摘要
本文研究了2005年8月24日强磁暴(事件A,Dst<200 nT,AE指数平均值为436 nT)与2006年10月28日弱磁暴(事件B,Dst>50 nT,AE指数平均值为320 nT)期间同步轨道高能电子通量的演化过程.LANL和GOES-12卫星观测数据表明:恢复相期间,事件A和事件B中高能电子通量均上升约10倍;随着亚暴持续的发生,Cluster C4卫星均观测到同步轨道存在强烈的哨声波合声模(波强达到10 5nT2/Hz),波幅主要依赖于亚暴AE指数,与Dst指数关联较弱.采用高斯波谱拟合,求解了控制波粒相互作用的Fokker-Planck扩散方程.模拟结果表明:两例事件中的合声模能有效加速1 MeV左右的高能电子,且在高投掷角区域加速作用更加明显;加速时间尺度和幅度与观测数据基本吻合.本文研究为合声模加速辐射带高能电子过程提供了新的观测支持.
引文
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