Interannual impact of tropical southern Atlantic SST on surface air temperature over East Asia during boreal spring

被引:3
|
作者
Sheng, Chen [1 ]
Zhang, Shaoyu [1 ,2 ]
Liu, Yimin [1 ,2 ]
Wu, Guoxiong [1 ,2 ]
He, Bian [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geoph, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
FGOALS-F3-L MODEL DATASETS; WINTER MONSOON; EL-NINO; ARCTIC-OSCILLATION; OCEAN CAPACITOR; SEA-ICE; ENSO; SUMMER; VARIABILITY; TELECONNECTION;
D O I
10.1038/s41612-023-00515-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Using reanalysis data and simulations, this study revealed a pronounced negative interannual relationship between tropical southern Atlantic (TSA) sea surface temperature (SST) and East Asian surface air temperature (SAT) during boreal spring (March-May). Results confirm that the March-May TSA-SST anomaly can be considered an independent tropical driver unrelated to El Nino-Southern Oscillation. A possible mechanism linking TSA-SST and East Asian spring SAT involves an atmospheric wave train, energy conversion, and potential vorticity (PV)-theta dynamics. The anomalous TSA-SST induces an anomalous Walker circulation, which initiates a wave train that extracts energy from a westerly jet and propagates toward East Asia. Subject to PV-theta dynamics, the East Asian PV anomaly embedded within this wave train leads to bowed isentropes and resultant notable anomalous East Asian SAT. In particular, the bootstrapping results suggest that TSA-SST anomaly can cause an approximately sevenfold increase in the occurrence probability of extreme East Asian spring SAT.
引用
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页数:9
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