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Supplementary Material to Aerosol and Ozone changes as forcing for Climate Evolution between 1850 and 2100 Climate Dynamics , Szopa et al. ; LSCE-IPSL, France sophie.szopa@lsce.ipsl.fr. Total aerosol Optical depth. RCP60 (11 year mean around 2005). AEROCOM MEDIAN.
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Supplementary Material to Aerosol and Ozone changes as forcing for Climate Evolution between 1850 and 2100 ClimateDynamics, Szopa et al. ; LSCE-IPSL, France sophie.szopa@lsce.ipsl.fr
Total aerosol Optical depth RCP60 (11 yearmeanaround 2005) AEROCOM MEDIAN Figure S1 : Comparison of the LMDz-OR-INCA total aerosolsresultswith the AEROCOM median and with the aeronet observations.
LMDz-OR-INCA AEROCOM MEDIAN Black Carbon ParticulateOrganicMatter Sulfates Seasalt Dust Figure S2 : Comparison of the LMDz-OR-INCAresultswith the AEROCOM median for annualmean (separated by aerosol components).
LMDz-OR-INCA AEROCOM MEDIAN Total aerosol Dust Seasalt Figure S3 : Comparison of the LMDz-OR-INCAresultswith the AEROCOM median for monthlymean in january and july (for total aerosol and natural components).
LMDz-OR-INCA AEROCOM MEDIAN Black Carbon ParticulateOrganicMatter Sulfates Figure S4 : Comparison of the LMDz-OR-INCAresultswith the AEROCOM median for monthlymean in january and july (for anthropogenic components).
Historical RCP8.5 RCP6.0 RCP4.5 RCP2.6 Global surface CH4 (ppb) Year Figure S5: Time evolution of globally-averaged surface methane concentration in the historicalperiod (1850-2000) and for the four RCPs (2000-2100) simulated by LMDz-OR-INCA (solidlines) and recommended for the CMIP5 climate simulations (dashedlines) LMDz-OR-INCA model CAM3.5 model (Lamarque et al. 2011) 0.14 0.12 0.10 Aerosol Optical Depth 0.08 0.06 Figure S6: Time evolution of globally-averagedaerosolopticaldepthat 550nm in the historicalperiod (1850-2000) simulated by LMDz-OR-INCA (11 yearrollingmean, orange line) and by CAM3.5 (annual values, black line). 1850 1900 1950 2000 700 hPa 35N-60N LMDz-OR-INCA model PUCCINI & CAM3.5 model mean (Cionni et al. 2011) Figure S7: Time evolution of globally-averaged ozone concentration at 700hPa in the historicalperiod (1850-2000) simulated by LMDz-OR-INCA (orange line) and derivedfrom PUCCINI and CAM3.5 (black line).
Figure S8: Time evolution of tropical stratospheric ozone in the IPSL-CM5 climatology for historicalfollowed by RCP6.0 projection