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contributor authorGrotjahn, Richard
contributor authorChen, Min
contributor authorTribbia, Joseph
date accessioned2017-06-09T14:32:52Z
date available2017-06-09T14:32:52Z
date copyright1995/03/01
date issued1995
identifier issn0022-4928
identifier otherams-21404.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157740
description abstractThe eigenvalue problems for the original Eady model and a modified Eady model (the G model) are examined with no friction, Ekman friction only, and both Ekman and interior friction. When both Ekman and interior friction are included in the models, normal modes show little additional change when compared to the case with Ekman friction only, whereas the relevant ?continuum modes? have large negative growth rates. Interior friction has a much greater effect on the continuum modes than on the normal modes because inviscid continuum modes have a delta-function vertical profile of potential vorticity q. In contrast, normal modes have much smoother profiles of q in the interior. Streamfunction profiles for the continuum modes are notably different in the two models. The continuum modes in the more realistic G model have sharp peak amplitudes that are not as broad in the vertical as in the Eady model.
publisherAmerican Meteorological Society
titleLinear Instability with Ekman and Interior Friction. Part I: Quasigeostrophic Eigenanalysis
typeJournal Paper
journal volume52
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1995)052<0754:LIWEAI>2.0.CO;2
journal fristpage754
journal lastpage763
treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 006
contenttypeFulltext


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