Evidence of meso-scale structure in the high-latitude thermosphere
There is a widely held assumption that the thermospheric neutral gas is slow to respond to magnetospheric forcing owing to its large inertia and therefore, may be treated as a steady state background medium for the more dynamic ionosphere. This is shown to be over simplistic. The data presented here...
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EUROPEAN GEOPHYSICAL SOCIETY
2001
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ftucl:oai:eprints.ucl.ac.uk.OAI2:9160 2023-05-15T16:04:40+02:00 Evidence of meso-scale structure in the high-latitude thermosphere Aruliah, AL Griffin, E 2001-01 http://discovery.ucl.ac.uk/9160/ unknown EUROPEAN GEOPHYSICAL SOCIETY open ANN GEOPHYS-GERMANY , 19 (1) 37 - 46. (2001) atmospheric composition and structure (airglow and aurora instruments and techniques) ionosphere (ionosphere-atmosphere interactions) GEOMAGNETIC POLAR-CAP SOLAR-CYCLE NEUTRAL WINDS FIELD TEMPERATURES IONOSPHERE MINIMUM MODEL Article 2001 ftucl 2016-01-14T23:56:49Z There is a widely held assumption that the thermospheric neutral gas is slow to respond to magnetospheric forcing owing to its large inertia and therefore, may be treated as a steady state background medium for the more dynamic ionosphere. This is shown to be over simplistic. The data presented here compare direct measurements of the thermospheric neutral winds made in Northern Scandinavia by Fabry-Perot Interferometers (FPIs) with direct measurements of the ionosphere made by the EISCAT radar and with model simulations. These comparisons will show that the neutral atmosphere is capable of responding to ionospheric changes on meso-scale levels, i.e., spatial and temporal scale sizes of less than a few hundred kilometres and tens of minutes, respectively. Article in Journal/Newspaper EISCAT University College London: UCL Discovery |
institution |
Open Polar |
collection |
University College London: UCL Discovery |
op_collection_id |
ftucl |
language |
unknown |
topic |
atmospheric composition and structure (airglow and aurora instruments and techniques) ionosphere (ionosphere-atmosphere interactions) GEOMAGNETIC POLAR-CAP SOLAR-CYCLE NEUTRAL WINDS FIELD TEMPERATURES IONOSPHERE MINIMUM MODEL |
spellingShingle |
atmospheric composition and structure (airglow and aurora instruments and techniques) ionosphere (ionosphere-atmosphere interactions) GEOMAGNETIC POLAR-CAP SOLAR-CYCLE NEUTRAL WINDS FIELD TEMPERATURES IONOSPHERE MINIMUM MODEL Aruliah, AL Griffin, E Evidence of meso-scale structure in the high-latitude thermosphere |
topic_facet |
atmospheric composition and structure (airglow and aurora instruments and techniques) ionosphere (ionosphere-atmosphere interactions) GEOMAGNETIC POLAR-CAP SOLAR-CYCLE NEUTRAL WINDS FIELD TEMPERATURES IONOSPHERE MINIMUM MODEL |
description |
There is a widely held assumption that the thermospheric neutral gas is slow to respond to magnetospheric forcing owing to its large inertia and therefore, may be treated as a steady state background medium for the more dynamic ionosphere. This is shown to be over simplistic. The data presented here compare direct measurements of the thermospheric neutral winds made in Northern Scandinavia by Fabry-Perot Interferometers (FPIs) with direct measurements of the ionosphere made by the EISCAT radar and with model simulations. These comparisons will show that the neutral atmosphere is capable of responding to ionospheric changes on meso-scale levels, i.e., spatial and temporal scale sizes of less than a few hundred kilometres and tens of minutes, respectively. |
format |
Article in Journal/Newspaper |
author |
Aruliah, AL Griffin, E |
author_facet |
Aruliah, AL Griffin, E |
author_sort |
Aruliah, AL |
title |
Evidence of meso-scale structure in the high-latitude thermosphere |
title_short |
Evidence of meso-scale structure in the high-latitude thermosphere |
title_full |
Evidence of meso-scale structure in the high-latitude thermosphere |
title_fullStr |
Evidence of meso-scale structure in the high-latitude thermosphere |
title_full_unstemmed |
Evidence of meso-scale structure in the high-latitude thermosphere |
title_sort |
evidence of meso-scale structure in the high-latitude thermosphere |
publisher |
EUROPEAN GEOPHYSICAL SOCIETY |
publishDate |
2001 |
url |
http://discovery.ucl.ac.uk/9160/ |
genre |
EISCAT |
genre_facet |
EISCAT |
op_source |
ANN GEOPHYS-GERMANY , 19 (1) 37 - 46. (2001) |
op_rights |
open |
_version_ |
1766400280019075072 |