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Further Work on the Kitaigorodskii Roughness Length Model: A New Derivation Using Lettau's Expression on Steep Waves

机译:Kitaigorodskii粗糙度长度模型的进一步工作:使用陡波上的Lettau表达式的新推导

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摘要

A model for the roughness of the sea surface is derived by a combination of two ideas: a) Kitaigorodskii's (1973) about wavelets being roughness elements that move with their associated phase speed; b) Lettau's (1969) about the roughness of a field of roughness elements with characteristic dimensions. The resulting sea surface roughness is related to a wave spectrum consisting of a Kitaigorodskii (1983) inertial form and a Phillips (1958) saturation form. The variation of roughness with wave age is discussed and related to the corresponding variation of the Phillips constant B.
机译:海面粗糙度的模型是通过两个思想的组合得出的:a)Kitaigorodskii(1973)的关于小波是随其相关的相速度移动的粗糙度元素; b)Lettau(1969)关于具有特征尺寸的粗糙度元素场的粗糙度。产生的海面粗糙度与由Kitaigorodskii(1983)惯性形式和Phillips(1958)饱和形式组成的波谱有关。讨论了粗糙度随波龄的变化,并与菲利普斯常数B的相应变化有关。

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