globalchange  > 气候减缓与适应
DOI: 10.1029/2017JD027939
Scopus记录号: 2-s2.0-85047480547
论文题名:
The Rainfall Responses of Typhoon Soudelor (2015) to Radiative Processes of Cloud Species
作者: Wang B.; Xu H.; Zhai G.; Li X.
刊名: Journal of Geophysical Research: Atmospheres
ISSN: 2169897X
出版年: 2018
卷: 123, 期:8
起始页码: 4284
结束页码: 4293
语种: 英语
英文关键词: cloud species ; net condensation ; radiative cooling ; radiative effects
Scopus关键词: cloud ; cloud water ; condensation ; cooling ; heat flux ; ice ; radiative transfer ; raindrop ; rainfall ; snow ; stratosphere-troposphere interaction ; typhoon
英文摘要: In this study, the three-dimensional Weather Research and Forecasting model is used to conduct sensitivity experiments of Typhoon Soudelor in 2015 to examine rainfall responses to radiative effects of cloud species. Time and model domain mean analysis shows that the radiative effects of cloud ice and snow on rainfall are significantly stronger than those of cloud water and raindrops. The peak of snow appears in the upper troposphere (9 km). The inclusion of radiative effects of snow enhances radiative cooling in the upper troposphere and suppresses radiative cooling in midtroposphere and lower troposphere. The enhanced radiative cooling in the upper troposphere and the suppressed in midmidtroposphere and lower troposphere reduce stability in the troposphere and thus enhance vertical mass divergence and associated divergence of heat flux. The increases in net condensation and rainfall correspond to the increase in release of latent heat associated with the enhancement in divergence of heat flux. The maximum of cloud ice occurs around the tropopause (11 km). The inclusion of radiative effects of cloud ice weakens radiative cooling in the upper troposphere, while it enhances radiative cooling in the lower stratosphere. The weakened radiative cooling in the upper troposphere increases stability in the troposphere and thus reduces vertical mass divergence and associated divergence of heat flux. The reductions in net condensation and rainfall correspond to the decrease in release of latent heat associated with the suppression in divergence of heat flux. ©2018. American Geophysical Union. All Rights Reserved.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/114053
Appears in Collections:气候减缓与适应

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作者单位: Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, China

Recommended Citation:
Wang B.,Xu H.,Zhai G.,et al. The Rainfall Responses of Typhoon Soudelor (2015) to Radiative Processes of Cloud Species[J]. Journal of Geophysical Research: Atmospheres,2018-01-01,123(8)
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