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Observations of the quasi 2-day wave from the High Resolution Doppler Imager on UARSA strong westward traveling oscillation, with a period of 2 days and zonal wave number 3, is observed in the mesospheric and lower thermospheric winds from the High Resolution Doppler Imager (HRDI) on the Upper Atmosphere Research Satellite (UARS). The important events happen in January, July, and September/October, of which the occurrence in January is the strongest with an amplitude over 60 m/s. Detailed analyses for the periods of January 1992 and January 1993 reveal a cause-and-effect relationship in the wave developing process at 95 km. The global structures of the wave amplitude and phase are also presented.
Document ID
19950047211
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Wu, D. L.
(Univ. of Michigan, Ann Arbor, MI United States)
Hays, P. B.
(Univ. of Michigan, Ann Arbor, MI United States)
Skinner, W. R.
(Univ. of Michigan, Ann Arbor, MI United States)
Marshall, A. R.
(Univ. of Michigan, Ann Arbor, MI United States)
Burrage, M. D.
(Univ. of Michigan, Ann Arbor, MI United States)
Lieberman, R. S.
(Univ. of Michigan, Ann Arbor, MI United States)
Ortland, D. A.
(Univ. of Michigan, Ann Arbor, MI United States)
Date Acquired
August 16, 2013
Publication Date
December 23, 1993
Publication Information
Publication: Geophysical Research Letters
Volume: 20
Issue: 24
ISSN: 0094-8276
Subject Category
Geophysics
Accession Number
95A78810
Funding Number(s)
CONTRACT_GRANT: NAS5-27751
Distribution Limits
Public
Copyright
Other

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