Gravity wave signatures at mesopause heights

The ALOMAR SOUSY Radar operated at 53.5 MHz has been used in a five-beam configuration to study dynamical processes at gravity wave periods in the summer polar mesosphere. A case study of a gravity wave with a period of about 9 min is presented and analysed in some detail. The three-dimensional...

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Main Authors: R. Rüster, P. Czechowsky, P. Hoffmann, W. Singer
Format: Article
Language:English
Published: Copernicus Publications 1996-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/14/1186/1996/angeo-14-1186-1996.pdf
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author R. Rüster
P. Czechowsky
P. Hoffmann
W. Singer
author_facet R. Rüster
P. Czechowsky
P. Hoffmann
W. Singer
author_sort R. Rüster
collection DOAJ
description The ALOMAR SOUSY Radar operated at 53.5 MHz has been used in a five-beam configuration to study dynamical processes at gravity wave periods in the summer polar mesosphere. A case study of a gravity wave with a period of about 9 min is presented and analysed in some detail. The three-dimensional wave number vector is determined from the phase information of the 9-min velocity oscillations obtained in all beam directions and all range gates. The horizontal wavelengths in the north and east direction are estimated to be about 60 and 50 km, respectively. The echo power variations, simultaneously observed at different beam pointing positions, are investigated using cross-correlation analysis. The results show that these wave-associated variations lead to horizontal and vertical deformation of the echoing layers. The horizontal wavelength in the north-south direction, derived from the echo power modification, is in good agreement with the one obtained from the velocity analysis.
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spelling doaj.art-4eefb02e708c4177b9a2429afedb81d82022-12-22T00:28:41ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761996-11-01141186119110.1007/s00585-996-1186-0Gravity wave signatures at mesopause heightsR. Rüster0P. Czechowsky1P. Hoffmann2W. Singer3Max-Planck-Institut für Aeronomie, Postfach 20, 37189 Katlenburg-Lindau, GermanyMax-Planck-Institut für Aeronomie, Postfach 20, 37189 Katlenburg-Lindau, GermanyInstitut für Atmosphärenphysik der Universität Rostock, Schloßstraße 4-6, 18225 Kühlungsborn, GermanyInstitut für Atmosphärenphysik der Universität Rostock, Schloßstraße 4-6, 18225 Kühlungsborn, GermanyThe ALOMAR SOUSY Radar operated at 53.5 MHz has been used in a five-beam configuration to study dynamical processes at gravity wave periods in the summer polar mesosphere. A case study of a gravity wave with a period of about 9 min is presented and analysed in some detail. The three-dimensional wave number vector is determined from the phase information of the 9-min velocity oscillations obtained in all beam directions and all range gates. The horizontal wavelengths in the north and east direction are estimated to be about 60 and 50 km, respectively. The echo power variations, simultaneously observed at different beam pointing positions, are investigated using cross-correlation analysis. The results show that these wave-associated variations lead to horizontal and vertical deformation of the echoing layers. The horizontal wavelength in the north-south direction, derived from the echo power modification, is in good agreement with the one obtained from the velocity analysis.https://www.ann-geophys.net/14/1186/1996/angeo-14-1186-1996.pdf
spellingShingle R. Rüster
P. Czechowsky
P. Hoffmann
W. Singer
Gravity wave signatures at mesopause heights
Annales Geophysicae
title Gravity wave signatures at mesopause heights
title_full Gravity wave signatures at mesopause heights
title_fullStr Gravity wave signatures at mesopause heights
title_full_unstemmed Gravity wave signatures at mesopause heights
title_short Gravity wave signatures at mesopause heights
title_sort gravity wave signatures at mesopause heights
url https://www.ann-geophys.net/14/1186/1996/angeo-14-1186-1996.pdf
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