Investigation of Magnetic Reconnection in Space Plasma
Investigation of Magnetic Reconnection in Space Plasma
批准号:
07044105
负责人:
NISHIDA Atsuhiro
金额:
$3.46万
依托单位国家:
日本
项目类别:
Grant-in-Aid for international Scientific Research
财政年份:
1995
资助国家:
日本
项目状态:
已结题
起止时间:
1995 至 1996
中文摘要
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英文摘要
Magnetic reconnection processes have been studied in detail on the hasis of analysis of the GEOTAIL data obtained in the geomagnetic tail at distances of 10 to 30 Re away from the Earth. Collaborative studies with US satellites of WIND and POLAR and with Russian satellite Interball-Tail were highly useful to elucidate the reconnection processes in substorms. A number of important results have been brought forth, which have been (and will be) published in scientific journals. Some selected results are listed below.1.The GEOTAIL observations have revealed the kinetic structure of slow-mode shocks exising between the lobe-plasma sheet boundary in the geomagnetic tail. Based on detiled analysis of the ion distribution functions, it is found taht 3-20 % of the heating of cold ions passing through the slow-mode shock occurs in the foreshock region. Interaction with the electromagnetic ion cyclotron waves generated by the counterstreaming ion beams was suggested as a candidate of this heating … More .2.The GEOTAIL observations have found the existence of ion beams of the lobe origin streaming along the magnetic field lines deep inside plasmoids, as evidence of the plasmoid formation by magnetic reconnections. The existence of non-gyrotropic ion beams is also found in a region which is considered as near the diffusion region. These observational results agree well with those of computer simulations of magnetic reconnections.3.Based collaborative studies of GEOTAIL with WIND and POLAR satellites, it is found that the magnetic reconnection was initiated in the plasma sheet at distances of -25 Re downtail prior to a substorm onset, suggesting that the reconnections trigger substorms at least in some cases.4.Joint studies between GEOTAIL and Interball-Tail data have evidence that magnetic reconnections took place in the plasma sheet at distances between 13 and 28 Re downtail.5.Statistical analysis of fast plasma flows has revealed that magnetic reconnections occur around midnight to the duskside in the magnetotail at distances of 20 to 30 Re in association with substorm onset, and the reconnection region is widened in the dawndusk direction as it moves downtail. Less
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M.Hirahara and T.Terasawa: "Cold ion streams Consisting of Double Proton Populations and Singly-Charged Oxygen Observed at the Distant Magnetopause by Geotail : A Case Study" J.Geophys.Res. 102. 2359-2372 (1997)
M.Hirahara 和 T.Terasawa:“Geotail 在遥远磁层顶观测到的由双质子群和单电荷氧组成的冷离子流:案例研究”J.Geophys.Res。
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M.Fijimoto,et al.: "Plasma Entry from the Flanks of the Near-Earth Magnetotail : GEOTAIL Observations in the Dawnside LLBL and the Plasma Sheet" J.Geomag.Geoelectr.48. 711-728 (1996)
M.Fijimoto 等人:“从近地磁尾侧面进入的等离子体:Dawnside LLBL 和等离子体片中的 GEOTAIL 观测”J.Geomag.Geolectr.48。
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H.Shirai and K.Maezawa: "Drop-off of the polar rain flux near the plasma sheet boundary" J.Geophys.Res.102. 2271-2278 (1997)
H.Shirai 和 K.Maezawa:“等离子层边界附近极地雨通量的下降”J.Geophys.Res.102。
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S.Kokubun.et al.: "Quasi-Periodic Oscillations of the Magnetopause during Northward Sheath Magnetic Field" Geophys.Res.Lett.21. 2883-2886 (1994)
S.Kokubun.et al.:“北向鞘磁场期间磁层顶的准周期振荡”Geophys.Res.Lett.21。
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D.H.Fairfield,et al.: "Geotail Observations of an Unusual Magnetotail under Very Northward IMF Conditions" J.Geomag.Geoelectr.48. 473-488 (1996)
D.H.Fairfield 等人:“极北 IMF 条件下异常磁尾的 Geotail 观测”J.Geomag.Geolectr.48。
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Investigation of the Geomagnetic Tail by the GEOTAIL Satellite
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批准号:04044168
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项目类别:Grant-in-Aid for international Scientific Research
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资助金额:$16.0万
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财政年份:1992
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负责人:NISHIDA Atsuhiro
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依托单位:
海外基金