On the entry and transit of high-density plasma across the polar cap
[1] Observations are presented from SuperDARN and the EISCAT Svalbard Radar of two intense polar cap patch events on 6 February 2001. The interplanetary magnetic field (IMF) was dominated by a large positive By component, and for both events the electron density exceeded 1012 m−3 in the F region. Wi...
Published in: | Journal of Geophysical Research: Space Physics |
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Language: | English |
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American Geophysical Union (AGU); Wiley
2012
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Online Access: | http://hdl.handle.net/2381/19090 http://onlinelibrary.wiley.com/doi/10.1029/2010JA015817/abstract https://doi.org/10.1029/2010JA015817 |
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ftleicester:oai:lra.le.ac.uk:2381/19090 2023-05-15T16:04:37+02:00 On the entry and transit of high-density plasma across the polar cap Oksavik, K. Barth, V. L. Moen, J. Lester, M. 2012-10-24T09:06:20Z http://hdl.handle.net/2381/19090 http://onlinelibrary.wiley.com/doi/10.1029/2010JA015817/abstract https://doi.org/10.1029/2010JA015817 English eng American Geophysical Union (AGU); Wiley Journal of Geophysical Research-SPACE PHYSICS, 2010, 115 0148-0227 http://hdl.handle.net/2381/19090 http://onlinelibrary.wiley.com/doi/10.1029/2010JA015817/abstract doi:10.1029/2010JA015817 Copyright © 2010 by the American Geophysical Union. All rights reserved. Archived with reference to Usage Permissions granted to authors, available at http://publications.agu.org/author-resource-center/usage-permissions/ Web of Science http://webofknowledge.com Science & Technology Physical Sciences Astronomy & Astrophysics GRADIENT DRIFT INSTABILITY F-LAYER PATCHES MAGNETOPAUSE RECONNECTION RATE SMALL-SCALE IRREGULARITIES DAYSIDE AURORAL ACTIVITY HIGH-LATITUDE CONVECTION EISCAT SVALBARD RADAR NORTH MAGNETIC-POLE HF-RADAR SUBSTORM CYCLES Journal Article 2012 ftleicester https://doi.org/10.1029/2010JA015817 2019-03-22T20:16:51Z [1] Observations are presented from SuperDARN and the EISCAT Svalbard Radar of two intense polar cap patch events on 6 February 2001. The interplanetary magnetic field (IMF) was dominated by a large positive By component, and for both events the electron density exceeded 1012 m−3 in the F region. With SuperDARN we tracked the events all the way across the polar cap, from the dayside Svalbard sector to the nightside Alaska sector. The flow speed was highly dynamic and pulsed, and both patches underwent substantial rotation in the polar cap. On the nightside the leading edge had become the trailing edge. It suggests that the first patch to enter the polar cap on the dayside may not always be the first patch to reach the nightside; plasma might be stagnant in the polar cap or even overtaken. The study also provides evidence that momentum transfer in the dayside polar cap can last significantly longer than 10 min after reconnection, especially for extremely long field lines where IMF By is dominating, i.e., on “old open field lines.” Knowledge of the solar wind driver and the coupling processes is therefore extremely important for predicting the motion of a polar cap patch event across the polar cap. Gradients in the plasma flow associated with the rotation of the extreme density may in itself lead to a stronger growth of ionospheric irregularities. These irregularities may continue to grow all the way across the polar cap. The result is more efficient creation of ionospheric irregularities. Peer-reviewed Publisher Version 44193 Article in Journal/Newspaper EISCAT North Magnetic Pole Svalbard Alaska University of Leicester: Leicester Research Archive (LRA) Svalbard Journal of Geophysical Research: Space Physics 115 A12 n/a n/a |
institution |
Open Polar |
collection |
University of Leicester: Leicester Research Archive (LRA) |
op_collection_id |
ftleicester |
language |
English |
topic |
Science & Technology Physical Sciences Astronomy & Astrophysics GRADIENT DRIFT INSTABILITY F-LAYER PATCHES MAGNETOPAUSE RECONNECTION RATE SMALL-SCALE IRREGULARITIES DAYSIDE AURORAL ACTIVITY HIGH-LATITUDE CONVECTION EISCAT SVALBARD RADAR NORTH MAGNETIC-POLE HF-RADAR SUBSTORM CYCLES |
