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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 5, issue 4
Atmos. Chem. Phys., 5, 1125-1156, 2005
https://doi.org/10.5194/acp-5-1125-2005
© Author(s) 2005. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Atmos. Chem. Phys., 5, 1125-1156, 2005
https://doi.org/10.5194/acp-5-1125-2005
© Author(s) 2005. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  31 Mar 2005

31 Mar 2005

The aerosol-climate model ECHAM5-HAM

P. Stier1, J. Feichter1, S. Kinne1, S. Kloster1, E. Vignati2, J. Wilson2, L. Ganzeveld3, I. Tegen4, M. Werner4, Y. Balkanski5, M. Schulz5, O. Boucher6, A. Minikin7, and A. Petzold7 P. Stier et al.
  • 1Max Planck Institute for Meteorology, Hamburg, Germany
  • 2Institute for the Environment and Sustainability, European Commission Joint Research Centre, Ispra, Italy
  • 3Max Planck Institute for Chemistry, Mainz, Germany
  • 4Max Planck Institute for Biogeochemistry, Jena, Germany
  • 5Laboratoire des Sciences du Climat et de l’Environnement, Gif-sur-Yvette, France
  • 6CNRS, USTL, Villeneuve d’Ascq, France
  • 7German Aerospace Agency DLR, Oberpfaffenhofen, Germany

Abstract. The aerosol-climate modelling system ECHAM5-HAM is introduced. It is based on a flexible microphysical approach and, as the number of externally imposed parameters is minimised, allows the application in a wide range of climate regimes. ECHAM5-HAM predicts the evolution of an ensemble of microphysically interacting internally- and externally-mixed aerosol populations as well as their size-distribution and composition. The size-distribution is represented by a superposition of log-normal modes. In the current setup, the major global aerosol compounds sulfate (SU), black carbon (BC), particulate organic matter (POM), sea salt (SS), and mineral dust (DU) are included. The simulated global annual mean aerosol burdens (lifetimes) for the year 2000 are for SU: 0.80 Tg(S) (3.9 days), for BC: 0.11 Tg (5.4 days), for POM: 0.99 Tg (5.4 days), for SS: 10.5 Tg (0.8 days), and for DU: 8.28 Tg (4.6 days). An extensive evaluation with in-situ and remote sensing measurements underscores that the model results are generally in good agreement with observations of the global aerosol system. The simulated global annual mean aerosol optical depth (AOD) is with 0.14 in excellent agreement with an estimate derived from AERONET measurements (0.14) and a composite derived from MODIS-MISR satellite retrievals (0.16). Regionally, the deviations are not negligible. However, the main patterns of AOD attributable to anthropogenic activity are reproduced.

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