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| 研究生： |
陳柏宇 Chen Po-Yu |
|---|---|
| 論文名稱： |
蘇祿海表層環流之數值模式研究 Numerical studies on the surface circulation of the Sulu Sea |
| 指導教授： |
吳朝榮
Wu, Chau-Ron |
| 學位類別： |
碩士 Master |
| 系所名稱： |
地球科學系 Department of Earth Sciences |
| 論文出版年： | 2010 |
| 畢業學年度： | 98 |
| 語文別： | 中文 |
| 論文頁數： | 60 |
| 中文關鍵詞： | 蘇祿海 、表層環流 、數值模式 、民多羅海峽 、巴拉巴克海峽 、錫布圖通道 |
| 英文關鍵詞： | Sulu Sea, surface circulation, numerical model, Mindoro Strait, Balabac Strait, Sibutu Passage |
| 論文種類： | 學術論文 |
| 相關次數： | 點閱：101 下載：3 |
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蘇祿海 (Sulu Sea) 位於117°E~123°E、5°N~12.5°N，為一個東北–西南走向的半封閉海盆，經由民多羅海峽及巴拉巴克海峽與南海交換水體，藉由錫布圖通道通往西里伯斯海，同時也是南海貫穿流(South China Sea Throughflow, SCSTF) 通過的區域，進出蘇祿海的水體，對於南海、西里伯斯海與西太平洋環流的水量平衡有相當程度的影響，是西太平洋區域上很重要的邊緣海。
本研究利用海洋數值模式配合衛星觀測資料，來探討蘇祿海的表層環流型態與其季節變化。透過模式模擬的結果顯示，蘇祿海的表層環流型態主要受到蘇祿海貫穿流 (Sulu Sea Throughflow) 的影響，有明顯的季節性變化，在春季時流向向北，而夏秋冬三季則是流向向南，同時也受到科氏力的作用，使得海流主軸進到海盆後偏右轉向。此外，風場也是改變環流型態的因素之一，夏季時海流主軸位置會較遠離海盆西側並沿海盆中央向南流，隨著風力減弱及風向改變，逐漸向海盆西側靠近，到了冬季時海流主軸位置會最靠近海盆西側，沿著巴拉望島東南沿岸向南流。
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Chen, C.-T.A., W.-P. Hou, T. Gamo, and S.L. Wang (2006): Carbonate-related Parameters of Subsurface Waters in the West Philippine. South China and Sulu Sea, Marine Chemistry, 99, 151-161.
Chiang, T.-L., C.-R. Wu, and S.-Y. Chao (2008): Physical and Geographical Origins of the South China Sea Warm Current. Journal of Geophysical Research, 113, 4794-4806.
Fang, G., D. Susanto, I. Soesilo, Q. Zheng, F. Qiao, and Z. Wei, (2005): A Note on the South China Sea Shallow Interocean Circulation. Advances in Atmospheric Sciences, 22, 945-954.
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Yaremchuk, M., J. McCreary, Z. Yu, and R. Furue (2009) : The South China Sea Throughflow Retrieved from Climatological Data. Journal of Physical Oceanography, 31,753-667.