spellingShingle |
Science & Technology Physical Sciences Astronomy & Astrophysics GRADIENT DRIFT INSTABILITY F-LAYER PATCHES MAGNETOPAUSE RECONNECTION RATE SMALL-SCALE IRREGULARITIES DAYSIDE AURORAL ACTIVITY HIGH-LATITUDE CONVECTION EISCAT SVALBARD RADAR NORTH MAGNETIC-POLE HF-RADAR SUBSTORM CYCLES Oksavik, K. Barth, V. L. Moen, J. Lester, M. On the entry and transit of high-density plasma across the polar cap |
topic_facet |
Science & Technology Physical Sciences Astronomy & Astrophysics GRADIENT DRIFT INSTABILITY F-LAYER PATCHES MAGNETOPAUSE RECONNECTION RATE SMALL-SCALE IRREGULARITIES DAYSIDE AURORAL ACTIVITY HIGH-LATITUDE CONVECTION EISCAT SVALBARD RADAR NORTH MAGNETIC-POLE HF-RADAR SUBSTORM CYCLES |
description |
[1] Observations are presented from SuperDARN and the EISCAT Svalbard Radar of two intense polar cap patch events on 6 February 2001. The interplanetary magnetic field (IMF) was dominated by a large positive By component, and for both events the electron density exceeded 1012 m−3 in the F region. With SuperDARN we tracked the events all the way across the polar cap, from the dayside Svalbard sector to the nightside Alaska sector. The flow speed was highly dynamic and pulsed, and both patches underwent substantial rotation in the polar cap. On the nightside the leading edge had become the trailing edge. It suggests that the first patch to enter the polar cap on the dayside may not always be the first patch to reach the nightside; plasma might be stagnant in the polar cap or even overtaken. The study also provides evidence that momentum transfer in the dayside polar cap can last significantly longer than 10 min after reconnection, especially for extremely long field lines where IMF By is dominating, i.e., on “old open field lines.” Knowledge of the solar wind driver and the coupling processes is therefore extremely important for predicting the motion of a polar cap patch event across the polar cap. Gradients in the plasma flow associated with the rotation of the extreme density may in itself lead to a stronger growth of ionospheric irregularities. These irregularities may continue to grow all the way across the polar cap. The result is more efficient creation of ionospheric irregularities. Peer-reviewed Publisher Version 44193 |
format |
Article in Journal/Newspaper |
author |
Oksavik, K. Barth, V. L. Moen, J. Lester, M. |
author_facet |
Oksavik, K. Barth, V. L. Moen, J. Lester, M. |
author_sort |
Oksavik, K. |
title |
On the entry and transit of high-density plasma across the polar cap |
title_short |
On the entry and transit of high-density plasma across the polar cap |
title_full |
On the entry and transit of high-density plasma across the polar cap |
title_fullStr |
On the entry and transit of high-density plasma across the polar cap |
title_full_unstemmed |
On the entry and transit of high-density plasma across the polar cap |
title_sort |
on the entry and transit of high-density plasma across the polar cap |
publisher |
American Geophysical Union (AGU); Wiley |
publishDate |
2012 |
url |
http://hdl.handle.net/2381/19090 http://onlinelibrary.wiley.com/doi/10.1029/2010JA015817/abstract https://doi.org/10.1029/2010JA015817 |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
EISCAT North Magnetic Pole Svalbard Alaska |
genre_facet |
EISCAT North Magnetic Pole Svalbard Alaska |
op_source |
Web of Science http://webofknowledge.com |
op_relation |
Journal of Geophysical Research-SPACE PHYSICS, 2010, 115 0148-0227 http://hdl.handle.net/2381/19090 http://onlinelibrary.wiley.com/doi/10.1029/2010JA015817/abstract doi:10.1029/2010JA015817 |
op_rights |
Copyright © 2010 by the American Geophysical Union. All rights reserved. Archived with reference to Usage Permissions granted to authors, available at http://publications.agu.org/author-resource-center/usage-permissions/ |
op_doi |
https://doi.org/10.1029/2010JA015817 |
container_title |
Journal of Geophysical Research: Space Physics |
container_volume |
115 |
container_issue |
A12 |
container_start_page |
n/a |
op_container_end_page |
n/a |
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1766400225877950464 |