Physics of Auroral Phenomena

Abstract. On February 16, 2003 EISCAT-Heating experiment was carried out on observation of heating induced disturbances in the magnetosphere. A pump wave of 4.04 MHz in X-mode was used for the ionosphere modification from 19:55 to 23:59:59 UT in square modulation regime with 5 minutes ON / 5 minutes...

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Main Authors: A B Pashin, A L Kotikov, T Yeoman, M T Rietveld, M I Pudovkin, A A Mochalov, A Maulini, S Shibkov, Yu A Kopytenko
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.2460
http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1048.2460 2023-05-15T16:04:48+02:00 Physics of Auroral Phenomena A B Pashin A L Kotikov T Yeoman M T Rietveld M I Pudovkin A A Mochalov A Maulini S Shibkov Yu A Kopytenko The Pennsylvania State University CiteSeerX Archives 2004 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.2460 http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.2460 http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf text 2004 ftciteseerx 2020-04-05T00:22:37Z Abstract. On February 16, 2003 EISCAT-Heating experiment was carried out on observation of heating induced disturbances in the magnetosphere. A pump wave of 4.04 MHz in X-mode was used for the ionosphere modification from 19:55 to 23:59:59 UT in square modulation regime with 5 minutes ON / 5 minutes OFF cycle. During the interval of good conjugation of CLUSTER with the heating facility spacecraft 4 (Tango) recorded clear variations of electric field at modulation frequency lasting around 30 minutes. Spectral peak of the variations at 1.67 mHz is more pronounced in the y-component. Slow temporal variations of the conductivity in the heated volume due to electron density increasing in the E-region related with the heating duty cycle provide the same variations of disturbed electric field. Polarization of the disturbances is almost linear; it corresponds to constant ratio of Hall to Pedersen conductivity variations. The analysis of the signal waveform shows that at ~ 23.30 UT the phase of the variations is changed together with a sign of DC electric field. The transverse size of the disturbed structure in the magnetosphere is near 0.1 R E . The observed behavior of the disturbances may be interpreted in terms of Alfven mode propagation of the disturbed ionospheric electric field into the magnetosphere. The electric field disturbances being uniform in the region of modified conductivity have a discontinuity at its border of the region and decay as two-dimensional dipole outside it. Field-aligned currents are related with conductivity gradients and distinct magnetic field variations are clear seen in quick-look plots around 20.30 UT. For further study of this event records of magnetic variations onboard CLUSTER satellites would be very important. Text EISCAT Unknown Pedersen ENVELOPE(140.013,140.013,-66.668,-66.668) The ''Y'' ENVELOPE(-112.453,-112.453,57.591,57.591)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Abstract. On February 16, 2003 EISCAT-Heating experiment was carried out on observation of heating induced disturbances in the magnetosphere. A pump wave of 4.04 MHz in X-mode was used for the ionosphere modification from 19:55 to 23:59:59 UT in square modulation regime with 5 minutes ON / 5 minutes OFF cycle. During the interval of good conjugation of CLUSTER with the heating facility spacecraft 4 (Tango) recorded clear variations of electric field at modulation frequency lasting around 30 minutes. Spectral peak of the variations at 1.67 mHz is more pronounced in the y-component. Slow temporal variations of the conductivity in the heated volume due to electron density increasing in the E-region related with the heating duty cycle provide the same variations of disturbed electric field. Polarization of the disturbances is almost linear; it corresponds to constant ratio of Hall to Pedersen conductivity variations. The analysis of the signal waveform shows that at ~ 23.30 UT the phase of the variations is changed together with a sign of DC electric field. The transverse size of the disturbed structure in the magnetosphere is near 0.1 R E . The observed behavior of the disturbances may be interpreted in terms of Alfven mode propagation of the disturbed ionospheric electric field into the magnetosphere. The electric field disturbances being uniform in the region of modified conductivity have a discontinuity at its border of the region and decay as two-dimensional dipole outside it. Field-aligned currents are related with conductivity gradients and distinct magnetic field variations are clear seen in quick-look plots around 20.30 UT. For further study of this event records of magnetic variations onboard CLUSTER satellites would be very important.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author A B Pashin
A L Kotikov
T Yeoman
M T Rietveld
M I Pudovkin
A A Mochalov
A Maulini
S Shibkov
Yu A Kopytenko
spellingShingle A B Pashin
A L Kotikov
T Yeoman
M T Rietveld
M I Pudovkin
A A Mochalov
A Maulini
S Shibkov
Yu A Kopytenko
Physics of Auroral Phenomena
author_facet A B Pashin
A L Kotikov
T Yeoman
M T Rietveld
M I Pudovkin
A A Mochalov
A Maulini
S Shibkov
Yu A Kopytenko
author_sort A B Pashin
title Physics of Auroral Phenomena
title_short Physics of Auroral Phenomena
title_full Physics of Auroral Phenomena
title_fullStr Physics of Auroral Phenomena
title_full_unstemmed Physics of Auroral Phenomena
title_sort physics of auroral phenomena
publishDate 2004
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.2460
http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf
long_lat ENVELOPE(140.013,140.013,-66.668,-66.668)
ENVELOPE(-112.453,-112.453,57.591,57.591)
geographic Pedersen
The ''Y''
geographic_facet Pedersen
The ''Y''
genre EISCAT
genre_facet EISCAT
op_source http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1048.2460
http://pgia.ru:81/seminar/archive/2004/3_waves/pashin.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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