Midlatitude TEC enhancements during the October 2003 superstorm

[1] We use observations from the array of North American GPS receivers to examine the formation and severity of midlatitude enhancements and steep gradients in total electron content (TEC) during the October 30–31, 2003 superstorm. A large (∼10x) enhancement in dayside TEC was observed over the US m...

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Main Authors: Foster, John C, Rideout, William C
Other Authors: Haystack Observatory
Format: Article
Language:en_US
Published: American Geophysical Union (AGU) 2018
Online Access:http://hdl.handle.net/1721.1/114705
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author Foster, John C
Rideout, William C
author2 Haystack Observatory
author_facet Haystack Observatory
Foster, John C
Rideout, William C
author_sort Foster, John C
collection MIT
description [1] We use observations from the array of North American GPS receivers to examine the formation and severity of midlatitude enhancements and steep gradients in total electron content (TEC) during the October 30–31, 2003 superstorm. A large (∼10x) enhancement in dayside TEC was observed over the US mainland during these events as Dst decreased sharply and strong SAPS electric fields eroded the outer reaches of the post‐noon plasmasphere boundary layer (PBL) forming poleward‐streaming plumes of storm enhanced density. TEC increased to >250 TECu equatorward of the PBL. TEC gradients across the PBL over the central US exceeded 60 TECu per deg latitude. While intense, these features are qualitatively similar to those seen in lesser storms.
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spelling mit-1721.1/1147052022-09-26T17:37:09Z Midlatitude TEC enhancements during the October 2003 superstorm Foster, John C Rideout, William C Haystack Observatory Foster, John C Foster, John C Rideout, William C [1] We use observations from the array of North American GPS receivers to examine the formation and severity of midlatitude enhancements and steep gradients in total electron content (TEC) during the October 30–31, 2003 superstorm. A large (∼10x) enhancement in dayside TEC was observed over the US mainland during these events as Dst decreased sharply and strong SAPS electric fields eroded the outer reaches of the post‐noon plasmasphere boundary layer (PBL) forming poleward‐streaming plumes of storm enhanced density. TEC increased to >250 TECu equatorward of the PBL. TEC gradients across the PBL over the central US exceeded 60 TECu per deg latitude. While intense, these features are qualitatively similar to those seen in lesser storms. 2018-04-13T16:17:53Z 2018-04-13T16:17:53Z 2005-04 2004-12 Article http://purl.org/eprint/type/JournalArticle 0094-8276 http://hdl.handle.net/1721.1/114705 Foster, J. C., and W. Rideout. “Midlatitude TEC Enhancements During the October 2003 Superstorm.” Geophysical Research Letters 32, 12 (April 2005): L12S04 © 2005 American Geophysical Union en_US http://dx.doi.org/10.1029/2004GL021719 Geophysical Research Letters Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Geophysical Union (AGU) John C. Foster
spellingShingle Foster, John C
Rideout, William C
Midlatitude TEC enhancements during the October 2003 superstorm
title Midlatitude TEC enhancements during the October 2003 superstorm
title_full Midlatitude TEC enhancements during the October 2003 superstorm
title_fullStr Midlatitude TEC enhancements during the October 2003 superstorm
title_full_unstemmed Midlatitude TEC enhancements during the October 2003 superstorm
title_short Midlatitude TEC enhancements during the October 2003 superstorm
title_sort midlatitude tec enhancements during the october 2003 superstorm
url http://hdl.handle.net/1721.1/114705
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