陳慶生2006-08-232018-06-282006-08-232018-06-282002http://ntur.lib.ntu.edu.tw//handle/246246/29331由三維渦漩解析模式探討南海中、下層 的環流,結果顯示受到呂宋海峽內黑潮支 流入侵南海及海面季風演變的雙重影響, 一千公尺以下的深處全年都有一氣旋型環 流。南海深層的湧升應與此環流有關。此 外在季節性斜溫層(250 米)以下還有一 年週期的渦度波由東向西傳。From a 3-dimensional eddy-resolving numerical model of the South China Sea (SCS), we found that there is a cyclonic circulation in the deep basin (below 1000m) throughout the year. The strong upwelling of the deep SCS water is associated with this circulation pattern. Besides the mean cyclonic circulation, there is also a westward propagating Rossby wave of an annual period in the depth region below the main thermocline (below 250 m).application/pdf647039 bytesapplication/pdfzh-TW國立臺灣大學海洋研究所渦漩解析模式氣旋型環流South China Seacyclonic circulationRossby wave黑潮上游海區海洋動力學實驗─子計畫一:黑潮上游海域潮汐及底層環流的研究(Ⅲ)reporthttp://ntur.lib.ntu.edu.tw/bitstream/246246/29331/1/902611M002021OP2.pdf