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Pc3-4 ULF waves observed by Cluster prenoon in outer magnetosphere

机译:外磁层团簇正午观测到的Pc3-4 ULF波

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Pc3-4 pulsations generally result from field line resonance in the inner magnetosphere or guided Alfven waves in the outer magnetosphere. Regular Pc3-4 pulsations were observed over 0700-1100UT on 13 April 2004 by the Cluster constellation of four satellites on an outbound leg from L∼5.9 to L∼11.1 near 10 MLT in the high latitude cusp region. The waves were mainly transverse with toroidal and poloidal components, and frequency decreasing with increasing L-value, from ∼25 mHz to ∼10mHz. The magnitude of toroidal mode waves significantly increased with L-value, reaching a maximum close to the magnetopause. The poloidal mode did not show the same increase. The waves propagated earthward and westward, perpendicular to the geomagnetic field direction. Furthermore, the sense of polarization was variable, clearly changed from left-hand to right-hand at a crossing point identified by the interval where the main wave packet occurred near the magnetopause. The Poynting flux was in range of 0.04∼0.07mW/m nearly perpendicular to the magnetic field vector. The wave properties were also correlated with the solar wind parameters. We conclude that the Pc3-4 waves observed adjacent to the magnetopause are field line resonances, driven by the upstream fast waves.
机译:Pc3-4脉动通常是由内部磁层中的磁力线共振或外部磁层中的Alfven引导波引起的。 2004年4月13日在0700-1100UT上方观测到有规律的Pc3-4脉动,这是由四颗卫星的星群组成的,在高纬度尖端地区的10 MLT附近,从L〜5.9到L〜11.1的出站腿上。这些波主要是横向的,具有环形和极向分量,并且频率随着L值的增加而降低,从〜25 mHz到〜10mHz。环形波的强度随着L值的增加而显着增加,达到接近磁绝经的最大值。极向模式没有显示出相同的增加。这些波垂直于地磁场方向向地球和向西传播。此外,极化的感觉是可变的,在主波包在磁绝经附近发生的间隔所确定的交叉点处,从左手到右手明显改变。 Poynting磁通量几乎垂直于磁场矢量,范围为0.04-0.07mW / m。波浪性质也与太阳风参数相关。我们得出的结论是,邻近磁层顶的Pc3-4波是场线共振,由上游快速波驱动。

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