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Spectral characteristics of protons in the Earth's plasmasheet: statistical results from Cluster CIS and RAPID

机译:地球等离子薄片中质子的光谱特征:CIS和RAPID簇的统计结果

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We present a study of the spectral characteristics ofprotons in the Earth's plasma sheet for various geomagnetic disturbance levels. The study isbased on about 5400 h of data combined from the Cluster RAPID and CISinstruments obtained during the tail season (July–October). The overall proton spectral shapeis generally that of a κ distribution, that is, resembling a Maxwellian at lower energieswhich smoothly merges into a power-law tail at higher energies.The actual spectral long-term slope depends on various magnetospheric driver parameters,but is on average around 3.5–4. During disturbed conditions, such as geomagnetic stormor substorm periods, a shift in the characteristic energy is observed. For two individual storms,we also found a hardening of the spectra.Unlike the electron spectra, we do not see any significant local time dependence in the spectral slope,but we find higher average ion fluxes in the dusk side.We also do not find any direct response in the energy spectra to changes in the interplanetarymagnetic field or solar wind dynamic pressure. This suggests that energization ofthe ions are mainly due to internal processes in the plasma sheet.
机译:我们对各种地磁干扰水平的地球等离子薄片中质子的光谱特征进行了研究。这项研究基于大约5400小时的数据,这些数据来自于尾季(7月至10月)中的Cluster RAPID和CIS仪器。整体质子光谱形状通常是κ分布的形状,即在较低能量下类似于麦克斯韦方程,在较高能量下平滑地融合为幂律尾部。实际的光谱长期斜率取决于各种磁层驱动参数,但在平均约3.5–4。在受干扰的条件下,例如地磁风暴或亚暴雨时期,可以观察到特征能量的变化。对于两个单独的风暴,我们还发现了光谱的硬化。与电子光谱不同,我们在光谱斜率中没有看到任何明显的本地时间依赖性,但是在黄昏侧发现了更高的平均离子通量。我们也没有发现能量谱中对星际磁场或太阳风动压变化的任何直接响应。这表明离子的激发主要是由于等离子片中的内部过程。

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