The Shape of Strongly Disturbed Dayside Magnetopause

During strong geomagnetic disturbances, the Earth¡¦s magnetosphere exhibits unusual and nonlinear interaction with the incident flow of magnetized solar wind plasma. Global Magneto-hydro-dynamic (MHD) modeling of the magnetosphere predicts that the storm-time effects at the magnetopause result from...

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Main Author: Alexei V. Dmitriev Alla V. Suvorova
Format: Article
Language:English
Published: Chinese Geoscience Union 2013-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v242p225.pdf
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spelling doaj-39a80808577948eda21f3b9c9e8a45d82020-11-24T22:14:43ZengChinese Geoscience UnionTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802013-01-0124222510.3319/TAO.2012.09.26.02(SEC)1126The Shape of Strongly Disturbed Dayside MagnetopauseAlexei V. Dmitriev Alla V. SuvorovaDuring strong geomagnetic disturbances, the Earth¡¦s magnetosphere exhibits unusual and nonlinear interaction with the incident flow of magnetized solar wind plasma. Global Magneto-hydro-dynamic (MHD) modeling of the magnetosphere predicts that the storm-time effects at the magnetopause result from the abnormal plasma transport and/or extremely strong field aligned currents. In-situ observations of the magnetospheric boundary, magnetopause, by Geosynchronous Operational Environmental Satellite (GOES) allowed us to find experimentally such effects as a saturation of the dayside reconnection, unusual bluntness and prominent duskward skewing of the nose magnetopause. The saturation and duskward skewing were attributed to the storm-time magnetopause formation under strong southward interplanetary magnetic field (IMF). The unusual bluntness was observed during both high solar wind pressure and strong southward IMF. We suggest that these phenomena are caused by a substantial contribution of the cross-tail current magnetic field and the hot magnetospheric plasma from the asymmetrical ring current into the pressure balance at the dayside magnetopause. http://tao.cgu.org.tw/images/attachments/v242p225.pdf MagnetopauseMagnetospheric currentsGeomagnetic storm
collection DOAJ
language English
format Article
sources DOAJ
author Alexei V. Dmitriev Alla V. Suvorova
spellingShingle Alexei V. Dmitriev Alla V. Suvorova
The Shape of Strongly Disturbed Dayside Magnetopause
Terrestrial, Atmospheric and Oceanic Sciences
Magnetopause
Magnetospheric currents
Geomagnetic storm
author_facet Alexei V. Dmitriev Alla V. Suvorova
author_sort Alexei V. Dmitriev Alla V. Suvorova
title The Shape of Strongly Disturbed Dayside Magnetopause
title_short The Shape of Strongly Disturbed Dayside Magnetopause
title_full The Shape of Strongly Disturbed Dayside Magnetopause
title_fullStr The Shape of Strongly Disturbed Dayside Magnetopause
title_full_unstemmed The Shape of Strongly Disturbed Dayside Magnetopause
title_sort shape of strongly disturbed dayside magnetopause
publisher Chinese Geoscience Union
series Terrestrial, Atmospheric and Oceanic Sciences
issn 1017-0839
2311-7680
publishDate 2013-01-01
description During strong geomagnetic disturbances, the Earth¡¦s magnetosphere exhibits unusual and nonlinear interaction with the incident flow of magnetized solar wind plasma. Global Magneto-hydro-dynamic (MHD) modeling of the magnetosphere predicts that the storm-time effects at the magnetopause result from the abnormal plasma transport and/or extremely strong field aligned currents. In-situ observations of the magnetospheric boundary, magnetopause, by Geosynchronous Operational Environmental Satellite (GOES) allowed us to find experimentally such effects as a saturation of the dayside reconnection, unusual bluntness and prominent duskward skewing of the nose magnetopause. The saturation and duskward skewing were attributed to the storm-time magnetopause formation under strong southward interplanetary magnetic field (IMF). The unusual bluntness was observed during both high solar wind pressure and strong southward IMF. We suggest that these phenomena are caused by a substantial contribution of the cross-tail current magnetic field and the hot magnetospheric plasma from the asymmetrical ring current into the pressure balance at the dayside magnetopause.
topic Magnetopause
Magnetospheric currents
Geomagnetic storm
url http://tao.cgu.org.tw/images/attachments/v242p225.pdf
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