Three Dimensional Computer Modeling of Magnetospheric Substorm

Magnetospheric substorm in the magnetotail region is studied numericallu by means of a three dimensional MHD code. The analytic solution for the quiet magnetotail is employed as an initial configuration. The localized solar wind is modeled to enter the simulation domain through the boundaries locate...

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Main Author: Kyoung W. Min
Format: Article
Language:English
Published: Korean Space Science Society (KSSS) 1989-06-01
Series:Journal of Astronomy and Space Sciences
Online Access:http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/1989/v6n1/OJOOBS_1989_v6n1_1.pdf
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spelling doaj-71bf7c9be5c54dcaacde00d1b476dcdd2020-11-24T20:41:22ZengKorean Space Science Society (KSSS)Journal of Astronomy and Space Sciences2093-55872093-14091989-06-0161115Three Dimensional Computer Modeling of Magnetospheric SubstormKyoung W. Min0Korea Institute of Technology, Taejon 302-338, KoreaMagnetospheric substorm in the magnetotail region is studied numericallu by means of a three dimensional MHD code. The analytic solution for the quiet magnetotail is employed as an initial configuration. The localized solar wind is modeled to enter the simulation domain through the boundaries located in the magnetotail lobe region. As a result of the interaction between the solar wind and the magnetosphere, the magnetic field lines are stretched, and the plasma sheet becomes thinner and thinner. When the current driven resistivity is generated, magnetic reconnection is triggered by this resistivity. The resulting plasma jetting is found to be supper-magnetosonic. Although the plasmoid formation and its tailward motion is not quite clear as in the two dimensional simulation, which is mainly because of the numerical model chosen for the present simulation, the rarification of the plasmas near the x-point is observed. Field aligned currents are observed in the late expansive stage of the magnetospheric substorm. These field aligned currents flow from the tail toward the ionosphere on the dawn side and from the ionosphere toward the tail on the dusk side, namely in the same sense of the region 1 current. As the field aligned currents develop, it is found that the cross tail current in the earth side midnight section of the magnetic x-point is reduced.http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/1989/v6n1/OJOOBS_1989_v6n1_1.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Kyoung W. Min
spellingShingle Kyoung W. Min
Three Dimensional Computer Modeling of Magnetospheric Substorm
Journal of Astronomy and Space Sciences
author_facet Kyoung W. Min
author_sort Kyoung W. Min
title Three Dimensional Computer Modeling of Magnetospheric Substorm
title_short Three Dimensional Computer Modeling of Magnetospheric Substorm
title_full Three Dimensional Computer Modeling of Magnetospheric Substorm
title_fullStr Three Dimensional Computer Modeling of Magnetospheric Substorm
title_full_unstemmed Three Dimensional Computer Modeling of Magnetospheric Substorm
title_sort three dimensional computer modeling of magnetospheric substorm
publisher Korean Space Science Society (KSSS)
series Journal of Astronomy and Space Sciences
issn 2093-5587
2093-1409
publishDate 1989-06-01
description Magnetospheric substorm in the magnetotail region is studied numericallu by means of a three dimensional MHD code. The analytic solution for the quiet magnetotail is employed as an initial configuration. The localized solar wind is modeled to enter the simulation domain through the boundaries located in the magnetotail lobe region. As a result of the interaction between the solar wind and the magnetosphere, the magnetic field lines are stretched, and the plasma sheet becomes thinner and thinner. When the current driven resistivity is generated, magnetic reconnection is triggered by this resistivity. The resulting plasma jetting is found to be supper-magnetosonic. Although the plasmoid formation and its tailward motion is not quite clear as in the two dimensional simulation, which is mainly because of the numerical model chosen for the present simulation, the rarification of the plasmas near the x-point is observed. Field aligned currents are observed in the late expansive stage of the magnetospheric substorm. These field aligned currents flow from the tail toward the ionosphere on the dawn side and from the ionosphere toward the tail on the dusk side, namely in the same sense of the region 1 current. As the field aligned currents develop, it is found that the cross tail current in the earth side midnight section of the magnetic x-point is reduced.
url http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/1989/v6n1/OJOOBS_1989_v6n1_1.pdf
work_keys_str_mv AT kyoungwmin threedimensionalcomputermodelingofmagnetosphericsubstorm
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