Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence

Neutral thermospheric wind pattern at high latitudes obtained from cross-track acceleration measurements of the CHAMP satellite above both polar regions are used to deduce statistical neutral wind vorticity distributions and were analyzed in their dependence on the Interplanetary Magnetic Field...

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Main Authors: M. Förster, S. E. Haaland, E. Doornbos
Format: Article
Language:English
Published: Copernicus Publications 2011-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/29/181/2011/angeo-29-181-2011.pdf
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spelling doaj-d4cd04b69c2c4417b0e13fdcb5a02ead2020-11-25T00:52:44ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762011-01-012918118610.5194/angeo-29-181-2011Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependenceM. Förster0S. E. Haaland1S. E. Haaland2E. Doornbos3GFZ German Research Centre for Geosciences, Helmholtz Centre Potsdam, GermanyMax-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, GermanyDepartment of Physics and Technology, University of Bergen, NorwayDelft Institute for Earth Observation and Space Systems (DEOS), Delft, The NetherlandsNeutral thermospheric wind pattern at high latitudes obtained from cross-track acceleration measurements of the CHAMP satellite above both polar regions are used to deduce statistical neutral wind vorticity distributions and were analyzed in their dependence on the Interplanetary Magnetic Field (IMF). The average pattern confirms the large duskside anticyclonic vortex seen in the average wind pattern and reveals a cyclonic vorticity on the dawnside, which is almost equal in magnitude to the duskside minimum. The outer shape of the vorticity pattern agrees approximately with the outer boundary of region-1 currents in the well-known average current distributions of Iijima and Potemra (1976) The IMF dependence of the vorticity pattern resembles the characteristic FAC and ionospheric plasma drift pattern known from various statistical studies obtained under the same sorting conditions.https://www.ann-geophys.net/29/181/2011/angeo-29-181-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Förster
S. E. Haaland
S. E. Haaland
E. Doornbos
spellingShingle M. Förster
S. E. Haaland
S. E. Haaland
E. Doornbos
Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
Annales Geophysicae
author_facet M. Förster
S. E. Haaland
S. E. Haaland
E. Doornbos
author_sort M. Förster
title Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
title_short Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
title_full Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
title_fullStr Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
title_full_unstemmed Thermospheric vorticity at high geomagnetic latitudes from CHAMP data and its IMF dependence
title_sort thermospheric vorticity at high geomagnetic latitudes from champ data and its imf dependence
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2011-01-01
description Neutral thermospheric wind pattern at high latitudes obtained from cross-track acceleration measurements of the CHAMP satellite above both polar regions are used to deduce statistical neutral wind vorticity distributions and were analyzed in their dependence on the Interplanetary Magnetic Field (IMF). The average pattern confirms the large duskside anticyclonic vortex seen in the average wind pattern and reveals a cyclonic vorticity on the dawnside, which is almost equal in magnitude to the duskside minimum. The outer shape of the vorticity pattern agrees approximately with the outer boundary of region-1 currents in the well-known average current distributions of Iijima and Potemra (1976) The IMF dependence of the vorticity pattern resembles the characteristic FAC and ionospheric plasma drift pattern known from various statistical studies obtained under the same sorting conditions.
url https://www.ann-geophys.net/29/181/2011/angeo-29-181-2011.pdf
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AT sehaaland thermosphericvorticityathighgeomagneticlatitudesfromchampdataanditsimfdependence
AT sehaaland thermosphericvorticityathighgeomagneticlatitudesfromchampdataanditsimfdependence
AT edoornbos thermosphericvorticityathighgeomagneticlatitudesfromchampdataanditsimfdependence
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