global scale. The future wave climate variability
will experience both positive and negative trends at different regions. The last part consists
of reviewing climate change and coastal studies in Vietnam. It shows that most of the
research studies emphasize on hydro-meteorological change and sea level rise. There is no
research related to the change of wave climate along the coast of Vietnam.
2.1 Numerical Wind-Wave Models
Numerical wave models can be divided in two major categories as follows:
Deterministic (phase-resolving) models are based on an approximation of the fundamental
hydrodynamic equations and can be applied in shallow or intermediate water. Their basic
characteristic is the capability to translate the elevation time history from one point to
another point and provide a continuous high frequency description in space and time of the
evolution of the sea surface.
Spectral models (phase-averaged) provide a statistical description of the wave conditions
in space and time, typically at the nodes of a grid covering the area of interest. They
provide, point by point, the distribution of wave energy in frequency, direction and its
evolution in time. Spectral models are commonly divided into three generations as follows:
First generation is the early models, developed in the 1960s, which were designed to model
wave energy growth and dissipation. Their major limitation is that they do not account for
the nonlinear interactions between the different wave frequencies.
Second generation is the later generation of models using parameterized approximations to
model the nonlinear spectral interactions. Explicit calculation of these interactions is
computationally very expensive.
Third generation is developed in the late 1980s and provides a full description of the
physical processes governing wave evolution. This method requires fewer assumptions on
the nature of spectral evolution than the parameterized relationships used in the second
generation models. Third generation models generally share the following characteristics:
1) Ocean wave spectrum is free to develop without an a priori limit on the spectral
shape. The resulting spectrums are defined purely from the balance in the
source or sink terms.
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2) Nonlinear wave-wave interaction source term, Snl, is solved explicitly, and is
consistent with the same number of degrees of freedom as the discrete
representation of the spectrum.
3) Source or sink mechanisms are defined discretely in the frequency/direction
domain, and not formulated by parameterization.
2.1.1 Third Generation Spectral Wave Models
Spectral wave models are rapidly and recently developed based on the introduction of third
generation spectral wave models. There are several wave models that have been used
worldwide i.e., WAM, WAVEWATCH III, SWAN, MIKE21, TOMAWAC. They are
capable to be applied adequately anywhere with the appropriated bathymetries and wind
fields. The differences between these third generation wave models are normally found in
their source or sink term expressions.
Hasselmann and Hasselmann (1981) proposed a third generation model, EXACT-NL,
describing an explicit method for calculating the mean exchange of energy between wave
components within a spectrum. This model is based on the six-dimensional integral
expression proposed by Hasselmann (1962) and includes a representation of the dissipation
source term, incorporating assumptions of energy dissipation through whitecap breaking
by Hasselmann (1974). Hasselmann et al. (1985) introduced the Discrete Interaction
Approximation (DIA) method to compute the nonlinear transfer in a surface wave
spectrum in an attempt to reduce the overall computational time needed to solve the
spectral energy balance. DIA relaxes most of the constraints on spectral shape in
simulating wave growth in the parameterization of the nonlinear wave-wave interaction
source terms. The success of DIA is documented in Komen et al. (1994).
The Wave Modeling group (WAMDI group 1988) was formed with the goal of developing
the third generation model that could be implemented operationally on global as well as
regional scales, replacing the existing second generation models implemented
operationally. The group utilized the success of Komen et al., 1994 and developed the
WAve Modeling (WAM) model. The success of WAM can be greatly attributed to the
DIA algorithm for its ability to approximate nonlinear wave-wave interaction, Snl, with very
low computational cost. The DIA algorithm has allowed independent development of other
third generation models. Tolman and Chalikov (1996) present new formulations for source
terms. Sin source term is based on Chalikov and Belevich (1993) and Snl is based on DIA of
Hasselmann et al. (1985). Sds is divided into two constituents, a low and a high-frequency
source term.
Ris (1997) and Booij et al. (1999) implemented the third generation model, Simulating
WAves Nearshore (SWAN), for shallow waters and fetch limited areas. SWAN computes
the evolution of wind waves in coastal regions using the wave action balance equation.
This model shares the basic scientific philosophy with WAM of incorporating the
formulations for deep water processes of wave generation, dissipation and the quadruplet
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wave-wave interactions. Although it was designed for coastal regions, SWAN can also be
used on global and regional scales since it is an extension of WAM.
2.1.2 Wave Model Processes and Scales
Generally, the spectral wave models include these following processes:
1) Wave generation by wind input
2) Nonlinear interaction
3) White capping (wave breaking in deep water)
4) Bottom friction
5) Depth-induced wave breaking (wave breaking in shallow water)
6) Refraction and shoaling
Wave generation processes depend on wind speed, fetch and duration developed.
Nonlinearity is defined theoretically (quadruplet and triad wave interactions) and different
wave components of directional and frequency spectrum play an important role for the
nonlinear evolution. The white capping process depends on the wave action spectrum. The
processes of bottom friction, depth-induced wave breaking, refraction and shoaling depend
on the depth of water and characteristics of bottom materials or median grain size. The
relative importance of these processes was proposed by Battjes 1994 and Young 1999, as
shown in Table 2.1.
Wind-wave processes can be separated into three scales; generation, transformation and
local scale, shown in Figure 2.1. Wave generation typically occurs in relatively deep water
and across the continental shelf. The dominant processes for wave generation are
atmospheric or wind input, nonlinear wave-wave interactions, and energy dissipation due
to white-capping. In intermediate to shallow water depths, wave transformation processes
become dominant. These processes include wave shoaling, refraction, and breaking. In
shallow depths and near coastal structures, local-scale process of diffraction, reflection,
and wave nonlinearities govern. Although there is overlap in the wave processes between
scales, numerical modeling approaches naturally fit into these three scales.
Table 2.1 Relative importance of various wave model process in different regions of the
ocean: 1-Negligible; 2-Minor importance; 3-Significant; 4-Dominant (Battjes, 1994 and
Young, 1999)
Process Deep Ocean Shelf Seas Shoaling
Zone Harbors
Atmospheric input 4 4 2 1
White capping 4 4 2 1
Quadruplet wave interaction 4 4 2 1
Triad wave interaction 1 2 3 2
Current refraction 1 2 3 1
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Bottom friction 1 4 2 1
Depth-induced breaking 1 2 4 1
Refraction and shoaling 1 3 4 3
Diffraction 1 1 2 4
Figure 2.1 Scales of wave processes
(Source: ERDC/CHL CHETN-I-64, US Army Corps of Engineers)
The wave transformation processes of refraction, shoaling, breaking, and wind input
dominate in intermediate water depths (depth less than approximately 15 to 60 m), which
is within a few kilometer to almost a hundred of kilometer from the coast. Wave heights
may increase or decrease in shallower depths due to wave refraction and shoaling and
wave directions refract to become more shore normal (wave crests parallel to shore). In
very shallow depths, waves break where the wave height is of the same order as the water
depth. To represent the bathymetry features that cause refraction, shoaling, and breaking,
the transformation-scale grid resolution is of the order of 30 to 300 m. An accurate
nearshore bathymetry is required. The input to calculate wave transformation is the output
from a wave generation model or field wave measurements.
2.1.3 Modeling Spectral Wind-Wave with MIKE21 SW Model
MIKE21 SW is a third generation spectral wind-wave model developed by the DHI water
and Environment. The model simulates the growth, decay and transformation of wind
generated waves and swells in offshore and coastal waters. MIKE 21 SW includes two
different modes: the fully spectral formulation and the directional decoupled parametric
formulation.
Jose et al. (2007) employed the MIKE21 spectral wave model to estimate the wave
conditions at the ship shoal in the south-central Louisiana. The high resolution scale was
implemented to estimate wave attenuation over the shoal and to get a more detailed
description of the spectrum when stormy conditions occurred in the eastern ship shoal area.
The results revealed that the MIKE21 SW model has electively represented the wave
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attenuation by wave transformation from offshore to the coast in stormy seasons such as
cold fronts and hurricanes.
Moeini and Shahidi (2007) examined the different wind formulations between the two
numerical wave models MIKE21 SW and SWAN. Wind forcing was used as varying in
time and constant in domain in Lake Erie. The results showed the inconsistency between
the two models and found it to be due to differences between the wind input
parameterizations. Komen’s formulation in SWAN model led to more accurate prediction
of significant wave height than Janssen’s formulation in MIKE21 SW model.
Strauss et al. (2007) compared the performance of the numerical wave models, SWAN and
MIKE21 SW in the Gold Coast, Australia. Directional decouple parametric formulation
had been used in model formulation of MIKE21 SW. Comparison between MIKE21 SW
and SWAN indicated that MIKE21 SW has less sensitivity to wind fluctuations. Both
models overestimated the significant wave height at the coastline for swell waves. Wave
period showed slight differences.
2.2 Changing of Wave Climate from Climate Variability
The ‘wave climate’ is the long-term direction, frequency, energy and extremes of ocean
waves. Waves provide most of the energy that shapes the shoreline and potentially drives
coastal erosion. Impacts of changing waves in the coastal zone are:
1) Coastal inundation during severe storm events. It can be severe when combined
effects of sea-level rise, high ocean waves and storm surge.
2) Changes of the wave direction may alter the sand and sediments regimes
resulting in coastal erosion and changes of shoreline.
3) Affection of sub-tidal habitats due to seabed disturbance.
Climate change may change mean wave climates (wave height, wave period, wave
direction etc.) in many regions, in line with projected mean wind speed. Subsequently,
dynamic regional analysis is required to estimate possible changes in wave climate and
develop methods to assess the susceptibility of future wave climate scenarios.
Grabemann and Weisse (2008) analyzed the present mean and extreme wave conditions in
the North Sea in northern Europe to investigate the possible future changes due to
anthropogenic climate change. A 30 years period, from 2071 to 2100, from two global
circulation models with two forcing scenarios wind field, were simulated using wave
model WAM to realizations of future changes of waves. HadAM3H and
ECHAM4/OPYC3 GCMs were considered with A2 and B2 scenarios by the
Intergovernmental Panel on Climate Change, Special Report on Emission Scenarios. The
effects of the climate changes on the ocean waves were evaluated by analyzing four
CGM/emission scenario combinations and those in two control simulations representing
baseline wave climate conditions for the 30-year period 1961–1990. HadAM3H-driven
simulation has shown higher response than the ECHAM4/OPYC3-forced experiments.
Moreover, extreme wave heights were projected to increase in large parts in the southern
10
and eastern North Sea by about 0.25 to 0.35 m (5–8% of present values) towards the end of
the twenty first century due to global warming. All combinations also show an increase in
future frequency of severe sea state.
Figure 2.2 Layout of the forcing and output data sets: combinations of control (C) and
emission scenarios (A refers to A2; B refers to B2) and GCMs (H denotes HadAM3H; E
denotes ECHAM4/OPYC3) used as driving data for the regional climate model (R,
RCAO), and six WAM (W) output data sets named with respect to the six driving data sets
derived from the RCAO model (Grabemann, 2008).
Lionello (2008) studied the 30-year (2071-2100) simulation of the wave in the
Mediterranean Sea with the WAM model. A2, B2 emission scenarios were considered and
present climate period was considered from 1961 to 1990. Wind field was obtained from
regional climate model RegCM driven by the HadAM3H model with 50 km resolution.
The results showed that the mean significant wave height in large fraction of the
Mediterranean Sea was lower for the A2 scenario than the present climate during winter,
spring and autumn. Moreover, extreme significant wave height has shown smaller values
in the projected period than in the present period. In general, it has been showed that
changes of significant wave height, wind speed and atmospheric circulation are very small
in middle extreme events in future scenarios than in the present climate.
Mori et al. (2009) analyzed and predicted the future ocean wave climate in comparison
with those in present climate based on the climate model output. The research was
conducted on the basis of the climate model at Metrological Research Institute of Japan
Metrological Agency (JMA-MRI; Kakushin, 2008). The JMA-MRI climate model is the
atmospheric T959L60 single model with Sea Surface Temperature (SST) from coarse grid
coupled run of atmosphere and ocean simulation, and was computed for the three periods
of 1979-2004 (present), 2015-2028 (near future) and 2075-2100 (future) following A1B
scenario. The waves of the three periods were simulated using sea surface winds (U10) of
climate model by the SWAN model. The simulated U10 and wave height were analyzed to
predict wind and wave climate change from present to future in global and regional area.
Results showed that the mean waves will be increased at both the middle latitudes and also
in the Antarctic Ocean and decreased on the equator. The sea off the coast of Japan belongs
11
to the slightly decreased region where the mean winds and waves are decreased 5–10%
from those in the present climate. On the other hand, the extreme waves due to tropical
cyclones will be increased. These results show that the future wave climate changes to
lower mean and higher maximum wave heights in the middle latitudes, and higher mean
and maximum wave heights in the high latitudes. It expressed that the future wave climate
will experience both negative and positive change depending on the region.
Lowe et al. (2009) projected the future wave climate around the UK and the global climate
model HadCM3 provided winds for the Atlantic wave model and the regional climate
model has provided winds for the regional wave model. The PROWAM model (Monbaliu
et al. 2000), which is a modified version of the WAM cycle-4 third generation wave model
(Komen et al. 1994) was used to force the wave and that model was developed to run at
higher spatial resolution than the standard WAM model and also includes some extra
shallow-water processes. 12km nested grid was implemented in shallow water over the
North West European continental shelf. Boundary condition was obtained simulating the
large domain area; whole Atlantic, with grids of 1° × 1° degree. The wave models were run
for the periods 1960–1990 and 2070–2100 to represent present and future periods
respectively. The results revealed the projected mean and extreme wave height is changed
with location and projected mean values laid between –35 and +5 cm whereas the wave
period is changed with a very smaller value with maximum ± 1 s.
Hemer et al. (2010) developed an ensemble of wave model to future projections of wave
climate for the east coast of Australia. The study used three different GCMs (CSIRO
Mk3.5, GFDL CM2.0 and GFDL CM2.1 under A2 emission scenarios), and surface wind
forcing was obtained from GCM simulations that had been downscaled by Cubic
Conformal Atmospheric Model (CCAM), Commonwealth Scientific and Industrial
Research Organization (CSIRO) over the Australian region at approximately 60 km
resolution. Future wave climate simulations were carried out using three bias correction
methods for those three CCAM downscaled GCMs under the A2 and B1 emission scenario
for 2031-2050 and 2081-2100 period. The period of 1981-2000 was selected as the
baseline reference for the simulation of wave models. The bias adjustment of CCAM-
derived wind field was corrected biases in the mean and the variability of winds by
adjusting the joint probability distribution of both u and v wind component (JPD-UV) for
the first 20-year time slice for both CCAM and NRA-2-derived winds (observed winds).
The CCAM JPD-UV was then implemented for bivariate quantile-mapping on NRA-2
JPD-UV at each grid cell. The CCAM winds were used to force a coarse resolution of 0.5°
with the WaveWatch III (WW3) wave model for Australian region between the
coordinates of 90-240°E and 65-0°S, with a 0.1° nested fine resolution application of the
SWAN spectral wave model along the eastern Australian coast (150-155°E, 38-25°S).
Buoy wave data from six locations (at approximate 100 m depth) along a 1000 km stretch
of the coastline was used to validate the model for present conditions. The results showed
that the ensemble of wave model runs for the 2081-2100 time slice, presented a decrease in
mean significant wave height, Hs, along the east Australian coast relative to present climate
conditions. The magnitude of the projected change was relatively small, which is less than
12
0.2 m, and increased northwards along the north south Wales coast. A relatively small
(~5°) anticlockwise rotation in mean wave direction was projected to occur over the same
period.
Koontanakulwong and Chaowiwat (2010) studied the climate change impact assessment
and adaptation measures based on past observed data and future projected GCM data.
Present and future projection of hydrological conditions (precipitation and temperature)
had been conducted for the period of 1979-2006, 2015-2039 and 2075-2099, respectively.
GCM data had been bias-corrected using two statistical downscaling methods, SD Ratio
and modified rescaled downscaling methods, by verifying with past observed data. The
bias correction methods were applied to correct the bias from MRI GCM and verified the
performance respect to Thailand. The both bias correction method can reduce the bias of
MRI GCM, the coefficient of determination and RMSE are in acceptable range and keep
the changing trend of the original GCM data for both precipitation and temperature.
Weerasinghe (2010) determined the variation of offshore wave climate in the Gulf of
Thailand, particularly at Songkhla tidal inlet using the third generation spectral wind-wave
model, MIKE21 SW. Simulation domain on flexible mesh covered from 98-120°E in
longitude and 2-25°N in latitude with coarse resolution of less than 0.5° and nested to the
Songkhla coastlines with finer resolution of 0.1°. NCEP-DOE Reanalysis 2 and
downscaled CCAM wind data (ECHAM5 and GFDL CM2.1) were used as wind forcing
on the models in three time slices, baseline period of 1981-2000, projection period of
2041-2060 and 2081-2100. Analysis of variation changes in wind climate represented
considerable slightly changes in mean wind speed and direction. The model calibration
performed as a calibration period and was restricted by unavailability of observed buoy
wave data in some locations. The model results showed that the mean of northeast
monsoon wave had slightly increased and the mean wave direction had changed towards
the east.
2.3 Coastal Study and Climate Change in Vietnam
Pruszak et al (2002) carried out a numerical model study for sediment transport in the red
river delta. The impacts to destructive shoreline change which varied substantial and
dynamic changes from sediment supply sources from rivers and the sea i.e. typhoon, sea
level change, current, were taken into account. Assessment of sub-region sediment budget
computed wave height from offshore area. Morphodynamic processes can also be
determined. It showed a current deficit of sediment by 1,500,000 m3/year . It caused
erosion of the sediment from land and nearshore zone in the adjacent area. The erosion was
computed and found to be continuing but its rate would be decreasing in the future.
Ministry of Natural Resources and Environment, MONRE (2008) showed an increase of
sea level at Hon Dau station 20 cm for 50 years from 1960 to 2009. The rate is 3 mm /year
during 1993 to 2008.
