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Wavenumber spectrum of intermediate-scale ocean surface waves

机译:中尺度海面波的波数谱

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This paper presents an analysis of the wavenumber spectra of intermediate-scale waves (wavelengths between 0.02 and 6 m) under various sea-state conditions. The main result of the analysis is that the dependence of the dimensionless wave spectrum on the dimensionless wind friction velocity follows a power-law function. The coefficient and exponent of the power-law function vary systematically with the wavenumber. The wavenumber dependence of the coefficient and exponent serves as an empirical parameterization for computing the wavenumber spectra of intermediate-scale waves at different wind speeds. Calculation of the mean-square slope from the resulting wavenumber spectrum confirms that intermediate-scale waves are the dominant contributor of the ocean surface roughness. A simple formula is presented for calculating the band-pass filtered mean-square slope of the ocean surface for remote sensing applications.
机译:本文介绍了在各种海况条件下中尺度波(波长在0.02和6 m之间)的波数谱分析。分析的主要结果是,无量纲波谱对无量纲风摩擦速度的依赖性遵循幂律函数。幂律函数的系数和指数随波数而系统地变化。系数和指数的波数相关性用作计算不同风速下中尺度波的波数谱的经验参数化。从产生的波数频谱计算均方斜率可以确认中等规模的波是海洋表面粗糙度的主要贡献者。提出了一个简单的公式,用于计算遥感应用的海面带通滤波后的均方斜率。

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