Structure and kinetic properties of plasmoids and their boundary regions

被引:53
作者
Mukai, T
Fujimoto, M
Hoshino, M
Kokubun, S
Machida, S
Maezawa, K
Nishida, A
Saito, Y
Terasawa, T
Yamamoto, T
机构
[1] NAGOYA UNIV,DEPT PHYS,CHIKUSA KU,NAGOYA,AICHI 464,JAPAN
[2] NAGOYA UNIV,SOLAR TERR ENVIRONM LAB,TOYOKAWA,AICHI 442,JAPAN
[3] KYOTO UNIV,INST GEOPHYS,KYOTO 606,JAPAN
[4] UNIV TOKYO,DEPT EARTH & PLANETARY PHYS,TOKYO 113,JAPAN
来源
JOURNAL OF GEOMAGNETISM AND GEOELECTRICITY | 1996年 / 48卷 / 5-6期
关键词
D O I
10.5636/jgg.48.541
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Based on GEOTAIL/LEP observations in the distant magnetotail, this paper reports on several new features of velocity distribution functions of electrons and ions within a plasmoid and at its boundary. Here we use the term 'plasmoid' in a wider meaning than usual in spite of the presence of significant magnetic B-y fields. In the lobe, as expected from MHD simulations of magnetic reconnection processes, cold plasmas are pushed away from the plasma sheet before the arrival of plasmoids, while after the plasmoid passage the convection is enhanced toward the normal direction to the plasma sheet. The cold ions flow into the plasmoid along magnetic field lines, are heated and accelerated perpendicularly at the boundary, and finally merge with hot plasmas deeper inside the plasmoids. Deep inside plasmoids, however, the ion distribution functions often show the existence of counterstreaming ion beams, while the simultaneously measured electron distribution functions show a flat-top distribution. It is noted that the presence of the counterstreaming ions is a fine structure along magnetic field lines inside the whole distribution convecting tailward with speeds of 500-900 km/s. The relative velocity of the two components along the magnetic field line reaches 1000-1500 km/s, which is much higher than the local Alfven speed. Each component has an anisotropic distribution with respect to its center in the velocity space; the perpendicular temperature is several times higher than the parallel temperature. We conclude that these counterstreaming ions are most likely of lobe origin, and they have not had time enough for thermalization. They might have entered the plasmoid from the northern and southern lobes, being heated and accelerated through slow-mode shocks at the boundaries. Hence, these field lines are open, and both ends are connected to the northern and southern lobes. This phenomenon is observed predominantly in the latter part of the plasmoid after southward turning of the magnetic field, especially after the plasma bulk speed has increased stepwise and the B-y/B-z field magnitudes have attained the peak value. It is also observed even near the neutral sheet, where the magnetic B-x field is very small, but significant B-y and/or B-z fields exist. Since the tailward flow speed becomes faster associated with the above phenomenon, these open field lines would be draped around the leading (core) part of plasmoids. The compression due to the draping may increase the field intensity.
引用
收藏
页码:541 / 560
页数:20
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