13
Ministry of Natural Resources and Environment, MONRE (2009) studied the climate
change and sea level rise in Vietnam. The condition of temperature would rise 2.3 relative
to those in 1980 to 1999. The sea level would increase 30 and 75 cm by the mid and end of
21st century compared to those in the 1980 to 1999 for scenario B2. Results of scenario B1
and A1F for low and high emission were conducted with their variation around these
values. There are high uncertainties and the tolerance for climate change scenario was
recommended. The result is required to be regularly updated in 2010 and 2015. In addition,
the analysis of long recorded data showed that there would be more typhoons with high
intensity. Typhoon track moved to southward direction and its season would be ended
earlier. There would be more typhoons with abnormal movement. Other hydrological and
meteorological analyses for climate variation were conducted as well. On average, annual
rainfall would increase 5%. The northern climate area would have more increasing rainfall
than the south.
The effect of sea level rise will increase risk of coastal flooding. Duc et al (2012) studied
and analyzed the coastal erosion in the red river delta, Vietnam. The return period of storm
surge would be substantially reduced. The present 20 years return period of 2.6 m height
storm surge will be 9 and 4.5 year in 2050 and 2100. It means that the percentage of
occurrence will be increased from 5 percent to 11 and 22 percent, approximately. The risk
of flooding increased from possible 1 event in 20 years to 2 and 4 events in the similar
period.
From the results of literature survey, it is shown that most studies of climate change have
been carried out for hydrological and metrological topics. The study of coastal issue was
only sea level rise. Therefore the present study seems to be important as a pioneer work to
indicate the variability of wave climate in the future along Vietnam coast. The output for
offshore wave climate from the present study can be extended further to determine
variability of future sediment transport, extreme wave for improvement of design wave of
coastal structures for coastal protection. Besides, the sediment budget in a regional scale
can be revisited similarly to the work from Pruszik et al (2002) so that the pattern and
locations of erosion/accretion can be variable for its magnitude and severity.
14
CHAPTER 3
THEORETICAL CONSIDERATIONS
3.1 Spectral Wind-Wave Model
Regional wave models were implemented to use the MIKE21 SW model in order to derive
present and future offshore wave climate along Vietnam coast. The model can simulate
wave propagation in offshore area, including the effect of wave growth by the action of
wind, non-linear wave-wave interaction, dissipation by white-capping, dissipation by wave
breaking, dissipation due to bottom friction, refraction due to depth variations and wave-
current interaction. The full spectral formulation MIKE21 SW was applied in order to
formulate the wind-wave generation processes on the regional wave model, which takes
high computation cost, but gives more accurate wave climate parameters. Regional wave
model is forced by the analytical global wind field NCEP/CFSR in the present period
1981-2000 and the downscaled GCM wind fields, ECHAM5 and GFDL CM2.1 on the
ensemble runs in present period 1981-2000 and projection period 2041-2060 and 2081-
2100, over the entire domain. All wind forcing were created on Grid (.dfs2) varying in time
and domain on MIKE Zero.
3.1.1 Governing Equations and Formulations
Wind waves are expressed by the wave action density spectrum, ,N , where σ is the
relative angular frequency and θ is the direction of wave propagation. The relative angular
frequency can be related to the absolute angular frequency (ω) by linear dispersion
relationship as
tanhgk kd k U
(3.1)
where g is the acceleration of gravity, k is the wave number, d is the water depth, k is the
wave number vector with magnitude k and direction, θ and U is the current velocity
vector. The action density, ,N , can be related to the energy density, ,E , by
EN
(3.2)
There are two formulations in the model: (1) fully spectral formulation and (2) directional
decouple parametric formulation.
15
Fully spectral formulation is based on the wave action conservation equation in Komen et
al. (1994) and Young (1999), where directional-frequency wave action spectrum is the
dependent variable. The wave action conservation equations are formulated in either
Cartesian coordinates for small-scale applications or polar spherical coordinates for large
scale applications. The spectral energy balance in Cartesian co-ordinates can be expressed
by
, ; , , , ; , ,, ; , , , ; , ,gx gyC N x y t C N x y tN x y t S x y t
t x y
(3.3)
where , , , ,N x y t is the evolution of the action density, Cgx and Cgy are the
components in the x- and y-direction, respectively, of the group velocitiy, x and y are the
Cartesian co-ordinates, θ is direction of wave propagation. The terms, S is the source or
sink functions based on the action spectrum.
Decouple parametric formulation is based on wave action conservation equation in the
numerical solution extensions proposed by Holthuijsen et. al., (1989). Parameterization of
frequency is performed by introducing the zeroth, m0 and first moment, m1 of the wave
action spectrum as dependent variables. The source terms derived from the conservation
equations are as follow:
0 0 0
0
1 1 1
1
gx gy
gx gy
C m C m C mT
x y
C m C m C mT
x y
(3.4)
where m0(x,y,θ) and m1(x,y,θ) are the zeroth and first moment of action spectrum,
respectively. Cθ is the propagation speed in θ-direction. T0 and T1 are the source terms. The
propagation speeds, Cgx, Cgy and Cθ are derived based on linear wave theory. The function
on the left hand side takes into account the processes of refraction and shoaling. The source
terms on the right hand side take into account the effect of wind driven wave, dissipation
due to bottom friction, depth-induced breaking and wave-current interaction.
3.1.2 Source Term Functions
The energy source/sink term, S, described in the right-hand side of Eq. (3.3) represents
physical processes in which waves generate, dissipate or redistribute wave energy. The
source function term is given by
in nl ds bot surfS S S S S S
(3.5)
16
where Sin represents the momentum transfer of wind energy to wave generation, Snl is the
energy transfer due to nonlinear wave-wave interaction, Sds is the dissipation of wave
energy due to white capping (wave breaking in deep water), Sbot is the dissipation due to
bottom friction and Ssurf is the dissipation of wave energy due to depth-induced breaking
(wave breaking in shallow water).
3.1.2.1 Generation by wind, Sin
The basis of all formulation in this source term of the third generation models is described
by linear wave growth mechanisms. Numerical wind growth in MIKE 21 SW is described
by Eq. (3.6) based on Janssen (1989), Janssen et al. (1989) and Janssen (1991), where γ is
the wind growth rate.
, ,inS f E f
(3.6)
Wind growth formulation in MIKE 21 SW is similar to that of WAM, the growth rate due
to wind input and can be expressed as
2
4 *
2
1.2ln cos 1
0 1
aw
w
uz
c
(3.7)
where κ is Von Karman’s constant equals to 0.41, the dimensionless critical height,
0 exp /kz x , /a w is the ratio of density of air to water, *u is the wind friction
velocity, c is the phase speed, θ and θw are the wave and wind directions, respectively and
0z is the sea roughness. The sea roughness in coupled model is given by
1/21/2 2
0 21 1w charnock w
ob ow ob
air
z uz z z z
g u
(3.8)
where zob, zow are the effect of gravity-capillary waves and short gravity waves, zCharnock is
the Charnock parameter. τw is wave-induced stress, τ is the total stress.
3.1.2.2 Non-linear wave-wave interaction, Snl
Non-linear wave-wave interaction is the mechanism that affects wave growth, where
energy is transferred between waves from one component to another through resonance.
Energy is either gain or loss in this mechanism and only redistributed over spectrum. The
parameterization of Snl is required in order that the Discrete Interaction Approximation
17
(DIA), developed by S. Hasselmann et al. (1985) is used. S. Hasselmann et al. (1985)
constructed a non-linear interaction operator by the superposition of a small number of
discrete interaction configurations composed of neighbouring and finite distance
interaction combinations as described in Komen et al., 1994. The configurations are:
1 2 ,
3 1 ,
(3.9)
4 1
In deep water and intermediate areas, non-linear wave-wave interactions allow energy
transfers from the spectral peak to lower frequencies. While, shallow water transfers the
energy from lower frequencies to higher frequencies. In terms of the spectral energy
densities, ,E f , the increments to the sources functions, , /nl rS f E t at the
three interacting wave numbers are given as:
2
1 , , ,
1
nl
nl
nl
f
fS
fS f E E E
fS
f
f
(3.10)
3.1.2.3 White capping, Sds
The source function of the dissipation due to white-capping is based on the theory of
Hasselmann (1974), assuming the linear in the spectral density and the frequency and
obtained a dissipation function. Komen et al. (1984) later combined the processes of the
extent of whitecap coverage in the dissipation function and reformulated by the WAMDI
group (1988) in terms of wave number so to be applicable in finite water depth. With the
description of wind input of the Janssen et al. (1988), a proper balance between wind input
and dissipation at high frequencies was modified by Komen et al. (1994) and can be
expressed as
2
ˆ, 1 ,
ˆ
m
ds ds
PM
k kS f C E f
k k
(3.11)
18
where Cds, δ and m are constants, is the mean relative angular frequency, k is the wave
number, k is the mean wave number, ̂ is the overall steepness of wave field and ˆPM is
the integrated steepness of a fully developed Pierson-Moskowitz spectrum. MIKE 21 SW
allows white-capping dissipation formulation of WAM cycle 3 and WAM cycle 4 with
different values of Cds, and δ are 4.5 and 0.5, respectively.
3.1.2.4 Bottom friction, Sbot
As waves propagate into shallow water and feel the bottom, the source function of wave-
bottom interaction becomes important. The rate of energy dissipation due to bottom
friction is given by
, / ,sinh 2
bot f c
kS f C f u k k E f
kd
(3.12)
where Cf is the friction coefficient, k is the wave number, k is the mean wave number, d is
the water depth, fc is the friction coefficient for the current and u is the current velocity.
Bottom friction factor used in modeling can be specified as the friction coefficient (Cfw),
friction factor (fw), Nikuradse roughness parameter (ks) or sand grain size (D50).
3.1.2.5 Wave breaking, Ssurf
Depth-induced breaking occurs when waves propagate into shallow water areas and the
wave height can no longer be supported by the water depth. The formulation of wave
breaking in the model is based on the bore model of Battjes and Janssen (1978) and
Eldeberky and Battjes (1996). Gamma breaking parameter can be specified in the breaking
formulation. The source function can be written as
2
, ,BJ bsurf
Q fS f E f
X
(3.13)
where αBJ is the calibration constant, approximately equals to 1.0, Qb is the fraction of
wave breaking waves, f is the mean frequency and X is the ratio of the total energy in the
random wave train to the energy in a wave train with the maximum possible wave height.
The fraction of breaking waves, Qb can be determined from
19
2
max
1
ln
b rms
b
Q HX
Q H
(3.14)
2
max
1exp
/
b
b
rms
H H
(3.15)
21 2 exp 1/ 0.5
1 2.04 1 0.44 ; 1 ; 0.5
1 1
b
x x x
Q z z z x x
x
(3.16)
3.2 Energy Transfer
The nonlinear energy transfer among the wave field in the present study becomes
important for evolution of wave field in deep water and coastal areas. A quadruplet-wave
interaction, which is described by the accepted approximate Discrete Interaction
Approximate (DIA) (Komen et al. (1994), was applied on regional wave model. The
quadruplet-wave interaction controls: (1) the shape-stabilization of the high-frequency part
of the spectrum, (2) the downshift of energy to lower frequencies and (3) frequency-
dependent redistribution of directional distribution functions. A triad-wave interaction was
applied on the nearshore wave model.
3.3 Initial and Boundary Conditions
The initial conditions on regional wave model were applied by calculating the spectra from
empirical formulations from JONSWAP fetch growth expression and closed boundary at
offshore boundary. Various parameters such as maximum fetch length, maximum peak
frequency and maximum Philip’s constant, and etc. were defined. The land boundary is
specified along Vietnam while open boundary is used in the offshore area.
3.4 Model Outputs
The basic outputs from the simulations are integral wave parameters and spectral
parameters. The important integral parameters used in the present study are significant
wave height (Hm0), maximum wave height (Hmax), peak wave period (Tp), mean wave
period (Tm01), zero-crossing wave period (Tm02), peak wave direction (θp) and mean wave
direction (θm).
20
CHAPTER 4
METHODOLOGY AND DATA COLLECTION
4.1 Methodology
The Vietnam coast is connected with an open ocean to the South China Sea. Waves in this
region are not only limited on locally wind-generated waves. MIKE21 SW model is used
to derive present and future offshore wave with bathymetry input from GEBCO. The
model is forced by an analytical global wind field NCEP/CFSR in the present period
starting from 1981-2011 and the downscaled GCM derived winds, ECHAM5 and GFDL
CM2.1 in the present period started from 1981-2000 and projection period from 2041-2060
and 2081-2100 on numerical simulations. All required input data were prepared for
numerical simulations and the measured wave data were used for comparison purposes as
described in Section 4.3. Model setup for regional and nearshore wave models are briefly
described in section 4.4. Figure 4.1 shows a flow chart of the research framework. Figure
4.2 shows concept of modeling study.
4.2 Data Collection
There are several types of required data e.g., bathymetry, shoreline, wind field and wave
data. All of them are secondary data obtained from different sources. They are divided
based on their applications for ease of understanding and simplicity; input data and
observational data. The input data was obtained for the proposed numerical wave model
simulations. The observational data was obtained for model purposes. Summary of the
overall collected data and their sources are shown in Table 4.1.
Table 4.1 Types of data and sources
Data Types Sources Descriptions
Bathymetry GEBCO 30-arc-seconded grid
Shoreline NGDC, NOAA GSHHS Version 2.2 High resolution: 200-m
Wind field NOAA
NCEP/CFSR
6-hourly, 1981-2000
0.5º×0.5º, u and v wind components (m/s)
Wind field CCAM, CSIRO
ECHAM 5 & GFDL CM2.1 with A2 scenario
6-houtly, 1981-2000, 2041-2060, 2081-2100
0.5º×0.5º, u and v wind components (m/s)
Wave Data ERA-40 6-hourly, 1981-
Ship observation 6 hourly, longest record is 1993-2002
21
Figure 4.1 Research framework of this present study
Observational data
- Wave data
Research study
State problems and
objectives Research design
Data collection
Regional wave model
MIKE21 SW
Conclusion and
recommendations
Literature review
Input data
- Bathymetry
- Shoreline
- Wind fields
Model calibration and
validation
Analysis of present and future
offshore wave climate
22
Figure 4.2 Conceptual of modeling study
Bathymetry model
98°-120°E, 2°S-25°N
Input Wind forcing
Data
1) NCEP/CFSR:
1981-2000
2) ECHAM5 &
GFDL CM2.1:
1981-2000,
2041-2060 and
2081-2100
Regional wave model
Outputs wave
parameters
Hm0, Tm0, θm,
23
4.2.1 Input Data
The numerical simulations in this study required three types of input data: (1) bathymetry,
(2) shoreline, (3) wind field and (4) wave data.
Bathymetry data
Bathymetry data was obtained from the Generic Bathymetric Charts of the Oceans
(GEBCO), the latest released version of the GEBCO_08 Grid (20100927), the grid data
sets with the spatial resolution of 30 arc-second. The grid data sets are used to provide the
possible topography in the Gulf of Thailand and the South China Sea including Vietnam
coast, represented in terms of geographical points, longitude, latitude and depth (xyz).
The bathymetry data was downloaded from General Bathymetric Chart of the Oceans
(GEBCO) with one arc minute grid resolution. Figure 4.3 shows the bathymetric map of
computational domain between 98°-120° E and 2°S-25°N.
The shorelines were digitalized using MIKE zero mesh generator’s tools to use as
boundary lines in unstructured mesh generation. Afterward gridded bathymetry data was
imported as scatter data for depth interpolation to every mesh point in the unstructured
mesh.
Shoreline data
Shoreline data was obtained from the National Geophysical Data Center (NGDC), National
Oceanic and Atmospheric Administration (NOAA), the latest released version 2.2.0 of a
Global Self-consistent, Hierarchical, High-resolution and Shoreline (GSHHS) data.
GSHHS is shoreline and enclosed basin data that comes at a variety of resolutions, low
resolution data of 5 km, adequately. There is also intermediate resolution 1 km and high
resolution data of 0.2 km available. It was maintained in the forms of closed polygons and
extracted by using the ArcGIS software. Its main use here was in specifying shoreline
boundary onto the computational domain for the regional wave model.
Wind data
Recently, the developed ECHAM5 (European Centre for Medium Range Weather
Forecasts, ECMWF and Max Planck Institute for Meteorology) and GFDL CM 2.1
(Geophysical Fluid Dynamics Laboratory, NOAA) downscaled by CSIRO’s CCAM was
selected for the current study. Its high resolution, vintage and validity of wave climate
projection (Hemer et al. 2010) were also considered in the selection criteria.
Representation of the wave model forced plausible future scenarios of greenhouse gas
emissions, A2 from IPPC Special Report on Emission Scenarios (SRES) were selected as
the forcing scenario.
24
- ECHAM5 model
ECHAM5 is the fifth-generation atmospheric general circulation model developed
at the Max Planck Institute for Meteorology (MPIM). It uses 1.875° lon x 1.875° lat (T63)
horizontal resolution with 31 layers in atmosphere and 1.5° lon x 1.5° lat resolution with
40 layers in oceanic model. The model integrate advective and time-stepping schemes,
vertical coordinate and number of layers above 200 hPa and below 850 hPa. Climate
change experiments forced with observed atmospheric greenhouse gas and aerosol
concentrations since the middle of the 19th century. The model simulations explain a mean
global warming between 2.5 and 4.1 degrees Celsius towards the end of this century -
dependent on how much greenhouse gases are emitted into the atmosphere.
Figure 4.3 Bathymetric map of the computational domain
- GFDL CM 2.1 model
The GFDL CM 2.1 climate model is based on a prior model version (GFDL CM
2.0) and significant changes were made to all parts of the model (atmosphere, land surface,
25
ocean, and sea ice) with a view to reducing errors and climate drift in the CM 2.0 model.
The model is describing in the IPCC 4th assessment report and it consists of approximately
2.5° longitude and 2.0° latitude spacing equivalent to number of horizontal grids 144 x 90.
