Linear Normal Modes of a Moving, Shallow-Water Barotropic Vortex

1990 ◽  
Vol 47 (17) ◽  
pp. 2141-2148 ◽  
Author(s):  
H. E. Willoughby
Keyword(s):  
2021 ◽  
Vol 149 (4) ◽  
pp. A66-A67
Author(s):  
Sergei Sergeev ◽  
Konstantin Dmitriev ◽  
Andrey Shurup
Keyword(s):  

1982 ◽  
Vol 71 (S1) ◽  
pp. S11-S11
Author(s):  
Suzanne T. McDaniel
Keyword(s):  

2010 ◽  
Vol 18 (03) ◽  
pp. 245-257 ◽  
Author(s):  
DA ZHI GAO ◽  
NING WANG ◽  
HAO ZHONG WANG

For sound propagation in a shallow water waveguide, a dedispersion transform which can remove the dispersive effect of signal is described in this paper. The transform is a modified Fourier transform with two variables: translation and dispersion. Dispersive effect of signal for normal modes can be removed when these two variables match to real parameters. The validity of the present approach is verified in simulation and real data processing.


2015 ◽  
Author(s):  
Andrey S. Shurup ◽  
Sergei N. Sergeev ◽  
Valeriy V. Goncharov ◽  
Alexander I. Vedenev ◽  
Oleg A. Godin ◽  
...  

1990 ◽  
Vol 88 (S1) ◽  
pp. S58-S58
Author(s):  
Grayson H. Rayborn ◽  
Barry I. Barker ◽  
George E. Ioup ◽  
Juliette W. Ioup

Geophysics ◽  
1951 ◽  
Vol 16 (4) ◽  
pp. 594-612 ◽  
Author(s):  
K. E. Burg ◽  
Maurice Ewing ◽  
Frank Press ◽  
E. J. Stulken

On one particular prospect in shallow water repetitive patterns appeared on short spread seismograms in such prevalence as to jeopardize identification of desired reflections. It is demonstrated that under favorable conditions, less restrictive than thought necessary heretofore, a layer of water comprises an effective wave guide for seismic energy propagation. Reinforcement fronts formed by multiple reflection of sound in water can develop into a set of waves completely overshadowing other seismic arrivals. With but minor modifications conventional wave guide theory applies. Examples from the prospect are presented to illustrate various reinforcement patterns. Observed frequency characteristics, group velocity, and phase velocity magnitudes are investigated for normal modes of propagation.


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