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Journal ArticleDOI

Viscous damping of small amplitude waves in a non-homogeneous fluid of infinite depth

B.D. Dore
- 01 Jun 1968 - 
- Vol. 15, Iss: 3, pp 259-266
TLDR
In this article, a general formula for the viscous damping of small amplitude waves in a non-homogeneous fluid of infinite depth was derived and shown to be identical to that for a homogeneous fluid.
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This article is published in Deep Sea Research and Oceanographic Abstracts.The article was published on 1968-06-01. It has received 2 citations till now. The article focuses on the topics: Magnetic damping & Inviscid flow.

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Citations
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Journal ArticleDOI

Numerical comparisons of the damping of internal gravity waves in stratified fluids

TL;DR: In this paper, the attenuation of progressive internal waves in stratified fluids consisting of a representation of a single thermocline, a weak exponential density distribution and a two-layer system was compared.
Journal ArticleDOI

On secondary vorticity in internal waves

TL;DR: In this paper, the authors investigated the generation of secondary vorticity in maintained and temporallydecaying wave motions for internal waves in fluid of great depth, and established a steady state for maintained waves, and the mass transport velocity field was investigated.
References
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Journal ArticleDOI

The disintegration of wave trains on deep water Part 1. Theory

TL;DR: In this paper, a theoretical analysis of the stability of periodic wave trains to small disturbances in the form of a pair of side-band modes is presented, where the wave train becomes highly irregular far from its origin, even when the departures from periodicity are scarcely detectable at the start.
Journal ArticleDOI

Instability of Periodic Wavetrains in Nonlinear Dispersive Systems

TL;DR: In this article, it was shown that wavetrains are unstable to small disturbances of a certain kind, so that in practice they will disintegrate if the attempt is made to send them over great distances.
Journal ArticleDOI

The viscous damping of gravity waves in shallow water

TL;DR: In this paper, it is shown that le taux de dissipation visqueuse de l'energie d'une onde de gravite can be approximated by a 1/2-approximation.
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