吕宋海峡黑潮流套及南海北部的诱生环流之流型，会因黑潮本身以及副热带环流整体的变化而变化，也与海峡的宽度有关。
The Kuroshio Loop and the circulation being induced in northern SCS may be affected by the variation of the Kuroshio itself and the subtropical circulation, as well as the width of the strait.
利用验潮站海表高度差反演吐噶喇海峡黑潮的流量，分析了黑潮流量的年内和年际变化。
This paper USES TKC to reflect the volume transport of Kuroshio through the Tokara strait, analyzes the intra-annual and annual period of the volume of Kuroshio.
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