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dc.contributor.authorShang, S
dc.contributor.authorZhang, C
dc.contributor.authorHong, H
dc.contributor.author洪华生
dc.contributor.authorLiu, Q
dc.contributor.authorWong, GTF
dc.contributor.authorHu, C
dc.contributor.authorHuang, B
dc.date.accessioned2011-07-04T14:49:40Z
dc.date.available2011-07-04T14:49:40Z
dc.date.issued2005-06-02
dc.identifier.citationGEOPHYSICAL RESEARCH LETTERS,2005,32(11):L11601zh_CN
dc.identifier.issn0094-8276
dc.identifier.urihttp://dx.doi.org/doi: 10.1029/2005GL022578
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/9999
dc.description.abstractDuring the 1997 - 1998 El Nino event, the average sea surface temperature (SST) in the Taiwan Strait (TWS) in the winter was similar to 1.4 degrees C higher than that of the winter climatological mean. The areal ratio of the warm water ( >= 2 degrees C above the regional mean) to the cold water ( >= 2 degrees C below the regional mean) in the TWS increased by 25% while the area of the eutrophic water ( chlorophyll a > 1 mg m(-3)) was halved. Field observations also indicate that the mixed layer in the TWS became more nutrient-poor during this winter. These observations are consistent with a diminished advection of the cold and eutrophic Zhe-Min Coastal Water, and, concomitantly, an expansive intrusion of the warm and oligotrophic South China Sea Warm Current/ Kuroshio Branch Water to the TWS as the northeast monsoon was weakened. Thus, El Nino events potentially can have significant ecological impacts on the TWS.zh_CN
dc.language.isoenzh_CN
dc.publisherAMER GEOPHYSICAL UNIONzh_CN
dc.titleHydrographic and biological changes in the Taiwan Strait during the 1997-1998 El Nino winterzh_CN
dc.typeArticlezh_CN


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