The role of carbonaceous aerosols on short‐term variations of precipitation over North Africa

Subtropical North Africa has been subject to extensive droughts in the late 20th century, linked to changes in the sea surface temperature (SST). However, climate models forced by observed SSTs cannot reproduce the magnitude of the observed rainfall reduction. Here, we propose aerosol indirect effec...

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Bibliographic Details
Published inAtmospheric science letters Vol. 17; no. 7; pp. 407 - 414
Main Authors Yoon, Jin‐Ho, Rasch, Philip J., Wang, Hailong, Vinoj, V., Ganguly, Dilip
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.07.2016
John Wiley & Sons, Inc
Royal Meteorological Society
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Summary:Subtropical North Africa has been subject to extensive droughts in the late 20th century, linked to changes in the sea surface temperature (SST). However, climate models forced by observed SSTs cannot reproduce the magnitude of the observed rainfall reduction. Here, we propose aerosol indirect effects (AIE) as an important positive feedback mechanism. Model results are presented using two sets of sensitivity experiments designed to distinguish the role of aerosol direct/semi‐direct and indirect effects on regional precipitation. Changes in cloud properties due to the presence of carbonaceous aerosols are proposed as a key mechanism to explain the reduced rainfall over subtropical North Africa.
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USDOE
AC05-76RL01830
PNNL-SA-88624
ISSN:1530-261X
1530-261X
DOI:10.1002/asl.672