波粒相互作用导致环电流质子沉降的卫星共轭观测

王杰, 袁志刚, 余雄东, 薛祖祥. 2020. 波粒相互作用导致环电流质子沉降的卫星共轭观测. 地球物理学报, 63(6): 2131-2140, doi: 10.6038/cjg2020N0313
引用本文: 王杰, 袁志刚, 余雄东, 薛祖祥. 2020. 波粒相互作用导致环电流质子沉降的卫星共轭观测. 地球物理学报, 63(6): 2131-2140, doi: 10.6038/cjg2020N0313
WANG Jie, YUAN ZhiGang, YU XiongDong, XUE ZuXiang. 2020. Precipitation of ring current protons caused by wave-particle interactions with satellite conjugated observation. Chinese Journal of Geophysics (in Chinese), 63(6): 2131-2140, doi: 10.6038/cjg2020N0313
Citation: WANG Jie, YUAN ZhiGang, YU XiongDong, XUE ZuXiang. 2020. Precipitation of ring current protons caused by wave-particle interactions with satellite conjugated observation. Chinese Journal of Geophysics (in Chinese), 63(6): 2131-2140, doi: 10.6038/cjg2020N0313

波粒相互作用导致环电流质子沉降的卫星共轭观测

  • 基金项目:

    国家自然科学基金(41874194,41374168,41521063)资助

详细信息
    作者简介:

    王杰, 男, 1995年生, 硕士研究生, 主要从事电离层磁层物理方面的研究.E-mail:w-jie@whu.edu.cn

    通讯作者: 袁志刚, 男, 1974年生, 教授, 主要从事电离层磁层耦合方面的研究.E-mail:y_zgang@vip.163.com
  • 中图分类号: P354;P353

Precipitation of ring current protons caused by wave-particle interactions with satellite conjugated observation

More Information
  • 波粒相互作用是环电流损失的重要机制之一,但波粒相互作用导致的环电流离子沉降而损失迄今为止缺乏直接的观测证据.基于磁层及电离层卫星的协同观测,本文报道了发生在2015年9月7日,由电磁离子回旋波(EMIC波)导致环电流质子沉降的共轭观测事件.在等离子体层的内边界,Van Allen Probe B卫星观测到,存在EMIC波的区域和不存在EMIC波的区域相比,离子通量的投掷角分布的各向异性变弱.我们将Van Allen Probe B卫星沿着磁力线投影到电离层高度,同时在该投影区域内DMSP 16卫星在亚极光区域观测到环电流质子沉降.而且,通过从理论上计算质子弹跳平均扩散系数,我们进一步证实观测的EMIC波确实能将环电流质子散射到损失锥中.本文的研究工作为EMIC波导致环电流质子沉降提供了直接的观测证据,揭示了环电流衰减的重要物理机制:EMIC波将环电流质子散射到损失锥中,从而沉降到低高度大气层中而损失.

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  • 图 1 

    DMSP 16卫星和Van Allen Probe B卫星共轭观测位置图

    Figure 1. 

    Conjugated observation map of DMSP 16 and Van Allen Probe B satellites

    图 2 

    Van Allen Probe B卫星观测的波动分析

    Figure 2. 

    Wave analysis observed by Van Allen Probe B

    图 3 

    DMSP 16卫星观测的粒子通量

    Figure 3. 

    Particle data from DMSP 16 SSJ5

    图 4 

    (a) EMIC波的高斯拟合曲线(蓝色实线); (b)质子对应于赤道损失锥角(3.2°)的弹跳平均扩散系数〈Dαα〉(黑线),其中红线表示强投掷角扩散系数DSD; (c)投掷角为0°~90°的质子弹跳平均扩散系数〈Dαα〉,其中黄色虚线对应子图(b)中的〈Dαα

    Figure 4. 

    (a) Gaussian fitting (blue solid line); (b) Bounce-averaged pitch angle diffusion rates for protons 〈Dαα〉 (black line) near the equatorial loss cone (3.2°), and the red line represents the rate of strong pitch diffusion (DSD); (c) Bounce-averaged pitch angle diffusion rates for protons 〈Dαα〉 with pitch angles of 0°~90° and the yellow dashed line corresponds to 〈Dαα〉 in subgraph (b)

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出版历程
收稿日期:  2019-10-26
修回日期:  2019-12-11
上线日期:  2020-06-25

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