1 / 7

Total aerosol Optical depth

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.

kishi
Download Presentation

Total aerosol Optical depth

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. 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

  2. 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.

  3. 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).

  4. 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).

  5. 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).

  6. 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).

  7. Figure S8: Time evolution of tropical stratospheric ozone in the IPSL-CM5 climatology for historicalfollowed by RCP6.0 projection

More Related