A predictable prospect of the South Asian summer monsoon

被引:18
|
作者
Zhang, Tuantuan [1 ,2 ]
Jiang, Xingwen [3 ]
Yang, Song [1 ,2 ]
Chen, Junwen [4 ]
Li, Zhenning [5 ]
机构
[1] Sun Yat Sen Univ, Sch Atmospher Sci, Southern Lab Ocean Sci & Engn Zhuhai, Zhuhai 519082, Guangdong, Peoples R China
[2] Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Zhuhai 519082, Guangdong, Peoples R China
[3] China Meteorol Adm, Inst Plateau Meteorol, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610072, Sichuan, Peoples R China
[4] Shenzhen Wiselec Technol Co Ltd, Shenzhen 518048, Guangdong, Peoples R China
[5] Hong Kong Univ Sci & Technol, Div Environm & Sustainabil, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
INTERANNUAL VARIABILITY; INDIAN MONSOON; REGRESSION SHRINKAGE; RAINFALL; ENSO; TELECONNECTION; SELECTION; CLIMATE; PATTERN; INDEX;
D O I
10.1038/s41467-022-34881-7
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Prediction of the South Asian summer monsoon (SASM) has remained a challenge for both scientific research and operational climate prediction for decades. By identifying two dominant modes of the SASM, here we show that the unsatisfactory prediction may be due to the fact that the existing SASM indices are mostly related to the less predictable second mode. The first mode, in fact, is highly predictable. It is physically linked to the variation of the Indian monsoon trough coupled with large rainfall anomalies over core monsoon zone and the northern Bay of Bengal. An index is constructed as a physical proxy of this first mode, which can be well predicted one season in advance, with an overall skill of 0.698 for 1979-2020. This result suggests a predictable prospect of the SASM, and we recommend the new index for real-time monitoring and prediction of the SASM. The authors identify a predictable component of the South Asian summer monsoon that is associated with the variability of the monsoon trough modulated by tropical sea surface temperatures.
引用
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页数:10
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