Asymptotics of Far Fields of Internal Gravity Waves Caused by Localized Sources in an Infinite Deep Stratified Medium

IF 1 4区 工程技术 Q4 MECHANICS
V. V. Bulatov
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引用次数: 0

Abstract

In this work, the far fields of internal gravity waves excited by a perturbation source moving in a vertically infinite stratified medium are studied. Propagation of waves in inviscid, incompressible medium with an exponential distribution of unperturbed density is considered. In the linear approximation and in the Boussinesq approximation, uniform asymptotics of excited fields of internal gravity waves far from the moving perturbation source are built, including those in the neighborhood of the traverse plane and the motion horizon. The obtained asymptotic solutions allow effectively computing the main amplitude-phase characteristics of excited far fields of internal gravity waves at certain modes of generation and, in addition, qualitatively analyzing the obtained solutions, which is important to correct formulation of more sophisticate mathematical models of wave dynamics of real natural stratified media.

无限深分层介质中局部源引起的内部引力波远场渐近学
摘要 本文研究了在垂直无限分层介质中运动的扰动源激发的内重力波的远场。研究考虑了波在无粘性、不可压缩、未扰动密度呈指数分布的介质中的传播。在线性近似和布西内斯克近似中,建立了远离运动扰动源的内部重力波激发场的均匀渐近线,包括横移平面和运动水平线附近的激发场。所获得的渐近解可以有效地计算内重力波在某些产生模式下的激发远场的主要振幅相位特征,此外,还可以对所获得的解进行定性分析,这对于正确建立更复杂的真实自然分层介质波动力学数学模型非常重要。
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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来源期刊
Fluid Dynamics
Fluid Dynamics MECHANICS-PHYSICS, FLUIDS & PLASMAS
CiteScore
1.30
自引率
22.20%
发文量
61
审稿时长
6-12 weeks
期刊介绍: Fluid Dynamics is an international peer reviewed journal that publishes theoretical, computational, and experimental research on aeromechanics, hydrodynamics, plasma dynamics, underground hydrodynamics, and biomechanics of continuous media. Special attention is given to new trends developing at the leading edge of science, such as theory and application of multi-phase flows, chemically reactive flows, liquid and gas flows in electromagnetic fields, new hydrodynamical methods of increasing oil output, new approaches to the description of turbulent flows, etc.
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