Remote influence of North Atlantic SST on the equatorial westerly wind anomalies in the western Pacific for initiating an El Nino event: an Atmospheric General Circulation Model Study
[Wang, Xin] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA; [Wang, Xin; Wang, Chunzai] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA; Wang, Dongxiao] Chinese Acad Sci, State Key Lab Trop Oceanog, South China Sea Inst Oceanol, Guangzhou, Guangdong, Peoples R China; [Zhou, Wen] City Univ Hong Kong, Sch Energy & Environm, Guy Carpenter Asia Pacific Climate Impact Ctr, Hong Kong, Hong Kong, Peoples R China; [Liu, Lin] State Ocean Adm, Inst Oceanog 1, Ctr Ocean & Climate Res, Qingdao, Peoples R China; Xin.Wang.AOML@noaa.gov
2013
发表期刊ATMOSPHERIC SCIENCE LETTERS
ISSN1530-261X
卷号14期号:2页码:107-111
摘要This article uses an atmospheric general circulation model to show that the cooler North Atlantic sea surface temperature anomalies in summer can produce a Rossby wave-like teleconnection pattern strengthening the Siberian High in winter and next spring. The stronger Siberian High enhances the continent northerlies over East Asia and the associated cyclonic circulation over the western North Pacific, which provides a tropical westerly background for occurrence of the westerly wind bursts. The stronger northerlies over East Asia can also induce frequent cold surges, which tend to produce the equatorial westerly wind anomalies in the western Pacific for initiating an El Nino event. Copyright. (C) 2013 Royal Meteorological Society
部门归属LTO
关键词Climate El Nino Onset Enso Westerly Wind Bursts
学科领域Geochemistry & Geophysics ; Meteorology & Atmospheric Sciences
资助者This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML).
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资助者This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML). ; This work was supported by National Basic Research Program of China (2010CB950304 and 2013CB430301), National Natural Science Foundation of China (Grant Nos. 40906010 and 41175079), the Chinese Academy of Sciences, the National Oceanic and Atmospheric Administration (NOAA) Climate Program Office and the base funding of NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML).
WOS记录号WOS:000317862300009
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文献类型期刊论文
条目标识符http://ir.scsio.ac.cn/handle/344004/10922
专题热带海洋环境国家重点实验室(LTO)
通讯作者Xin.Wang.AOML@noaa.gov
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[Wang, Xin] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA,[Wang, Xin,Wang, Chunzai] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA,et al. Remote influence of North Atlantic SST on the equatorial westerly wind anomalies in the western Pacific for initiating an El Nino event: an Atmospheric General Circulation Model Study[J]. ATMOSPHERIC SCIENCE LETTERS,2013,14(2):107-111.
APA [Wang, Xin] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA.,[Wang, Xin.,Wang, Chunzai] NOAA, Atlantic Oceanog & Meteorol Lab, Miami, FL 33149 USA.,Wang, Dongxiao] Chinese Acad Sci, State Key Lab Trop Oceanog, South China Sea Inst Oceanol, Guangzhou, Guangdong, Peoples R China.,[Zhou, Wen] City Univ Hong Kong, Sch Energy & Environm, Guy Carpenter Asia Pacific Climate Impact Ctr, Hong Kong, Hong Kong, Peoples R China.,...&Xin.Wang.AOML@noaa.gov.(2013).Remote influence of North Atlantic SST on the equatorial westerly wind anomalies in the western Pacific for initiating an El Nino event: an Atmospheric General Circulation Model Study.ATMOSPHERIC SCIENCE LETTERS,14(2),107-111.
MLA [Wang, Xin] Univ Miami, Cooperat Inst Marine & Atmospher Studies, Miami, FL USA,et al."Remote influence of North Atlantic SST on the equatorial westerly wind anomalies in the western Pacific for initiating an El Nino event: an Atmospheric General Circulation Model Study".ATMOSPHERIC SCIENCE LETTERS 14.2(2013):107-111.
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