Evaluation of Ocean-Wave Dependence of Sea Surface Roughness Using Wave-Boundary Layer Model

Naoto Kihara, S. Ishihara, Hiromaru Chi
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Abstract

Ocean-wave dependence of sea surface roughness is investigated using a wave boundary layer model, which is based ona recently obtained knowledge of air-sea interaction. The momentum flux is estimated by solving the model with meteorologicaland ocean wave information, which is obtained by carrying out the WRF and WWIII simulations. When windwaveis predominant, the results show clear relationships between Charnock coefficient and the wave age, between theroughness normalized by significant wave height z0/Hs and the wave age, and between the z0/Hs and the wave steepness.On the other hand, when swell is predominant, the results do not show clear dependence of Charnock coefficient on thewave age, and that of z0/Hs on the wave steepness, although that of z0/Hs on the wave age is observed.
用波浪边界层模型评价海面粗糙度对海浪的依赖性
基于最近获得的海气相互作用知识,采用波浪边界层模型研究了海波对海面粗糙度的依赖性。动量通量是通过利用WRF和二战模拟得到的气象和海浪信息求解模型来估计的。当风波为主时,Charnock系数与波龄、显著波高归一化后的通度z0/Hs与波龄、z0/Hs与波陡之间存在明显的关系。另一方面,在以浪涌为主的情况下,查诺克系数与浪龄的关系不明显,z0/Hs与浪陡的关系不明显,但z0/Hs与浪龄有关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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