However, the exact horizontal grid locations are not the same in the two models. The
model has 24 vertical levels with ocean and sea ice model components have 200 x 360
numbers of horizontal grids.
- CCAM regional climate model
The CCAM has been developed at CSIRO over resent year with grid conformal-
cubic grids that was appealing because of its quasi-uniformity, orthogonality and isotropy.
CCAM process another significant feature is the reversible staggering procedure for the
winds (McGregor, 2005b) possible because of the cyclic nature of the grid. All variables
are located at the centres of grid cells. During semi-implicit calculations u and v are
transformed to the indicated centered grid locations as shown in Figure 4.4.
Figure 4.4 CCAM and representation of wind components (McGregor, 2005)
The monthly Sea Surface Temperature (SST) biases have been corrected in GFDL CM 2.1
GCM to first order and then the atmosphere has re-run for consistency with the new SSTs.
Consequently, those data sets have been downscaled by CCAM to get the 0.5 degree
resolution range of ensemble members. In the present study, the six hourly wind speeds (u
and v components) at 10m elevation from ground were obtained from CSIRO’s CCAM.
Wind data was extracted for three 20 year periods of 1981-2000, 2041-2060 and 2081-
2100 used for the analysis of base line period climate and future climate scenarios. Here,
1981-2000 was considered as a base line period and other two periods were considered for
future periods.
- NCEP/CFSR analytical global wind field
An analytical global wind field, National Centers for Environmental Prediction
(NCEP) Climate Forecast System Reanalysis (CFSR) obtained from National Oceanic and
Atmospheric Administration (NOAA) was used as wind forcing on numerical simulations
26
and for model calibration and validation purposes. NCEP/CFSR was a combination of the
atmosphere, ocean, sea ice and land, and satellite data executed in a coupled mode with
modern assimilation system. NCEP/CFSR provides spatial resolution of 0.5°×0.5° with
six-hourly data 0600, 1200, 1800, 0000 for the present period of 1981-2000 (20 years). It
was maintained in the forms of geographical coordinates and u- and v-wind components, at
10 m height.
Wave data
Wave data used for calibration and comparison are obtained from 2 sources, which are
ERA-40 and Ship Observation.
- ERA-40 wave data
ERA-40 is the European Center for Medium-Range Weather forecasts (ECMWF)
re-analysis of the global atmosphere and surface conditions for 45-years, over the period
from September 1957 to August 2002 by ECMWF. Many sources of the meteorological
observations were used, including radiosondes, balloons, aircraft, buoys, satellites,
scatterometers. This data was run through the ECMWF computer model at a 40 km
resolution. As the ECMWF's computer model is one of the most highly-regarded in the
field of forecasting, many scientists take its reanalysis to have similar merit. The data is
stored in GRIB format. The reanalysis was done in an effort to improve the accuracy of
historical weather maps and aid in a more detailed analysis of various weather systems
through a period that was severely lacking in computerized data. With the data from
reanalysis such as this, many of the more modern computerized tools for analyzing storm
systems can be utilized, at least in part, because of this access to a computerized simulation
of the atmospheric state.
Model of 2-D wave spectra use 10 m height wind speed. There are 12 directions of wave
spectrum with 25 frequencies. Computed wave data are 2.5 for interval distance and
available at every 6 hours i.e. 0000, 0600, 1200 and 1800 UTC each day. Period of wave
data is from 1981 to 2002. The present study shows location of wave data near Vietnam
coast in Figure 4.5. There are totally 22 locations starting from A, B, C, E,.., S, T, U to V.
- Ship Observation
Ship observed wave data are obtained from communication with Dr. Roshanka
Ranasinghe. There are 6 locations showed in Figure 4.5. Most of stations are in the north
Vietnam. The longest measured duration for the 3 locations, Hon Dau, Bach Long Vy and
Hon Ngu are from 1993 to 2002. Station Phu Quy which is the most southward direction
has short period of recorded wave from June 2006 to July 2007. Other three stations have
only summary of statistic wave. Table 4.2.1 shows summary of wave data. These wave
data will be used to compare and calibrate with computed wave data from model MIKE21
SW.
27
Figure 4.5 Locations of ERA-40 and ship observation
28
Table 4.2.1 Summary of wave data
Wave Data Station Period
1. ERA-40 A, B, C, E, G, L, K, O 6 hours interval 1981-2002 (22 years)
(selected 8 stations)
2. Ship Observation Hon Dau 1993-2002
Bach Long Vy 1993-2002
Hon Ngu 1993-2002
Con Co Statistic data only for monthly / flood
season and annual during 1980-1996
Quang Ngai Statistic data only for monthly 1966-1980
Phu Quy June 2006 - July 2007
(Hon Dau and Hon Ngu
are two selected
stations)
All data is 6 hour interval
29
CHAPTER 5
RESULTS AND DISCUSSION
5.1 Model Calibration
There are six stations of ship observed wave data but some stations have only wave
statistics and some do not have a long record. Therefore two stations at Hon Dau and Hon
Ngu are selected as measured wave data for model calibration and comparison. Data from
ERA-40 wave at Point B, E and K are selected and used for model calibration as shown in
Figure 5.1-1. Input wind data is from NCEP/CFSR. Measured wave characteristics from
ship observation are significant wave height and wave direction while those from ERA-40
are significant wave height, wave period and wave direction.
Calibration is performed to adjust the model parameters in order to reproduce time series
of wave at five locations illustrated in Figure 5.1-1. Calibrating parameters, used in
MIKE21 SW are illustrated as follows:
Bottom friction
An increase of the bottom friction coefficient in shallow water depths usually
leads to increased energy dissipation and thus decreased wave heights and
increased wave periods. The converse is also the case. In deep water the effect of
bottom friction will be negligible, since the waves will not feel the bottom.
Breaking parameters
There are two calibration parameters, γ and α in wave breaking. Parameter α
controls the rate of energy dissipation after breaking as well as γ (depth-induced)
controls the amount of depth related breaking. An increase in α, is increase the rate
of energy dissipation while increasing γ reduces the amount of depth related wave
breaking.
White-capping
In most application it will apply the default values of the two free parameters
controlling the rate of white-cap (or steepness induced) dissipation; Cds and δ. The
default values (Cds=4.5 and δ=0.5) are identical to the recommendations made in
Komen et al., (1994).
Calibration of the model is performed with wave data sets at five locations in offshore area.
The statistical parameters, such as root mean square error, efficiency index and correlation
coefficient are computed for the model performance analysis between observed and
30
modeled data. In this case, the breaking parameters in the offshore or white-capping area
Cds is used as calibrated parameters.
Figure 5.1-1 Locations of wave data for model calibration
The results of model calibrations can be summarized as follows:
Model calibration at Hon Dau is shown in Figure 5.1-2, 5.1-3 and Table 5.1-1. The
comparison of the plots of wave time series between ship observation and computed result
from model shows good agreement. Scatter plot shows that correlation coefficient (R2) is
0.43 which considered as fair result. There are a number of statistic indicators as shown in
a Table 5.1-1, starting from the followings:
- Efficiency Index (EI); It shows good side of modeling performance. When the
error is equal to zero or the matching of measured and computed is perfect, EI is equal to 1.
31
- Root Mean Squared Error (RMSE); It shows mathematically square root of
summation of square error. When RMSE is zero, there is no difference between measured
and computed results.
- Mean Absolute Error (MAE); This indicator is the mean of absolute error which
does not take into account the sign of error. When error is zero, MAE is equal to zero as
well.
- Root Mean Square Error Mean (RMSEM); This indicator is ratio of RMSE to
its mean value showing the proportion of error relative to its mean value.
- Root Mean Square Error over Standard Deviation (RMSES); This indicator is
the ratio of RMSE to its standard deviation. It shows how big RMSE is when it is
compared to standard deviation.
Table 5.1-1 shows a summary of the statistic performance of the modeling results at two
ship observations which are Hon Dau and Hon Ngu, and three ERA-40 wave locations
which are Point B, E and K. The model calibration at Hon Dau, Hon Ngu, Station B, E and
K is shown in Figure 5.1-2 to 5.1-11.
Model calibration at Hon Dau and Hon Ngu using ship observation data shows moderate
model performance with small value of EI in the range of 0.48 to 0.57 for significant wave
height and 0.48 to 0.57 for wave direction. Overall R show good correlation of computed
significant wave height and direction with the ship observation wave data.
Model calibration at Station B, E and K using ERA-40 wave data shows good model
performance of EI values in the range of 0.69 to 0.84 for significant wave height and 0.56
to 0.64 for wave direction with small RMSE. Scatter plot shows high value of correlation
coefficient and coefficient of determination.
Overall model performance gives moderate to good values of EI, R and R2 for the
comparison between computed and ship observation and ERA-40 significant wave height
and wave direction by calibrating parameter, Cds. Using Cds parameter equals to 4.5 which
is recommended value in numerical simulations, this helps to improve model results and
also gives good model results. The best model performance, EI, R and R2 gives good
model results is at Station E and the minimum value is at Hon Ngu.
Table 5.1-1 Summary of statistic performance of modeling result at Hon Dau, Hon Ngu,
Point B, E and K
Index Hon Dau Hon Ngu Point B Point E Point K
Hm0 θm Hm0 θm Hm0 θm Hm0 θm Hm0 θm
EI 0.57 0.48 0.48 0.57 0.69 0.57 0.89 0.56 0.84 0.64
RMSE (m, deg) 0.29 47.10 0.22 47.37 0.24 53.90 0.20 8.09 0.25 0.96
MAE (m, deg) 0.21 33.12 0.10 35.25 0.16 33.00 0.16 6.45 0.19 0.76
RMSEM 0.45 0.37 0.26 0.43 0.36 0.48 0.12 0.15 0.24 0.16
RMSES 1.11 0.82 0.55 0.74 0.81 1.03 0.33 0.66 0.39 0.60
R 0.71 0.63 0.58 0.59 0.70 0.59 0.97 0.95 0.95 0.91
R2 0.43 0.22 0.43 0.45 0.49 0.47 0.94 0.90 0.90 0.71
32
a) Time series of ship observation and NCEP/CFSR wave height at Hon Dau
b) Time series of ship observation and NCEP/CFSR wave direction at Hon Dau
Figure 5.1-2 Result of model calibration at Hon Dau
Figure 5.1-3 Scatter plot of wave height at Hon Dau
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
01-Jul-96 16-Jul-96 31-Jul-96 15-Aug-96 30-Aug-96 14-Sep-96 29-Sep-96
Wave H
eig
ht,
Hm
0 (
m)
Date
Time Series of Ship Observation and NCEP/CFSR Wave Height at Hon Dau
Hm0 (m) : Ship Observation Hm0 (m) : NCEP/CFSR
0
45
90
135
180
225
270
315
360
01-Jul-96 16-Jul-96 31-Jul-96 15-Aug-96 30-Aug-96 14-Sep-96 29-Sep-96
Wave D
irecti
on
, θm
(d
eg
)
Date
Time Series of Ship Observation and NCEP/CFSR Wave Direction at Hon Dau
Wave Direction : Ship Observation Wave Direction : NCEP/CFSR
R² = 0.43
0
1
2
3
4
0 1 2 3 4
Hm
0 (
m)
: N
CE
P/C
FS
R
Hm0 (m) : Ship Observation
33
a) Time series of ship observation and NCEP/CFSR wave height at Hon Ngu
b) Time series of ship observation and NCEP/CFSR wave direction at Hon Ngu
Figure 5.1-4 Result of model calibration at Hon Ngu
Figure 5.1-5 Scatter plot of wave height at Hon Ngu
0.0
0.5
1.0
1.5
2.0
2.5
3.0
01-Aug-94 31-Aug-94 30-Sep-94 30-Oct-94 29-Nov-94 29-Dec-94
Wave H
eig
ht,
Hm
0 (
m)
Date
Time Series of Ship Observation and NCEP/CFSR Wave Height at Hon Ngu
Hm0 (m) : Ship Observation Hm0 (m) : NCEP/CFSR
0
45
90
135
180
225
270
315
360
01-Aug-94 31-Aug-94 30-Sep-94 30-Oct-94 29-Nov-94 29-Dec-94
Wave D
irecti
on
, θm
(d
eg
))
Date
Time Series of Ship Observation and NCEP/CFSR Wave Direction at Hon Ngu
Wave Direction : Ship Observation Wave Direction : NCEP/CFSR
0
1
2
3
4
0 1 2 3 4
Hm
0 (
m)
: N
CE
P/C
FS
R
Hm0 (m) : Ship Observation
R2=0.43
34
a) Time series of ERA-40 and NCEP/CFSR wave height at Point B
b) Time series of ERA-40 and NCEP/CFSR wave direction at Point B
Figure 5.1-6 Result of model calibration at Point B
Figure 5.1-7 Scatter plot of wave height at Point B
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
01-May-90 21-May-90 10-Jun-90 30-Jun-90 20-Jul-90
Wave H
eig
ht,
Hm
0 (
m)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Height at Point B
Hm0 (m) : ERA-40 Hm0 (m) : NCEP/CFSR
0
45
90
135
180
225
270
315
360
01-May-90 21-May-90 10-Jun-90 30-Jun-90 20-Jul-90
Wave D
irecti
on
, θm
(d
eg
)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Direction at Point B
Wave Direction : ERA-40 Wave Direction : NCEP/CFSR
R² = 0.49
0
1
2
3
4
0 1 2 3 4
Hm
0 (
m)
: N
CE
P/C
FS
R
Hm0 (m) : ERA-40
35
a) Time series of ERA-40 and NCEP/CFSR wave height at Point E
b) Time series of ERA-40 and NCEP/CFSR wave direction at Point E
Figure 5.1-8 Result of model calibration at Point E
Figure 5.1-9 Scatter plot of wave height at Point E
0.0
1.0
2.0
3.0
4.0
5.0
01-Nov-94 16-Nov-94 01-Dec-94 16-Dec-94 31-Dec-94 15-Jan-95 30-Jan-95
Wave H
eig
ht,
Hm
0 (
m)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Height at Point E
Hm0 (m) : ERA-40 Hm0 (m) : NCEP/CFSR
0
45
90
135
180
225
270
315
360
01-Nov-94 16-Nov-94 01-Dec-94 16-Dec-94 31-Dec-94 15-Jan-95 30-Jan-95
Wave D
irecti
on
. θm
(d
eg
)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Direction at Point E
Wave Direction : ERA-40 Wave Direction : NCEP/CFSR
R² = 0.94
0
1
2
3
4
5
0 1 2 3 4 5
Hm
0 (
m)
: N
CE
P/C
FS
R
Hm0 (m) : ERA-40
36
a) Time series of ERA-40 and NCEP/CFSR wave height at Point K
b) Time series of ERA-40 and NCEP/CFSR wave direction at Point K
Figure 5.1-10 Result of model calibration at Point K
Figure 5.1-11 Scatter plot of wave height at Point K
0.0
1.0
2.0
3.0
4.0
01-Aug-93 21-Aug-93 10-Sep-93 30-Sep-93 20-Oct-93 09-Nov-93 29-Nov-93 19-Dec-93
Wave H
eig
ht,
Hm
0 (
m)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Height at Point K
Hm0 (m) : ERA-40 Hm0 (m) : NCEP/CFSR
0
45
90
135
180
225
270
315
360
01-Aug-93 21-Aug-93 10-Sep-93 30-Sep-93 20-Oct-93 09-Nov-93 29-Nov-93 19-Dec-93
Wave D
irecti
on
, θm
(d
eg
)
Date
Time Series of ERA-40 and NCEP/CFSR Wave Direction at Point K
Wave Direction : ERA-40 Wave Direction : NCEP/CFSR
R² = 0.90
0
1
2
3
4
5
0 1 2 3 4 5
Hm
0 (
m)
: N
CE
P/C
FS
R
Hm0 (m) : ERA-40
37
5.2 Modeling Result of Present Wave Climate
The modeling work of MIKE21 SW is conducted at ten locations along the coast of
Vietnam. There are the stations Hon Dau, Hon Ngu, A, B, C, C1, E, E1, G, G1, K, L, L1
and O as shown in Figure 5.2-1. There are three wind fields used as model input, which are
NECP/CFSR, ECHAM5 and GFDL. Results of mean monthly ten stations significant wave
height, significant wave period and wave direction, are shown in Figure 5.2-2 and 5.2-3
from Hon Dau and Point G.
Monthly mean result at Hon Dau shows that computed significant wave height has similar
value from the three wind fields. Significant wave period from NCEP/CFSR is a bit higher
than those two results and mean wave direction is a bit lower. Result of Point G is similar
to Hon Dau. All results of significant wave height at the 14 wave locations from north to
South Vietnam are shown in Figure 5.2-4. Wave height in nearest monsoon from
October/November to March has bigger wave height than other months, especially in Point
E, G and L which are located in very deep water, at depths from 400 to 1,700 m. Its mean
significant wave height is greater than two meters. Table B-1 to B-14 shows annual mean
of significant wave height, wave period and wave direction. The plot of the results and
their differences is shown in Figure 5.2-5.
Comparison of mean significant wave height between results from NCEP/CFSR, ECHAM
and GFDL for 1981 to 2000 in Figure 5.2-5 shows that most of them have small different
value except the south cost of Vietnam, Point K, L and O showing higher mean value for
NCEP/CFSR. For mean significant wave period, they show the same result but those from
NCEP/CFSR have clearly higher values than the other two at only one station, Hon Ngu in
the northern coast of Vietnam and gradually reduced to small difference toward the south.
Mean wave direction shows small differences except in one station, Hon Ngu with lower
values compared to others.
