Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM

Aerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud condensation and ice nuclei and may have an influence on the hydrological cycle. Here we investigate aerosol effects on convective clouds by extending the double-moment cloud microphysics scheme deve...

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Main Author: U. Lohmann
Format: Article
Language:English
Published: Copernicus Publications 2008-04-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/2115/2008/acp-8-2115-2008.pdf
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spelling doaj-914209662133402ba17aa0ad7e4e1dc12020-11-25T00:37:43ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-04-018721152131Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAMU. LohmannAerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud condensation and ice nuclei and may have an influence on the hydrological cycle. Here we investigate aerosol effects on convective clouds by extending the double-moment cloud microphysics scheme developed for stratiform clouds, which is coupled to the HAM double-moment aerosol scheme, to convective clouds in the ECHAM5 general circulation model. This enables us to investigate whether more, and smaller cloud droplets suppress the warm rain formation in the lower parts of convective clouds and thus release more latent heat upon freezing, which would then result in more vigorous convection and more precipitation. In ECHAM5, including aerosol effects in large-scale and convective clouds (simulation ECHAM5-conv) reduces the sensitivity of the liquid water path increase with increasing aerosol optical depth in better agreement with observations and large-eddy simulation studies. In simulation ECHAM5-conv with increases in greenhouse gas and aerosol emissions since pre-industrial times, the geographical distribution of the changes in precipitation better matches the observed increase in precipitation than neglecting microphysics in convective clouds. In this simulation the convective precipitation increases the most suggesting that the convection has indeed become more vigorous. http://www.atmos-chem-phys.net/8/2115/2008/acp-8-2115-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author U. Lohmann
spellingShingle U. Lohmann
Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
Atmospheric Chemistry and Physics
author_facet U. Lohmann
author_sort U. Lohmann
title Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
title_short Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
title_full Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
title_fullStr Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
title_full_unstemmed Global anthropogenic aerosol effects on convective clouds in ECHAM5-HAM
title_sort global anthropogenic aerosol effects on convective clouds in echam5-ham
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2008-04-01
description Aerosols affect the climate system by changing cloud characteristics in many ways. They act as cloud condensation and ice nuclei and may have an influence on the hydrological cycle. Here we investigate aerosol effects on convective clouds by extending the double-moment cloud microphysics scheme developed for stratiform clouds, which is coupled to the HAM double-moment aerosol scheme, to convective clouds in the ECHAM5 general circulation model. This enables us to investigate whether more, and smaller cloud droplets suppress the warm rain formation in the lower parts of convective clouds and thus release more latent heat upon freezing, which would then result in more vigorous convection and more precipitation. In ECHAM5, including aerosol effects in large-scale and convective clouds (simulation ECHAM5-conv) reduces the sensitivity of the liquid water path increase with increasing aerosol optical depth in better agreement with observations and large-eddy simulation studies. In simulation ECHAM5-conv with increases in greenhouse gas and aerosol emissions since pre-industrial times, the geographical distribution of the changes in precipitation better matches the observed increase in precipitation than neglecting microphysics in convective clouds. In this simulation the convective precipitation increases the most suggesting that the convection has indeed become more vigorous.
url http://www.atmos-chem-phys.net/8/2115/2008/acp-8-2115-2008.pdf
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