Relationships among the monsoon-like southwest Australian circulation, the Southern Annular Mode, and winter rainfall over southwest Western Australia

被引:0
作者
Juan Feng
Jianping Li
Yun Li
Jianlei Zhu
Fei Xie
机构
[1] Beijing Normal University,College of Global Change and Earth System Science
[2] Chinese Academy of Sciences,State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics
[3] Joint Center for Global Change Studies,Data Analytics
[4] CSIRO Digital Productivity FlagshipFloreat,undefined
来源
Advances in Atmospheric Sciences | 2015年 / 32卷
关键词
monsoon-like Southwest Australian Circulation; Southern Annular Mode; southwestWestern Australian winter rainfall;
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学科分类号
摘要
This study examines the relationships among the monsoon-like southwest Australian circulation (SWAC), the Southern Annular Mode (SAM), and southwest Western Australia winter rainfall (SWR), based on observed rainfall, reanalysis datasets, and the results of numerical modeling. By decomposing the SWAC into two components using a linear model, i.e. the component related to SAM (RSAM) and the component unrelated to SAM (SWACI*), we find it is the SWACI* that shows a significant influence on SWR. Similarly, it is the component of SAM associated with SWAC that exhibits an impact on SWR, whereas the component unrelated to SAM. A similar result is obtained in terms of the circulation associated with SWAC and the SAM. These facts suggest the SAM plays an indirect role in influencing SWR, and raise the possibility that SWAC acts as a bridge between the SAM and SWR, by which the SAM passes its influences onto SWR. This is due to the fact that the variations of SWAC are closely linked to the thermal contrast between land and sea across the southern Indian Ocean and southwest Australia. By contrast, the SAM does not significantly relate to this thermal structure, particularly for the component unrelated to SWAC. The variations of surface sea temperature over the southern Indian Ocean contribute to the favored rainfall circulation patterns. This finding is supported by the numerical modeling results. The strong coupling between SWAC and SWR may be instrumental for understanding the interactions between SWR and the southern Indian Ocean, and provides another perspective in examining the variations in SWR.
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页码:1063 / 1076
页数:13
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[1]  
Allan R.(1993)Circulation features associated with the winter rainfall decrease in southwestern Australia J. Climate 6 1356-1367
[2]  
Haylock M.(2000)Evidence for decadal variability in southern Australian rainfall and relationships with regional pressure and sea surface temperature Int. J. Climatol. 20 1113-1129
[3]  
Ansell T.J.(2008)Key findings from the Indian Ocean climate initiative and their impact on policy development in Australia Climatic Change 89 339-354
[4]  
Reason C.J. C.(2002)Modes of interannual variability of the Southern Hemisphere circulation simulated by the CSIRO climate model J. Climate 15 1159-1174
[5]  
Smith I.N.(2005)Multidecadal fluctuations of winter rainfall over southwest Western Australia simulated in the CSIRO Mark 3 coupled model Geophys. Res. Lett. 32 12701-4325
[6]  
Keay K.(2011)Does the Southern Annular Mode contribute to the persistence of the multidecade-long drought over southwest Western Australia Geophys. Res. Lett. 38 14712-142
[7]  
Bates B.C.(2000)Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part I: Role of the subtropical ridge J. Climate 13 4310-1969
[8]  
Hope P.(2005)The East Asian summer monsoon: A review Meteor. Atmos. Phys. 89 117-1353
[9]  
Ryan B.(2006)Interannual rainfall extremes over southwest Western Australia linked to Indian Ocean variability J. Climate 19 1948-6089
[10]  
Smith I.(2010)A monsoon-like southwest Australian circulation and its relation with rainfall in southwest Western Australia J. Climate 23 1334-4789