首页> 外文期刊>Journal of Geophysical Research. Biogeosciences >Geotail observations of low-frequency waves from 0.001 to 16 Hz during the November 24, 1996, Geospace Environment Modeling substorm challenge event
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Geotail observations of low-frequency waves from 0.001 to 16 Hz during the November 24, 1996, Geospace Environment Modeling substorm challenge event

机译:在1996年11月24日,Geospace Environment Modeling亚暴挑战事件中对0.001至16 Hz低频波的地尾观测

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We present observations of low-frequency waves from 0.001 Hz up to the lower hybrid frequency during the time periods corresponding to the growth, expansion, and recovery phases of a substorm that occurred from similar to 2100 to 2310 UT on November 24, 1996, while Geotail was located in the magnetotail at X-GSE similar to 25 R-E and 0100 LT. Large-amplitude waves near the lower hybrid frequency were observed when large-scale density and magnetic field gradients were present during thinning of the plasma sheet at substorm onset and the beginning of the recovery phase. Later in the recovery phase, waves near the lower hybrid frequency were observed close to the neutral sheet in localized areas with strong small-scale density and magnetic field gradients. Fluctuations of the electric and magnetic fields near the ion gyrofrequency were also observed during this event; however, the amplitudes were smaller than those often observed in the near tail in association with substorms. Compressional fluctuations of the magnetic field in the Pi2 frequency range were observed close to substorm onset. Although Geotail was not in the region considered in recent studies of Pi2 pulsations, it may still be possible that the magnetic field fluctuations observed by Geotail during the November 24, 1996, substorm are related to this phenomenon since little is known about propagation of the compressional pulses and generation of the waves. [References: 26]
机译:我们呈现了在与1996年11月24日的2100至2310 UT类似的亚暴的生长,扩展和恢复阶段相对应的时间段内,从0.001 Hz到较低的混合频率的低频波的观测结果,而Geotail位于X-GSE的磁尾中,类似于25 RE和0100 LT。在亚暴开始和恢复阶段开始时,在等离子薄片变薄期间出现大规模密度和磁场梯度时,观察到了较低混合频率附近的大振幅波。在恢复阶段的后期,在具有强小尺度密度和磁场梯度的局部区域中,靠近中性板附近观察到了较低混合频率附近的波。在此事件中,还观察到了离子陀螺频率附近的电场和磁场的波动。但是,其振幅小于与亚暴有关的近尾部经常观察到的振幅。观察到Pi2频率范围内的磁场压缩波动接近亚暴雨发作。尽管在最近的Pi2脉动研究中并未考虑Geotail,但Geotail在1996年11月24日亚暴期间观察到的磁场波动仍可能与这种现象有关,因为对压缩空气的传播知之甚少脉冲和波浪的产生。 [参考:26]

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