Gravity waves in Fabry–Perot measurements made at Mt. John (44°S,170°E), New Zealand
Observations of winds in mesospheric airglow layers have been made at Mt. John (44°S,170°E), New Zealand for some years. We present a modelling study of airglow emissions which shows that the properties of wind detection based on airglow emission means that high-frequency gravity waves are effective...
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Published in | Journal of atmospheric and solar-terrestrial physics Vol. 64; no. 3; pp. 367 - 376 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Elsevier Ltd
01.02.2002
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Subjects | |
Online Access | Get full text |
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