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contributor authorManson, A. H.
contributor authorGregory, J. B.
contributor authorStephenson, D. G.
date accessioned2017-06-09T14:18:24Z
date available2017-06-09T14:18:24Z
date copyright1975/09/01
date issued1975
identifier issn0022-4928
identifier otherams-16898.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152731
description abstractThe results of radiowave, partial reflection drift (wind) measurements from 60?110 km, for the years 1973?74, at Saskatoon, Canada (52°N, 107°W), are presented. Intensive soundings (12 profiles per hour) have provided hourly, weekly and monthly profiles for the prevailing winds and also for the amplitudes of internal gravity (I.G.) waves (τ≈60 min). A relationship between the heights of reversals of the mean flow and of maxima in the I. G. wave amplitude profiles is demonstrated for 1973 and 1974. Hourly changes in the flow are also shown to be consistent with the effects of longer period (τ≈120 min) I. G. waves and/or momentum deposition by I. G. waves (τ?60 min). It is shown that gravity waves are a major contribution to the dynamical and energetic balance of the lower thermosphere (80?110 km).
publisherAmerican Meteorological Society
titleWinds and Wave Motions to 110 km at Mid-Latitudes. IV. Coupling Between Internal Gravity Waves and the Mean Flow
typeJournal Paper
journal volume32
journal issue9
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1975)032<1682:WAWMTK>2.0.CO;2
journal fristpage1682
journal lastpage1688
treeJournal of the Atmospheric Sciences:;1975:;Volume( 032 ):;issue: 009
contenttypeFulltext


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