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Evaluation of a Roughness Length Model and Sea Surface Properties with Data from the Baltic Sea

机译:利用波罗的海的数据评估粗糙度长度模型和海面特性

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摘要

The exchange of momentum between the oceans and atmosphere is important for many atmospheric and oceanic processes and is mainly governed by the roughness of sea surface. The roughness can be expressed by a roughness length z_0. A roughness length model, based on the concept that z_0 is determined by stochastic wave breaking, is presented. The model performance is evaluated using measurements from the OEstergarnsholm site, in the Baltic Sea, and pertinent information from other recent investigations. The wave field and the roughness length variations are investigated during various sea state conditions dominated by wind-driven waves. It is found that several parameters, describing the characteristics of the wave field, are dependent on the amount of energy that long waves have relative to the energy of short, wind-driven waves of the sea spectrum (called the swell ratio). The impact of swell ratio on z_0 can explain the discrepancies found in various results among relevant investigations. The roughness length model can well reproduce the observed roughness length.
机译:海洋与大气之间的动量交换对于许多大气和海洋过程都很重要,并且主要由海面的粗糙度决定。粗糙度可以由粗糙度长度z_0表示。基于z_0由随机波破坏确定的概念,提出了一种粗糙度长度模型。使用来自波罗的海的OEstergarnsholm站点的测量结果以及来自其他近期调查的相关信息来评估模型性能。在以风为主导的各种海况条件下,研究了波场和粗糙度长度变化。已经发现,描述波场特征的几个参数取决于长波相对于海谱的短的,由风驱动的波的能量(称为膨胀比)的量。膨胀率对z_0的影响可以解释相关研究中各种结果中发现的差异。粗糙度长度模型可以很好地再现观察到的粗糙度长度。

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  • 来源
    《Journal of Physical Oceanography》 |2010年第9期|P.2007-2024|共18页
  • 作者单位

    Department of Earth Sciences, Uppsala University, Villavagen 16, 752 36 Uppsala, Sweden;

    rnWater Resources and Environmental Engineering Division, School of Civil Engineering, National Technical University of Athens, Athens, Greece;

    rnDepartment of Earth Sciences, Uppsala University, Uppsala, Sweden;

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