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  1. National Taiwan Ocean University Research Hub
  2. 海洋科學與資源學院
  3. 海洋環境資訊系
請用此 Handle URI 來引用此文件: http://scholars.ntou.edu.tw/handle/123456789/25807
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dc.contributor.authorTseng, Yu-Haoen_US
dc.contributor.authorHo, Chung-Ruen_US
dc.contributor.authorZheng, Quananen_US
dc.contributor.authorZheng, Zhe-Wenen_US
dc.date.accessioned2025-06-07T06:12:56Z-
dc.date.available2025-06-07T06:12:56Z-
dc.date.issued2025/2/1-
dc.identifier.issn2169-9275-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/25807-
dc.description.abstractThis study aimed to examine the variations in vorticity in the northern South China Sea (NSCS) resulting from the cut-off of the Kuroshio main path east of Taiwan Island. Absolute dynamic topography and satellite altimeter eddy tracking data from 1993 to 2021 were employed to analyze the momentum ratio of the Kuroshio and mesoscale eddies concerning Kuroshio cut-off events through their interaction. The results revealed 12 events where mesoscale cyclonic eddies east of Taiwan Island cut off the Kuroshio main path, resulting in intensified loop currents in the Luzon Strait and increased negative vorticity in the NSCS. Six of these events occurred between 1998 and 2013, coinciding with the negative Pacific Decadal Oscillation (PDO) regime. During this period, negative vorticity triggered by Kuroshio cut-off events rose by 79% in the NSCS, compared to 34% during the positive PDO regime. The Kuroshio interacted with mesoscale cyclonic eddies east of Taiwan for 28 days during the negative PDO regime and 41 days during the positive PDO regime. The Kuroshio velocity strengthened east of Luzon Island but weakened east of Taiwan Island during the negative PDO regime, elucidating the observed disparity. The average duration between the occurrence of mesoscale cyclonic eddy impinging on the Kuroshio east of Taiwan Island and the peak negative vorticity observed in the NSCS was approximately 28 days. This was comparable to data obtained using field measurements.en_US
dc.language.isoEnglishen_US
dc.publisherAMER GEOPHYSICAL UNIONen_US
dc.relation.ispartofJOURNAL OF GEOPHYSICAL RESEARCH-OCEANSen_US
dc.subjectKuroshioen_US
dc.subjectglobal warming hiatusen_US
dc.subjectmesoscale eddyen_US
dc.subjectvorticityen_US
dc.subjectloop currenten_US
dc.subjectSouth China seaen_US
dc.titleLoop Current West of the Luzon Strait Triggered by Kuroshio Cut-Off Events East of Taiwan Islanden_US
dc.typejournal articleen_US
dc.identifier.doi10.1029/2024JC021572-
dc.identifier.isiWOS:001408295800001-
dc.relation.journalvolume130en_US
dc.relation.journalissue2en_US
dc.identifier.eissn2169-9291-
item.languageiso639-1English-
item.fulltextno fulltext-
item.openairetypejournal article-
item.grantfulltextnone-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
item.cerifentitytypePublications-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptDepartment of Marine Environmental Informatics-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.orcid0000-0001-7629-2765-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
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