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contributor authorManson, A. H.
contributor authorMeek, C. E.
date accessioned2017-06-09T14:27:51Z
date available2017-06-09T14:27:51Z
date copyright1987/12/01
date issued1987
identifier issn0022-4928
identifier otherams-19701.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155847
description abstractThe wind field of the middle atmosphere (60-100 kin) is sampled by the Saskatoon Medium Frequency radar: temporal resolution is normally 5 rain, and vertical is 1.5/3 kin. Profiles are analyzed for gravity waves (GW), and periods r from 10 rain-10 h are measured, with 3,z > 2 km and amplitudes > 5 m s-. The profiles are quite similar to those from rocket soundings. Wind vector shears are also consistent with "wind corners" evident in recent rocket data. Vertical shears of the horizontal wind and GW amplitudes (10 < r < 60 rain)are calculated and shown as annual height-time cross sections; values near 60 km are compared with rocket data from nearby Primrose Lake. Regions favoring dynamic and convective instability and GW saturation are located. The scattered radar power is shown as a seasonal cross section and compared to the shear and GW features. Finally, the dissipation rate of GW kinetic energy is calculated and compared with related MF radar and rocket wind estimations.
publisherAmerican Meteorological Society
titleSmall-Scale Features in the Middle Atmosphere Wind Field at Saskatoon, Canada(52°N, 107°W): An Analysis of MF Radar Data with Rocket Comparisons
typeJournal Paper
journal volume44
journal issue24
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1987)044<3661:SSFITM>2.0.CO;2
journal fristpage3661
journal lastpage3672
treeJournal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 024
contenttypeFulltext


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