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- The Spreading of the South China Sea Water to the East of Taiwan during Summertime
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題 名 | The Spreading of the South China Sea Water to the East of Taiwan during Summertime=夏季期間南海水團在臺灣東部海域的擴散 |
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作 者 | 陳慶生; 王冑; | 書刊名 | 臺灣海洋學刊 |
卷 期 | 36:2 1998.02[民87.02] |
頁 次 | 頁97-109 |
分類號 | 351.9 |
關鍵詞 | 南海; 菲律賓海; 水團; 黑潮; South china sea; Philippine sea; Water mass; |
語 文 | 英文(English) |
中文摘要 | 南海是位於臺灣南邊的一個廣大的邊緣海。他的海水特徵與鄰近的菲律賓海水有 很大的差異,與菲律賓海水相比,南海水的溫度躍層深度比較淺但強度大很多。南海水的鹽 度極大值,約為 34.8psu,小於菲律賓海水的對應數值,但是,南海水的鹽度極小值,約為 34.4psu,大於菲律賓海水的 34.3psu。 夏季時西南季風會驅動南海表層水向北流,經呂宋海峽擴散到臺灣東側海域。受到臺東外海 海底地形的阻擋作用,鹽度極小值以下深度的南海水不會出現在臺灣東側海域。 |
英文摘要 | The South China Sea (SCS) is a vast marginal area at the south of Taiwan. Its water masses have distinct characteristics when compared to the adjacent Philippine Sea water. For example, the SCS water has a more shallow but stronger thermocline, while its salinity maximum, about 34.8 psu, is smaller. On the other hand, the salinity minimum of the SCS water, about 34.4 psu, is lager than that of the Philippine Sea water. During summer, the southwestern winds drive the surface SCS water northward and transport it to the region east of Taiwan. However, due to the blocking by a submarine ridge to the east of southern Taiwan, the intermediate SCS water, corresponding to the depth of the salinity minimum, does not occur to the east of Taiwan. |
本系統中英文摘要資訊取自各篇刊載內容。