The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes

The VHF radar system at Aberystwyth (52.4° N, 4.1°E) has been used to make high-time-resolution, multi-beam observations of mesospheric summer echo layers. These show that the altitude and the sense of vertical movement of the layers can vary over time-scales of minutes and horizontal scales of...

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Main Authors: D. A. Hooper, L. Thomas
Format: Article
Language:English
Published: Copernicus Publications 1997-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/15/1037/1997/angeo-15-1037-1997.pdf
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author D. A. Hooper
L. Thomas
author_facet D. A. Hooper
L. Thomas
author_sort D. A. Hooper
collection DOAJ
description The VHF radar system at Aberystwyth (52.4° N, 4.1°E) has been used to make high-time-resolution, multi-beam observations of mesospheric summer echo layers. These show that the altitude and the sense of vertical movement of the layers can vary over time-scales of minutes and horizontal scales of kilometres. In general, the altitude profiles of signal-to-noise ratio provide evidence of a bifurcated structure with sharp changes in the horizontal wind vector and vertical velocity, and enhanced spectral width occurring at the bifurcation level. The implications of the small-scale structure for studies of the aspect sensitivity of radar returns are discussed, and the changes in wind-field at the bifurcation level are compared with 'wind corners' observed in rocket studies of the mesosphere at polar latitudes.
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spelling doaj.art-f85e71230f4c42a8a0bf286f9e0026032022-12-21T19:11:32ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761997-08-01151037104710.1007/s00585-997-1037-7The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudesD. A. Hooper0L. Thomas1Department of Physics, University of Wales, Aberystwyth, SY23 3Bz, UKDepartment of Physics, University of Wales, Aberystwyth, SY23 3Bz, UKThe VHF radar system at Aberystwyth (52.4° N, 4.1°E) has been used to make high-time-resolution, multi-beam observations of mesospheric summer echo layers. These show that the altitude and the sense of vertical movement of the layers can vary over time-scales of minutes and horizontal scales of kilometres. In general, the altitude profiles of signal-to-noise ratio provide evidence of a bifurcated structure with sharp changes in the horizontal wind vector and vertical velocity, and enhanced spectral width occurring at the bifurcation level. The implications of the small-scale structure for studies of the aspect sensitivity of radar returns are discussed, and the changes in wind-field at the bifurcation level are compared with 'wind corners' observed in rocket studies of the mesosphere at polar latitudes.https://www.ann-geophys.net/15/1037/1997/angeo-15-1037-1997.pdf
spellingShingle D. A. Hooper
L. Thomas
The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
Annales Geophysicae
title The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
title_full The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
title_fullStr The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
title_full_unstemmed The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
title_short The small-scale structure of VHF mesospheric summer echo layers observed at mid-latitudes
title_sort small scale structure of vhf mesospheric summer echo layers observed at mid latitudes
url https://www.ann-geophys.net/15/1037/1997/angeo-15-1037-1997.pdf
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