Arabian Sea mini warm pool and the monsoon onset vortex

被引：2
|
作者：
Vinayachandran, P. N. [1 ]
Shankar, D.
Kurian, J.
Durand, F.
Shenoi, S. S. C.
机构：
[1] Indian Inst Sci, Ctr Atmospher & Ecean Sci, Bangalore 560012, Karnataka, India
[2] Natl Inst Oceanog, Panaji 403004, Goa, India
[3] CNRS, UMR5566, CNES IRD UPS, LEGOS, F-31400 Toulouse, France
来源：
CURRENT SCIENCE | 2007年 / 93卷 / 02期
关键词：
arabian Sea; mini warm pool; monsoon onset vortex;
D O I：
暂无
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：
Warm pools - regions with sea surface temperature (SST) in excess of 28 degrees C - in the ocean occupy a special place in tropical climate owing to their impact on tropical convection. The southeastern Arabian Sea presents SST in excess of 30 degrees C for two to three months preceding the onset of the summer (southwest) monsoon over India. Recently, several attempts have been made to understand the processes that cause such high SSTs in the region. The literature is also strewn with observations and modelling of a 'monsoon onset vortex' forming over the warm pool. This paper is a review of our current understanding of the Arabian Sea mini warm pool and its possible role in the formation of the monsoon onset vortex.
引用
收藏
页码：203 / 214
页数：12
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