Variability of the extent of the Hadley circulation in the southern hemisphere: a regional perspective

被引:54
|
作者
Nguyen, H. [1 ]
Hendon, H. H. [1 ]
Lim, E. -P. [1 ]
Boschat, G. [3 ,4 ]
Maloney, E. [2 ]
Timbal, B. [1 ]
机构
[1] Bur Meteorol, Melbourne, Vic, Australia
[2] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[3] Univ Melbourne, ARC Ctr Excellence Climate Syst Sci, Melbourne, Vic, Australia
[4] Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia
基金
澳大利亚研究理事会; 美国国家科学基金会;
关键词
ANNULAR MODE; EL-NINO; ATMOSPHERIC CIRCULATION; CLIMATE; OSCILLATION; CONNECTION; REANALYSES; EXPANSION; PACIFIC; TROPICS;
D O I
10.1007/s00382-017-3592-2
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In order to understand the regional impacts of variations in the extent of the Hadley circulation in the Southern Hemisphere, regional Hadley circulations are defined in three sectors centered on the main tropical heat sources over Africa, Asia-Pacific (Maritime Continent) and the Americas. These regional circulations are defined by computing a streamfunction from the divergent component of the meridional wind. A major finding from this study is that year-to-year variability in the extent of the hemispheric Hadley circulation in the Southern Hemisphere is primarily governed by variations of the extent of the Hadley circulation in the Asia-Pacific sector, especially during austral spring and summer when there is little co-variability with the African sector, and the American sector exhibits an out of phase behavior. An expanded Hadley circulation in the Southern Hemisphere (both hemispherically and in the Asia-Pacific sector) is associated with La Nina conditions and a poleward expansion of the tropical wet zone in the Asia-Pacific sector. While La Nina also promotes expansion in the American and African sectors during austral winter, these tropical conditions tend to promote contraction in the two sectors during austral summer as a result of compensating convergence over the Americas and Africa sectors: a process driven by variations in the Walker circulation and Rossby wave trains emanating from the tropical Indian Ocean.
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页码:129 / 142
页数:14
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