Table 5.2-1 Summary of depths and distances from shoreline at 14 locations
Station Depth (m) Distance (km) Remark
Hon Dau -36 0.60 N
Hon Ngu -35 3 N
Station A -27 105 N
Station B -60 60 N
Station C -156 250 O
Station C1 -47 25 N
Station E -419 117 O
Station E1 -50 33 N
Station G -1,724 64 O
Station G1 -50 43 N
Station K -23 50 N
Station L -1,496 194 O
Station L1 -48 40 N
Station O -52 120 N
Remark: “O” means Offshore and “N” means Nearshore
38
Figure 5.2-1 Locations of wave climate output from modeling
39
Figure 5.2-2 Present wave parameter at Hon Dau
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
40
Figure 5.2-3 Present wave parameter at Point G
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
41
Figure 5.2-4 Monthly mean significant wave height (Hm0)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
42
Figure 5.2-4 Monthly mean significant wave height (Hm0) (Cont’d)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
43
Figure 5.2-4 Monthly mean significant wave height (Hm0) (Cont’d)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
44
Figure 5.2-4 Monthly mean significant wave height (Hm0) (Cont’d)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
45
Figure 5.2-4 Monthly mean significant wave height (Hm0) (Cont’d)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
46
Figure 5.2-5 Summary of mean wave parameters and their differences
-0.4
-0.2
0.0
0.2
0.4
0.6
0.8
1.0
1.2
1.4
1.6
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
Me
an
Hs a
nd
∆H
s (
m)
NCEP/CFSR ECHAM GFDL NCEP/CFSR-ECHAM NCEP/CFSR-GFDL
-1.0
0.0
1.0
2.0
3.0
4.0
5.0
6.0
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
Me
an
Ts
an
d ∆
Ts
(s
)
NCEP/CFSR ECHAM GFDL NCEP/CFSR-ECHAM NCEP/CFSR-GFDL
-20
0
20
40
60
80
100
120
140
160
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
Me
an
θa
nd
∆θ
(de
g)
NCEP/CFSR ECHAM GFDL NCEP/CFSR-ECHAM NCEP/CFSR-GFDL
47
5.3 Modeling Result of Future Wave Climate
The computed results of future wave climate from MIKE21 SW can be analyzed and
presented in three categories which are mean monthly (and annual), probability distribution
and spatial distribution of three wave parameters i.e., significant wave height, period and
wave direction.
The first analysis shows the temporal distribution of wave climate in a monthly basis and
annual value at 10 locations along Vietnam coast which are Hon Dau, Hon Ngu, A, B,
C,…, L and O, and 4 additional nearshore wave locations which are C1, E1, G1 and L1 in
order to obtain wave conditions that could be a direct use in potential future longshore
sediment transport calculations. The second one shows the change of probability
distribution which includes small to high wave height and wave period. The last one shows
spatial distribution of wave climate using all results from model to show the change of
their mean value.
Table 5.3-1 Summary of depths and distances from shoreline at 14 locations
Station Depth (m) Distance (km) Remark
Hon Dau -36 0.60 N
Hon Ngu -35 3 N
Station A -27 105 N
Station B -60 60 N
Station C -156 250 O
Station C1 -47 25 N
Station E -419 117 O
Station E1 -50 33 N
Station G -1,724 64 O
Station G1 -50 43 N
Station K -23 50 N
Station L -1,496 194 O
Station L1 -48 40 N
Station O -52 120 N
Remark: “O” means Offshore and “N” means Nearshore
5.3.1 Monthly and Annual Mean Wave Climate
The results of computed monthly mean wave climate for present (1981 to 2000) and future
(2041 to 2060 and 2060 to 2100) are presented in tabular form in Table C-1 to C-42. Their
differences are computed and shown in Table C-43 to C-57. Plots of mean wave climate
distribution are shown in Figure C-1 to C-14. Plots of differences of monthly wave climate
are in Figure C-15 to C-28. For two stations, at Hon Dau and Point G are in Figure 5.3.1-1
and 5.3.1-2 and Table 5.3.1-1. It is noted that the difference of positive or increasing wave
direction means changing of wave direction in clockwise direction and negative or
decreasing wave direction means changing of wave direction in counter-clockwise
direction.
48
Monthly mean wave climate at Hon Dau derived by wind fields derived wave, ECHAM
and GFDL show variation of slightly decreasing trends of mean significant wave height by
negative difference in Figure 5.3.1-1 and has the maximum difference by 0.16 m (21%, as
percent different from present period) in October and the minimum difference is 0.04 m
(7%) in April. The average monthly mean significant wave height from 2081 to 2100 is
gradually decreasing in similar qualitative related to average mean significant wave height
in 2040-2061. Monthly mean wave period is slightly changing in an increasing trend by 0-
0.28 s with the maximum difference of 0.28 s (5%) in November and the minimum
difference of 0.02 s (0.4%) in February and October. Variation of monthly mean wave
direction is varied between 0-15 degrees. Average monthly mean wave direction turns
clockwise throughout the year, with the maximum difference in clockwise direction by 15
degrees (13%) in September and the minimum difference is change by 0.01 degree (0.1%)
in May.
Figure 5.3.1-2 shows the monthly mean wave climate at Station G and how the monthly
mean significant wave height varies between 0-0.30 m. The average mean significant wave
height in 2041-2060 decreases throughout the year. On the other hand, the average mean
significant wave height in 2081-2100 shows that the significant wave height is reduced
during May to October from 0-0.10 m (less than 10%) and significantly increased during
November to January by 0.30 m (17%). Average of monthly mean wave period has similar
trend with average of monthly mean significant wave height. The maximum difference is
0.43 s (9%) in September and November and the minimum difference is 0.02 s (0.5%) in
March. Variation of monthly mean wave direction varies between 0-13 degrees. In April
and May, monthly mean wave direction is slightly change by 9 degrees (9%) in counter-
clockwise direction and in September, wave direction is turned to by 13 degrees (8%) in
clockwise direction.
Differences of average future and present waves between 2041 to 2060 and 1981 to 2000
and between 2081 to 2100 and 1981 to 2000 for 14 locations are shown in Figure 5.3.1-3
and Table 5.3.1-1. Changes of future wave climate and can be categorized into three major
areas (1) North coast (i.e., Station Hon Dau, Hon Ngu, A and B) (2) Central coast (i.e.,
Station C, C1, E and E1) and (3) South coast (i.e., Station G, G1, K, L, L1 and O) of
Vietnam.
In north Vietnam (Station Hon Dau, Hon Ngu, A and B), future significant wave height
slightly decreases along the coast by 1-5 cm (1-7%) in year 2041 to 2060 and 3-8 cm (3-
12%) in year 2081 to 2100 except at Station B, which results contrarily increased by 5 cm
(4%). For changes of future wave period, the results show slightly increasing trend at all
stations by 0.03-0.08 s (1-2%) in year 2041 to 2060 and 0.12-0.19 s (2-4%) in year 2081 to
2100. Future wave direction turns to clockwise direction (towards the south) by 1-3
degrees (1-2%) in year 2041-2060 and slightly more to 3-4 degrees (2-3%) in year 2081-
2100 from south-easterly wave in present.
In central Vietnam (Station C, C1, E and E1), future significant wave height along the
coast trends to decrease around 4-6 cm (3-7%) in year 2041 to 2060 and increase by 4-5
49
cm (1-5%) in year 2081 to 2100, which is remaining as present value. For the wave period,
the result at each station tends to slightly decrease by 0.02-0.07 s (1%) from 2041 to 2060
and increase by 0.07-0.10 s (1-2%) in year 2081 to 2100 except at Station C1 that reduces
0.02 s. Future wave direction turns to clockwise direction (toward the south) with the
changes of 1-5 degrees (1-4%) in year 2041 to 2060 and 1-6 degrees (1-5%) in year 2081
to 2100 from south-easterly wave in present.
In south Vietnam (Station G, G1, K, L, L1 and O), future significant wave height is slightly
decreased by 3-6 cm (1-8%) in year 2041 to 2060 and increased by 2-7 cm (1-5%) from
year 2081 to 2100. Future wave period slightly decreases by 0.03-0.11 s (1-2%) from year
2041 to 2060 and adversely increases by 0.02-0.16 s (1-3%) in year 2081 to 2100. Future
wave direction turns to counter clockwise direction (towards the north) with the changes of
2-5 degrees (1-4%) in year 2041 to 2060 and 3-8 degrees (2-6%) in year 2081 to 2100 from
easterly wave in present.
Table 5.3.1-1 Differences in average significant wave height, wave period and wave
direction between 2041 to 2060 and 1981 to 2000 and 2081 to 2100 and 1981 to 2000 at 14
locations
Stations
Difference of Wave Parameters
b/w 2041 to 2060 - 1981 to 2000
Difference of Wave Parameters
b/w 2081 to 2100 - 1981 to 2000
Average
Hm0 (m)
Average
Tm0 (s)
Average
θm (deg)
Average
Hm0 (m)
Average
Tm0 (s)
Average
θm (deg)
Hon Dau -0.05 0.08 2.44 -0.08 0.19 3.55
Hon Ngu -0.05 0.08 2.44 -0.08 0.19 3.55
Point A -0.01 0.07 2.79 -0.03 0.15 3.34
Point B -0.02 0.03 0.63 0.05 0.12 2.47
Point C -0.04 -0.02 4.56 -0.01 0.10 4.37
Point C1 -0.07 -0.04 1.39 0.05 -0.02 5.79
Point E -0.06 -0.07 1.21 0.05 0.07 1.09
Point E1 -0.06 -0.05 0.50 0.04 0.08 1.22
Point G -0.06 -0.11 -1.39 0.07 0.03 -2.49
Point G1 -0.05 -0.09 -0.45 0.07 0.02 -0.77
Point K -0.04 -0.05 -2.94 0.02 0.16 -4.70
Point L -0.06 -0.10 -4.96 0.05 0.06 -6.78
Point L1 -0.05 -0.09 -1.88 0.04 0.10 -4.48
Point O -0.03 -0.03 -5.45 0.04 0.15 -7.95
50
Figure 5.3.1-1 Change of monthly mean wave parameters at Hon Dau
-0.20
-0.10
0.00
0.10
0.20
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
51
Figure 5.3.1-2 Change of monthly mean wave parameters at Point G
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
52
Figure 5.3.1-3 Change of annual wave parameters
-0.20
-0.15
-0.10
-0.05
0.00
0.05
0.10
0.15
0.20
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
∆H
s (
m)
∆Hs (m) : ECHAM (2041 to 2060) - (1981 to 2000) ∆Hs (m) : GFDL (2041 to 2060) - (1981 to 2000)
∆Hs (m) : Average (2041 to 2060) - (1981 to 2000) ∆Hs (m) : ECHAM (2081 to 2100) - (1981 to 2000)
∆Hs (m) : GFDL (2081 to 2100) - (1981 to 2000) ∆Hs (m) : Average (2081 to 2100) - (1981 to 2000)
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
∆T
s (
s)
∆Ts (m) : ECHAM (2041 to 2060) - (1981 to 2000) ∆Ts (m) : GFDL (2041 to 2060) - (1981 to 2000)
∆Ts (m) : Average (2041 to 2060) - (1981 to 2000) ∆Ts (m) : ECHAM (2081 to 2100) - (1981 to 2000)
∆Ts (m) : GFDL (2081 to 2100) - (1981 to 2000) ∆Ts (m) : Average (2081 to 2100) - (1981 to 2000)
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
6.0
8.0
10.0
Hon Dau Hon Ngu Point A Point B Point C Point C1 Point E Point E1 Point G Point G1 Point K Point L Point L1 Point O
∆θ
(de
g)
∆θ (m) : ECHAM (2041 to 2060) - (1981 to 2000) ∆θ (m) : GFDL (2041 to 2060) - (1981 to 2000)
∆θ (m) : Average (2041 to 2060) - (1981 to 2000) ∆θ (m) : ECHAM (2081 to 2100) - (1981 to 2000)
∆θ (m) : GFDL (2081 to 2100) - (1981 to 2000) ∆θ (m) : Average (2081 to 2100) - (1981 to 2000)
53
5.3.2 Probability Distribution
The result of the model can be plotted in the form of a probability distribution in order to
show the distribution of wave height, wave period and direction.
Figure D-1 to D-14 show the probability distribution of wave climate at present and future
conditions. Change of future wave climate compared to present in term of probability plot
can be shown in Figure D-15 to D-28. Result at station Hon Dau and Point G are in Figure
5.3.2-1 to 5.3.2-4.
The deviation of the probability distribution of significant wave height from present to
future condition [∆p(Hm0)] provides information of changing of number of waves at
different scales. At Hon Dau, the upper north station, in year 2041 to 2060, the number of
significant wave height which is less than 1 m increases, while those which are greater than
1 m to 2.5 m decrease. The same results are clearly shown from 2081 to 2100 in Figure
D15 and 5.3.2-3. Similar results can be seen along the Vietnam coast from north to south
from stations Hon Ngu, A, E, E1, G, G1, K, L, L1 and O. Opposite results can be found in
Stations B, C, C1 and D, where the number of small waves decreases and the number of
wave height which are greater than 1 m increases. These stations are located in the same
area upper of central Vietnam. The highest change is less than 5%.
For deviation of significant wave period from present to future conditions [∆p(Tm0)] at
Hon Dau, it shows that the number of small wave period, less than 5 second is slightly
reduced and the number of wave period up to 7 second increases. The same results are
highlighted for results from the year 2081 to 2100. Similar discussion can be made at
stations A, B. The opposite results can be found at stations C, C1, G, G1, K, L, L1 and O.
The results do not have any patterns at stations Hon Ngu, E and E1. It can be concluded
that the slightly change of probability distribution of significant wave period can be
divided into 2 groups, one in the north, which are stations Hon Dau, A and B, and the other
one in the south, with the stations C, G, K, L and L1. The maximum changes of probability
density function do not exceed 0.05 or 5%.
For deviation of wave direction [∆p(θm0], it shows increment of probability of wave angle
around 135° at station Hon Dau and Hon Ngu. At station C and C1, Wave direction is
clearly seen to be increased for its probability density function around 90°, around 60°at
Station E and E1 and 45° at Station L and L1. The maximum values do not exceed 5%.
Figure 5.3.2-5 shows summary of areas that have probability change for significant wave
height and period.
Figure 5.3.2-5 shows Point G, G1, K, L, L1 and O increase in small wave height less than
1 m. and reduction of wave height greater than 1 m. The highest value change is less than
5%. There is an increase in the number of small wave period which is less than 5 seconds
and the number of those greater than 7 seconds is reduced.
54
Figure 5.3.2-1 Probability distribution of present and future wave climate at Hon Dau
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
55
Figure 5.3.2-2 Probability distribution of present and future wave climate at Point G
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
56
Figure 5.3.2-3 Change of probability distribution at Hon Dau
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
57
Figure 5.3.2-4 Change of probability distribution at Point G
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
58
Figure 5.3.2-5 Probability change of significant wave height and wave period
59
5.3.3 Spatial Distribution
Time averaged mean significant wave height, wave period and wave direction derived
from climate model derived wind fields ECHAM and GFDL for three-time slices in
present period 1981 to 2000, projection periods 2041 to 2060 and 2081 to 2100 and their
average differences between 2081 to 2100 and 1981 to 2000 are used to represent changes
of future wave climate spatially. Positive changes in wave direction indicate clockwise
rotation (toward the south) and negative changes indicate counter clockwise rotation
(toward the north) of future wave directions.
Mori et al., 2010 showed the results of global wave climate projection changes depend on
the regions being negatively or positively as illustrated by following Figure 5.3.3-1. This
global mean significant wave height had been projected to increase at both middle latitude
and Antarctic Ocean, and decrease at the Equator. Projected time averaged mean
significant wave height difference between present and future period, 1979 to 2004 and
2075 to 2100. Similarly to this present modeling results shown in Figure 5.3.3-2, spatial
distribution of mean significant wave height shows that the highest wave height mostly
occurs off the north coast in deep water area. Comparing mean significant wave height
between 2081 to 2100 and 1981 to 2000, future wave height is increased by 4-8 cm along
north, central and south coasts except the coastal shelter area near Hon Dau and Hon Ngu,
which future wave height is reduced by 4-8 cm. Spatial distribution of future wave period
shows an increasing trend along Vietnam coast by 0.20 s in north and south coast and less
than 0.08 s in central coast (Figure 5.3.3-3).
Spatial distribution of future wave direction represented in Figure 5.3.3-4, shows that wave
direction changes by 4-8 degrees in clockwise direction (toward the south) along north and
central coast, while south-easterly waves in this area change to be more south-easterly. In
south coast, future mean wave direction changes by 4-8 degrees in counter clockwise
direction (toward the north), while mostly easterly waves in this area change to be more
north-easterly.
Figure 5.3.3-1 Time averaged mean significant wave height difference between future and
present period (Source: Mori et al., 2010)
∆Hs (m)
60
Aver
age
2081
-2100
Dif
fere
nce
of
signif
ican
t w
ave
hei
ght
bet
wee
n 2
08
1-2
100 a
nd 1
981-2
000
Aver
age
2041
-2060
Aver
age
1981
-2000
Figure 5.3.3-2 Spatial distribution of average ECHAM and GFDL mean significant wave
height in 1981-2000, 2041-2060, 2081-2100 and its difference between 2081-2100 and
1981-2000
61
Aver
age
2081
-2100
Dif
fere
nce
of
wav
e per
iod b
etw
een 2
081
-2100 a
nd 1
981
-2000
Aver
age
2041
-2060
Aver
age
1981
-2000
Figure 5.3.3-3 Spatial distribution of average ECHAM and GFDL mean wave period in
1981-2000, 2041-2060, 2081-2100 and its difference between 2081-2100 and 1981-2000
62
Aver
age
2081
-2100
Dif
fere
nce
of
wav
e dir
ecti
on b
etw
een 2
081
-2100 a
nd 1
981
-2000
Aver
age
2041
-2060
Aver
age
1981
-2000
Figure 5.3.3-4 Spatial distribution of average ECHAM and GFDL mean wave direction in
1981-2000, 2041-2060, 2081-2100 and its difference between 2081-2100 and 1981-2000
63
CHAPTER 6
CONCLUSIONS
1. The present study has successfully explored variations of present and future wave
climate at offshore waves at 14 locations along Vietnam coast using the numerical spectral
wave model, MIKE21 SW, which has been forced by NCEP/CFSR winds and climate
model derived wind from A2 scenario, downscaled from CCAM with ECHAM5 and
GFDL CM2.1 for three time slices; 1981 to 2000, 2041 to 2060 and 2081 to 2100.
