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内波吸引子的数值模拟

王刚 乔方利

王刚, 乔方利. 内波吸引子的数值模拟[J]. 海洋学报, 2010, 32(6): 25-34.
引用本文: 王刚, 乔方利. 内波吸引子的数值模拟[J]. 海洋学报, 2010, 32(6): 25-34.
WANG Gang, QIAO Fang-li. Numerical simulation on internal wave attractors[J]. Haiyang Xuebao, 2010, 32(6): 25-34.
Citation: WANG Gang, QIAO Fang-li. Numerical simulation on internal wave attractors[J]. Haiyang Xuebao, 2010, 32(6): 25-34.

内波吸引子的数值模拟

基金项目: 国家高技术研究发展计划(863)(2008AA09A402);自然科学基金重点项目(40730842);国家海洋局第一海洋研究所基本科研业务经费(GY02-2009G08);中国科学院海洋环流与波动重点实验室开放基金项目(KLOCAW0905)。

Numerical simulation on internal wave attractors

  • 摘要: 密度稳定层结的流体中产生的内波沿着由内波固有频率、流体浮力频率等因素所确定的特征线(或内波射线)传播。边界上的反射不改变内波的频率,从而也不改变反射后的内波特征线与重力方向所成的夹角。侧边界倾斜的封闭容器内,内波能量沿特征线传播的过程中经侧壁、表面和底面的反射可能会集中在一个封闭的轨道上,形成内波吸引子。该现象已经得到水槽试验、线性理论和数值试验的验证。本文利用非线性非静压的环流模式MITgcm,模拟了二维封闭区域中(1,1)-吸引子和(2,1)-吸引子的形成过程,并讨论初值条件对它们的影响。稳定的(1,1)-吸引子其极限环两侧流速出现很强的剪切流。当减小地形的坡度时,由于线性因素的增加,吸引子的结构不变,但吸引子厚度在相空间中的收缩速度加快。对于(2,1)-吸引子,由于轨道所成的两个环中间的节点耗散了部分能量,吸引子的收敛速度较慢。节点处,流体速度始终为0,但存在强烈混合,流体浮力频率呈现振幅较大的周期变化。
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出版历程
  • 收稿日期:  2010-05-30
  • 修回日期:  2010-06-22

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