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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Forward modelling with the LMDz-INCA coupled climate-chemistry model; Inverse modelling and data assimilation; IASI/METOP instrument CH4 distribution D. Hauglustaine, P. Bousquet, F. Chevallier LSCE, Gif-sur-Yvette, France C. Clerbaux Service d’Aéronomie, Paris, France
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October LMDzINCA Model Atmospheric chemistry in the troposphere and stratosphere; Long-lived greenhouse gases (CO 2,CH 4, N 2 O, CFC); Aerosols (sulfur, carbon, natural); Data assimilation and inverse modelling (CO 2, CH 4, CO, CH 2 O, O 3, NO 2 ); Global-regional coupling LMDzINCA-CHIMERE.
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Forward modelling of nitrous oxide Hauglustaine et al., JGR, 2004.
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Forward modelling of molecular hydrogen Hauglustaine and Ehhalt, JGR, 2002.
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Forward modelling of molecular hydrogen Hauglustaine et al., JGR, 2004.
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CEA, 10 Octobre 2006 F. Chevallier/ LSCE slide 6 Bayesian inference @ LSCE To estimate sources and sinks of CO 2 and CH 4 using measurements of atmospheric concentrations Bousquet et al., Science, 2000 Peylin et al., 2002, 2005 Bousquet et al., ACP, 2005 Bousquet et al., Nature, 2006 Bayes’ theorem applied with Gaussian pdfs Linear framework Matrix formulation Use LMDZ model of atmospheric tracer transport
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Wetlands contribute the most to the methane inter-annual variability. Biomass burning contributes less except during specific events as 1997-98 (El Niño). Since 1999, compensation between rising fossil fuel emissions and decreasing wetland emissions associated to general dryness of the northern hemisphere. Explain the decrease in CH4 growth rate. Inverse modelling results in good agreement with satellite data derived emissions for biomass burning and wetlands. Bousquet et al., Nature, 2006 Methane inverse modelling (1/2)
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October Variability in global OH concentration contributes to methane inter-annual variability. Tropical methane sources contribute the most to the inter-annual variability. Northern hemisphere sources contribute the most to long-term methane variability. Bousquet et al., Nature, 2006 Methane inverse modelling (1/2)
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Hauglustaine et al. - HYMN KO Meeting - 10-11th October 19602000 Long-term simulations : oxidizing capacity - hydroxyl radical OH Consistent with top-down estimates ? Bousquet et al., ACP, 2005
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CEA, 10 Octobre 2006 F. Chevallier/ LSCE slide 10 Variational formulation @ LSCE To process many more observations and estimate many more variables Chevallier et al., 2005, 2006 Inference problem solved by minimizing a cost function TL and AD of LMDZ tracer transport manually coded for an efficient computation of the gradient of the cost function
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CEA, 10 Octobre 2006 F. Chevallier/ LSCE slide 11 LMDZ vs. ECMWF for tracer transport LMDZ 3.75 o x2.5 o 19L nudged to ECMWF winds ECMWF T159 (125km) 60L (thanks to S. Serrar and R. Engelen) 1 Nov. 2003, 0 UTC 3-month simulation CO2 conc. @ 550 hPa (ppm)
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CEA, 10 Octobre 2006 F. Chevallier/ LSCE slide 12 Application NASA’s OCO (2008) Estimated uncertainty reduction [0-1] on weekly CO 2 fluxes brought by OCO measurements 0 = no reduction1 = certainty
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CEA, 10 Octobre 2006 F. Chevallier/ LSCE slide 13 Simplified chemistry model
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CO - MOPITT Remote sensing of CH4 using the thermal infrared spectral range @ Service d’Aéronomie IMG (1996-1997) IASI (2006-2020)
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Ts CO CH 4 O3O3 Clerbaux et al., IEEE 1999; JGR 2001 Hadji-Lazaro et al., JGR 1999 IMG distributions using IASI processing tools Turquety et al. GRL 2002 Clerbaux et al., ACP 2003 Hadji-Lazaro et al., GRL 2001 SA-NN [Turquety et al, JGR 2004]
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+ GOME-2 Launch scheduled on October 17
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