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contributor authorElson, Lee S.
date accessioned2017-06-09T14:26:16Z
date available2017-06-09T14:26:16Z
date copyright1986/03/01
date issued1986
identifier issn0022-4928
identifier otherams-19240.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155335
description abstractGeopotential height fields, based on high vertical resolution radiometer measurements, have been used to infer the circulation in the stratosphere from 100 to 1 mb, in the Northern Hemisphere, on a daily basis during February and March of 1979. Initial calculations were based on geostrophy in the traditional way. In addition to demonstrating the benefits of high vertical resolution, these calculations show that for the disturbed conditions present at this time, many of the terms in the momentum equation which were neglected would have made nonnegligible contributions to the balance of terms. In particular, the convergence of meridional wave flux can affect the zonally averaged meridional component of the momentum budget. Ageostrophic terms can affect the zonally varying part of the momentum budgets as well, although an accurate assessment of their importance is complicated by nonlinear processes. These and other results suggest that studies using diagnostically derived winds should include a scale analysis of the momentum budget to verify that the approximations used are valid. Revised estimates have been made of both the zonally averaged and zonally varying components of the wind that include important ageostrophic contributions.
publisherAmerican Meteorological Society
titleAgeostrophic Motions in the Stratosphere from Satellite Observations
typeJournal Paper
journal volume43
journal issue5
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1986)043<0409:AMITSF>2.0.CO;2
journal fristpage409
journal lastpage418
treeJournal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 005
contenttypeFulltext


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