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contributor authorHyde, Richard A.
date accessioned2017-06-09T14:24:23Z
date available2017-06-09T14:24:23Z
date copyright1984/01/01
date issued1984
identifier issn0022-4928
identifier otherams-18706.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154741
description abstractAsymptotic solutions, to first order, are found for linearized, shallow water, inertia-gravity (Kelvin and Poincaré) waves in a zonal channel for two different cases in which the environment varies linearly with latitude: a beta plane (variable rotation, constant depth) and an equivalent beta plane (variable depth, constant rotation). Unlike the results for quasi-geostrophic motions, the solutions show that the environments of varying rotation and varying depth produce markedly different behaviors in the inertia-gravity waves The equivalent beta-plane environment is found to perturb the inertia-gravity waves considerably more than the beta-plane environment, but in both case long zonal waves are generally more resilient than short waves to changes in their environment. The results indicate also that the channel inertia-gravity waves respond somewhat differently than do coastal Kelvin, edge and shelf waves to the two different environments; nevertheless, similarities are also found.
publisherAmerican Meteorological Society
titleThe Influence of Variable Rotation and Variable Depth on Barotropic Kelvin and Poinearé Waves
typeJournal Paper
journal volume41
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1984)041<0038:TIOVRA>2.0.CO;2
journal fristpage38
journal lastpage50
treeJournal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 001
contenttypeFulltext


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