The ionospheric response during an interval of Pc5 ULF wave activity

A preliminary analysis of Pc5, ULF wave activity observed with the IMAGE magnetometer array and the EISCAT UHF radar in the post midnight sector indicates that such waves can be caused by the modulation of the ionospheric conductivity as well as the wave electric field. An observed Pc5 pulsation is...

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Published in:Annales Geophysicae
Main Authors: Lester, M., Davies, J. A., Yeoman, T. K.
Format: Article in Journal/Newspaper
Language:English
Published: SPRINGER VERLAG 2012
Subjects:
Online Access:http://hdl.handle.net/2381/18444
http://www.ann-geophys.net/18/257/2000/angeo-18-257-2000.html
https://doi.org/10.1007/s00585-000-0257-x
id ftleicester:oai:lra.le.ac.uk:2381/18444
record_format openpolar
spelling ftleicester:oai:lra.le.ac.uk:2381/18444 2023-05-15T16:04:33+02:00 The ionospheric response during an interval of Pc5 ULF wave activity Lester, M. Davies, J. A. Yeoman, T. K. 2012-10-24T09:05:34Z http://hdl.handle.net/2381/18444 http://www.ann-geophys.net/18/257/2000/angeo-18-257-2000.html https://doi.org/10.1007/s00585-000-0257-x English eng SPRINGER VERLAG ANNALES GEOPHYSICAE-ATMOSPHERES HYDROSPHERES AND SPACE SCIENCES, 2000, 18 (2), pp. 257-261 0992-7689 http://hdl.handle.net/2381/18444 http://www.ann-geophys.net/18/257/2000/angeo-18-257-2000.html doi:10.1007/s00585-000-0257-x Copyright © European Geosciences Union 2000 Web of Science http://webofknowledge.com Science & Technology Physical Sciences Astronomy & Astrophysics Geosciences Multidisciplinary Meteorology & Atmospheric Sciences Geology ionosphere (electric fields and currents) Magnetospheric physics (magnetosphere-ionosphere interaction MHD waves and instabilities) RADAR OBSERVATIONS NUMBER Journal Article 2012 ftleicester https://doi.org/10.1007/s00585-000-0257-x 2019-03-22T20:16:42Z A preliminary analysis of Pc5, ULF wave activity observed with the IMAGE magnetometer array and the EISCAT UHF radar in the post midnight sector indicates that such waves can be caused by the modulation of the ionospheric conductivity as well as the wave electric field. An observed Pc5 pulsation is divided into three separate intervals based upon the EISCAT data. In the first and third, the Pc5 waves are observed only in the measured electron density between 90 and 112 km and maxima in the electron density at these altitudes are attributed to pulsed precipitation of electrons with energies up to 40 keV which result in the height integrated Hall conductivity being pulsed between 10 and 50 S. In the second interval, the Pc5 wave is observed in the F-region ion temperature, electron density and electron temperature but not in the D and E region electron densities. The analysis suggests that the wave during this interval is a coupled Alfven and compressional mode. 42269 Article in Journal/Newspaper EISCAT University of Leicester: Leicester Research Archive (LRA) Annales Geophysicae 18 2 257 261
institution Open Polar
collection University of Leicester: Leicester Research Archive (LRA)
op_collection_id ftleicester
language English
topic Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
ionosphere (electric fields and currents)
Magnetospheric physics (magnetosphere-ionosphere interaction
MHD waves and instabilities)
RADAR OBSERVATIONS
NUMBER
spellingShingle Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
ionosphere (electric fields and currents)
Magnetospheric physics (magnetosphere-ionosphere interaction
MHD waves and instabilities)
RADAR OBSERVATIONS
NUMBER
Lester, M.
Davies, J. A.
Yeoman, T. K.
The ionospheric response during an interval of Pc5 ULF wave activity
topic_facet Science & Technology
Physical Sciences
Astronomy & Astrophysics
Geosciences
Multidisciplinary
Meteorology & Atmospheric Sciences
Geology
ionosphere (electric fields and currents)
Magnetospheric physics (magnetosphere-ionosphere interaction
MHD waves and instabilities)
RADAR OBSERVATIONS
NUMBER
description A preliminary analysis of Pc5, ULF wave activity observed with the IMAGE magnetometer array and the EISCAT UHF radar in the post midnight sector indicates that such waves can be caused by the modulation of the ionospheric conductivity as well as the wave electric field. An observed Pc5 pulsation is divided into three separate intervals based upon the EISCAT data. In the first and third, the Pc5 waves are observed only in the measured electron density between 90 and 112 km and maxima in the electron density at these altitudes are attributed to pulsed precipitation of electrons with energies up to 40 keV which result in the height integrated Hall conductivity being pulsed between 10 and 50 S. In the second interval, the Pc5 wave is observed in the F-region ion temperature, electron density and electron temperature but not in the D and E region electron densities. The analysis suggests that the wave during this interval is a coupled Alfven and compressional mode. 42269
format Article in Journal/Newspaper
author Lester, M.
Davies, J. A.
Yeoman, T. K.
author_facet Lester, M.
Davies, J. A.
Yeoman, T. K.
author_sort Lester, M.
title The ionospheric response during an interval of Pc5 ULF wave activity
title_short The ionospheric response during an interval of Pc5 ULF wave activity
title_full The ionospheric response during an interval of Pc5 ULF wave activity
title_fullStr The ionospheric response during an interval of Pc5 ULF wave activity
title_full_unstemmed The ionospheric response during an interval of Pc5 ULF wave activity
title_sort ionospheric response during an interval of pc5 ulf wave activity
publisher SPRINGER VERLAG
publishDate 2012
url http://hdl.handle.net/2381/18444
http://www.ann-geophys.net/18/257/2000/angeo-18-257-2000.html
https://doi.org/10.1007/s00585-000-0257-x
genre EISCAT
genre_facet EISCAT
op_source Web of Science
http://webofknowledge.com
op_relation ANNALES GEOPHYSICAE-ATMOSPHERES HYDROSPHERES AND SPACE SCIENCES, 2000, 18 (2), pp. 257-261
0992-7689
http://hdl.handle.net/2381/18444
http://www.ann-geophys.net/18/257/2000/angeo-18-257-2000.html
doi:10.1007/s00585-000-0257-x
op_rights Copyright © European Geosciences Union 2000
op_doi https://doi.org/10.1007/s00585-000-0257-x
container_title Annales Geophysicae
container_volume 18
container_issue 2
container_start_page 257
op_container_end_page 261
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