2. Model calibration has been conducted by applying NCEP/CFSR wind field and the
model results have been compared to the wave data from the ship observations at two
locations, Hon Dau and Hon Ngu and to ERA-40 wave data at three locations, Point B,
Point E and Point K. Calibrating parameter, Cds with appropriated value of 4.5 gives
moderate to good model results compared with the wave data from two sources.
3. The comparison of the present mean significant wave height, wave period and wave
direction among the three computed results from NCEP/CFSR, ECHAM and GFDL from
year 1981 to 2000 showed small differences among the 3 sets of results. Only three stations
in the south coast of Vietnam (Station K, L and O) showed higher mean value of
significant wave height for NCEP/CFSR. Results of significant wave period from
NCEP/CFSR show higher values at only one station (Station Hon Ngu). Due to small
number of stations with different results, it can be interpreted that all wind field input data
provides more or less similar model outputs.
4. Future mean significant wave height in north coast of Vietnam is projected to be smaller
by about 8 cm with slightly longer wave period (increase of 0.20 s) and future wave
direction is projected to shift towards the south (clockwise) by less than 4 degrees. In the
central coast, future mean significant wave height is projected to slightly increase by 5 cm,
wave period to increase by less than 0.08 s and wave direction is projected to shift to the
south (clockwise) by less than 6 degrees. In south coast, the future mean significant wave
height is projected to slightly increase by 7 cm with longer wave period (increase of 0.16 s)
and future wave direction along south coast is projected to shift to the north (counter
clockwise) by less than 8 degrees.
5. The projected future changes of probability density function at the south coast of
Vietnam showed an increase of small wave heights less than 1 m and wave periods less
than 7 s. At the same time, a reduction of higher wave height and longer wave period was
found. The results could be emphasized towards the year 2100 but the biggest changes are
still unlikely exceed 5%.
6. The spatial distribution of the future mean significant wave height showed decreases of
wave height in north coast (Station Hon Dau, Hon Ngu, A and B) of less than 8 cm and
64
increases of wave height in the south coast (Station G, G1, K, L, L1 and O) of less than 4
cm. The spatial distribution of future mean wave period was projected to increase along
Vietnam Coast by less than 0.20 s in north and less than 0.20 s in south coast. The spatial
distribution of future wave direction showed a change of wave direction clockwise
(towards the south) of less than 8 degrees in north coast (Station Hon Dau, Hon Ngu, A
and B) and central coast (Station C, C1, E and E1). On the other hand, future wave
direction changed counter clockwise (towards the north) along the south coast (Station G,
G1, K, L, L1 and O) by less than 8 degrees.
65
Changes of future wave direction
in 2041 to 2060
Changes of future wave direction
in 2081 to 2100
North coast
at Hon Ngu
Central
coast at
Station C1
South coast
at Station O
Figure 6.1 Changes of future wave direction in north (Hon Ngu), central (Station C1) and
south (Station O) coast of Vietnam in year 2041-2060 and 2081-2100
66
REFERENCES
Atilla Bayram.,Magnus Larson., Han Hanson (2007). A New Formula for the Total
Longshore Sediment Transport Rate. Science Direct Coastal Engineering 54, pp
700-710.
Chin-I Lin.,Tai-An Shih and Jung-Chang Su (2002). Coastal Morphological Evolution
Investigattion on Yunlin Offshore Industrial Estate. Proceedings of the Twelfth
International Offshore and Polar Engineering Conference Kitakyushu, Japan,
pp745-749.
C. Briere., S.Abdie.,P. Bretel and P.Lang (2007). Assessment of TELEMAC System
Performances, a Hydrodynamic Case Study of Anglet, France. Science Direct
Coastal Engineering 54, pp 345-356.
Danish Hydraulic Institute (DHI), MIKE 21 Flow Model FM Hydrodynamic module, DHI
Software, Copenhegen, 2011.
Danish Hydraulic Institute (DHI), MIKE 21 & Mike 3 Flow Model FM Hydrodynamic and
Transport module, DHI Software, Copenhegen, 2011.
Danish Hydraulic Institute (DHI), MIKE 21 & Mike 3 Flow Model FM Sand Transport
module, DHI Software, Copenhegen, 2011.
Danish Hydraulic Institute (DHI), MIKE 21 Spectral Wave module, DHI Software,
Copenhegen, 2007.
Danish Hydraulic Institute (DHI), MIKE 21 Nearshore Spectral Wind-Wave module, DHI
Software, Copenhegen, 2009.
D. Strauss., H. Mirferendesk and R. Tomlinson (2007). Comparison of Two Wave Models
for Gold Coast, Australia. Journal of Coastal Research,50 (SI), pp 312-316.
Duc D.M., Nhuan M.T. and Ngoi C.V. (2012), “An Analysis of Coastal Erosion in the
Tropical Rapid Accretion Delta of the red River, Vietnam”, Journal of Asian Earth
Science, Vol.43, pp 98-109.
Ernet R. Smith., Ping Wang., Bruce A. Ebersole and Jun Zhang (2009) Dependenc of Total
Longshore Sediment Transport Rates on Incident Wave Parameters and Breaker
Type. Journal of Coastal Research,25 (3) (SI), 675-683.
Hemer, M.A., Church, J.A. and Hunter, J.R., (2007). Waves and climate change on the
Australian coast, Journal of Coastal Research, 50 (SI), 432-437.
Holthuijsen, L. H. (2007). Waves in Oceanic and Coastal Waters. United Kingdom:
Cambridge University Press.
67
I.Fairley., M.Davidson.,and K.Kinston (2009). The Morpho-dynamics of a Beach Protected
by Detached Breakwaters in a High Energy Tidal Environment. Journal of coastal
research, special Issue 56,607-611.
Jorgen Fredsoe and Rolf Deigaard. Mechanics of coastal sediment transport, World
Scientific Publishing, JBW Printers & Binders Pte. Ltd., Singapore, 1992.
Jose, F., Kobashi, D. and Stone, G.W. (2007). Spectral Wave Transformation over an
Elongated Sand Shoal off South-central Louisiana, U.S.A., Journal of Coastal
Research, 50(SI), 757 – 761.
Kavin A. Haas and Daniel M. Hanes ( 2004). Process Based Modeling of Total Longshore
Sediment Transport. Journal of Coastal Research,20 (3) (SI), 853-861.
Koman, G.K., Cavaleri, L., Donelan, M., Hasselmann, K., Hasselmann, S., and Janssen,
P.A.E.M. (1994). Dynamics and modeling of Ocean Waves. Cambridge University
Press.
Kurian.N.P., Rajiith.K., Shahul Hameed.T.S., Sheela Nair.L., Ramana Murthy.M.V.,
Arjun.S., Shamji.V.R. (2008) Wind Wave and Sediment Transport Regime off the
South-central Kerala coast, India. Springer Science Business Media B.V. 49:325-
345.
Ministry of Natural Resources and Environment (2008),Unpublished report.
Ministry of Natural Resources and Environment (2009), “Climate Change , Sea Level Rise
Scenarios for Vietnam”, 34 pages.
Moeini, M. H. and Shahidi, A. E.,(2009) Wave parameter hindcasting in a Lake using the
SWAN model. Transaction A: Civil Engineering at Sharif University of
Technology, 16 (2), 156-164.
Moeini, M.H. and Shahidi, A.E (2007) Application of two numerical models for wave
hindcasting in Lake Erie, Applied Ocean Research, 29, 137–145.
Nafiza,G.. Thidarat, B.. Marut, R.. and Chaiyut,C (2011) Hydrodynamics Analysis in The
Upper Gulf of Thailand, Journal of KMUTT, pp 90-117.
Nguyen Ngoc Thach., Nguyen Ngoc Truc and Luong Phuong Hau (2007). Studying
Shoreline Change by Using LITPACK Mathematical model (case study in Cat Hai
Island, Hai Phong City, Vietnam). VNU Journal of Science, Earth Science 23(2007)
pp 244-252.
Nikom, O and Pramot, S (2010) Application of Numerical Model for Water Circulation
around Had Khanom-Mu Ko Thale Tai, Burapha Sci Journal 15,23-30.
Pruszik Z., Szmytkiewicz M., Hung N.M. and Ninh P.V. (2002) “Coastal Processes in the
Red River Delta area, Vietnam”, Coastal Engineering Journal, Vol.44(2), pp 97-
126.
68
Rattanamanee, P. (1995). Contol of coastal erosion near Songkhla deep-sea port. (Master
thesis No. WM-95-6, Asian Institute of Technology, 1995). Bangkok: Asian
Institute of Technology.
Robert G. Dean and Robert A. Darymple (2000), Water Wave Mechanics for Engineers
and Scientists, Singapore: World Scientific Publishing Pte., Co. Ltd.
Sorensen, O.R, Hansen, H.K, Rugbjerg, M. and Sorensen, L.S. (2004). A third-generation
spectral wave model using an unstructured finite volume technique, Proceedings of
the 29th International Conference on Coastal Engineering, pp1-13.
Usama M. Saied (2004) Intregrated Coastal Engineering Modeling. Doctoral Thesis of
McMaster University 2004.
T.Liiv and U.Liiv(2005). Sediment Transport Balance Investigations for the Saaremaa
Harbour with MIKE 21 Models. Environmental research, engineering and
management, 2005 No.2(32), pp 19-24.
Stephan Mai.,Nino Ohle and Claus Zimmermann (1999) Applicability of Wave Model in
Shallow Coastal Waters. Proceedings of 5th international, Cape Town, South Africa
pp 170-179.
Strauss, D., Mirferendesk, H. and Tomlinson, R., (2007). Comparison of two wave models
for Gold Coast, Australia. Journal of Coastal Research, 50 (SI), pp 312-316.
K. Mangor, Shoreline management guidelines, Danish Hydraulic Institute, Copenhegen,
2001.
Wattana,K., Seree,S., and I-Ming T., (2005). Ocean Wave Forecasting in The Gulf of
Thailand during Typhoon Linda 1997. ScienceAsia 31, pp 243-250.
Worachat,W.,Prungchan.W.,Wiriya.L., Usa.W., (2011). The Application of One-Way
Nested Grid for The Energy Balance Equation by Wave Model. Australian Journal
of Basic and Applied Sciences, 5(3); pp 75-80.
World Meteorological Organization. (1998). Guide to Wave Analysis and Forecasting (2nd
ed.), WMO-No. 702.
W. Terink.,R.T.W.L.Hurkmans.,P.J.J.F.Torfs and R. Uijlenhoet (2010) Evaluation of a
Bias Correction Method Applied to Downscaled Precipitation and Temperature
Reanalysis Data for the Rhine Basin. Hydrology and Earth Science 14, pp 687-703.
69
Appendix A
Performance Measurement
70
Table A-1 Performance Measurement
Formula Optimum
Value Prediction
Percentage of water
balance (%)
Xi Y
i
i1
n
Xi
i1
n
100 0.00
(+) Overestimate
(-) Underestimate
or Mass balance
Peak flow difference
(unit)
p pX Y -
Mass balance and
routing
Percentage of Peak Flow
Error (PPE), (%) PPE
Ypeak
Xpeak
Xpeak
100 0.00 -
Percentage of Runoff
Volume Error (PVE),
(%)
PVE Vol
YVol
X
VolY
100 0.00 -
Root Mean Squared
Error (RMSE), (unit) RMSE
1
nXi Y
i 2
i1
n
0.00 Mass balance and
routing
Efficiency Index (EI) EI
Xi X
2
i1
n
Xi Y
i 2
i1
n
Xi X
2
i1
n
1.00 -
Standard Deviation (s),
(unit)
sx
Xi X 2
i1
n
n 1
sy
Yi Y 2
i1
n
n 1
- -
Correlation coefficient
(R)
R covXY
sxsy
covXY
Xi X Yi Y
i1
n
n 1
0.00
1.00
-1.00
No relationship
Positive relationship
Negative relationship
71
Coefficient of
determination (R2) R2 1
Xi Y
i 2
i1
n
Xi X
2
i1
n
1.00
Mass balance and
routing
Mean Absolute Error
(MAE), (unit) MAE
1
nXi Y
i
i1
n
0.00 -
Mean Percentage Error
(MPE), (%) MPE
1
n
XiY
i
Xi
i1
n
100 0.00 -
Mean Percentage Error
(MPE), (%) MPE
1
n
XiY
i
Xi
i1
n
100 0.00 -
Formula Optimum
Value Prediction
Mean Absolute
Percentage Error
(MAPE), (%)
MAPE MPE 1
n
XiY
i
Xii1
n
100 0.00 -
Root Mean Square Error
Mean (RMSEM)
RMSE
RMSEMX
0.00
Root Mean Square Error
over Standard Deviation
(RMSES)
RMSE
RMSESs
0.00
Root Mean Square
Relative Error (ER)
2
1
2
1 100n
i
i
n
i i
i
X
X Y
ER
0.00
Remark : X: Observed value
Y: Computed value
72
Appendix B
Result of Present Wave Climate
73
Table B-1 Mean parameters from model ensembles for present period at Hon Dau
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 0.67 0.62 (0.05) 0.74 (-0.07)
Mean wave period, Tm0 (s) 4.84 4.54 (0.30) 4.48 (0.36)
Mean Wave Direction, θm (deg) 118.95 130.14 (-11.19) 131.15 (-12.20)
Table B-2 Mean parameters from model ensembles for present period at Hon Ngu
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 0.69 0.62 (0.06) 0.74 (-0.06)
Mean wave period, Tm0 (s) 5.30 4.54 (0.76) 4.48 (0.82)
Mean Wave Direction, θm (deg) 102.03 130.14 (-28.11) 131.15 (-29.11)
Table B-3 Mean parameters from model ensembles for present period at Point A
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 0.92 0.79 (0.13) 0.83 (0.08)
Mean wave period, Tm0 (s) 4.77 4.56 (0.20) 4.54 (0.23)
Mean Wave Direction, θm (deg) 113.28 129.98 (-16.70) 131.44 (-18.16)
Table B-4 Mean parameters from model ensembles for present period at Point B
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.00 1.03 (-0.03) 1.04 (-0.04)
Mean wave period, Tm0 (s) 5.36 5.04 (0.32) 4.99 (0.37)
Mean Wave Direction, θm (deg) 102.71 126.54 (-23.84) 128.44 (-25.73)
Table B-5 Mean parameters from model ensembles for present period at Point C
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.26 1.26 (0.00) 1.31 (-0.05)
Mean wave period, Tm0 (s) 5.72 5.39 (0.33) 5.44 (0.28)
Mean Wave Direction, θm (deg) 115.16 124.91 (-9.75) 121.69 (-6.53)
Table B-6 Mean parameters from model ensembles for present period at Point C1
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.01 0.97 (3.67) 1.01 (0.05)
Mean wave period, Tm0 (s) 5.84 5.49 (5.91) 5.50 (5.78)
Mean Wave Direction, θm (deg) 94.14 116.01 (-23.24) 115.85 (-23.06)
74
Table B-7 Mean parameters from model ensembles for present period at Point E
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.28 1.21 (0.06) 1.25 (0.03)
Mean wave period, Tm0 (s) 5.70 5.43 (0.28) 5.45 (0.25)
Mean Wave Direction, θm (deg) 106.78 116.99 (-10.21) 114.92 (-8.14)
Table B-8 Mean parameters from model ensembles for present period at Point E1
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.08 1.07 (0.01) 1.14 (-0.06)
Mean wave period, Tm0 (s) 5.82 5.42 (0.40) 5.38 (0.45)
Mean Wave Direction, θm (deg) 97.86 113.92 (-16.06) 112.44 (-14.58)
Table B-9 Mean parameters from model ensembles for present period at Point G
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.24 1.13 (0.11) 1.16 (0.08)
Mean wave period, Tm0 (s) 5.61 5.39 (0.23) 5.42 (0.20)
Mean Wave Direction, θm (deg) 106.91 113.93 (-7.01) 112.84 (-5.93)
Table B-10 Mean parameters from model ensembles for present period at Point G1
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.09 1.03 (0.05) 1.08 (0.01)
Mean wave period, Tm0 (s) 5.76 5.47 (0.28) 5.44 (0.32)
Mean Wave Direction, θm (deg) 101.93 110.11 (-8.18) 108.61 (-6.55)
Table B-11 Mean parameters from model ensembles for present period at Point K
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.03 0.79 (0.23) 0.79 (0.24)
Mean wave period, Tm0 (s) 5.08 4.87 (0.21) 4.85 (0.24)
Mean Wave Direction, θm (deg) 134.71 137.20 (-2.50) 137.77 (-3.06)
