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ULF waves in the outer magnetosphere: Geotail observation 1 transverse waves

机译:外磁层中的ULF波:地尾观测1横向波

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A survey of ULF waves in the Pc 5 frequency range during the six year period (1995-2000) has been made for the field line resonance waves in the outer magnetosphere,using plasma flow and magnetic field measurements with the Geotail spacecraft. On the morning side a series of wave trains often appears during several hours. In contrast such a series of wave trains with a long duration is rarely observed in the afternoon to evening sector. Most of waves in the afternoon sector are isolated,of which duration is approximately one hour. The existence of a set of preferential frequencies and the pronounced dawn-dusk asymmetry of wave occurrence and wave features,which were found in ground-based and ionospheric measurements of geomagnetic ULF pulsations,were statistically confirmed. It is also noted that the background plasma flow is sunward in the evening sector without exception. Transverse waves are generally observed in the condition of plasma β below 1.5. Highβ cases are mostly associated with events on the dusk side. As for the relation to solar wind conditions,Pc 5 waves tend to occur under the condition of more radial than the average IMF spiral angle,or of low cone angle.
机译:利用Geotail航天器的等离子流和磁场测量,对外磁层中的磁力线共振波在六年周期(1995-2000年)内对Pc 5频率范围内的ULF波进行了调查。在早上,经常在几个小时内出现一系列波浪列车。相反,在下午到晚上,很少会观察到这样一系列持续时间长的波列。下午的大部分海浪是孤立的,持续时间约为一小时。从统计上证实了在地磁和电离层地磁ULF脉动测量中发现的一组优先频率的存在以及显着的波发生和波特征的黎明-黄昏不对称性。还应注意的是,背景血浆流在傍晚时分都是朝阳的。通常在血浆β低于1.5的条件下观察到横向波。高β病例主要与黄昏事件有关。至于与太阳风条件的关系,Pc 5波倾向于在比平均IMF螺旋角更大的径向或较低锥角的条件下发生。

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