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dc.contributor.authorLi, Jiaxun
dc.contributor.authorWang, Guihua
dc.contributor.authorXie, Shang-Ping
dc.contributor.authorZhang, Ren
dc.contributor.authorSun, Zhenyu
dc.contributor.author孙振宇
dc.date.accessioned2013-02-25T03:05:50Z
dc.date.available2013-02-25T03:05:50Z
dc.date.issued2012-08-29
dc.identifier.citationJOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2012,117zh_CN
dc.identifier.issn0148-0227
dc.identifier.urihttp://dx.doi.org/10.1029/2012JC008189
dc.identifier.uriWOS:000308321400004
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/14890
dc.description.abstractA winter warm pool off the southwest coast of Hainan Island is uncovered from high resolution satellite measurements and field observations. The warm pool is characterized by warm temperature relative to the surroundings. It forms in October, intensifies from November to next January, and decays in February. Our results show that the wind wake in the northeast winter monsoon due to the orographic blockage by mountains of Hainan Island plays an important role in generating the warm pool by reducing surface latent heat flux. The core temperature of the warm pool is correlated with the El Nino and Southern Oscillation.zh_CN
dc.description.sponsorshipNational Science Foundation of China (NSFC) for Distinguished Young Scholars [41125019]; National Basic Research Program of China [2012CB955601]; NSFC [40976017]; Natural Science Foundation of Zhejiang for Innovative Research Groups [2009R50044]; SOA of China ["908-01-ST09"]zh_CN
dc.language.isoenzh_CN
dc.publisherAMER GEOPHYSICAL UNIONzh_CN
dc.subjectSEA-SURFACE TEMPERATUREzh_CN
dc.subjectUPPER-OCEAN RESPONSEzh_CN
dc.subjectCHINA SEAzh_CN
dc.subjectINTERANNUAL VARIABILITYzh_CN
dc.subjectCHLOROPHYLL-Azh_CN
dc.subjectEL-NINOzh_CN
dc.subjectCLIMATEzh_CN
dc.subjectGULFzh_CN
dc.titleA winter warm pool southwest of Hainan Island due to the orographic wind wakezh_CN
dc.typeArticlezh_CN


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