Table B-12 Mean parameters from model ensembles for present period at Point L
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.43 1.11 (0.32) 1.11 (0.32)
Mean wave period, Tm0 (s) 5.47 5.27 (0.20) 5.34 (0.14)
Mean Wave Direction, θm (deg) 119.24 123.79 (-4.54) 123.38 (-4.14)
75
Table B-13 Mean parameters from model ensembles for present period at Point L1
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.11 1.01 (0.06) 1.05 (5.77)
Mean wave period, Tm0 (s) 5.44 5.26 (0.18) 5.26 (3.38)
Mean Wave Direction, θm (deg) 116.01 122.07 (-6.32) 122.33 (-5.45)
Table B-14 Mean parameters from model ensembles for present period at Point O
Wave Parameters NCEP/CFSR
1981-2000
ECHAM
1981-2000
GFDL
1981-2000
Mean significant wave height, Hm0 (m) 1.04 0.74 (0.30) 0.72 (0.32)
Mean wave period, Tm0 (s) 5.08 4.74 (0.34) 4.73 (0.35)
Mean Wave Direction, θm (deg) 136.97 134.76 (2.21) 137.15 (-0.18)
76
Figure B-1 Present wave parameter at Hon Dau
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
77
Figure B-2 Present wave parameter at Hon Ngu
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
78
Figure B-3 Present wave parameter at Point A
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
79
Figure B-4 Present wave parameter at Point B
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
80
Figure B-5 Present wave parameter at Point C
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
81
Figure B-6 Present wave parameter at Point C1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
82
Figure B-7 Present wave parameter at Point E
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
83
Figure B-8 Present wave parameter at Point E1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
84
Figure B-9 Present wave parameter at Point G
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
85
Figure B-10 Present wave parameter at Point G1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
86
Figure B-11 Present wave parameter at Point K
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
87
Figure B-12 Present wave parameter at Point L
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
88
Figure B-13 Present wave parameter at Point L1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
89
Figure B-14 Present wave parameter at Point O
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
GFDL CM2.1 1981-2000
90
91
Appendix C
Result of Monthly Mean Future Wave Climate
92
Table C-1 Annual and monthly mean significant wave height for three-time slices at Hon
Dau
Table C-2 Annual and monthly mean wave period for three-time slices at Hon Dau
Table C-3 Annual and monthly mean wave direction for three-time slices at Hon Dau
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 0.73 0.75 0.84 0.72 0.68 0.68 0.68
Feb 0.74 0.73 0.83 0.71 0.71 0.72 0.67
Mar 0.75 0.75 0.80 0.70 0.70 0.67 0.67
Apr 0.68 0.68 0.82 0.73 0.73 0.70 0.66
May 0.63 0.57 0.76 0.65 0.74 0.59 0.60
Jun 0.63 0.53 0.63 0.51 0.54 0.53 0.54
Jul 0.63 0.49 0.62 0.55 0.54 0.58 0.51
Aug 0.52 0.36 0.50 0.40 0.39 0.40 0.41
Sep 0.51 0.35 0.44 0.34 0.38 0.31 0.32
Oct 0.72 0.74 0.80 0.70 0.64 0.57 0.62
Nov 0.75 0.80 0.98 0.88 0.76 0.76 0.76
Dec 0.76 0.75 0.89 0.71 0.71 0.72 0.70
Annual 0.67 0.62 0.74 0.63 0.63 0.60 0.59
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 5.09 4.93 4.68 5.00 4.77 4.99 5.12
Feb 5.08 4.68 4.70 4.75 4.70 4.85 4.75
Mar 5.06 4.66 4.45 4.55 4.58 4.62 4.66
Apr 4.78 4.32 4.32 4.40 4.47 4.54 4.45
May 4.51 4.07 4.19 4.26 4.43 4.28 4.25
Jun 4.55 4.09 4.04 4.15 4.16 4.23 4.33
Jul 4.55 4.32 4.33 4.46 4.51 4.68 4.55
Aug 4.41 4.02 4.17 4.09 4.14 4.33 4.38
Sep 4.37 3.85 3.87 3.84 3.89 3.88 3.93
Oct 5.05 5.04 4.86 4.91 4.99 4.89 5.04
Nov 5.30 5.34 5.13 5.53 5.36 5.55 5.53
Dec 5.37 5.14 5.08 5.22 5.11 5.44 5.46
Annual 4.84 4.54 4.48 4.60 4.59 4.69 4.70
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 97.13 113.14 112.46 114.04 122.29 117.75 117.47
Feb 102.00 129.54 122.00 126.02 130.67 128.82 131.87
Mar 114.21 130.74 137.07 134.52 135.37 136.57 137.79
Apr 126.17 136.69 142.34 142.05 139.18 139.90 138.41
May 132.18 140.37 149.62 145.61 144.45 139.68 141.75
Jun 148.58 163.51 163.78 166.83 163.45 162.49 163.85
Jul 155.84 178.97 184.15 180.44 186.01 176.32 177.54
Aug 148.93 165.30 172.13 167.06 172.06 173.90 171.89
Sep 115.13 112.28 116.46 123.92 119.85 133.79 125.50
Oct 97.32 92.35 88.58 91.83 98.13 105.03 99.29
Nov 94.56 96.09 88.40 91.13 94.72 96.81 96.05
Dec 95.32 102.75 96.79 100.75 103.62 105.09 103.13
Annual 118.95 130.14 131.15 132.02 134.15 134.68 133.71
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
93
Table C-4 Annual and monthly mean significant wave height for three-time slices at Hon
Ngu
Table C-5 Annual and monthly mean wave period for three-time slices at Hon Ngu
Table C-6 Annual and monthly mean wave direction for three-time slices at Hon Ngu
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 0.87 0.75 0.84 0.72 0.68 0.68 0.68
Feb 0.84 0.73 0.83 0.71 0.71 0.72 0.67
Mar 0.80 0.75 0.80 0.70 0.70 0.67 0.67
Apr 0.67 0.68 0.82 0.73 0.73 0.70 0.66
May 0.55 0.57 0.76 0.65 0.74 0.59 0.60
Jun 0.48 0.53 0.63 0.51 0.54 0.53 0.54
Jul 0.46 0.49 0.62 0.55 0.54 0.58 0.51
Aug 0.41 0.36 0.50 0.40 0.39 0.40 0.41
Sep 0.48 0.35 0.44 0.34 0.38 0.31 0.32
Oct 0.82 0.74 0.80 0.70 0.64 0.57 0.62
Nov 0.91 0.80 0.98 0.88 0.76 0.76 0.76
Dec 0.94 0.75 0.89 0.71 0.71 0.72 0.70
Annual 0.69 0.62 0.74 0.63 0.63 0.60 0.59
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 5.93 4.93 4.68 5.00 4.77 4.99 5.12
Feb 5.77 4.68 4.70 4.75 4.70 4.85 4.75
Mar 5.54 4.66 4.45 4.55 4.58 4.62 4.66
Apr 5.09 4.32 4.32 4.40 4.47 4.54 4.45
May 4.73 4.07 4.19 4.26 4.43 4.28 4.25
Jun 4.59 4.09 4.04 4.15 4.16 4.23 4.33
Jul 4.52 4.32 4.33 4.46 4.51 4.68 4.55
Aug 4.46 4.02 4.17 4.09 4.14 4.33 4.38
Sep 4.68 3.85 3.87 3.84 3.89 3.88 3.93
Oct 5.74 5.04 4.86 4.91 4.99 4.89 5.04
Nov 6.20 5.34 5.13 5.53 5.36 5.55 5.53
Dec 6.38 5.14 5.08 5.22 5.11 5.44 5.46
Annual 5.30 4.54 4.48 4.60 4.59 4.69 4.70
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 84.81 113.14 112.46 114.04 122.29 117.75 117.47
Feb 87.45 129.54 122.00 126.02 130.67 128.82 131.87
Mar 96.72 130.74 137.07 134.52 135.37 136.57 137.79
Apr 104.59 136.69 142.34 142.05 139.18 139.90 138.41
May 110.97 140.37 149.62 145.61 144.45 139.68 141.75
Jun 128.58 163.51 163.78 166.83 163.45 162.49 163.85
Jul 135.82 178.97 184.15 180.44 186.01 176.32 177.54
Aug 128.54 165.30 172.13 167.06 172.06 173.90 171.89
Sep 98.25 112.28 116.46 123.92 119.85 133.79 125.50
Oct 84.43 92.35 88.58 91.83 98.13 105.03 99.29
Nov 81.89 96.09 88.40 91.13 94.72 96.81 96.05
Dec 82.38 102.75 96.79 100.75 103.62 105.09 103.13
Annual 102.03 130.14 131.15 132.02 134.15 134.68 133.71
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
94
Table C-7 Annual and monthly mean significant wave height for three-time slices at Point A
Table C-8 Annual and monthly mean wave period for three-time slices at Point A
Table C-9 Annual and monthly mean wave direction for three-time slices at Point A
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.05 0.92 0.90 0.89 0.81 0.85 0.86
Feb 1.05 0.86 0.89 0.83 0.81 0.86 0.79
Mar 1.02 0.86 0.82 0.79 0.79 0.78 0.75
Apr 0.90 0.78 0.83 0.83 0.84 0.81 0.76
May 0.82 0.70 0.81 0.80 0.89 0.75 0.74
Jun 0.84 0.72 0.74 0.72 0.74 0.74 0.78
Jul 0.84 0.73 0.80 0.85 0.84 0.87 0.78
Aug 0.68 0.50 0.62 0.56 0.58 0.59 0.62
Sep 0.66 0.44 0.48 0.41 0.48 0.40 0.43
Oct 1.01 0.99 0.94 0.94 0.84 0.75 0.85
Nov 1.08 1.06 1.16 1.20 1.01 1.06 1.08
Dec 1.10 0.95 1.02 0.92 0.90 0.96 0.94
Annual 0.92 0.79 0.83 0.81 0.80 0.79 0.78
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 5.05 4.92 4.70 5.00 4.77 4.98 5.06
Feb 5.05 4.70 4.76 4.82 4.75 4.90 4.79
Mar 5.02 4.72 4.52 4.63 4.67 4.69 4.76
Apr 4.73 4.35 4.35 4.43 4.51 4.59 4.50
May 4.47 4.10 4.21 4.27 4.45 4.27 4.25
Jun 4.50 4.21 4.16 4.25 4.27 4.27 4.41
Jul 4.48 4.47 4.54 4.67 4.72 4.79 4.67
Aug 4.31 4.08 4.28 4.15 4.23 4.38 4.44
Sep 4.25 3.83 3.87 3.78 3.87 3.82 3.87
Oct 4.93 5.03 4.84 4.87 4.92 4.79 4.95
Nov 5.16 5.26 5.13 5.47 5.26 5.45 5.45
Dec 5.24 5.10 5.08 5.14 5.04 5.34 5.33
Annual 4.77 4.56 4.54 4.62 4.62 4.69 4.71
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 81.93 106.40 107.78 105.67 117.41 109.72 108.90
Feb 88.64 127.78 118.05 122.27 128.54 125.52 128.78
Mar 105.46 128.80 136.37 133.66 134.52 135.53 136.74
Apr 122.49 138.39 143.51 144.77 140.99 140.42 138.66
May 132.07 146.52 154.98 152.31 150.38 144.01 146.68
Jun 156.00 176.43 173.00 181.09 177.58 176.28 177.21
Jul 167.10 195.47 201.62 196.73 202.58 192.11 193.83
Aug 158.50 180.23 187.32 181.78 188.01 189.92 188.95
Sep 110.03 109.50 115.81 125.78 123.02 136.44 127.61
Oct 82.59 78.06 76.66 78.22 85.46 92.54 87.01
Nov 77.04 81.29 75.70 74.76 79.47 80.75 79.71
Dec 77.50 90.83 86.45 87.06 91.94 91.24 88.58
Annual 113.28 129.98 131.44 132.01 134.99 134.54 133.55
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
95
Table C-10 Annual and monthly mean significant wave height for three-time slices at Point B
Table C-11 Annual and monthly mean wave period for three-time slices at Point B
Table C-12 Annual and monthly mean wave direction for three-time slices at Point B
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.28 1.33 1.24 1.29 1.17 1.35 1.39
Feb 1.17 1.07 1.23 1.09 1.05 1.16 1.14
Mar 1.06 1.06 0.98 0.95 0.99 1.00 1.05
Apr 0.86 0.75 0.78 0.75 0.83 0.85 0.85
May 0.72 0.58 0.60 0.57 0.63 0.61 0.61
Jun 0.69 0.68 0.65 0.67 0.70 0.66 0.76
Jul 0.67 0.88 0.91 1.03 1.06 1.00 1.00
Aug 0.63 0.64 0.73 0.71 0.78 0.86 0.91
Sep 0.69 0.56 0.59 0.47 0.58 0.51 0.59
Oct 1.25 1.54 1.41 1.38 1.32 1.27 1.36
Nov 1.45 1.77 1.79 1.87 1.64 1.89 1.86
Dec 1.51 1.53 1.58 1.48 1.43 1.67 1.65
Annual 1.00 1.03 1.04 1.02 1.01 1.07 1.10
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.23 6.02 5.62 6.14 5.75 6.12 6.20
Feb 5.92 5.34 5.57 5.55 5.38 5.55 5.57
Mar 5.52 5.27 4.83 5.04 5.14 5.14 5.34
Apr 4.98 4.56 4.41 4.43 4.66 4.74 4.78
May 4.64 4.05 3.99 3.99 4.12 4.13 4.06
Jun 4.46 3.88 3.90 3.84 3.90 3.81 3.97
Jul 4.31 4.16 4.29 4.38 4.44 4.36 4.35
Aug 4.31 3.85 4.06 3.96 4.05 4.13 4.21
Sep 4.65 4.16 4.27 4.04 4.18 4.00 4.04
Oct 5.96 6.11 6.00 5.90 5.98 5.83 5.95
Nov 6.58 6.64 6.54 6.79 6.57 6.81 6.75
Dec 6.81 6.44 6.43 6.47 6.32 6.72 6.68
Annual 5.36 5.04 4.99 5.04 5.04 5.11 5.16
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 72.41 86.04 90.85 83.00 92.66 86.84 86.14
Feb 75.97 102.09 95.65 95.88 101.04 98.45 99.23
Mar 90.00 101.78 107.38 102.76 102.34 104.55 102.73
Apr 100.75 112.94 117.77 114.44 109.93 109.20 108.15
May 114.50 142.98 148.23 145.72 139.82 132.24 140.24
Jun 148.75 200.40 201.16 210.98 205.21 200.28 208.43
Jul 158.83 229.35 230.42 229.97 232.63 222.14 232.76
Aug 159.81 217.46 219.69 215.31 225.85 228.78 234.75
Sep 103.48 119.57 124.46 134.93 130.80 148.70 164.90
Oct 72.35 63.72 65.97 62.14 68.77 70.53 68.41
Nov 67.96 68.02 66.11 61.12 65.36 65.44 61.68
Dec 67.69 74.19 73.60 70.84 73.31 74.31 70.21
Annual 102.71 126.54 128.44 127.26 128.98 128.45 131.47
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
96
Table C-13 Annual and monthly mean significant wave height for three-time slices at Point C
Table C-14 Annual and monthly mean wave period for three-time slices at Point C
Table C-15 Annual and monthly mean wave direction for three-time slices at Point C
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.61 1.69 1.61 1.70 1.49 1.70 1.76
Feb 1.39 1.26 1.54 1.35 1.24 1.31 1.32
Mar 1.19 1.23 1.05 1.07 1.12 1.08 1.14
Apr 0.98 0.89 0.88 0.82 0.90 0.89 0.91
May 0.86 0.68 0.71 0.69 0.75 0.69 0.67
Jun 0.95 0.70 0.70 0.73 0.73 0.69 0.72
Jul 0.91 0.90 0.93 1.04 1.10 1.01 0.98
Aug 0.88 0.70 0.80 0.78 0.83 0.90 0.93
Sep 0.89 0.70 0.83 0.63 0.70 0.64 0.70
Oct 1.58 1.98 1.98 1.77 1.78 1.65 1.76
Nov 1.92 2.34 2.48 2.46 2.21 2.45 2.36
Dec 2.01 2.03 2.23 2.02 1.91 2.20 2.17
Annual 1.26 1.26 1.31 1.26 1.23 1.27 1.29
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.44 6.28 5.99 6.48 5.99 6.42 6.52
Feb 6.08 5.44 5.88 5.74 5.46 5.71 5.79
Mar 5.60 5.32 4.93 5.08 5.15 5.17 5.37
Apr 5.08 4.61 4.54 4.44 4.63 4.75 4.86
May 4.90 4.26 4.26 4.20 4.32 4.32 4.29
Jun 5.10 4.37 4.38 4.33 4.37 4.27 4.41
Jul 4.98 4.86 4.97 5.01 5.09 5.00 5.01
Aug 5.09 4.60 4.80 4.60 4.74 4.81 4.88
Sep 5.07 4.62 4.88 4.49 4.63 4.51 4.60
Oct 6.33 6.52 6.53 6.34 6.40 6.21 6.49
Nov 6.91 7.03 7.13 7.32 7.05 7.34 7.36
Dec 7.07 6.81 6.97 6.91 6.74 7.16 7.22
Annual 5.72 5.39 5.44 5.41 5.38 5.47 5.57
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 74.55 83.16 84.05 80.66 91.83 84.57 84.50
Feb 85.31 103.30 89.25 96.62 102.78 99.35 95.71
Mar 106.73 105.97 105.39 108.40 107.35 108.23 102.19
Apr 123.23 123.02 121.73 126.00 123.66 116.91 114.93
May 137.52 143.23 150.02 150.30 149.43 137.98 143.08
Jun 163.95 187.02 183.16 195.30 193.32 185.78 195.23
Jul 172.43 218.14 216.14 218.71 224.20 207.41 220.65
Aug 173.66 207.98 203.87 207.76 214.90 220.29 225.84
Sep 121.56 118.17 114.25 130.83 127.02 140.05 152.38
Oct 78.59 67.84 62.23 69.02 70.77 72.12 71.60
Nov 72.39 69.21 62.67 66.32 68.65 70.56 68.01
Dec 72.01 71.89 67.47 71.76 72.94 74.75 71.98
Annual 115.16 124.91 121.69 126.81 128.90 126.50 128.84
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
97
Table C-16 Annual and monthly mean significant wave height for three-time slices at Point C1
Table C-17 Annual and monthly mean wave period for three-time slices at Point C1
Table C-18 Annual and monthly mean wave direction for three-time slices at Point C1
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.40 1.45 1.34 1.44 1.25 1.52 1.58
Feb 1.20 1.02 1.29 1.12 1.02 1.16 1.17
Mar 0.99 0.98 0.87 0.88 0.91 0.96 1.02
Apr 0.79 0.66 0.69 0.63 0.70 0.76 0.77
May 0.65 0.44 0.46 0.43 0.46 0.49 0.47
Jun 0.58 0.37 0.39 0.38 0.38 0.40 0.42
Jul 0.54 0.47 0.50 0.52 0.54 0.56 0.56
Aug 0.53 0.38 0.46 0.42 0.44 0.53 0.55
Sep 0.66 0.53 0.61 0.45 0.52 0.49 0.55
Oct 1.33 1.62 1.57 1.44 1.45 1.39 1.49
Nov 1.66 1.97 2.03 2.04 1.84 2.17 2.08
Dec 1.76 1.75 1.86 1.70 1.62 1.97 1.94
Annual 1.01 0.97 1.01 0.95 0.93 1.03 1.05
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.89 6.75 6.33 6.90 6.39 6.74 6.83
Feb 6.41 5.75 6.18 6.04 5.74 5.87 5.95
Mar 5.76 5.56 5.09 5.29 5.36 5.27 5.49
Apr 5.16 4.79 4.63 4.57 4.77 4.82 4.90
May 4.92 4.33 4.23 4.24 4.33 4.35 4.24
Jun 4.89 3.98 4.08 3.99 3.99 3.90 3.90
