atmospheric internal solitary waves observed by meris/asar in the mozambique channel, africa. jorge...
TRANSCRIPT
Atmospheric Internal Solitary Waves Atmospheric Internal Solitary Waves observed by MERIS/ASAR in the observed by MERIS/ASAR in the
Mozambique Channel, Africa.Mozambique Channel, Africa.
Jorge Magalhães ([email protected]), J. C. da Silva, Institute of Oceanography & Department of Physics, University of Lisbon
Roger Grimshaw and Mathew Pearce.Department of Mathematical Sciences, Loughborough University, U.K..
SeptemberSeptember 29, 2005 29, 2005ESA-ESRIN, Frascati, Italy.ESA-ESRIN, Frascati, Italy.
AcknowledgementsAcknowledgements
ESA project AOPT-2423, A Multi-sensor Analysis and Interpretation System for the Coastal Zone Remote Sensing (AMAZING).
INTAS – SIMP (03-51-4987): Slicks as Indicators of Marine Processes.
Modis satellite data: http://daac.gsfc.nasa.gov
Atmospheric soundings: http://weather.uwyo.edu
Surface wind velocity data: www.ssmi.com
MotivationsMotivations
Atmospheric internal solitary waves are recognized to be an important component of the dynamics of the atmospheric boundary layer.
They represent a fundamental element in the weather evolution for tropical Africa (Leroux, 2001).
In the Mozambique Channel this kind of phenomena is often associated with rain and thunderstorms (Leroux, 2001).
Why is this important for Remote Sensing? Discrimination between oceanic and atmospheric internal waves.
AimsAims::
Recently discovered area, with high occurrence frequency of internal waves, both atmospheric and oceanic.
Their main physical properties and propagation characteristics.
New physical parameter which seems to be a strong indicator of favorable propagating conditions for the atmospheric internal waves.
New possible method to detect and reveal the presence of atmospheric internal waves (synergy of MERIS /Scatterometer/ SAR).
IntroductionIntroductionAtmospheric internal solitary waves are very popular in the Gulf of
Carpentaria (Australia).
The so called...Morning Glories
IntroductionIntroduction
Characterized by horizontal scales of a 100 meters to a few kilometers and phase speeds in the order of 10 ms-1.
They usually appear as an amplitude-order series of waves of elevation.
Atmospheric internal waves that propagate in the atmosphere fall broadly in to two classes:
Those that propagate in a fairly shallow stratified layer above the earth’s surface.
Those that occupy the entire troposphere.
MozambiqueMozambique ChannelChannel
Recently discovered area, very promising potential, never studied before…
Very rich in oceanic and atmospheric internal waves.
Why the Mozambique Channel?
MozambiqueMozambique ChannelChannel
Statistical approach referring to 2nd semester of 2002.
Data collected from Meris, ASAR and Modis sensors.
Daily record of atmospheric internal waves presence in the Mozambique Channel.
Column charts addressing the phenomenon's temporal and spatial variability.
MozambiqueMozambique Channel Channel
INTERNAL WAVES SATELLITE OBSERVATION, SECOND SEMESTER 2002
16
19
1112
2
00
2
4
6
8
10
12
14
16
18
20
July August September October November December
Num
ber
of w
ave
trai
ns
.
Similar conclusions for all three sensors:
High frequency of atmospheric internal
waves during the winter period
(Southern Hemisphere).
Atmospheric internal waves in Atmospheric internal waves in the Mozambiquethe Mozambique Channel Channel
High frequency of atmospheric internal waves in the Mozambique Channel.
Enables us to conduct a systematic and trustworthy survey capable of characterizing the phenomena's physical properties.
Supplies with the means necessary to compare the experimental outcomes with those predicted by theoretical models.
Atmospheric internal waves in Atmospheric internal waves in the Mozambiquethe Mozambique ChannelChannel
How to describe atmospheric internal gravity waves from a physical point of view and indicate their more salient properties?
Using a computer program, developed with IDL computer language, that analyses the available data, and calculates several physical parameters of particular interest such as the buoyancy frequency and the Scorer parameter.
Absolute necessity for the existence of internal waves is a horizontal wave guide which inhibits the wave energy from propagating away in the vertical direction.
Comparing data results with Comparing data results with theoretical modelstheoretical models
How can we characterize the wave guide from a physical point of a view?
What constitutes suitable boundary conditions?
Determine the depth of the waveguide.
Comparing data results with Comparing data results with theoretical modelstheoretical models
Analyze Scorer’s Parameter vertical profile.
Scorer ParameterScorer Parameter
Brunt-Väisälä frequency
Wave’s phase speedMean wind velocity component in the
direction of the wave propagation
Scorer ParameterScorer Parameter
Scorer Parameter's behavior is govern by two intrinsically distinct factors:
N2: Measures the atmospheres stability.
dz2
: Indicator of shear effect.d2u0
Meris High Resolution ImageMeris High Resolution Image
Mozambique Channel, 16 September 2004
Case Case studystudy: 16 : 16 AugustAugust 2002 2002
Buoyancy Frequency (s-1)
Shear Effect (s-2)
Scorer Parameter (m-2)
Subsidence ParameterSubsidence Parameter
Represents a strong indicator of favorable propagating conditions for atmospheric internal waves.
Measures the strength of sudden and abrupt changes in dew point temperature vertical profile.
Typical dew point temperature vertical profile.
Subsidence Parameter =
Subsidence Area!!
Total ΔT
To
tal Δ
Z
ΔT/ΔZ in the Subsidence Area
Total ΔT/Total ΔZ
Subsidence ParameterSubsidence Parameter
Evolution of the Scorer parameter over time for the Antananarivo station August, 2002
High Resolution ImageHigh Resolution Image
Mozambique Channel, 16 August 2002
Strong correlation between high values of the Subsidence Parameter and the presence of internal waves.
Represents a starting point in atmospheric internal wave’s favorable generating conditions forecast.
Atmospheric internal waves play important role in the weather evolution for tropical Africa.
Important from the meteorological point of a view.
Subsidence ParameterSubsidence Parameter
A new insight:A new insight:
Present what seems to be a new remote sensing method to detect and reveal internal solitary waves.
Is it possible for the solitary waves to produce a signature in the surface wind velocity field?
Present the wind velocity field in the Mozambique Channel at the surface level for 22nd of August 2004.
A new insight:A new insight:
Mozambique Channel, 22 August 2004
A new insight:A new insight:
Mozambique Channel, 22 August 2004
Meris High Resolution ImageMeris High Resolution Image
Mozambique Channel, 22 August 2004
A new insight:A new insight:
Mozambique Channel, 22 August 2004
ConclusionsConclusions::
Mozambique Channel → High potential for internal wave’s study.
Importance of the Scorer Parameter to the definition of the waveguide’s properties.
Positive correlation between the presence of atmospheric internal waves and high values of the Subsidence Parameter.
Atmospheric solitary waves produce a measurable signature in the wind velocity field (Scatterometer /ASAR).