climate change impacts on phytoplankton biodiversity & impacts on the ecosystem of the arabian...
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CLIMATE CHANGE IMPACTS ON PHYTOPLANKTON BIODIVERSITY & IMPACTS ON THE ECOSYSTEM OF THE ARABIAN SEA. Joaquim I. Goes & Helga Gomes, Bigelow Lab. USA. Prabhu Matondkar & Sushma Parab NIO, India. Prasad Thoppil, John Kindle & Sergio de Rada, NRL, USA. - PowerPoint PPT PresentationTRANSCRIPT
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CLIMATE CHANGE IMPACTS ON PHYTOPLANKTON BIODIVERSITY &
IMPACTS ON THE ECOSYSTEM OF THE ARABIAN SEA
Joaquim I. Goes & Helga Gomes, Bigelow Lab. USA
Prasad Thoppil, John Kindle & Sergio de Rada, NRL, USA
Adnan Al Azri, Sultan Qaboos Univ., Oman
Prabhu Matondkar & Sushma Parab NIO, India
R. M. Dwivedi, Space Applications, Centre, India
John Fasullo, NCAR, USA, Fei Chai, Univ. Maine, USA
Richard Barber, Duke Univ., USA
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UNIQUE FEATURES OF THE ARABIAN SEA
Comes under the influence of the monsoon winds which reverse their direction seasonally driving one the most energetic current systems and the greatest seasonal variability of phytoplankton biomass
Is a tropical sea and the northwestern landlocked arm of the Indian Ocean
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Reversal of the winds and their intensity is strongly regulated by thermal gradient between land and sea
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Schematic showing snow cover extent and wind direction superimposed on an ocean color chlorophyll image for the northeast monsoon season
(Nov-Feb).
LOW
HIGH
0.1 0.5 1.0 2.0 5.0 10.0 20.0
WINTER MONSOON
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Schematic showing the reversal in wind direction during the southwest monsoon (Jun-Sept), superimposed on satellite derived chlorophyll fields
LOW
HIGH
0.1 0.5 1.0 2.0 5.0 10.0 20.0
SUMMER MONSOON
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LESS PHYTO
COLDER LANDMASS
SEA
MORE SNOW
WEAKER SW MONSOON WINDS
WEAKER UPWELLING
WEAKER LAND SEA PRESSURE GRADIENT
HIGHER ALBEDO
SEA
LESS SNOW
STRONGER SW MONSOON WINDS
STRONGER LAND SEA PRESSURE GRADIENT
WARMER LANDMASS
LOWER ALBEDO
Schematic showing the SW Monsoon response of the Arabian Sea to snow cover over the Himalayan-Tibetan
Plateau
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Warming of SW Eurasia mirrors the global-land signal, but recent warming anomalies are >50% larger than global temperature trends.
SW Eurasian-Land Warming
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-8
-4
0
4
8
1967 1971 1975 1979 1983 1987 1991 1995 1999 2003
Sn
ow
Co
ver
Ext
ent
(%)
-8
-4
0
4
8
YEAR
Southwest Asia
Himalayan-Tibetan Plateau
Trend line showing anomalies (departures from monthly means) of snow cover extent over Southwest Asia and
Himalayas-Tibetan Plateau between 1967 and 2003.
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70 years of global warming?: Photograph of the Pindari glacier in the Himalayas taken on October 7, 1936, by then Deputy Conservator of Forests F W Champion. 70 years later at the exact spot, his grandson James Champion photographed the same glacier. (Source Sunday Indian Express, 29th Dec. 2006).
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Interannual changes in chlorophyll along coast of Somalia since 1997
(Goes et al., Science, 2005 )
0
0.4
0.8
1.2
1.6
2
1997 1998 1999 2000 2001 2002 2003 2004
Year
Chlor
ophy
ll (mg
m-3
)
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SeaWiFS derived chlorophyll fields during the peak southwest monsoon growth season of 1997 and 2006
Sept. 1997
India
Oman
Sept. 2006
India
Oman
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The Arabian Sea’s permanent oxygen minimum zone
0.1 0.5 1.0 2.0 5.0 10.0 20.0
OMZ
OMAN
SOMALIA
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FISH MORTALITY OMAN – NOV 2005FISH MORTALITY OMAN – NOV 2005
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SEA
LESS SNOW
WARMER AND HUMID WINDS
WARMER LANDMASS
WEAKER CONVECTIVE MIXING
LESS PHYTO
STRONGER CONVECTIVE MIXING
MORE PHYTO
COLDER LANDMASS
SEA
MORE SNOW
COLDER AND DRIER WINDS (E>P)_
NORTHEAST MONSOON
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Air-temperature and Relative humidity for the northern Arabian Sea (60°E-70°E, 14°N-25°N).
