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Pressure-Slope Momentum Transfer in Ocean Surface Boundary Layers Coupled with Gravity Waves

机译:重力波耦合作用下海洋表面边界层压力-坡面动量传递

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摘要

The paper focuses on the consequences of including surface and subsurface, wind-forced pressure-slope momentum transfer into the oceanic water column, a transfer process that competes with now-conventional turbulence transfer based on mixing coefficients. Horizontal homogeneity is stipulated as is customary when introducing a new surface boundary layer model or significantly new vertical momentum transfer physics to an existing model. An introduction to pressure-slope momentum transfer is first provided by a phase-resolved, vertically dependent analytical model that excludes turbulence transfer. There follows a discussion of phase averaging; an appendix is an important adjunct to the discussion. Finally, a coupled wave-circulation model, which includes pressure-slope and turbulence momentum transfer, is presented and numerically executed. The calculated temperatures compare well with measurements from ocean weather station Papa.
机译:本文着重研究了包括表面和地下在内的后果,风压坡向动量转移到海洋水柱中的过程,这种转移过程与现在基于混合系数的湍流转移竞争。在引入新的表面边界层模型或在现有模型中引入明显的新的垂直动量传递物理过程时,通常会规定水平均匀性。首先通过相位解析的垂直相关分析模型(不包括湍流传递)来介绍压力-坡度动量传递。接下来讨论相位平均。附录是讨论的重要附件。最后,给出了包含压力-坡度和湍流动量传递的耦合波循环模型,并进行了数值计算。计算出的温度与海洋气象站Papa的测量值相吻合。

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  • 来源
    《Journal of Physical Oceanography》 |2013年第10期|2173-2184|共12页
  • 作者

    George Mellor;

  • 作者单位

    George Mellor, Program in Atmospheric and Oceanic Sciences, Sayre Hall, Forrestal Campus,Princeton University, Princeton, NJ 08540;

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  • 正文语种 eng
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