Thermospheric density structures over the polar regions observed with CHAMP

We report on the unexpected detection of considerable structure in high latitude thermospheric densities, as derived from an accelerometer onboard the CHAMP satellite. The width of the structures, which can either be maxima or minima, varies between a few hundred km and 2000 km. The amplitudes of...

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Main Authors: K. Schlegel, H. Lühr, J.-P. St.-Maurice, G. Crowley, C. Hackert
Format: Article
Language:English
Published: Copernicus Publications 2005-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/23/1659/2005/angeo-23-1659-2005.pdf
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spelling doaj-104e9e151259455184c9a22c10fdc2af2020-11-24T23:55:13ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-07-01231659167210.5194/angeo-23-1659-2005Thermospheric density structures over the polar regions observed with CHAMPK. Schlegel0H. Lühr1J.-P. St.-Maurice2G. Crowley3C. Hackert4Max-Planck-Institut für Sonnensystemforschung, Katlenburg-Lindau, GermanyGeoForschungsZentrum Potsdam, Potsdam, GermanyInstitute for Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, CanadaSouthwest Research Institute, San Antonio, TX, USASouthwest Research Institute, San Antonio, TX, USAWe report on the unexpected detection of considerable structure in high latitude thermospheric densities, as derived from an accelerometer onboard the CHAMP satellite. The width of the structures, which can either be maxima or minima, varies between a few hundred km and 2000 km. The amplitudes of these density extrema can reach 50% of ambient. Maxima cluster around 75° (N and S), while minima are found closer to the poles. In a magnetic latitude-magnetic local time frame the maxima are found mainly around the cusp region. Overall, the observed structures somewhat resemble so-called density cells previously found in model calculations. However the models generate their cells around 140–300 km altitude and show little, if any remnant at 400 km or above. This has to be contrasted with the fact that the CHAMP observations were obtained near 430 km altitude. We have explored Joule heating as a possible mechanism for the generation of the structures, at least in density enhancement regions, using Hall currents measured on CHAMP and simultaneous incoherent scatter measurements with EISCAT. However, the electric fields were usually quite small during the period of observation, making the quest for an explanation for the structures all the more challenging.<br><br> <b>Keywords.</b> Meteorology and atmospheric dynamics (Thermospheric dynamics) – Magnetospheric physics (Polar cap phenomena) – Atmospheric composition and structure (Pressure, density, and temperature)https://www.ann-geophys.net/23/1659/2005/angeo-23-1659-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author K. Schlegel
H. Lühr
J.-P. St.-Maurice
G. Crowley
C. Hackert
spellingShingle K. Schlegel
H. Lühr
J.-P. St.-Maurice
G. Crowley
C. Hackert
Thermospheric density structures over the polar regions observed with CHAMP
Annales Geophysicae
author_facet K. Schlegel
H. Lühr
J.-P. St.-Maurice
G. Crowley
C. Hackert
author_sort K. Schlegel
title Thermospheric density structures over the polar regions observed with CHAMP
title_short Thermospheric density structures over the polar regions observed with CHAMP
title_full Thermospheric density structures over the polar regions observed with CHAMP
title_fullStr Thermospheric density structures over the polar regions observed with CHAMP
title_full_unstemmed Thermospheric density structures over the polar regions observed with CHAMP
title_sort thermospheric density structures over the polar regions observed with champ
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2005-07-01
description We report on the unexpected detection of considerable structure in high latitude thermospheric densities, as derived from an accelerometer onboard the CHAMP satellite. The width of the structures, which can either be maxima or minima, varies between a few hundred km and 2000 km. The amplitudes of these density extrema can reach 50% of ambient. Maxima cluster around 75° (N and S), while minima are found closer to the poles. In a magnetic latitude-magnetic local time frame the maxima are found mainly around the cusp region. Overall, the observed structures somewhat resemble so-called density cells previously found in model calculations. However the models generate their cells around 140–300 km altitude and show little, if any remnant at 400 km or above. This has to be contrasted with the fact that the CHAMP observations were obtained near 430 km altitude. We have explored Joule heating as a possible mechanism for the generation of the structures, at least in density enhancement regions, using Hall currents measured on CHAMP and simultaneous incoherent scatter measurements with EISCAT. However, the electric fields were usually quite small during the period of observation, making the quest for an explanation for the structures all the more challenging.<br><br> <b>Keywords.</b> Meteorology and atmospheric dynamics (Thermospheric dynamics) – Magnetospheric physics (Polar cap phenomena) – Atmospheric composition and structure (Pressure, density, and temperature)
url https://www.ann-geophys.net/23/1659/2005/angeo-23-1659-2005.pdf
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AT gcrowley thermosphericdensitystructuresoverthepolarregionsobservedwithchamp
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