Regime-based analysis of aerosol-cloud interactions

Previous global satellite studies into the indirect aerosol effect have relied on determining the sensitivity of derived Cloud Droplet Number Concentration (Nd) to co-located Aerosol Optical Depth (AOD). These studies generally find a positive Nd sensitivity to AOD changes over ocean, but some find...

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Main Authors: Gryspeerdt, E, Stier, P
Format: Journal article
Language:English
Published: American Geophysical Union 2012
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author Gryspeerdt, E
Stier, P
author_facet Gryspeerdt, E
Stier, P
author_sort Gryspeerdt, E
collection OXFORD
description Previous global satellite studies into the indirect aerosol effect have relied on determining the sensitivity of derived Cloud Droplet Number Concentration (Nd) to co-located Aerosol Optical Depth (AOD). These studies generally find a positive Nd sensitivity to AOD changes over ocean, but some find a negative sensitivity over land, in contrast to that predicted by models and theory. Here we investigate the Nd sensitivity to AOD in different cloud regimes, determined using a k-means clustering process on retrieved cloud properties. We find the strongest positive Nd sensitivity in the stratiform regimes over both land and ocean, providing the majority of the total sensitivity. The negative sensitivity previously observed over land is generated by the low cloud fraction regimes, suggesting that it is due to the difficulty of retrieving Nd at low cloud fractions. When considering a mean sensitivity, weighted by liquid cloud fraction to account for sampling biases, we find an increased sensitivity over land, in some regions becoming positive. This highlights the importance of regime based analysis when studying aerosol indirect effects.
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spelling oxford-uuid:c0e0a56f-bbf8-4370-a758-f09f7db8c8d42022-03-27T05:57:33ZRegime-based analysis of aerosol-cloud interactionsJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:c0e0a56f-bbf8-4370-a758-f09f7db8c8d4EnglishSymplectic Elements at OxfordAmerican Geophysical Union2012Gryspeerdt, EStier, PPrevious global satellite studies into the indirect aerosol effect have relied on determining the sensitivity of derived Cloud Droplet Number Concentration (Nd) to co-located Aerosol Optical Depth (AOD). These studies generally find a positive Nd sensitivity to AOD changes over ocean, but some find a negative sensitivity over land, in contrast to that predicted by models and theory. Here we investigate the Nd sensitivity to AOD in different cloud regimes, determined using a k-means clustering process on retrieved cloud properties. We find the strongest positive Nd sensitivity in the stratiform regimes over both land and ocean, providing the majority of the total sensitivity. The negative sensitivity previously observed over land is generated by the low cloud fraction regimes, suggesting that it is due to the difficulty of retrieving Nd at low cloud fractions. When considering a mean sensitivity, weighted by liquid cloud fraction to account for sampling biases, we find an increased sensitivity over land, in some regions becoming positive. This highlights the importance of regime based analysis when studying aerosol indirect effects.
spellingShingle Gryspeerdt, E
Stier, P
Regime-based analysis of aerosol-cloud interactions
title Regime-based analysis of aerosol-cloud interactions
title_full Regime-based analysis of aerosol-cloud interactions
title_fullStr Regime-based analysis of aerosol-cloud interactions
title_full_unstemmed Regime-based analysis of aerosol-cloud interactions
title_short Regime-based analysis of aerosol-cloud interactions
title_sort regime based analysis of aerosol cloud interactions
work_keys_str_mv AT gryspeerdte regimebasedanalysisofaerosolcloudinteractions
AT stierp regimebasedanalysisofaerosolcloudinteractions