Please use this identifier to cite or link to this item: http://rportal.lib.ntnu.edu.tw:80/handle/20.500.12235/42862
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dc.contributor國立臺灣師範大學海洋環境科技研究所zh_tw
dc.contributor.authorOey, L.-Y.en_US
dc.contributor.authorY.-C. Hsinen_US
dc.contributor.authorC.-R. Wuen_US
dc.date.accessioned2014-12-02T06:42:35Z-
dc.date.available2014-12-02T06:42:35Z-
dc.date.issued2010-04-01zh_TW
dc.identifierntnulib_tp_C1001_01_019zh_TW
dc.identifier.issn1616-7341zh_TW
dc.identifier.urihttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/42862-
dc.description.abstractObservations indicate that off the northeastern coast of Taiwan a branch of the Kuroshio intrudes farther northward in winter onto the shelf of the East China Sea. We demonstrate that this seasonal shift can be explained solely by winter cooling. Cooling produces downslope flux of dense shelf water that is compensated by shelfward intrusion. Parabathic isopycnals steepen eastward in winter and couple with the cross-shelf topographic slope (the “JEBAR” effect) to balance the enhanced intrusion. The downslope flow also increases vortex stretching and decreases the thickness of the inertial boundary layer, resulting in a Kuroshio that shifts closer to the shelf break.en_US
dc.description.urihttp://phyoce.geos.ntnu.edu.tw/pdf/OD_Why%20does%20the%20Kuroshio%20northeast%20of%20Taiwan%20shift%20shelfward%20in%20winter.pdfzh_TW
dc.languageen_USzh_TW
dc.publisherSpringer-Verlagen_US
dc.relationOcean Dynamics, 60(2), 413-426.en_US
dc.relation.urihttp://dx.doi.org/10.1007/s10236-009-0259-5zh_TW
dc.subject.otherKuroshio migration Model simulation Cooling JEBARen_US
dc.titleWhy does the Kuroshio northeast of Taiwan shift shelfward in winter?en_US
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