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contributor authorTomikawa, Yoshihiro
contributor authorSato, Kaoru
contributor authorShepherd, Theodore G.
date accessioned2017-06-09T16:53:14Z
date available2017-06-09T16:53:14Z
date copyright2006/12/01
date issued2006
identifier issn0022-4928
identifier otherams-75985.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218381
description abstractThe spatial structure and phase velocity of tropopause disturbances localized around the subpolar jet in the Southern Hemisphere are investigated using 6-hourly European Centre for Medium-Range Weather Forecasts reanalysis data covering 15 yr (1979?93). The phase velocity and phase structure of the tropopause disturbances are in good agreement with those of an edge wave vertically trapped at the tropopause. However, the vertical distribution of the ratio of potential to kinetic energy exhibits maxima above and below the tropopause and a minimum around the tropopause, in contradiction to edge wave theory for which the ratio is unity throughout the troposphere and stratosphere. This difference in vertical structure between the observed tropopause disturbances and edge wave theory is attributed to the effects of a finite-depth tropopause together with the next-order corrections in Rossby number to quasigeostrophic dynamics.
publisherAmerican Meteorological Society
titleA Diagnostic Study of Waves on the Tropopause
typeJournal Paper
journal volume63
journal issue12
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS3800.1
journal fristpage3315
journal lastpage3332
treeJournal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 012
contenttypeFulltext


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