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contributor authorJustus, C. G.
contributor authorWoodrum, Arthur
date accessioned2017-06-09T14:17:10Z
date available2017-06-09T14:17:10Z
date copyright1973/10/01
date issued1973
identifier issn0022-4928
identifier otherams-16439.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4152222
description abstractPreviously collected data on atmospheric pressure, density, temperature and winds between 25 and 200 km from sources including Meteorological Rocket Network data, ROBIN falling sphere data, grenade release and pitot tube data, meteor winds, chemical release winds, satellite data, and others were analysed by a daily-difference method, and results on the magnitude of atmospheric perturbations interpreted as gravity waves and planetary waves are presented. Traveling planetary-wave contributions in the 25?85 km range were found to have a significant height and latitudinal variation. It was found that observed gravity-wave density perturbations and wind are related to one another in the manner predicted by gravity-wave theory. It was determined that, on the average, gravity-wave energy deposition or reflection occurs at all altitudes except the 55?75 km region of the mesosphere.
publisherAmerican Meteorological Society
titleUpper Atmospheric Planetary-Wave and Gravity-Wave Observations
typeJournal Paper
journal volume30
journal issue7
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1973)030<1267:UAPWAG>2.0.CO;2
journal fristpage1267
journal lastpage1275
treeJournal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007
contenttypeFulltext


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