Eddy generation mechanism in the eastern South China Sea

Chen Jiajia Cheng Xuhua Chen Xiao

陈佳佳, 程旭华, 陈晓. 南海东部中尺度涡生成机制[J]. 海洋学报英文版, 2019, 38(4): 20-28. doi: 10.1007/s13131-019-1409-3
引用本文: 陈佳佳, 程旭华, 陈晓. 南海东部中尺度涡生成机制[J]. 海洋学报英文版, 2019, 38(4): 20-28. doi: 10.1007/s13131-019-1409-3
Chen Jiajia, Cheng Xuhua, Chen Xiao. Eddy generation mechanism in the eastern South China Sea[J]. Acta Oceanologica Sinica, 2019, 38(4): 20-28. doi: 10.1007/s13131-019-1409-3
Citation: Chen Jiajia, Cheng Xuhua, Chen Xiao. Eddy generation mechanism in the eastern South China Sea[J]. Acta Oceanologica Sinica, 2019, 38(4): 20-28. doi: 10.1007/s13131-019-1409-3

南海东部中尺度涡生成机制

doi: 10.1007/s13131-019-1409-3
基金项目: The National Natural Science Foundation of China under contract Nos 41522601, 41876002, 41876224 and 4170060064; the Fundamental Research Funds for the Central Universities under contract Nos 2017B04714 and 2017B4114.

Eddy generation mechanism in the eastern South China Sea

  • 摘要: 利用高度计海面高度异常数据和非线性1½层约化重力模式研究了南海东部中尺度涡的生成机制。模式结果表明,南海内区风场是南海东部中尺度涡生成的主要驱动力,且南海内区高频风场能解释约54%的南海东部中尺度涡。从西太平洋传来的信号同样有十分重要的作用,由西太区域高频风场大致能解释南海东部40%的中尺度涡。风驱动的赤道附近的海面异常信号能经过锡布图通道和民都洛海峡传播到吕宋岛西海岸,其中有部分能量会以罗斯贝波的形式往西传播。这种信号在西传的过程中会发生不稳定,可能形成孤立的涡旋。
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  • 收稿日期:  2018-06-14

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