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首页> 外文期刊>Journal of Physical Oceanography >Large Eddy Simulation of the Ocean Mixed Layer: The Effects of Wave Breaking and Langmuir Circulation
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Large Eddy Simulation of the Ocean Mixed Layer: The Effects of Wave Breaking and Langmuir Circulation

机译:海洋混合层的大涡模拟:波浪破碎和朗缪尔环流的影响

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摘要

Large eddy simulation (LES) of the ocean mixed layer was performed in which both wave breaking and Langmuir circulation are realized. Wave breaking was represented by random forcing consistent with the observed near-surface turbulence, and Langmuir circulation was realized by the Craig-Leibovich vortex force. High-resolution simulations were carried out using parallel computing with or without each contribution, wave breaking and Langmuir circulation, with an aim to clarify their respective roles in the ocean mixed layer. The effects of wave breaking were found to be mainly limited to the near-surface zorie of the upper few meters. Langmuir circulations below it are not significantly modified, although they become somewhat weakened and less coherent. Under the influence of wave breaking, however, the turbulence production in the upper-ocean mixed layer becomes dominated by the turbulent kinetic energy flux, contrary to the case of the atmospheric boundary layer where it is dominated by shear production. The comparison of the results from the LES and the ocean mixed layer model also reveals the significances of wave breaking and Langmuir circulation in the vertical mixing process of the ocean mixed layer.
机译:对海洋混合层进行了大涡模拟(LES),同时实现了波浪破碎和朗缪尔环流。波浪破裂是由与观察到的近地表湍流一致的随机强迫表示的,朗缪尔环流是由克雷格-莱波维奇涡旋力实现的。高分辨率模拟是使用并行计算进行的,无论有无贡献,波浪破碎和朗缪尔环流,目的是阐明它们各自在海洋混合层中的作用。发现波浪破坏的影响主要限于上部几米的近地表zorie。尽管其下方的朗缪尔环流变弱了一些,并且连贯性降低了,但并没有明显改变。但是,在波浪的破坏作用下,上层海洋混合层中的湍流产生由湍动能通量控制,而大气边界层的情况则以剪切产生力为主。 LES和海洋混合层模型结果的比较还揭示了波浪破碎和Langmuir循环在海洋混合层垂直混合过程中的重要意义。

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