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PHYSICS OF MAGNETOSPHERIC POLAR CAP BY ANALYSIS OF FIELD-ALIGNED CURRENTS.

PHYSICS OF MAGNETOSPHERIC POLAR CAP BY ANALYSIS OF FIELD-ALIGNED CURRENTS.
通过磁场对准电流分析来了解磁层极盖的物理学。
批准号:
61540305
负责人:
IIJIMA Takesi
金额:
$1.22万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for General Scientific Research (C)
财政年份:
1986
资助国家:
日本
项目状态:
已结题
起止时间:
1986 至 1988

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中文摘要
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英文摘要
I have obtained new knowledge on magnetospheric physics, by analyzing the geomagnetic field data that was acquired with various artificial satellites, which includes the following:1. Large-scale field-aligned current systems associated with northward interplanetary magnetic field (NBZ current system).The NBZ field-aligned currents are thought to flow so as to transfer the sunward plasma stress down to the polar cap ionosphere so that large-scale sunward plasma convection is maintained in the central polar-cap plasma domain. The acquisition of this sunward plasma stress from the interplanetary medium is thought to take place in the magnetospheric high-latitude boundary layer often called the plasma mantle.2. Large-scale Region 1 and Region 2 field-aligned current systems.The region 1 current system is thought to originated in the magnetospheric voltage generator, whereas the region 2 current system is ascribable to the combination of the voltage generator and current generator.3. Large-scale magnetospheric equatorial currents.The electric current flowing parallel to and near the geomagnetic equatorial plane is comprised of an azimuthal current flowing westward and a radial current flowing toward the earth in the evening sector and away from the earth in the morning sector. These horizontal currents exhibit a net positive divergence (source) in the evening sector and a net negative divergence (sink) in the morning sector. The location, flow direction and the intensities of these divergent currents are almost identical with those of the region 2 field-aligned current system. The westward ring current and the region 2 current system are closely connected.4. Substorm-associated field-aligned currents.The three-dimensional current system throughout the course of substorm is not solely ascribable to a diversion of magnetospheric cross-tail current but a development of radial current is essental.
期刊论文(19)
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会议论文
T.IIJIMA: Journal of Geophysical Research. 92. 2408 (1987)
T.IIJIMA:地球物理研究杂志。
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T.IIJIMA: Transactions, American Geophysical Union. 68. 1423 (1987)
T.IIJIMA:《交易》,美国地球物理联盟。
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T.IIJIMA.: AURORAL PHYSICS edited by C.-I.MENG Cambridge univ.Press. (1989)
T.IIJIMA.:AURORAL PHYSICS 由 C.-I.MENG 剑桥大学出版社编辑。
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T.IIJIMA: Journal of Geophysical Research. (1989)
T.IIJIMA:地球物理研究杂志。
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16
    Study of Magnetospheric Substorms : Present and Perspective
    • 批准号:
      02302027
    • 项目类别:
      Grant-in-Aid for Co-operative Research (A)
    • 资助金额:
      $6.66万
    • 财政年份:
      1990
    • 负责人:
      IIJIMA Takesi
    • 依托单位:
    STUDY OF MAGNETOSPHERIC PHYSICS BASED UPON THE DATA ACQUIRED WITH SATELLITES
    • 批准号:
      01044035
    • 项目类别:
      Grant-in-Aid for Overseas Scientific Survey.
    • 资助金额:
      $0.0万
    • 财政年份:
      1989
    • 负责人:
      IIJIMA Takesi
    • 依托单位:
    Coupling of magnetospheric and field-aligned currents by satellite-based observations
    • 批准号:
      01540348
    • 项目类别:
      Grant-in-Aid for General Scientific Research (C)
    • 资助金额:
      $1.15万
    • 财政年份:
      1989
    • 负责人:
      IIJIMA Takesi
    • 依托单位: