globalchange  > 影响、适应和脆弱性
DOI: 10.1007/s00382-017-3953-x
Scopus记录号: 2-s2.0-85031128403
论文题名:
Origin of Indian summer monsoon rainfall biases in CMIP5 multimodel ensemble
作者: Wang Z.; Li G.; Yang S.
刊名: Climate Dynamics
ISSN: 9307575
出版年: 2018
卷: 51, 期:2018-01-02
起始页码: 755
结束页码: 768
语种: 英语
英文关键词: CMIP5 ; Indian summer monsoon ; Modeling biases ; Northern Indian Ocean ; Rainfall ; Sea surface temperature
Scopus关键词: atmospheric modeling ; climate prediction ; CMIP ; ensemble forecasting ; monsoon ; rainfall ; sea surface temperature ; summer ; Indian Ocean ; Indian Ocean (North)
英文摘要: Significant biases of coupled general circulation models (CGCMs) lead to considerable uncertainty in climate predictions and projections. Based on the historical simulations in the phase 5 of the Coupled Model Intercomparison Project (CMIP5), we identify that state-of-the-art CGCMs commonly simulate insufficient Indian summer monsoon (ISM) rainfall along with too weak monsoon circulations. Such ISM rainfall/circulation biases, however, are absent in the Atmospheric Model Intercomparison Project simulations forced by observed sea surface temperature (SST), suggesting that the common ISM biases are not intrinsic errors of the atmospheric models but arise from the interaction between the monsoon and the oceans. A multimodel statistical analysis further shows that the ISM rainfall/circulation biases in CMIP5 models can be traced back to the excessively cold SST over the northern Indian Ocean (NIO). The systemic cold SST biases in the NIO suppress local convective activity and reduce air temperature, resulting in a weak north–south thermal contrast in the mid-upper troposphere. This would induce an excessively weak ISM circulation and resultant insufficient monsoon rainfall. Furthermore, the dynamic effect of cold NIO SST biases on the ISM rainfall/circulation simulations is also confirmed through several sensitivity experiments by using the widely-applied Weather Research and Forecasting model. To the extent that the cold SST biases over the NIO may originate from an excessively strong Indian winter monsoon, improving the winter monsoon simulation is an important prerequisite for better summer climate simulations and predictions/projections over the broad ISM region. © 2017, Springer-Verlag GmbH Germany.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109207
Appears in Collections:影响、适应和脆弱性
气候变化事实与影响

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作者单位: School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China; Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou, China; College of Oceanography, Hohai University, Nanjing, China

Recommended Citation:
Wang Z.,Li G.,Yang S.. Origin of Indian summer monsoon rainfall biases in CMIP5 multimodel ensemble[J]. Climate Dynamics,2018-01-01,51(2018-01-02)
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