Cohen I J, Turner D L, Michael A T, Sorathia K A, Ukhorskiy A Y
The Johns Hopkins University Applied Physics Laboratory Laurel MD USA.
J Geophys Res Space Phys. 2021 Jun;126(6):e2021JA029261. doi: 10.1029/2021JA029261. Epub 2021 Jun 3.
Radiation belt flux dropout events are sudden and often significant reductions in high-energy electrons from Earth's outer radiation belts. These losses are theorized to be due to interactions with the dayside magnetopause and possibly connected to observations of escaping magnetospheric particles. This study focuses on radiation belt losses during a moderate-strength, nonstorm dropout event on November 21, 2016. The potential loss mechanisms and the linkage to dayside escape are investigated using combined energetic electron observations throughout the dayside magnetosphere from the Magnetospheric Multiscale and Van Allen Probes spacecraft along with global magnetohydrodynamic and test particle simulations. In particular, this nonstorm-time event simplifies the magnetospheric conditions and removes ambiguity in the interpretation of results, allowing focus on subsequent losses from enhanced outward radial transport that can occur after initial compression and relaxation of the magnetopause boundary. The evolution of measured phase space density profiles suggest a total loss of approximately 60% of the initial radiation belt content during the event. Together the in situ observations and high-resolution simulations help to characterize the loss by bounding the following parameters: (a) the duration of the loss, (b) the relative distribution of losses and surface area of the magnetopause over which loss occurs, and (c) the escaping flux (i.e., loss) rate across the magnetopause. In particular, this study is able to estimate the surface area of loss to less than 2.9 × 10 R and the duration of loss to greater than 6 h, while also demonstrating the magnetic local time-dependence of the escaping flux and energy spectrum.
辐射带通量下降事件是地球外辐射带中高能电子突然且往往显著的减少。理论上,这些损失是由于与日间磁层顶的相互作用,并且可能与磁层粒子逃逸的观测结果有关。本研究聚焦于2016年11月21日一次中等强度、非风暴的通量下降事件期间的辐射带损失。利用磁层多尺度探测器和范艾伦探测器在整个日间磁层的高能电子联合观测数据,以及全球磁流体动力学和测试粒子模拟,研究了潜在的损失机制以及与日间逃逸的联系。特别是,这次非风暴期间的事件简化了磁层条件,消除了结果解释中的模糊性,使得能够专注于磁层顶边界初始压缩和松弛后增强的向外径向输运导致的后续损失。实测相空间密度剖面的演化表明,在该事件期间,初始辐射带含量总共损失了约60%。现场观测和高分辨率模拟共同有助于通过界定以下参数来描述损失情况:(a)损失的持续时间;(b)损失的相对分布以及发生损失的磁层顶表面积;(c)穿过磁层顶的逃逸通量(即损失)率。特别是,本研究能够估计损失表面积小于2.9×10 R ,损失持续时间大于6小时,同时还证明了逃逸通量和能谱的磁地方时依赖性。