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Time-series observations in the Northern Indian Ocean
V.V.S.S. SarmaNational Institute of Oceanography
Visakhapatnam, India
The Second GEOSS Asia-Pacific Symposium, Tokyo, 14-16th April 2008
Seasonal variations in winds, currents and ITCZ in NIO
Importance of N. Indian Ocean
5.2-13.3 5.6-7.3
0.4-6.5
0.81-6.3
0.07-5.5
0.7-5.2
0.6-3.4
0.6-3.4
8.1-10.5
Primary production Sea-to-air flux of CO2
Oxygen at 500 m deepSinking organic carbon
mmol C/m2/d micromol/kg
NCP and sea-to-air fluxes of CO2
Region Sea-to-air flux (F) New/NCP(NP) F/NP Ratio
Eq.Pacific (HNLC) 0.80 to 1.00 0.65 to 0.98 1.0-1.2(1980-2000) (Feely et al., 2002) (LeBorgne et al., 2002)
Arabian Sea 0.07 to 0.09 0.17 to 0.20 0.4-0.45 (1995) (Sarma., 2003) (Sarma, 2004)
Bay of Bengal 0.0025 to 0.005 0.059-0.077 0.19-0.22 (Takahashi et al., 2002) (Sarma, 2006)
(PgC y-1)
Deep water DIC in the World Oceans
Sarma et al. 2007
(µmol kg-1)Source: WOCE data on sigma-3: 41.488 (~3000m)
-1.4
-1.2
-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
PgC
y-1
Antarctic
S Indian
S Pacific
S Atlantic
N Indian
Eq Indian
Eq Pacific
Eq Atlantic
N.Cen Pacific
N.Cen Atlantic
N Pacific
N Atlantic
0
0.2
0.4
0.6
0.8
degr
ee C
Antarctic
S Indian
S Pacific
S Atlantic
N Indian Eq
Indian
Eq Pacific
Eq Atlantic
N.Cen Pacific
N.Cen Atlantic
N Pacific
N Atlantic
-80
-60
-40
-20
0
20
40
60
80
Perc
ent c
hang
e
Antarctic S Indian
S Pacific
S Atlantic
N Indian
Eq Indian
Eq Pacific
Eq Atlantic
N.Cen Pacific
N.Cen Atlantic
N Pacific
N Atlantic
-10
0
10
20
Per
cent
cha
nge
Antarctic
S Indian
S Pacific
S Atlantic
N Indian
Eq Indian
Eq Pacific
Eq Atlantic
N.Cen Pacific
N.Cen Atlantic
N Pacific N
Atlantic
Primary Production SST
Fe deposition Scalar wind stress
Change in conditions from SeaWiFS to CZCS era
Gregg et al., 2002
Physical forcing..upwelling in the Arabian Sea
Nutrients + Mineral ballast
Bottom flow
Lateral Input
Scavenging
Biological production + Particle aggregation
Fresh water
Particle ballast in the Bay of Bengal
Phytoplankton Blooms in the Bay of Bengal
Vinayachandran et al 2003
Tracks of cyclones and depressions in the Bay of Bengal
1997 1998 1999
2000 2001 2002
2003
2006
2004 2005
2007
Source : http://www.weather.unisys.com
Time-series observations in the northwestern Indian Ocean
•Impact of anthropogenic perturbations on oceanographic –atmospheric processes in and around India in the context of Global Change (CSIR Network Project No. CMM 009)Since 2002
Ongoing time-series projects in thewest coast of India (eastern Arabian Sea)
Sampling at Monthly Scale
0 60 120 180 240 300 36030
20
10
0
(a) Temp (ºC)
0 60 120 180 240 300 36030
20
10
0
(c) Oxygen (µM)
0 60 120 180 240 300 36030
20
10
0
(d) Nitrate (µM)
Days
0 60 120 180 240 300 36030
20
10
0
(b) Salinity
Evolution .. anoxia & H2S..
0 60 120 180 240 300 36030
20
10
0
(i) Chlorophyll amg m-3
Evolution .. anoxia & H2S..
Days
Dep
th (m
)
0 60 120 180 240 300 36030
20
10
0(e) Nitrite (µM)
0 60 120 180 240 300 36030
20
10
0
(f) Nitrous Oxide (nM)
0 60 120 180 240 300 36030
20
10
0(g) Ammonia (µM)
Days0 60 120 180 240 300 360
30
20
10
0
14
Evolution anoxia & H2S..
(h) Hydrogen sulphide(µM)
Time-series observations in the northeastern Indian Ocean
Visakhapatnam BOBFLUXSOLAS
•Biogeochemical Response of coastal waters off VisakhapatnamTo extreme climatic events and human interference – SurfaceOcean Lower Atmosphere Study (SOLAS) since 2006
•Bay of Bengal Carbon Flux Study (BOBFLUX) – Council of Scientific and Industrial Research (CSIR) Since 2008
•Variability of Ecosystem and Biogeochemistry in Godavari Estuarine System (VEBGES) – Supra Institutional Project (SIP)Of Council of Scientific and Industrial Research (CSIR) since2007.
