EISCAT observations of plasma patches at sub-auroral cusp latitudes

A sequence of 3 patches of high-density (1012 m−3) cold plasma on a horizontal scale-size of 300–700 km was observed near magnetic noon by the EISCAT VHF radar above Svalbard on 17 December 2001. The patches followed a trajectory towards the cusp inflow region. The combination of radar and all-sky o...

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Published in:Annales Geophysicae
Main Authors: Moen, J., Carlson, H. C., Oksavik, K., Nielsen, C. P., Pryse, S. E., Middleton, H. R., McCrea, I. W., Gallop, P.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2006
Subjects:
Online Access:https://doi.org/10.5194/angeo-24-2363-2006
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00033066 2023-05-15T16:04:35+02:00 EISCAT observations of plasma patches at sub-auroral cusp latitudes Moen, J. Carlson, H. C. Oksavik, K. Nielsen, C. P. Pryse, S. E. Middleton, H. R. McCrea, I. W. Gallop, P. 2006-09 electronic https://doi.org/10.5194/angeo-24-2363-2006 https://noa.gwlb.de/receive/cop_mods_00033066 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033020/angeo-24-2363-2006.pdf https://angeo.copernicus.org/articles/24/2363/2006/angeo-24-2363-2006.pdf eng eng Copernicus Publications Annales Geophysicae -- http://www.bibliothek.uni-regensburg.de/ezeit/?1458425 -- https://www.ann-geophys.net/ -- https://www.ann-geophys.net/volumes.html -- http://link.springer.com/journal/585 -- 1432-0576 https://doi.org/10.5194/angeo-24-2363-2006 https://noa.gwlb.de/receive/cop_mods_00033066 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033020/angeo-24-2363-2006.pdf https://angeo.copernicus.org/articles/24/2363/2006/angeo-24-2363-2006.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2006 ftnonlinearchiv https://doi.org/10.5194/angeo-24-2363-2006 2022-02-08T22:45:57Z A sequence of 3 patches of high-density (1012 m−3) cold plasma on a horizontal scale-size of 300–700 km was observed near magnetic noon by the EISCAT VHF radar above Svalbard on 17 December 2001. The patches followed a trajectory towards the cusp inflow region. The combination of radar and all-sky observations demonstrates that the patches must have been segmented equatorward of the cusp/cleft auroral display, and hence their properties had not yet been influenced by cusp particle showers and electrodynamics on open flux tubes. The last patch in the sequence was intersected by radio tomography observations, and was found to be located adjacent to a broader region of the same high electron density further south. The patches occurred under moderately active conditions (Kp=3) and the total electron content (TEC) of the high-density plasma was 45 TEC units. The train of patches appeared as a segmentation of the tongue of ionization. The sequence of patches occurred in association with a sequence of flow bursts in the dusk cell return flow. It is proposed that reconnection driven pulsed convection is able to create sub-auroral patches in the region where high density mid-latitude plasma is diverted poleward toward the cusp. It is the downward Birkeland current sheet located at the equatorward boundary of the flow disturbance that represents the actual cutting mechanism. Article in Journal/Newspaper EISCAT Svalbard Niedersächsisches Online-Archiv NOA Svalbard Birkeland ENVELOPE(16.587,16.587,68.594,68.594) Annales Geophysicae 24 9 2363 2374
institution Open Polar
collection Niedersächsisches Online-Archiv NOA
op_collection_id ftnonlinearchiv
language English
topic article
Verlagsveröffentlichung
spellingShingle article
Verlagsveröffentlichung
Moen, J.
Carlson, H. C.
Oksavik, K.
Nielsen, C. P.
Pryse, S. E.
Middleton, H. R.
McCrea, I. W.
Gallop, P.
EISCAT observations of plasma patches at sub-auroral cusp latitudes
topic_facet article
Verlagsveröffentlichung
description A sequence of 3 patches of high-density (1012 m−3) cold plasma on a horizontal scale-size of 300–700 km was observed near magnetic noon by the EISCAT VHF radar above Svalbard on 17 December 2001. The patches followed a trajectory towards the cusp inflow region. The combination of radar and all-sky observations demonstrates that the patches must have been segmented equatorward of the cusp/cleft auroral display, and hence their properties had not yet been influenced by cusp particle showers and electrodynamics on open flux tubes. The last patch in the sequence was intersected by radio tomography observations, and was found to be located adjacent to a broader region of the same high electron density further south. The patches occurred under moderately active conditions (Kp=3) and the total electron content (TEC) of the high-density plasma was 45 TEC units. The train of patches appeared as a segmentation of the tongue of ionization. The sequence of patches occurred in association with a sequence of flow bursts in the dusk cell return flow. It is proposed that reconnection driven pulsed convection is able to create sub-auroral patches in the region where high density mid-latitude plasma is diverted poleward toward the cusp. It is the downward Birkeland current sheet located at the equatorward boundary of the flow disturbance that represents the actual cutting mechanism.
format Article in Journal/Newspaper
author Moen, J.
Carlson, H. C.
Oksavik, K.
Nielsen, C. P.
Pryse, S. E.
Middleton, H. R.
McCrea, I. W.
Gallop, P.
author_facet Moen, J.
Carlson, H. C.
Oksavik, K.
Nielsen, C. P.
Pryse, S. E.
Middleton, H. R.
McCrea, I. W.
Gallop, P.
author_sort Moen, J.
title EISCAT observations of plasma patches at sub-auroral cusp latitudes
title_short EISCAT observations of plasma patches at sub-auroral cusp latitudes
title_full EISCAT observations of plasma patches at sub-auroral cusp latitudes
title_fullStr EISCAT observations of plasma patches at sub-auroral cusp latitudes
title_full_unstemmed EISCAT observations of plasma patches at sub-auroral cusp latitudes
title_sort eiscat observations of plasma patches at sub-auroral cusp latitudes
publisher Copernicus Publications
publishDate 2006
url https://doi.org/10.5194/angeo-24-2363-2006
https://noa.gwlb.de/receive/cop_mods_00033066
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033020/angeo-24-2363-2006.pdf
https://angeo.copernicus.org/articles/24/2363/2006/angeo-24-2363-2006.pdf
long_lat ENVELOPE(16.587,16.587,68.594,68.594)
geographic Svalbard
Birkeland
geographic_facet Svalbard
Birkeland
genre EISCAT
Svalbard
genre_facet EISCAT
Svalbard
op_relation Annales Geophysicae -- http://www.bibliothek.uni-regensburg.de/ezeit/?1458425 -- https://www.ann-geophys.net/ -- https://www.ann-geophys.net/volumes.html -- http://link.springer.com/journal/585 -- 1432-0576
https://doi.org/10.5194/angeo-24-2363-2006
https://noa.gwlb.de/receive/cop_mods_00033066
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00033020/angeo-24-2363-2006.pdf
https://angeo.copernicus.org/articles/24/2363/2006/angeo-24-2363-2006.pdf
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op_doi https://doi.org/10.5194/angeo-24-2363-2006
container_title Annales Geophysicae
container_volume 24
container_issue 9
container_start_page 2363
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