Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century

Recent simulations of deep convection with a spectral microphysics cloud model show that an increase in aerosol concentration can have a significant effect on the nature of convection with more ice precipitation and less warm rain in polluted air. The cloud lifetime and the area covered by cloud anv...

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Main Authors: M. Bister, M. Kulmala
Format: Article
Language:English
Published: Copernicus Publications 2011-05-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/4577/2011/acp-11-4577-2011.pdf
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author M. Bister
M. Kulmala
author_facet M. Bister
M. Kulmala
author_sort M. Bister
collection DOAJ
description Recent simulations of deep convection with a spectral microphysics cloud model show that an increase in aerosol concentration can have a significant effect on the nature of convection with more ice precipitation and less warm rain in polluted air. The cloud lifetime and the area covered by cloud anvils of deep convection are also larger for polluted air. Therefore, it is possible that the increase of anthropogenic aerosols in most of the 20th century has increased humidity and perhaps also cloudiness in the mid- to upper troposphere. Satellite data of upper tropospheric relative humidity in 1979–1997 and observed changes in cloudiness support this hypothesis. As changes in upper tropospheric humidity strongly affect longwave radiation, it is possible that anthropogenic aerosols have had a significant warming effect in addition to their other known effects on radiation.
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spelling doaj.art-0cc9b8717fd747c8a77bfd65e14c7d042022-12-21T19:27:13ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-05-011194577458610.5194/acp-11-4577-2011Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th centuryM. BisterM. KulmalaRecent simulations of deep convection with a spectral microphysics cloud model show that an increase in aerosol concentration can have a significant effect on the nature of convection with more ice precipitation and less warm rain in polluted air. The cloud lifetime and the area covered by cloud anvils of deep convection are also larger for polluted air. Therefore, it is possible that the increase of anthropogenic aerosols in most of the 20th century has increased humidity and perhaps also cloudiness in the mid- to upper troposphere. Satellite data of upper tropospheric relative humidity in 1979–1997 and observed changes in cloudiness support this hypothesis. As changes in upper tropospheric humidity strongly affect longwave radiation, it is possible that anthropogenic aerosols have had a significant warming effect in addition to their other known effects on radiation.http://www.atmos-chem-phys.net/11/4577/2011/acp-11-4577-2011.pdf
spellingShingle M. Bister
M. Kulmala
Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
Atmospheric Chemistry and Physics
title Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
title_full Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
title_fullStr Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
title_full_unstemmed Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
title_short Anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
title_sort anthropogenic aerosols may have increased upper tropospheric humidity in the 20th century
url http://www.atmos-chem-phys.net/11/4577/2011/acp-11-4577-2011.pdf
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AT mkulmala anthropogenicaerosolsmayhaveincreaseduppertropospherichumidityinthe20thcentury