Evaluating satellite ocean color-derived export production in the Southern Ocean using atmospheric O 2 /N 2 data Cindy Nevison University of Colorado Mati Kahru, Ralph Keeling, Manfredi Manizza, B. Greg Mitchell Scripps Institution of Oceanography Matt Charette, Kanchan Maiti Woods Hole Oceanographic Institution Acknowledgements: NASA NNX08AB48G, Michael Bender, Nicolas Cassar, Ray Langenfelds, N 2 O and CFC-12 data from AGAGE, NOAA CCGG and CSIRO
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Cindy Nevison University of Colorado Mati Kahru, Ralph Keeling, Manfredi Manizza, B. Greg Mitchell
Evaluating satellite ocean color-derived export production in the Southern Ocean using atmospheric O 2 /N 2 data. Cindy Nevison University of Colorado Mati Kahru, Ralph Keeling, Manfredi Manizza, B. Greg Mitchell Scripps Institution of Oceanography Matt Charette, Kanchan Maiti - PowerPoint PPT Presentation
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Evaluating satellite ocean color-derived export production in the Southern Ocean
using atmospheric O2/N2 dataCindy Nevison
University of Colorado
Mati Kahru, Ralph Keeling, Manfredi Manizza, B. Greg MitchellScripps Institution of Oceanography
Matt Charette, Kanchan Maiti Woods Hole Oceanographic Institution
Acknowledgements:NASA NNX08AB48G, Michael Bender, Nicolas Cassar, Ray Langenfelds, N2O
and CFC-12 data from AGAGE, NOAA CCGG and CSIRO
Outline
1) Export Production from Ocean Color
2) Atmospheric O2/N2 Data
3) Decomposition of O2/N2 seasonal cycle into Component Signals (land, thermal, ventilation, production)
4) Atmospheric Transport Model Uncertainty – APO Transcom Experiment
Improved Chl-a Algorithm for Southern Ocean
B.G. Mitchell et al.
NPP estimated from Ocean ColorModified Behrenfeld and Falkowski = f(Surface T, Chl-a, PAR)
Palmer LTER data using SPGANT algorithm (Kahru and Mitchell)
Export Production = ef*NPPexport fraction (ef) = f(NPP, SST)
Southern Ocean in situ data compiled from the literature (Maiti et al.)
Export Production from Ocean Color
Atmospheric O2/N2 Monitoring Stations
SIO (R. Keeling), Princeton (M. Bender, N.
Cassar)
Global South of 50S 18 Pg C/yr 1.6 Pg C/yr (Unmodified Laws model for ef)12 Pg C/yr 1.0 Pg C/yr (Laws scaled to Schlitzer, 2002)
Atmospheric O2/N2: Decreasing Trend and Seasonal Cycles
Bender et al., 2005
per m
eg
Atmospheric Potential Oxygen: Barrow, AlaskaRemove Land Signal from O2/N2 using CO2 data
O2/N2 APO
CO X1.1 /NO APO 2
o222
What causes Seasonal Cycles in APO?How are they linked to carbon export production?
Adapted from Keeling et al., 1993Corg 1 to sediment
Base of Seasonal Thermocline
Euphotic Zone
Deep Ocean
Main Thermocline
Corg 20
Corg 2
Corg 10
Production 100Consumption 80
Atmosphere O2 Flux 15
O2 Flux 5
O2 Flux 3
O2 Flux 1
Wintertime VentilationO2 Flux 8
Thermocline VentilationO2 Flux 4
Deep Water VentilationO2 Flux 3
Consumption 10
Consumption 8
Consumption 1
O2 Flux 1
Export Production
APO Seasonal Cycle at Cape Grim, TasmaniaCompare to MATCH:NCEP transport model run with satellite-derived export flux
Compare Decomposed APO Seasonal Cycle at Cape Grim to MIT Ocean Model Results
M. Manizza
N2O Seasonal Cycles in Individual Years at Macquarie Island (CSIRO Data)
Separating Stratospheric and Oceanic N2O Signals at Macquarie Island
Decomposition of APO and N2O Seasonal Cycles at Macquarie Island
N2O APO thermal + ventilation thermal + ventilation + production
Decomposition of APO Seasonal Cycle at Palmer Station, Antarctica
30 per meg * 0.2095 * 10-6 = O2/N (moles O2/moles dry air)But what is N? Some fraction of 1.77 x 1020 total moles dry air
Atmospheric Transport Model (ATM) Uncertainty
Evaluation of oceanic O2 fluxes based on observed APO seasonal cycles or latitudinal gradient, e.g., Naegler et al. [2007]
Conclusion: These evaluations are difficult because shortcomings in ATMs and problems of data representativity cannot be distinguished from uncertainties in the O2 fluxes.
APO Transcom Experiment (Blaine, 2005)
9 atmospheric transport models forced with Garcia and Keeling [2001] monthly oceanic O2 and N2 flux anomalies. Below: APO seasonal cycles at Cape Grim, Tasmania
APO Transcom Seasonal Amplitude vs. Vertical Gradient at four Southern Hemisphere Stations
Summer Winter
Red dotted line is observed APO amplitude
APO Transcom Vertical Profiles near Cape Grim, Tasmania vs. CSIRO Aircraft Data
Summer Winter
Data courtesy of Ray Langenfelds
Conclusions1) Satellite ocean color data: uncertainties compounded in the sequence from Chl-a to NPP to Export Production.
2) Partitioning of net biological APO signal into surface production and deep ventilation: Atmospheric N 2O-based method, MIT ocean model and satellite ocean color data converge on similar answer.
3) Can now compare surface production signal in APO directly to export production from ocean color, but some major uncertainties:
1) Need for atmospheric transport model as intermediary 2) N2O cycle decomposition – thermal and stratospheric signals
Supplementary Slides
Southern Ocean CO2 Sinkand Biological Pump
Takahashi et al., 2009 CO2 Flux Export Production from Ocean Color Satellite 14º-50ºS sink = 1.05 Pg C/yr
Southern Ocean as Source and Sink of CO2
.
Note scale differenceLovenduski et al., 2007
Components of net biological signal in APO: Three Possible Views observed – thermal = net biological = production + ventilation
MIT Ocean Model Results from M. Manizza
APO at Cape Grim, TasmaniaRemove Land Signal from O2/N2 using CO2 data