Upper Atmospheric Planetary-Wave and Gravity-Wave ObservationsSource: Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007::page 1267DOI: 10.1175/1520-0469(1973)030<1267:UAPWAG>2.0.CO;2Publisher: American Meteorological Society
Abstract: Previously 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.
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contributor author | Justus, C. G. | |
contributor author | Woodrum, Arthur | |
date accessioned | 2017-06-09T14:17:10Z | |
date available | 2017-06-09T14:17:10Z | |
date copyright | 1973/10/01 | |
date issued | 1973 | |
identifier issn | 0022-4928 | |
identifier other | ams-16439.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4152222 | |
description abstract | Previously 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. | |
publisher | American Meteorological Society | |
title | Upper Atmospheric Planetary-Wave and Gravity-Wave Observations | |
type | Journal Paper | |
journal volume | 30 | |
journal issue | 7 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1973)030<1267:UAPWAG>2.0.CO;2 | |
journal fristpage | 1267 | |
journal lastpage | 1275 | |
tree | Journal of the Atmospheric Sciences:;1973:;Volume( 030 ):;issue: 007 | |
contenttype | Fulltext |