Group velocity and dispersion of Buchwald and Adams shelf waves. A new analytical approach

V. Gnevyshev, V. Travkin, T. Belonenko
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引用次数: 1

Abstract

In this paper, a new analysis of the known topographic models of Rossby waves for piecewise exponential topography profiles is performed. A mathematical method is proposed that allows us to find analytically the group velocity and variance. A numerical comparison is made of the relations presented in the study of Buchwald and Adams and the dependencies obtained within the framework of a new analytical approach. Numerical comparative analysis showed that the discrepancy for the phase velocities lies in the range of five percent. For group speeds, the discrepancy reaches nineteen percent for the first mode and decreases for higher mode numbers. We also consider long-wave asymptotics of eigenfunctions. It is established that the long-wave limit for Rossby shelf waves has specifics: the longitudinal wave number tends to zero, and the transverse wave number reaches a certain finite positive constant, which is the greater the higher the mode number. It is shown that in the long-wave limit, Rossby shelf waves transform into shelf topographic currents, while there is a certain self-similarity for the phase and group velocities of shelf currents depending on the value of the topography gradient.
布赫瓦尔德和亚当斯陆架波的群速和频散。一种新的分析方法
本文对分段指数地形剖面的已知罗斯比波地形模型进行了新的分析。提出了一种数学方法,可以解析地求出群速度和群方差。数值比较了Buchwald和Adams研究中提出的关系和在一种新的分析方法框架内获得的依赖关系。数值对比分析表明,两者相速度的差异在5%范围内。对于群速度,第一模式的差异达到19%,更高模式数的差异减小。我们还考虑了特征函数的长波渐近性。建立了罗斯比陆架波的长波极限有其特殊性:纵波数趋于零,横波数达到某一有限正常数,模态数越高,该正常数越大。结果表明,在长波极限下,罗斯比陆架波转化为陆架地形流,而陆架流的相速度和群速度随地形梯度的大小有一定的自相似性。
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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