A numerical study of the generation mechanism of internal solitary waves in the Luzon Strait

WANG Jing SUN Meiling ZHANG Xudong SUN Lina MENG Junmin

王晶, 孙美玲, 张旭东, 孙丽娜, 孟俊敏. 基于调制不稳定性的吕宋海峡内孤立波生成机理探讨[J]. 海洋学报英文版, 2015, 34(7): 38-43. doi: 10.1007/s13131-015-0695-7
引用本文: 王晶, 孙美玲, 张旭东, 孙丽娜, 孟俊敏. 基于调制不稳定性的吕宋海峡内孤立波生成机理探讨[J]. 海洋学报英文版, 2015, 34(7): 38-43. doi: 10.1007/s13131-015-0695-7
WANG Jing, SUN Meiling, ZHANG Xudong, SUN Lina, MENG Junmin. A numerical study of the generation mechanism of internal solitary waves in the Luzon Strait[J]. Acta Oceanologica Sinica, 2015, 34(7): 38-43. doi: 10.1007/s13131-015-0695-7
Citation: WANG Jing, SUN Meiling, ZHANG Xudong, SUN Lina, MENG Junmin. A numerical study of the generation mechanism of internal solitary waves in the Luzon Strait[J]. Acta Oceanologica Sinica, 2015, 34(7): 38-43. doi: 10.1007/s13131-015-0695-7

基于调制不稳定性的吕宋海峡内孤立波生成机理探讨

doi: 10.1007/s13131-015-0695-7

A numerical study of the generation mechanism of internal solitary waves in the Luzon Strait

  • 摘要: 中国南海由于地势环境的复杂性, 成为海洋内波的多发区, 其中中国南海北部大部分内波发源于吕宋海峡。本文通过调制不稳定探讨吕宋海峡内波生成机理。依据完全非线性薛定谔方程, 推导内潮波调制不稳定性的增益。从层化、内潮波的波长和初始振幅等方面计算了内潮波在吕宋海峡处增益峰值的变化, 从而分析吕宋海峡区域内潮波调制不稳定性的特点, 发现了吕宋海峡内潮波演变成内孤立波的条件。研究结果表明:内潮波在吕宋海峡处能够产生调制不稳定性, 其增益的峰值发生在东部山脊处, 内潮波在此处获得最大增益, 开始分裂成孤立波列。峰值增益的大小和范围与层化、内潮波初始条件有关。数值计算结果与实际观测结果吻合。
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出版历程
  • 收稿日期:  2014-08-08
  • 修回日期:  2014-11-13

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