Jul 4.75 4.17 4.35 4.24 4.27 4.33 4.22
Aug 4.77 4.08 4.28 4.11 4.14 4.14 4.15
Sep 5.06 4.63 4.87 4.46 4.63 4.32 4.36
Oct 6.59 6.96 6.93 6.73 6.79 6.48 6.74
Nov 7.29 7.57 7.59 7.81 7.51 7.72 7.70
Dec 7.56 7.33 7.44 7.36 7.20 7.54 7.56
Annual 5.84 5.49 5.50 5.48 5.43 5.46 5.50
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 66.82 74.19 76.65 71.79 80.28 76.08 75.96
Feb 72.40 87.89 80.73 82.86 88.22 86.65 84.92
Mar 86.32 89.40 93.48 90.87 90.47 92.70 88.55
Apr 97.87 99.87 104.88 102.16 99.47 96.99 95.71
May 109.42 118.48 129.63 122.08 121.42 115.39 124.02
Jun 129.06 184.69 181.34 188.93 192.03 182.02 202.26
Jul 137.72 224.39 224.11 224.68 228.68 206.54 230.83
Aug 138.74 213.16 209.82 206.85 219.63 228.32 236.36
Sep 96.68 112.08 110.44 118.58 112.34 146.35 168.38
Oct 65.26 58.93 56.68 59.63 62.45 62.66 65.30
Nov 64.30 62.74 58.68 59.36 61.56 62.42 60.23
Dec 65.06 66.35 63.74 65.10 66.20 67.78 64.87
Annual 94.14 116.01 115.85 116.08 118.56 118.66 124.78
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
98
Table C-19 Annual and monthly mean significant wave height for three-time slices at Point E
Table C-20 Annual and monthly mean wave period for three-time slices at Point E
Table C-21 Annual and monthly mean wave direction for three-time slices at Point E
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.71 1.80 1.60 1.82 1.57 1.91 2.00
Feb 1.39 1.19 1.50 1.34 1.20 1.31 1.36
Mar 1.11 1.11 0.92 1.00 1.04 1.05 1.12
Apr 0.91 0.77 0.76 0.73 0.79 0.82 0.83
May 0.83 0.57 0.61 0.58 0.63 0.59 0.58
Jun 0.92 0.60 0.64 0.63 0.61 0.60 0.61
Jul 0.87 0.79 0.90 0.85 0.87 0.86 0.84
Aug 0.86 0.67 0.80 0.70 0.72 0.78 0.79
Sep 0.82 0.67 0.77 0.60 0.65 0.63 0.68
Oct 1.55 1.85 1.78 1.64 1.69 1.58 1.73
Nov 2.06 2.35 2.35 2.38 2.22 2.61 2.52
Dec 2.29 2.20 2.31 2.11 2.07 2.51 2.49
Annual 1.28 1.21 1.25 1.20 1.17 1.27 1.30
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.73 6.62 6.20 6.73 6.23 6.71 6.81
Feb 6.25 5.60 6.03 5.84 5.58 5.83 5.96
Mar 5.55 5.34 4.94 5.08 5.17 5.18 5.45
Apr 4.88 4.52 4.42 4.33 4.54 4.68 4.80
May 4.64 4.09 4.05 4.00 4.09 4.17 4.13
Jun 4.80 4.10 4.16 4.02 4.06 3.98 4.07
Jul 4.72 4.46 4.64 4.45 4.53 4.56 4.53
Aug 4.92 4.35 4.59 4.28 4.40 4.43 4.48
Sep 5.07 4.64 4.88 4.49 4.62 4.42 4.50
Oct 6.46 6.79 6.76 6.53 6.61 6.37 6.63
Nov 7.10 7.41 7.44 7.66 7.36 7.71 7.69
Dec 7.35 7.19 7.30 7.17 7.07 7.55 7.56
Annual 5.70 5.43 5.45 5.38 5.36 5.47 5.55
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 58.73 64.13 67.14 60.64 72.27 65.85 64.87
Feb 70.09 82.74 71.69 77.58 83.28 80.10 75.80
Mar 92.63 87.63 87.98 90.29 88.38 89.24 82.57
Apr 113.11 110.40 111.13 111.11 109.32 100.71 101.06
May 137.99 147.16 152.78 147.29 149.83 136.15 142.81
Jun 167.31 193.55 193.41 193.50 193.67 188.24 198.92
Jul 170.28 209.41 211.05 209.96 211.06 198.53 210.24
Aug 172.35 208.49 206.42 204.06 209.10 209.72 216.54
Sep 121.75 141.18 129.87 144.77 137.86 153.44 172.74
Oct 67.06 53.06 48.73 53.91 56.93 50.20 60.02
Nov 55.32 51.80 47.40 49.62 49.92 52.15 48.92
Dec 54.73 54.33 51.48 53.25 54.39 56.95 53.38
Annual 106.78 116.99 114.92 116.33 118.00 115.11 118.99
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
99
Table C-22 Annual and monthly mean significant wave height for three-time slices at Point E1
Table C-23 Annual and monthly mean wave period for three-time slices at Point E1
Table C-24 Annual and monthly mean wave direction for three-time slices at Point E1
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.55 1.66 1.51 1.68 1.45 1.78 1.86
Feb 1.26 1.09 1.43 1.23 1.11 1.22 1.27
Mar 0.98 1.02 0.89 0.92 0.96 0.98 1.05
Apr 0.77 0.68 0.71 0.65 0.72 0.76 0.77
May 0.64 0.46 0.52 0.46 0.50 0.50 0.49
Jun 0.63 0.45 0.51 0.46 0.45 0.45 0.47
Jul 0.60 0.60 0.72 0.62 0.65 0.64 0.63
Aug 0.61 0.52 0.66 0.53 0.55 0.59 0.61
Sep 0.66 0.57 0.70 0.51 0.56 0.54 0.57
Oct 1.37 1.68 1.68 1.49 1.54 1.45 1.58
Nov 1.85 2.13 2.21 2.18 2.03 2.40 2.33
Dec 2.08 2.03 2.19 1.94 1.91 2.33 2.31
Annual 1.08 1.07 1.14 1.06 1.04 1.14 1.16
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 7.01 6.81 6.28 6.91 6.40 6.88 6.97
Feb 6.52 5.75 6.11 5.98 5.70 5.95 6.07
Mar 5.74 5.44 4.97 5.17 5.25 5.25 5.53
Apr 4.99 4.55 4.37 4.36 4.57 4.72 4.82
May 4.66 4.04 3.94 3.93 4.01 4.14 4.07
Jun 4.68 3.82 3.89 3.75 3.81 3.75 3.77
Jul 4.59 4.05 4.19 4.00 4.05 4.17 4.09
Aug 4.81 4.03 4.24 3.98 4.05 4.07 4.09
Sep 5.15 4.61 4.79 4.44 4.60 4.33 4.38
Oct 6.73 6.95 6.82 6.68 6.76 6.49 6.75
Nov 7.37 7.61 7.53 7.85 7.52 7.87 7.83
Dec 7.62 7.38 7.39 7.33 7.23 7.71 7.70
Annual 5.82 5.42 5.38 5.36 5.33 5.44 5.51
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 58.39 63.62 66.09 60.07 70.81 65.11 64.29
Feb 66.87 79.44 70.50 74.86 80.72 77.72 74.18
Mar 84.63 84.05 86.48 86.87 85.26 86.61 80.55
Apr 101.41 104.47 107.81 105.41 103.76 96.40 97.23
May 121.70 138.15 147.53 138.67 141.52 129.07 136.78
Jun 152.86 193.00 192.97 190.67 191.05 184.43 199.71
Jul 158.68 210.18 212.77 210.06 211.52 197.10 210.23
Aug 157.92 208.12 204.27 200.42 206.89 207.54 214.73
Sep 105.88 129.39 118.21 135.21 126.83 147.26 163.04
Oct 57.31 50.42 45.89 49.17 52.09 47.90 55.17
Nov 53.43 51.24 45.91 48.47 49.78 51.31 48.80
Dec 55.19 54.91 50.82 53.17 54.90 56.78 53.70
Annual 97.86 113.92 112.44 112.76 114.59 112.27 116.53
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
100
Table C-25 Annual and monthly mean significant wave height for three-time slices at Point G
Table C-26 Annual and monthly mean wave period for three-time slices at Point G
Table C-27 Annual and monthly mean wave direction for three-time slices at Point G
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.83 1.79 1.54 1.79 1.58 2.00 2.05
Feb 1.40 1.13 1.43 1.29 1.17 1.27 1.38
Mar 1.02 0.99 0.82 0.91 0.94 0.97 1.04
Apr 0.74 0.62 0.60 0.58 0.64 0.67 0.70
May 0.68 0.49 0.54 0.47 0.52 0.49 0.51
Jun 0.86 0.63 0.68 0.61 0.62 0.57 0.62
Jul 0.86 0.84 0.97 0.80 0.84 0.83 0.83
Aug 0.93 0.77 0.92 0.73 0.77 0.78 0.79
Sep 0.80 0.68 0.76 0.64 0.67 0.65 0.68
Oct 1.36 1.52 1.50 1.36 1.44 1.32 1.48
Nov 1.98 1.96 2.00 1.98 1.94 2.23 2.26
Dec 2.38 2.12 2.15 1.97 2.05 2.48 2.46
Annual 1.24 1.13 1.16 1.09 1.10 1.19 1.23
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.53 6.60 6.17 6.69 6.19 6.75 6.83
Feb 6.12 5.54 5.96 5.79 5.49 5.78 5.86
Mar 5.42 5.24 4.88 4.98 5.02 5.05 5.36
Apr 4.73 4.45 4.28 4.22 4.36 4.60 4.69
May 4.44 3.91 3.93 3.80 3.82 4.01 3.99
Jun 4.70 4.07 4.13 3.89 4.02 3.83 3.98
Jul 4.71 4.43 4.60 4.29 4.35 4.33 4.36
Aug 5.05 4.41 4.64 4.25 4.38 4.29 4.33
Sep 5.10 4.64 4.91 4.52 4.65 4.41 4.48
Oct 6.42 6.76 6.77 6.51 6.59 6.30 6.59
Nov 6.95 7.40 7.46 7.65 7.36 7.69 7.71
Dec 7.21 7.19 7.29 7.11 7.05 7.58 7.54
Annual 5.61 5.39 5.42 5.31 5.27 5.39 5.48
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 46.19 50.42 51.89 45.51 55.94 50.92 49.07
Feb 55.39 65.06 54.84 60.25 65.24 62.56 58.63
Mar 74.74 69.39 70.45 73.86 71.67 71.97 66.19
Apr 100.99 101.63 101.57 97.94 98.29 89.89 95.50
May 141.39 165.18 171.84 153.42 167.86 146.54 157.84
Jun 188.05 204.07 203.17 196.53 201.68 197.76 204.14
Jul 190.35 204.69 205.89 203.53 204.49 198.30 204.36
Aug 193.74 206.01 204.96 200.13 205.36 202.46 205.17
Sep 147.83 167.29 161.27 171.34 159.07 166.57 177.30
Oct 58.30 52.39 52.85 50.82 49.64 43.26 55.85
Nov 43.40 39.13 36.21 36.38 37.81 38.42 35.71
Dec 42.60 41.84 39.19 39.78 41.37 43.08 39.94
Annual 106.91 113.93 112.84 110.79 113.20 109.31 112.47
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
101
Table C-28 Annual and monthly mean significant wave height for three-time slices at Point G1
Table C-29 Annual and monthly mean wave period for three-time slices at Point G1
Table C-30 Annual and monthly mean wave direction for three-time slices at Point G1
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.64 1.67 1.48 1.69 1.47 1.87 1.94
Feb 1.28 1.07 1.38 1.22 1.10 1.21 1.30
Mar 0.94 0.95 0.81 0.87 0.91 0.94 1.02
Apr 0.69 0.59 0.59 0.56 0.62 0.67 0.69
May 0.59 0.42 0.47 0.41 0.44 0.45 0.45
Jun 0.64 0.48 0.54 0.47 0.47 0.46 0.49
Jul 0.63 0.64 0.76 0.61 0.63 0.65 0.66
Aug 0.68 0.59 0.72 0.56 0.59 0.62 0.63
Sep 0.67 0.59 0.68 0.53 0.57 0.56 0.58
Oct 1.28 1.49 1.49 1.33 1.40 1.31 1.46
Nov 1.84 1.93 1.99 1.96 1.89 2.21 2.22
Dec 2.17 2.00 2.10 1.89 1.93 2.37 2.35
Annual 1.09 1.03 1.08 1.01 1.00 1.11 1.15
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.82 6.81 6.28 6.89 6.37 6.90 6.98
Feb 6.40 5.72 6.07 5.96 5.64 5.92 6.00
Mar 5.66 5.37 4.93 5.10 5.14 5.15 5.45
Apr 4.88 4.53 4.30 4.29 4.44 4.65 4.74
May 4.52 3.99 3.93 3.85 3.87 4.07 4.03
Jun 4.64 4.00 4.06 3.85 3.98 3.78 3.88
Jul 4.63 4.31 4.42 4.16 4.21 4.21 4.20
Aug 4.95 4.33 4.51 4.18 4.29 4.17 4.21
Sep 5.18 4.70 4.93 4.57 4.71 4.42 4.48
Oct 6.67 6.94 6.86 6.68 6.77 6.45 6.74
Nov 7.23 7.60 7.57 7.83 7.53 7.84 7.83
Dec 7.49 7.39 7.41 7.30 7.24 7.73 7.69
Annual 5.76 5.47 5.44 5.39 5.35 5.44 5.52
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 51.33 54.81 55.16 50.29 60.48 55.06 53.73
Feb 58.92 68.67 59.13 63.68 69.36 66.17 62.97
Mar 76.33 72.58 74.16 76.52 74.93 75.26 69.72
Apr 97.64 99.19 101.25 97.17 97.84 89.60 94.11
May 129.48 150.74 158.45 143.68 154.91 135.38 146.99
Jun 174.97 194.76 194.85 188.53 191.24 189.64 198.00
Jul 179.04 198.51 200.88 197.44 198.54 192.50 200.27
Aug 180.12 199.22 198.18 193.33 197.54 197.35 201.29
Sep 126.63 147.52 136.04 154.55 139.31 151.04 163.60
Oct 54.77 46.09 43.71 45.38 46.47 41.45 47.80
Nov 46.51 42.70 38.49 40.24 41.82 42.21 40.14
Dec 47.45 46.59 43.01 44.29 46.32 47.26 44.58
Annual 101.93 110.11 108.61 107.93 109.90 106.91 110.27
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
102
Table C-31 Annual and monthly mean significant wave height for three-time slices at Point K
Table C-32 Annual and monthly mean wave period for three-time slices at Point K
Table C-33 Annual and monthly mean wave direction for three-time slices at Point K
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.73 1.29 1.13 1.20 1.20 1.45 1.39
Feb 1.42 0.96 1.13 1.04 0.98 1.02 1.09
Mar 1.07 0.83 0.72 0.78 0.81 0.83 0.80
Apr 0.71 0.46 0.44 0.45 0.50 0.49 0.48
May 0.55 0.36 0.41 0.34 0.39 0.34 0.37
Jun 0.65 0.52 0.53 0.44 0.49 0.42 0.48
Jul 0.65 0.66 0.71 0.58 0.59 0.57 0.63
Aug 0.75 0.67 0.72 0.57 0.61 0.58 0.61
Sep 0.64 0.57 0.61 0.53 0.54 0.48 0.54
Oct 0.88 0.79 0.76 0.71 0.77 0.70 0.75
Nov 1.43 1.08 1.06 1.04 1.06 1.19 1.18
Dec 1.84 1.33 1.31 1.18 1.31 1.57 1.49
Annual 1.03 0.79 0.79 0.74 0.77 0.80 0.82
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.45 6.18 5.60 6.22 5.82 6.44 6.61
Feb 5.72 5.01 5.42 5.27 5.07 5.26 5.45
Mar 4.98 4.74 4.40 4.49 4.66 4.61 4.94
Apr 4.24 4.11 3.91 3.96 4.07 4.27 4.36
May 3.91 3.46 3.49 3.45 3.40 3.68 3.61
Jun 3.95 3.54 3.53 3.44 3.57 3.49 3.52
Jul 4.02 3.89 3.98 3.76 3.76 3.77 3.89
Aug 4.21 3.98 4.09 3.80 3.87 3.88 3.99
Sep 4.28 4.09 4.15 3.92 4.03 3.95 3.98
Oct 5.66 6.01 6.03 5.84 6.01 5.77 6.15
Nov 6.46 6.64 6.77 6.92 6.75 7.05 7.36
Dec 7.10 6.77 6.76 6.58 6.59 7.14 7.24
Annual 5.08 4.87 4.85 4.80 4.80 4.94 5.09
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 79.65 78.09 79.51 76.69 80.76 78.79 79.75
Feb 82.74 86.19 80.31 83.46 86.04 85.29 84.91
Mar 90.66 89.00 92.43 92.77 91.44 91.13 94.82
Apr 111.70 118.06 120.74 106.16 111.66 108.54 120.69
May 158.45 183.50 193.64 164.24 187.21 164.21 177.55
Jun 208.91 214.11 214.97 201.71 210.08 199.66 208.94
Jul 207.51 205.14 204.39 203.53 205.92 196.60 202.82
Aug 212.96 206.21 202.65 199.69 205.89 196.44 198.29
Sep 189.57 194.66 200.80 200.86 192.05 186.42 195.25
Oct 112.47 117.67 109.92 118.00 105.68 102.33 110.52
Nov 82.94 79.48 79.95 78.72 78.44 75.66 76.77
Dec 78.91 74.29 73.90 73.57 74.58 75.29 76.02
Annual 134.71 137.20 137.77 133.28 135.81 130.03 135.53
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
103
Table C-34 Annual and monthly mean significant wave height for three-time slices at Point L
Table C-35 Annual and monthly mean wave period for three-time slices at Point L
Table C-36 Annual and monthly mean wave direction for three-time slices at Point L
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 2.33 1.86 1.54 1.79 1.67 2.10 2.09
Feb 1.74 1.18 1.45 1.34 1.22 1.31 1.45
Mar 1.20 0.97 0.81 0.89 0.94 0.95 0.99
Apr 0.76 0.54 0.49 0.51 0.55 0.58 0.60
May 0.67 0.46 0.49 0.41 0.44 0.44 0.47
Jun 1.05 0.72 0.71 0.58 0.66 0.56 0.66
Jul 1.07 0.86 0.94 0.76 0.78 0.75 0.84
Aug 1.27 0.87 0.94 0.75 0.82 0.76 0.80
Sep 1.01 0.79 0.86 0.76 0.77 0.70 0.76
Oct 1.32 1.31 1.31 1.18 1.26 1.14 1.29
Nov 2.04 1.70 1.72 1.69 1.68 1.88 1.98
Dec 2.69 2.05 2.00 1.82 1.99 2.37 2.37
Annual 1.43 1.11 1.11 1.04 1.06 1.13 1.19
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.56 6.51 6.14 6.64 6.18 6.76 6.86
Feb 5.92 5.42 5.95 5.75 5.48 5.71 5.83
Mar 5.24 5.19 4.89 4.97 5.07 5.04 5.43
Apr 4.62 4.46 4.35 4.23 4.43 4.63 4.74
May 4.29 3.76 3.85 3.69 3.68 3.92 3.88
Jun 4.53 3.92 3.93 3.69 3.86 3.72 3.83
Jul 4.56 4.21 4.37 4.05 4.05 4.02 4.16
Aug 4.90 4.29 4.41 4.07 4.19 4.08 4.18
Sep 4.84 4.46 4.65 4.34 4.46 4.24 4.33
Oct 6.21 6.57 6.67 6.37 6.50 6.19 6.50
Nov 6.78 7.30 7.50 7.65 7.36 7.68 7.76
Dec 7.22 7.15 7.32 7.11 7.02 7.61 7.55
Annual 5.47 5.27 5.34 5.21 5.19 5.30 5.42
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 39.47 41.20 43.86 36.57 43.93 40.58 38.29
Feb 47.30 53.44 43.30 49.09 51.61 51.31 45.98
Mar 61.12 55.54 59.03 60.12 57.20 58.03 55.90
Apr 86.85 98.40 94.83 84.29 84.61 85.90 95.16
May 151.46 186.97 200.06 164.14 189.19 165.78 182.63
Jun 220.08 226.07 225.14 210.49 224.03 209.43 223.82
Jul 221.36 218.59 216.43 213.97 218.53 207.70 216.00
Aug 227.90 220.66 215.80 211.62 219.42 209.08 212.39
Sep 199.08 205.83 217.98 213.35 200.68 198.63 212.31
Oct 91.69 102.87 92.56 96.70 81.74 78.94 87.33
Nov 47.06 42.47 40.33 33.23 36.41 31.71 30.26
Dec 37.55 33.40 31.26 32.51 33.45 34.31 31.91
Annual 119.24 123.79 123.38 117.17 120.07 114.28 119.33
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
104
Table C-37 Annual and monthly mean significant wave height for three-time slices at Point L1
Table C-38 Annual and monthly mean wave period for three-time slices at Point L1
Table C-39 Annual and monthly mean wave direction for three-time slices at Point L1
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.75 1.63 1.43 1.61 1.48 1.83 1.84
Feb 1.36 1.08 1.36 1.22 1.12 1.19 1.30
Mar 0.98 0.94 0.81 0.87 0.91 0.92 0.97
Apr 0.67 0.56 0.54 0.52 0.59 0.60 0.63
May 0.57 0.44 0.50 0.41 0.46 0.43 0.46
