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Impact of cloud radiative heating on East Asian summer monsoon circulation

Bibliographic Data

ID15548252
AuthorsZhun Guo (0000-0001-8102-5880, Chinese Academy of Sciences), Tianjun Zhou (0000-0002-5829-7279, Chinese Academy of Sciences, corresponding author), Minghuai Wang (0000-0002-9179-228X, South China Institute of Collaborative Innovation), Yun Qian (0000-0003-4821-1934, Pacific Northwest National Laboratory)
Year2015
Volume10
Issue7
Pages074014-074014
Publication date2015-07-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/10/7/074014
OpenAlexW2198685425
LanguageEN
References cited21

The impacts of cloud radiative heating on the East Asian Summer Monsoon (EASM) over southeastern China (105°–125°E, 20°–35°N) are addressed by using the Community Atmosphere Model version 5 (CAM5). Sensitivity experiments demonstrate that the radiative heating of clouds leads to a positive effect on the local EASM circulation over southeastern China. Without the radiative heating of clouds, the EASM circulation and precipitation would be much weaker than that in normal conditions. The longwave heating of clouds dominates the changes of EASM circulation. The positive effect of clouds on EASM circulation is explained by the thermodynamic energy equation, i.e. the different heating rate between cloud base and cloud top enhances the convective instability over southeastern China, which consequently enhances updraft. The strong updraft would further result in a southward meridional wind above the center of the updraft through Sverdrup vorticity balance

Atmospheric sciences · Climatology · Cloud computing · Cloud cover · Geography · Longwave · Meteorology · Physics · Precipitation · Radiative transfer · Atmospheric aerosols and clouds · Atmospheric chemistry and aerosols · Climate variability and models · Environmental Science · Geology

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Citation velocityhistorical
Highly citedNo

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