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Some Aspects of General Circulation and Tides in the Middle AtmosphereData from several sources suggest that between 100 and 200 km in the middle atmosphere, a layer of anomalous circulation must be situated, at least in middle latitudes. The mechanisms responsible for the circulation anomaly in this height region are discussed in terms of hydrodynamic equations. The current state of atmospheric tidal theory is also addressed.
Document ID
19850012160
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Ivanovskiy, A. I. (Institute of Applied Geophysics Moscow, Ussr)
Date Acquired
August 12, 2013
Publication Date
May 1, 1984
Publication Information
Publication: International Council of Scientific Unions Middle Atmosphere Program. Handbook for MAP, Vol. 10
Subject Category
Geophysics
Accession Number
85N20470
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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IDRelationTitle19850012140Collected WorksMiddle Atmosphere Program. Handbook for MAP, Volume 10
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