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Annual trends of net heat flux (NCEP-NCAR) (60-70°E, 14°N-25°N) and Mixed Layer Depth (XBT, JEDAC, USA)
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Observed and model-derived MLD for winter (Jan – Feb), and model derived Sea Surface Salinity (SSS, psu) during Jan – May for the 60°E-70°E, 14°N-25°N. Model derived fields are obtained from the ECCO-JPL Kalman Filter Assimilation project.
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Winter mean SeaWiFS Chl a averaged over the Eastern Arabian Sea (EAS, 66°E-70°E, 15°N-24°N) and in the western Arabian Sea (WAS, 55°E-62°E, 17.5°N-22.5°N).
EAS
WAS
0.5
0.7
0.9
1.1
1.3
1.5
1996 1998 2000 2002 2004 2006
Year
Chl
orop
hyll
a (m
g m
-3)
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High chlorophyll concentrations during the NEM are being caused by blooms of dinoflagellate Noctiluca miliaris
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Its appearance in bloom proportions during the NEM is unprecedented as no reports of blooms of this organism during Int. Arabian Sea JGOFS 1992 to 1996 or from Int. Indian Ocean Expeditions of the 1960’s.
It occurs in (cold) <22oC, nutrient rich and oxygen poor waters
Noctiluca is a heterotrophic dinoflagellate containing a green endosymbiont “Pedinomonas noctilucae”
Noctiluca appears to have replaced diatoms as the major bloom forming phytoplankton of the NEM.
CHARACTERISTICS OF ARABIAN SEA NOCTILUCA MILIARIS BLOOMS
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PHYTOPLANKTON BLOOM OF 2003
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Weekly SeaWiFS and MODIS/Aqua Level-3 merged Chl a images with Sea Surface Height anomalies and geostrophic velocity
vectors from TOPEX/POSEIDON and ERS-2
Gomes et al. (2008) Deep-Sea Research
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20th Feb 2008
OMAN
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Precipitable water from SSM/I for June showing particularly strong postive and pervasive trends in the Arabian Sea
(John Fasullo NCAR)
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Is the appearance of N. miliaris blooms the result of climate change or natural variability?
What are the long-term impact of this possible change in phytoplankton biodiversity and biological productivity on:
OUTSTANDING QUESTIONS FOR THE ARABIAN SEA
•Carbon delivery to deeper layers of the Arabian Sea
•Bacterial processes
•Denitrification rates
•The Oxygen Minimum Zone and
•Increased storm activity
•Coastal Fisheries
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• 1/8-degree NCOM (Navy Coastal Ocean Model)
• 30S to 30N, 30.5 to 121.5E
• Mercator grid (~13km), 40 Levels σ/z
• Boundary and initial conditions from Global NCOM
• 0.5-degree NOGAPS Atmospheric forcing
• MODAS: Full 3D Temperature and Salinity relaxation
• Initial simulation for 2007
INDIAN OCEAN CIRCULATION INDIAN OCEAN CIRCULATION MODELMODEL
((John Kindle & Sergio deRadaJohn Kindle & Sergio deRada))
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PhysicalModel
Nitrate[NO3]
Advection& Mixing
SmallPhytoplankton
[P1]NO3
Uptake
Micro-Zooplankton
[Z1]
Grazing
Ammonium[NH4]
Excretion
NH4
Uptake
Detritus-N[DN]
FecalPellet
Sinking Silicate[Si(OH)4]
Diatoms[P2]
Si-Uptake
N-UptakeMeso-zooplankton
[Z2]
Sinking
Detritus-Si[DSi]
GrazingFecalPellet
Sinking
Predation
Lost
Total CO2
[TCO2]
BiologicalUptake
Air-Sea Exchange
Dissolution
Carbon, Silicate, Nitrogen Ecosystem Model (CoSiNE) Chai et al. 2002; Dugdale et al. 2002
Chai et al., 1996; 2003
Iron
Iron
Iron
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SEAWIFSSEAWIFS MODELMODEL
3030thth Sept 2006 Sept 2006 3030thth Sept 2006 Sept 2006
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“Nothing in the sea falls haphazard; if we cannot predict, it is because we do not know the cause, or how the cause works..."
Henry Bryant Bigelow
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ACKNOWLEDGEMENTS
This work is being funded by NASA Oceans and Ice & NASA Biodiversity and Ecosystem Programs. We are thankful to the National Institute of Oceanography
and the Indian Space Research Organization for supporting ship
observations. Special thanks to Woody Turner and Paula Bontempi for their
support