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contributor authorDa Silva, Arlindo M.
contributor authorLindzen, Richard S.
date accessioned2017-06-09T14:31:12Z
date available2017-06-09T14:31:12Z
date copyright1993/01/01
date issued1993
identifier issn0022-4928
identifier otherams-20824.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157095
description abstractThe establishment of stationary waves in the Northern Hemisphere winter is investigated using stationary and time-dependent linear primitive equation models. Confirming the results of Nigam and Lindzen, we find that small displacements of the subtropical jet can cause significant changes in the stationary-wave response. The time scale for stationary establishment is found to be on the order of 5 days, both in the troposphere and in the lower stratosphere. The exception is for a northward shift of the subtropical jet, in which case the establishment of the new stationary solution in the stratosphere occurs on a longer time scale, which is mainly determined by dissipation. Implications for low-frequency atmospheric variability and mid- and long-range weather forecasting are discussed.
publisherAmerican Meteorological Society
titleOn the Establishment of Stationary Waves in the Northern Hemisphere Winter
typeJournal Paper
journal volume50
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1993)050<0043:OTEOSW>2.0.CO;2
journal fristpage43
journal lastpage61
treeJournal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 001
contenttypeFulltext


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