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contributor authorMILLER, ALVIN J.
date accessioned2017-06-09T15:59:48Z
date available2017-06-09T15:59:48Z
date copyright1971/12/01
date issued1971
identifier issn0027-0644
identifier otherams-58381.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198821
description abstractThe modulation of the vertical flux of kinetic energy to the stratosphere by the pressure-work effect at 100 mb is compared with variations in the hemispheric kinetic energy, the horizontal momentum and heat transports at ?low? latitudes, and the tropical zonal wind and temperature for the lower stratosphere. It is deduced that the variation of the vertical flux of geopotential is in phase with the kinetic energy in the lower stratosphere and is statistically related to the time rate of change of the horizontal transports of heat and momentum at 30°N. The association of these results to the general circulation of the lower stratosphere is considered.
publisherAmerican Meteorological Society
titleKINETIC ENERGY AND QUASI-BIENNIAL OSCILLATION
typeJournal Paper
journal volume99
journal issue12
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1971)099<0912:KEAQO>2.3.CO;2
journal fristpage912
journal lastpage918
treeMonthly Weather Review:;1971:;volume( 099 ):;issue: 012
contenttypeFulltext


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