Technical Note: Estimating aerosol effects on cloud radiative forcing

Estimating anthropogenic aerosol effects on the planetary energy balance through the aerosol influence on clouds using the difference in cloud radiative forcing from simulations with and without anthropogenic emissions produces estimates that are positively biased. A more representative method is su...

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Main Author: S. J. Ghan
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/13/9971/2013/acp-13-9971-2013.pdf
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author S. J. Ghan
author_facet S. J. Ghan
author_sort S. J. Ghan
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description Estimating anthropogenic aerosol effects on the planetary energy balance through the aerosol influence on clouds using the difference in cloud radiative forcing from simulations with and without anthropogenic emissions produces estimates that are positively biased. A more representative method is suggested using the difference in cloud radiative forcing calculated as a diagnostic with aerosol scattering and absorption neglected. The method also yields an aerosol radiative forcing decomposition that includes a term quantifying the impact of changes in surface albedo. The method requires only two additional diagnostic calculations: the whole-sky and clear-sky top-of-atmosphere radiative flux with aerosol scattering and absorption neglected.
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spelling doaj.art-95470321aacc4bb5843cc8e3bbe3e8dc2022-12-21T21:14:52ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242013-10-0113199971997410.5194/acp-13-9971-2013Technical Note: Estimating aerosol effects on cloud radiative forcingS. J. GhanEstimating anthropogenic aerosol effects on the planetary energy balance through the aerosol influence on clouds using the difference in cloud radiative forcing from simulations with and without anthropogenic emissions produces estimates that are positively biased. A more representative method is suggested using the difference in cloud radiative forcing calculated as a diagnostic with aerosol scattering and absorption neglected. The method also yields an aerosol radiative forcing decomposition that includes a term quantifying the impact of changes in surface albedo. The method requires only two additional diagnostic calculations: the whole-sky and clear-sky top-of-atmosphere radiative flux with aerosol scattering and absorption neglected.http://www.atmos-chem-phys.net/13/9971/2013/acp-13-9971-2013.pdf
spellingShingle S. J. Ghan
Technical Note: Estimating aerosol effects on cloud radiative forcing
Atmospheric Chemistry and Physics
title Technical Note: Estimating aerosol effects on cloud radiative forcing
title_full Technical Note: Estimating aerosol effects on cloud radiative forcing
title_fullStr Technical Note: Estimating aerosol effects on cloud radiative forcing
title_full_unstemmed Technical Note: Estimating aerosol effects on cloud radiative forcing
title_short Technical Note: Estimating aerosol effects on cloud radiative forcing
title_sort technical note estimating aerosol effects on cloud radiative forcing
url http://www.atmos-chem-phys.net/13/9971/2013/acp-13-9971-2013.pdf
work_keys_str_mv AT sjghan technicalnoteestimatingaerosoleffectsoncloudradiativeforcing