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Tightening of tropical ascent and high clouds key to precipitation change in a warmer climate

Title
Tightening of tropical ascent and high clouds key to precipitation change in a warmer climate
Authors
Su H.Jiang J.H.Neelin J.D.Shen T.J.Zhai C.Yue Q.Wang Z.Huang L.Choi Y.-S.Stephens G.L.Yung Y.L.
Ewha Authors
최용상
SCOPUS Author ID
최용상scopus
Issue Date
2017
Journal Title
Nature Communications
ISSN
2041-1723JCR Link
Citation
vol. 8
Publisher
Nature Publishing Group
Indexed
SCI; SCIE; SCOPUS WOS scopus
Abstract
The change of global-mean precipitation under global warming and interannual variability is predominantly controlled by the change of atmospheric longwave radiative cooling. Here we show that tightening of the ascending branch of the Hadley Circulation coupled with a decrease in tropical high cloud fraction is key in modulating precipitation response to surface warming. The magnitude of high cloud shrinkage is a primary contributor to the intermodel spread in the changes of tropical-mean outgoing longwave radiation (OLR) and global-mean precipitation per unit surface warming (dP/dT s) for both interannual variability and global warming. Compared to observations, most Coupled Model Inter-comparison Project Phase 5 models underestimate the rates of interannual tropical-mean dOLR/dT s and global-mean dP/dT s, consistent with the muted tropical high cloud shrinkage. We find that the five models that agree with the observation-based interannual dP/dT s all predict dP/dT s under global warming higher than the ensemble mean dP/dT s from the 20 models analysed in this study. © The Author(s) 2017.
DOI
10.1038/ncomms15771
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엘텍공과대학 > 환경공학전공 > Journal papers
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