Three-dimensional numerical simulation of M2 internal tides in the Luzon Strait

LI Bingtian CAO Anzhou LV Xianqing

李秉天, 曹安州, 吕咸青. 吕宋海峡M2内潮的三维数值模拟[J]. 海洋学报英文版, 2015, 34(11): 55-62. doi: 10.1007/s13131-015-0748-y
引用本文: 李秉天, 曹安州, 吕咸青. 吕宋海峡M2内潮的三维数值模拟[J]. 海洋学报英文版, 2015, 34(11): 55-62. doi: 10.1007/s13131-015-0748-y
LI Bingtian, CAO Anzhou, LV Xianqing. Three-dimensional numerical simulation of M2 internal tides in the Luzon Strait[J]. Acta Oceanologica Sinica, 2015, 34(11): 55-62. doi: 10.1007/s13131-015-0748-y
Citation: LI Bingtian, CAO Anzhou, LV Xianqing. Three-dimensional numerical simulation of M2 internal tides in the Luzon Strait[J]. Acta Oceanologica Sinica, 2015, 34(11): 55-62. doi: 10.1007/s13131-015-0748-y

吕宋海峡M2内潮的三维数值模拟

doi: 10.1007/s13131-015-0748-y
基金项目: The National High Technology Research and Development Program (863 Program) of China under contract Nos 2013AA122803 and 2013AA09A502; the National Natural Science Foundation of China under contract Nos 41206001 and 41371496; the National Science and Technology Support Program under contract No. 2013BAK05B04.

Three-dimensional numerical simulation of M2 internal tides in the Luzon Strait

  • 摘要: 本文利用一个三维密度坐标数值模型模拟了吕宋海峡的M2内潮,研究了它的生成、传播、垂向结构和转化率等特征.模拟结果,尤其是模拟的潮流振幅,与观测结果符合良好,表明了该模型的合理性和准确性.研究发现M2内潮水平方向传播主要有以下三条路径:向东进入西太平洋、向西至东沙群岛附近以及向西南方向传播进入南海.在水平方向上,离吕宋海峡越远,M2内潮的潮流振幅越小;而在垂向上,潮流振幅随着深度的增加而减小.由于M2内潮在超临界地形的反射,在吕宋海峡双脊之间会形成顺时针旋转的斜压能通量.受双脊高度和脊间距离的影响,M2内潮在19.5°至21.5°N产生共振.M2内潮在吕宋海峡能量转换约为14.20 GW.
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出版历程
  • 收稿日期:  2015-03-19
  • 修回日期:  2015-05-28

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