Jun 0.73 0.60 0.66 0.55 0.58 0.51 0.57
Jul 0.74 0.76 0.89 0.70 0.73 0.70 0.74
Aug 0.84 0.75 0.88 0.67 0.72 0.69 0.70
Sep 0.73 0.65 0.73 0.62 0.63 0.59 0.63
Oct 1.13 1.21 1.22 1.10 1.18 1.08 1.19
Nov 1.71 1.63 1.67 1.63 1.62 1.83 1.86
Dec 2.13 1.85 1.88 1.70 1.81 2.16 2.12
Annual 1.11 1.01 1.05 0.97 0.99 1.04 1.08
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.47 6.52 6.05 6.62 6.15 6.73 6.84
Feb 5.94 5.43 5.84 5.71 5.43 5.71 5.81
Mar 5.31 5.16 4.78 4.90 4.98 4.99 5.33
Apr 4.64 4.43 4.21 4.18 4.34 4.58 4.66
May 4.26 3.73 3.77 3.66 3.63 3.92 3.87
Jun 4.34 3.82 3.87 3.66 3.80 3.67 3.79
Jul 4.37 4.18 4.32 4.02 4.04 4.06 4.16
Aug 4.67 4.22 4.39 4.04 4.14 4.10 4.19
Sep 4.82 4.46 4.66 4.35 4.46 4.30 4.37
Oct 6.35 6.72 6.66 6.47 6.58 6.31 6.66
Nov 6.89 7.28 7.34 7.55 7.30 7.62 7.72
Dec 7.21 7.14 7.17 7.04 6.98 7.55 7.53
Annual 5.44 5.26 5.26 5.19 5.15 5.30 5.41
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 51.91 55.36 55.70 51.75 59.33 55.20 54.52
Feb 58.05 66.95 58.26 62.74 67.12 64.27 62.33
Mar 71.58 69.94 73.59 75.48 73.43 72.76 71.26
Apr 96.49 104.89 105.76 97.41 101.01 94.18 103.41
May 147.99 177.64 186.61 162.22 183.32 157.91 170.50
Jun 204.32 215.43 215.84 205.65 213.35 203.79 211.94
Jul 205.78 211.43 211.71 209.94 212.31 203.98 209.53
Aug 209.32 212.82 210.39 205.62 212.04 205.30 206.84
Sep 170.46 183.95 189.14 188.37 176.70 175.64 186.37
Oct 74.57 70.75 67.66 73.95 67.22 59.33 68.10
Nov 51.27 46.89 46.47 45.53 47.10 45.74 45.00
Dec 50.40 48.77 46.81 47.33 48.80 49.24 48.04
Annual 116.01 122.07 122.33 118.83 121.81 115.61 119.82
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
105
Table C-40 Annual and monthly mean significant wave height for three-time slices at Point O
Table C-41 Annual and monthly mean wave period for three-time slices at Point O
Table C-42 Annual and monthly mean wave direction for three-time slices at Point O
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 1.80 1.27 1.06 1.18 1.20 1.51 1.35
Feb 1.37 0.91 1.09 1.02 0.94 1.01 1.08
Mar 0.99 0.72 0.61 0.69 0.70 0.76 0.70
Apr 0.63 0.40 0.36 0.38 0.40 0.41 0.39
May 0.55 0.33 0.38 0.29 0.35 0.34 0.34
Jun 0.66 0.47 0.47 0.41 0.47 0.41 0.46
Jul 0.70 0.64 0.66 0.56 0.57 0.59 0.65
Aug 0.82 0.65 0.70 0.57 0.61 0.62 0.66
Sep 0.69 0.56 0.59 0.52 0.53 0.48 0.54
Oct 0.84 0.73 0.67 0.64 0.68 0.62 0.66
Nov 1.44 0.92 0.89 0.89 0.90 1.03 1.01
Dec 1.94 1.25 1.18 1.08 1.23 1.50 1.41
Annual 1.04 0.74 0.72 0.69 0.72 0.77 0.77
Projection 2041-2060 Projection 2081-2100Present 1981-2000Month
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 6.47 6.05 5.53 5.98 5.71 6.27 6.36
Feb 5.81 5.10 5.43 5.27 5.10 5.22 5.40
Mar 5.07 4.85 4.54 4.56 4.79 4.65 5.01
Apr 4.30 4.14 4.00 4.08 4.24 4.32 4.35
May 3.98 3.48 3.50 3.49 3.44 3.64 3.62
Jun 4.21 3.53 3.56 3.53 3.57 3.56 3.54
Jul 4.23 3.86 3.91 3.77 3.79 3.81 3.89
Aug 4.46 3.91 4.09 3.85 3.91 3.94 4.02
Sep 4.33 3.94 4.01 3.88 3.96 3.93 3.91
Oct 5.28 5.37 5.46 5.30 5.50 5.29 5.62
Nov 6.02 6.26 6.24 6.35 6.37 6.52 6.88
Dec 6.79 6.42 6.43 6.15 6.22 6.70 6.74
Annual 5.08 4.74 4.73 4.68 4.72 4.82 4.94
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
NCEP/CFSR ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1 ECHAM5 GFDL CM2.1
Jan 68.00 71.29 71.89 66.38 70.13 68.74 68.67
Feb 71.91 75.11 70.58 72.91 72.69 75.56 73.05
Mar 79.96 77.59 80.17 79.66 76.77 78.78 85.39
Apr 109.67 116.38 115.52 94.34 94.84 97.70 116.25
May 165.72 179.39 200.77 156.11 184.31 163.65 180.24
Jun 213.22 211.19 214.78 198.01 204.04 193.30 200.55
Jul 206.55 190.47 191.78 193.89 192.29 184.28 192.55
Aug 218.80 193.15 188.38 190.25 197.52 183.12 185.17
Sep 210.86 202.68 211.62 215.52 211.79 197.10 206.31
Oct 142.43 158.75 143.52 149.35 125.70 127.07 130.99
Nov 92.09 77.00 91.67 82.90 74.48 66.79 67.73
Dec 64.40 64.08 65.07 63.93 64.22 64.62 64.44
Annual 136.97 134.76 137.15 130.27 130.73 125.06 130.94
Projection 2041-2060 Projection 2081-2100Month
Present 1981-2000
106
Figure C-1 Present and projected wave parameters at Hon Dau
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Hon Dau
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
107
Figure C-2 Present and projected wave parameters at Hon Ngu
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Hon Ngu
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
108
Figure C-3 Present and projected wave parameters at Point A
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point A
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
109
Figure C-4 Present and projected wave parameters at Point B
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point B
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
110
Figure C-5 Present and projected wave parameters at Point C
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point C
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
111
Figure C-6 Present and projected wave parameters at Point C1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point C1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
112
Figure C-7 Present and projected wave parameters at Point E
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point E
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
113
Figure C-8 Present and projected wave parameters at Point E1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point E1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
114
Figure C-9 Present and projected wave parameters at Point G
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point G
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
115
Figure C-10 Present and projected wave parameters at Point G1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point G1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
116
Figure C-11 Present and projected wave parameters at Point K
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point K
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
117
Figure C-12 Present and projected wave parameters at Point L
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point L
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
118
Figure C-13 Present and projected wave parameters at Point L1
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point L1
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
119
Figure C-14 Present and projected wave parameters at Point O
0.0
0.5
1.0
1.5
2.0
2.5
3.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave H
eig
ht,
Hm
0 (
m)
Month
Monthly Mean Significant Wave Height (Hm0) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.0
1.0
2.0
3.0
4.0
5.0
6.0
7.0
8.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Wave P
eri
od
, T
m0 (
s)
Month
Monthly Mean Wave Period (Tm0) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0
45
90
135
180
225
270
315
360
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Mean
Wave D
irecti
on
, m
(d
eg
)
Month
Monthly Mean Wave Direction (m) at Point O
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
120
Figure C-15 Change of wave parameters at Hon Dau
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
121
Figure C-16 Change of wave parameters at Hon Ngu
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
122
Figure C-17 Change of wave parameters at Point A
-0.20
-0.10
0.00
0.10
0.20
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
123
Figure C-18 Change of wave parameters at Point B
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-50.0
-40.0
-30.0
-20.0
-10.0
0.0
10.0
20.0
30.0
40.0
50.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
124
Figure C-19 Change of wave parameters at Point C
-0.20
-0.15
-0.10
-0.05
0.00
0.05
0.10
0.15
0.20
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-30.0
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
30.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
125
Figure C-20 Change of wave parameters at Point C1
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-60.0
-50.0
-40.0
-30.0
-20.0
-10.0
0.0
10.0
20.0
30.0
40.0
50.0
60.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
126
Figure C-21 Change of wave parameters at Point E
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-40.0
-30.0
-20.0
-10.0
0.0
10.0
20.0
30.0
40.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
127
Figure C-22 Change of wave parameters at Point E1
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-40.0
-30.0
-20.0
-10.0
0.0
10.0
20.0
30.0
40.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
128
Figure C-23 Change of wave parameters at Point G
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
129
Figure C-24 Change of wave parameters at Point G1
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
130
Figure C-25 Change of wave parameters at Point K
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-12.0
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
6.0
8.0
10.0
12.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
131
Figure C-26 Change of wave parameters at Point L
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
132
Figure C-27 Change of wave parameters at Point L1
-0.25
-0.20
-0.15
-0.10
-0.05
0.00
0.05
0.10
0.15
0.20
0.25
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
6.0
8.0
10.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
133
Figure C-28 Change of wave parameters at Point O
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆H
s (
m)
∆Hs : Average (2041to2060) - (1981to2000) ∆Hs : Average (2081to2100) - (1981to2000)
-0.60
-0.50
-0.40
-0.30
-0.20
-0.10
0.00
0.10
0.20
0.30
0.40
0.50
0.60
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆T
s (
s)
∆Ts : Average (2041to2060) - (1981to2000) ∆Ts : Average (2081to2100) - (1981to2000)
-30.0
-25.0
-20.0
-15.0
-10.0
-5.0
0.0
5.0
10.0
15.0
20.0
25.0
30.0
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec∆θ
(de
g)
∆θ : Average (2041to2060) - (1981to2000) ∆θ : Average (2081to2100) - (1981to2000)
134
135
Appendix D
Result of Probability Future Wave Climate
136
Figure D-1 Probability distribution of present and future wave climate at Hon Dau
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
137
Figure D-2 Probability distribution of present and future wave climate at Hon Ngu
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
138
Figure D-3 Probability distribution of present and future wave climate at Point A
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
139
Figure D-4 Probability distribution of present and future wave climate at Point B
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
140
Figure D-5 Probability distribution of present and future wave climate at Point C
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
141
Figure D-6 Probability distribution of present and future wave climate at Point C1
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
142
Figure D-7 Probability distribution of present and future wave climate at Point E
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
143
Figure D-8 Probability distribution of present and future wave climate at Point E1
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
144
Figure D-9 Probability distribution of present and future wave climate at Point G
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
145
Figure D-10 Probability distribution of present and future wave climate at Point G1
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
146
Figure D-11 Probability distribution of present and future wave climate at Point K
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
147
Figure D-12 Probability distribution of present and future wave climate at Point L
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
148
Figure D-13 Probability distribution of present and future wave climate at Point L1
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
149
Figure D-14 Probability distribution of present and future wave climate at Point O
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.0 1.0 2.0 3.0 4.0 5.0
p(H
m0)
Hm0 (m)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
p(T
m0)
Tm0 (s)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
0.00
0.05
0.10
0.15
0.20
0.25
0 45 90 135 180 225 270 315 360
p(θ
m)
θm (deg)
NCEP/CFSR 1981-2000
ECHAM5 1981-2000
ECHAM5 2041-2060
ECHAM5 2081-2100
GFDL CM2.1 1981-2000
GFDL CM2.1 2041-2060
GFDL CM2.1 2081-2100
150
Figure D-15 Change of probability distribution at Hon Dau
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
151
Figure D-16 Change of probability distribution at Hon Ngu
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
152
Figure D-17 Change of probability distribution at Point A
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
153
Figure D-18 Change of probability distribution at Point B
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
154
Figure D-19 Change of probability distribution at Point C
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
155
Figure D-20 Change of probability distribution at Point C1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
156
Figure D-21 Change of probability distribution at Point E
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
157
Figure D-22 Change of probability distribution at Point E1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
158
Figure D-23 Change of probability distribution at Point G
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
159
Figure D-24 Change of probability distribution at Point G1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
160
Figure D-25 Change of probability distribution at Point K
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
161
Figure D-26 Change of probability distribution at Point L
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
162
Figure D-27 Change of probability distribution at Point L1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1
163
Figure D-28 Change of probability distribution at Point O
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.20
-0.16
-0.12
-0.08
-0.04
0.00
0.04
0.08
0.12
0.16
0.20
0.0 1.0 2.0 3.0 4.0 5.0
∆p
(Hm
0)
Hm0 (m)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14
∆p
(Tm
0)
Tm0 (s)
2081-2100 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2041-2060 Average
ECHAM5
GFDL CM2.1
-0.10
-0.08
-0.06
-0.04
-0.02
0.00
0.02
0.04
0.06
0.08
0.10
0 45 90 135 180 225 270 315 360
∆p
(θm
)
θm (deg)
2081-2100 Average
ECHAM5
GFDL CM2.1