Coupling of magnetospheric and field-aligned currents by satellite-based observations
Coupling of magnetospheric and field-aligned currents by satellite-based observations
批准号:
01540348
负责人:
IIJIMA Takesi
金额:
$1.15万
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:
1989
资助国家:
日本
项目状态:
已结题
起止时间:
1989 至 1991
中文摘要
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英文摘要
Electric current flowing in the near-equatorial magnetosphere(L--4-9 R_E)consists of two basic elements : azimuthal current and radial current. Azimuthal current flows westward around the earth. Radial current flows toward the earth in the late-evening to premidnight sector and away from the earth in the midnight to early-morning sector.Presence of magnetospheric radial current is consistent with the counter current of ionosphere Pedersen current at auroral latitudes that is projected in the magnetospheric equatorial plane.Inhomogenuity in azimuthal and radial current associates field-aligned current(FAC)and forms a three-dimensional current loop, respectively. Region 1 FAC and Region 2 FAC that are determined at low altitudes, manifest the superimposed, resultant effect of these current loops.During the substorm growth phase, ion plasma sheet that was inferred from the precipitating particles, consists of core part and cleft-like part. In the ion core part domain, enhanced westward azimuthal current loop associates Region 2-sense FAC and furthermore radial current loop causes Region 2 plus Region 1-sense FAC in pair. In the domain of ion cleft-like part, Region 1-sense FAC is associated with the convective flow vorticity in the near equatorial magnetotail. Whereas, in the expansion phase, disruption occurs rapidly in the preceding(growth phase), enhanced westward current and the growth phase-ion core part trns into the explosive part. Region 1-sense FAC is associated with this current disruption and reversed-Region I sense FAC(and/or multiple current shetts)is also associated, pole-ward of and adjacent-to the disruption region. The ion core part shifts far equator-ward and associates Region 2-sense FAC, and c upled Region 2 plus Region 1 FAC there.
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IIJIMA, T.: "The relationship between ion and electron precipitation patterns and field-aligned current systems during a substorm" Magnetospheric Substorms. Geophysical Monograph 64, American Geophysical Union. 92-110 (1991)
IIJIMA, T.:“亚暴期间离子和电子沉淀模式与场对准电流系统之间的关系”磁层亚暴。
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Takesi IIJIMA: "AGU Monograph “Magnetospheric Substorms" ーー Relationship between three distinctive parts comprised in ion and electron precipitation and fieldーaligned currents during substorm." American Geophysical Union, 300 (1991)
Takesi IIjima:“AGU 专着“磁层亚暴”- 亚暴期间离子和电子沉淀以及场对准电流中三个独特部分之间的关系。”美国地球物理联盟,300 (1991)
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Ohtani,S.: "Tail current disruption in the geosynchronous region." "Magnetospheric Substorms" Geophysical Monograph,American Geophysical Union. 64. 131-140 (1991)
Ohtani,S.:“地球同步区域的尾流中断。”
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AKASOFU, S. -I.: "Agreements between ground-based and satellite-based observations" Planet. Space Sci.38. 1533-1540 (1990)
AKASOFU, S. -I.:“地面和卫星观测之间的协议”星球。
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T.Iijima: "Large-scale characteristics of magnetospheric equatorial currents." Journal of Geophysical Research. 95. (1990)
T.Iijima:“磁层赤道流的大尺度特征。”
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共 27 条
Study of Magnetospheric Substorms : Present and Perspective
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批准号:02302027
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项目类别:Grant-in-Aid for Co-operative Research (A)
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资助金额:$6.66万
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财政年份:1990
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负责人:IIJIMA Takesi
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依托单位:
STUDY OF MAGNETOSPHERIC PHYSICS BASED UPON THE DATA ACQUIRED WITH SATELLITES
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批准号:01044035
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项目类别:Grant-in-Aid for Overseas Scientific Survey.
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资助金额:$0.0万
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财政年份:1989
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负责人:IIJIMA Takesi
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依托单位:
PHYSICS OF MAGNETOSPHERIC POLAR CAP BY ANALYSIS OF FIELD-ALIGNED CURRENTS.
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批准号:61540305
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项目类别:Grant-in-Aid for General Scientific Research (C)
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资助金额:$1.22万
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财政年份:1986
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负责人:IIJIMA Takesi
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依托单位: