破浪“白头”寿命的估计

A. E. Korinenko, V. Malinovsky, V. Dulov, V. Kudryavtsev
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引用次数: 0

摘要

本文介绍了风浪破浪(“白浪”)的寿命和沿长表面波剖面的起浪力矩的空间分布的研究结果。本文给出了在黑海某海洋平台进行的专门实验的结果。白浪的登记是根据海面的录像进行的。测量了表面波的特征,并在录像的同时记录了气象信息。结果表明,白浪的寿命分布可以用指数定律很好地描述。结果表明,单个白浪的寿命与破浪周期之比为0.3。上述比值在不同风浪条件下的分布是相似的。结果表明,白浪的产生主要发生在长波波峰区域,平均向波峰前坡偏移9.6个长波相位。在长波的生命周期中,在前缘产生的白浪向长波的后缘移动,使得破碎起始与白浪覆盖的表面分数最大值之间的相位差为21.6。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Estimation of the “whitecap” lifetime of breaking wave
The paper presents the results of a study of the lifetime of wind-wave breaking (“whitecaps”) and the spatial distribution of the moments of wave-breaking initiation along the profile of a long surface wave. The results obtained during the specialized experiments from an oceanographic platform in the Black Sea are given. The registration of the whitecaps was carried out based on the video recordings of the sea surface. The surface waves’ characteristics were measured and the meteorological information was recorded simultaneously with the video recordings. It is shown that the distribution of the whitecaps’ lifetime is well described by an exponential law. It was found that the ratio of the lifetime of an individual whitecap to the period of the breaking wave is 0.3. The distributions of the above-mentioned ratio are similar for different wind and wave conditions. It is indicated that the generation of whitecaps occurs mainly in the region of the crest of a long wave with a shift to its front slope on average by 9.6 of the phase of the long wave. The whitecap having arisen at the leading edge shifts to the trailing edge of the long wave during its lifetime, so that the phase difference between the breaking initiation and the maximum of the surface fraction covered by the whitecaps equals 21.6.
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