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On the Relationship Between Responses in Cloud Water and Precipitation to Changes in Aerosol : Volume 14, Issue 21 (11/11/2014)

By Lebo, Z. J.

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Book Id: WPLBN0003993489
Format Type: PDF Article :
File Size: Pages 15
Reproduction Date: 2015

Title: On the Relationship Between Responses in Cloud Water and Precipitation to Changes in Aerosol : Volume 14, Issue 21 (11/11/2014)  
Author: Lebo, Z. J.
Volume: Vol. 14, Issue 21
Language: English
Subject: Science, Atmospheric, Chemistry
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Publication Date:
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications


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Feingold, G., & Lebo, Z. J. (2014). On the Relationship Between Responses in Cloud Water and Precipitation to Changes in Aerosol : Volume 14, Issue 21 (11/11/2014). Retrieved from

Description: Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado, USA. Climate models continue to exhibit strong sensitivity to the representation of aerosol effects on cloud reflectance and cloud amount. This paper evaluates a proposed method to constrain modeled cloud liquid water path (LWP) adjustments in response to changes in aerosol concentration Na using observations of precipitation susceptibility. Recent climate modeling has suggested a linear relationship between relative LWP responses to relative changes in Na, i.e., dln LWP / dln Na, and the precipitation frequency susceptibility Spop, which is defined as the relative change in the probability of precipitation for a relative change in Na. Using large-eddy simulations (LES) of marine stratocumulus and trade wind cumulus clouds, we show that these two cloud regimes exhibit qualitatively different relationships between λ and Spop; in stratocumulus clouds, λ increases with Spop, while in trade wind cumulus, λ decreases with Spop. The LES-derived relationship for marine stratocumulus is qualitatively similar but quantitatively different than that derived from climate model simulations of oceanic clouds aggregated over much larger spatial scales. We explore possible reasons for variability in these relationships, including the selected precipitation threshold and the various definitions of precipitation susceptibility that are currently in use. Because aerosol–cloud–precipitation interactions are inherently small-scale processes, we recommend that when deriving the relationship between λ and Spop, careful attention be given to the cloud regime, the scale, and the extent of aggregation of the model output or the observed data.

On the relationship between responses in cloud water and precipitation to changes in aerosol

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