王冑2006-08-232018-06-282006-08-232018-06-281999http://ntur.lib.ntu.edu.tw//handle/246246/29296黑潮通過呂宋海峽時，有時產生 套流，有時入侵南海，而更多時段則 又什麼也不發生。為釐清上述問題， 我們沿著呂宋海峽佈放了觀測儀器， 根據這些結果發現恆春海脊上海流的 東分量以及當地之水位變化是兩個有 意義指標，可作為研判黑潮變動行為 的根據，並從而推斷出南海東北部海 盆內海洋環流與黑潮之互動情形。Various patterns of Kuroshio, such as a loop current, an intrusion event or a rapidly NE flow, are observed when the current flows through the Luzon Strait. Long term observations by instrument moorings are used for clarifying these obscurities. Two indexes, the eastward velocity component and the sub-inertial water level on the Heng-Chuen Ridge, are found to be useful to interpret the variability of Kuroshio as well as to infer the mutual interaction between Kuroshio and the circulation in the northeastern South China Sea basin.application/pdf24009 bytesapplication/pdfzh-TW國立臺灣大學海洋研究所黑潮南海套流入侵KuroshioSouth China SeaLoop CurrentIntrusionreporthttp://ntur.lib.ntu.edu.tw/bitstream/246246/29296/1/882611M002012AP7.pdf