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On the interaction between gravity waves and the OH Meinel (6-2) and the O sub 2 atmospheric (0-1) bands in the polar night airglow

Journal Article · · Journal of Geophysical Research; (USA)
;  [1]
  1. Univ. of Alaska, Fairbanks (USA)
The effect of gravity waves on the OH (6-2) and O{sub 2} (0-1) airglow emissions was examined using spectroscopic airglow data from Longyearbyen, Svalbard (78{degree}N), and Fairbanks, Alaska (64{degree}N). The analysis was done by fitting a synthetic spectrum to the data to infer the rotational temperature as well as the band intensity of each of the emissions. Quasiperiodic fluctuations in the band intensity and rotational temperature are assumed to be a result of modifications of a stable airglow layer by gravity waves. The relationship of the fluctuations in band intensity to rotational temperature may be expressed in terms of the parameters {eta}, which is defined as the ratio of the amplitudes of the fluctuations in intensity and temperature, and {theta}, which is the phase angle between the fluctuations in intensity and temperature. These parameters were observed to vary with wave period for both the OH and O{sub 2} emissions. The variations in {eta}(OH) and {theta}(OH) agreed fairly well with the most recent models for waves with periods of about 1 hour or longer. None of the models agree with the observed values of {eta}(OH) and {theta}(OH) for short-period waves. For the O{sub 2} emissions, the observed values of {eta}(O{sub 2}) is generally 180{degree} which is expected from first-order linear gravity wave theory.
OSTI ID:
5914903
Journal Information:
Journal of Geophysical Research; (USA), Journal Name: Journal of Geophysical Research; (USA) Vol. 94:A5; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English