•Coastal Ocean Monitoring and Prediction system (COMPAS)-Ministry of Earth Science since 2008
Ongoing time-series projects in theeast coast of India (western Bay of Bengal)
Sampling at Monthly Scale
Sampling at diurnal to seasonal Scale
Sampling at daily Scale
Sampling at seasonal Scale
Impact of rainfall on biogeochemical processes
Distance (km)
14-21 Sep 2007 22-29 Sep 2007 30-07 Oct 2007
08-15 Oct 2007 16-23 Oct 2007 23-31 Oct 2007
Impact of Rainfall on Chlorophyll distribution in the coastal Bay of Bengal
Source: Weekly average chlorophyll-a by SeaWiFS from NASA
9 Nov 07 11 Nov 07 14 Nov 07 16 Nov 07 23 Nov 07 26 Nov 07
8 Nov 07 10 Nov 07 14 Nov 07 15 Nov 07 16 Nov 07 18 Nov 07
Influence of episodic atmospheric events on SST & chl-a
NE NE NENWNWNW
SST
Chl
-aW
inds
Net community Production (mmol O2/m2/d)
Phytoplankton production versus Bacterial Biomass
Station Oct 2007 Nov 2007 Dec 2007 Jan 2008 Feb 2008
V1 147.2 137.8 699.7 260.30 297.9
V2 246.2 27.3 659.3 142.50 356.9
V4 61.8 40.9 2.5 0.60 -93.8
V6 97.7 75.8 -42.9 -78.8 -134.8
Distance (km)
October 2007
November 2007
December 2007
January 2008
February 2008
Janu
ary
2008
Dec
embe
r 200
7N
ovem
ber 2
007
Oct
ober
200
7Fe
brua
ry 2
008Chlorophyll-a Dissolved O2 Nitrate Silicate
Formation of sub-oxic conditions in the Shelf waters
Distance (km)
Variability of Ecosystem and Biogeochemistry in Godavari Estuarine System (VEBGES)
252 277 302 327 352 12 37
0
200000
400000
600000
252 277 302 327 352 12 37
0
200000
400000
600000
Time-series variations in Godavari EstuaryRiver discharge (Cusecs/sec)
Suspended matter (g/L)
Salinity
Nutrients (µmol/kg)
Silicate (µmol/kg)
Julien Days (Sep 07-Feb 08)
252 277 302 327 352 12 37
0
200000
400000
600000
252 277 302 327 352 12 37
0
200000
400000
600000
Julien Days (Sep 07-Feb 08)
River discharge (Cusecs/sec)
Bulk chlorophyll
>10 µm chlorophyll >0.2 & <2 µm chlorophyll
>2 & <10 µm chlorophyll
Time-series variations in Godavari Estuary
Rates of changes in salinity and nutrients in Godavari Estuary
Parameter Rate of change per day
Salinity +0.2 psu
Dissolved O2 +0.2 µmol/kg
Nitrate -0.1 µmol/kg
Phosphate -0.01 µmol/kg
Silicate -0.4 µmol/kg
-400
-200
0
200
400
600
800
mm
ol O
2 m-2 d
-1
0
200
400
600
mm
ol O
2 m-2 d
-1
240 280 320 360 400 440-400
0
400
800
1200
1600m
mol
O2 m
-2 d
-1
Net Comm. Prod.
Dark Comm. Resp.
Gross Pri. Prod.
Time-series variationsin plankton metabolicrates in Godavariestuary
35 75Julien day
Heterotrophy Autotrophy
2 fold increase in Production
~65% of the GPP is respired
Future plans:both coastal & estuary time-series stations
Time-series measurements of triple oxygen isotopes and O2/Ar ratios in the surface ocean
Time-series measurements of inorganic carbon parameters
Measurements of δ13C, δ15N of dissolved and particulate (both organic & Inorganic)
Processing HPLC and DOC samples and isotopic ratios of δ13C of DOC
Phytoplankton growth and grazing rates (once in a week!!)
Nutrients utilization rates (once in a week!!)
Bacterial respiration rates (Unisense sensor)
Consumption and exchanges rates of carbon at the Benthic boundary
Water exchange rates using Radon isotopes.
Bay of Bengal Carbon Flux Study (BOBFLUX)
Visakhapatnam BOBFLUX
Objectives of Bay of Bengal Carbon Flux Study (BOBFLUX)
1. What is the short-term to inter-annual variability in plankton metabolic rates suchas gross and net community production, and community respiration?
2. How river inputs influence the plankton metabolic rates?
3.What is the influence of cyclones on nutrient injections, primary production andair-sea exchange of trace gases?
4. What is the seasonal to inter-annual variability in export production?
5. What is the relationship between primary and export production?
6. What is the influence of river runoff on bacterial growth rates and respiration?
7. What are the seasonal variations in transfer velocities of trace gases?
8. What are the temporal and spatial variations in the air-sea exchange of tracegases?
Meteorological Buoy
Remote Access Sampler (30 m)
Sediment trap (150 m) – Weekly sampling
Optode/current meter (500 m)
ADCP (1800 m)
Sediment trap (1700 m) – Weekly sampling
Bottom (2000 m)
Optode/current meter (20 m)
Schematic of mooring in the Bay of Bengal
Floating sedimentTraps – samplingOnce in 3 months
VisakhapatnamBOBFLUX
BOBFLUX
Time-series transect observations
0.25o water column sampling for biogeo-chemical parameters – nutrients, chl-a,HPLC, DIC, TA, pH, DOC, SSM, O2isotopes, O2/Ar, Plankton composition etc. Underway pCO2 system, SST,SSS, Chl-a,& dissolved O2Underway plankton metabolic rates bytriple oxygen isotopes & O2/Ar Isotopic ratios of δ13C-DIC, DOC ofdissolved δ13C & δ15N of particulate matter
Sampling : Bi-monthlyStarts from September 2008
Thank You