CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH

The EISCAT radar has provided data for a comprehensive study of the high—latitude trough in electron concentration, which occurs in the auroral zone. In this paper the characteristics of the trough are illustrated, the method of its formation is outlined and important features of the trough are desc...

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Main Author: Dyfed Sy
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.694.6813
http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.694.6813 2023-05-15T16:04:36+02:00 CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH Dyfed Sy The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.694.6813 http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.694.6813 http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf text ftciteseerx 2016-01-08T18:34:41Z The EISCAT radar has provided data for a comprehensive study of the high—latitude trough in electron concentration, which occurs in the auroral zone. In this paper the characteristics of the trough are illustrated, the method of its formation is outlined and important features of the trough are described. A large upward velocity along the geomagnetic field line is shown to play a significant role in the formation of the trough. The large ion— neutral difference velocities which initiate the formation of the trough may also drive the plasma into a non—thermal state which should be taken into account during the analysis of incoherent scatter data. Text EISCAT Unknown
institution Open Polar
collection Unknown
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language English
description The EISCAT radar has provided data for a comprehensive study of the high—latitude trough in electron concentration, which occurs in the auroral zone. In this paper the characteristics of the trough are illustrated, the method of its formation is outlined and important features of the trough are described. A large upward velocity along the geomagnetic field line is shown to play a significant role in the formation of the trough. The large ion— neutral difference velocities which initiate the formation of the trough may also drive the plasma into a non—thermal state which should be taken into account during the analysis of incoherent scatter data.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Dyfed Sy
spellingShingle Dyfed Sy
CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
author_facet Dyfed Sy
author_sort Dyfed Sy
title CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
title_short CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
title_full CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
title_fullStr CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
title_full_unstemmed CHARACTERISTICS OF THE HIGH-LATITUDE TROUGH
title_sort characteristics of the high-latitude trough
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.694.6813
http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf
genre EISCAT
genre_facet EISCAT
op_source http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.694.6813
http://www.eiscat.rl.ac.uk/Members/mike/publications/pdfs/1990/63_Jonesetal_1990.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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