Nightside Electron Precipitation Patterns as Observed by ELFIN and CIRBE CubeSats

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-11-02 DOI:10.1029/2024JA033051
Kun Zhang, Anton V. Artemyev, Xinlin Li, Xiao-Jia Zhang, Vassilis Angelopoulos, Yang Mei, Zheng Xiang, Niklas Grimmich
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Abstract

The rapidly expanding fleet of low-altitude CubeSats equipped with energetic particle detectors brings new opportunities for monitoring the dynamics of the radiation belt and near-Earth plasma sheet. Despite their small sizes, CubeSats can carry state-of-the-art instruments that provide electron flux measurements with finer energy resolution and broader energy coverage, compared to conventional missions such as POES satellites. The recently launched CIRBE CubeSat measures 250–6,000 keV electrons with extremely high energy resolution, however, CIRBE typically only measures locally-trapped electrons and cannot directly measure the precipitating electrons. This work aims to develop a technique for identifying indications of nightside precipitation using the locally-trapped electron measurements by the CIRBE CubeSat. This study focuses on two main types of drivers for nightside precipitation: electron scattering by the curvature of magnetic field lines in the magnetotail current sheet and electron scattering by resonance with electromagnetic ion cyclotron (EMIC) waves. Using energy and pitch-angle resolved electron fluxes from the low-altitude ELFIN CubeSat, we reveal the features that distinguish between these two precipitation mechanisms based solely on locally-trapped flux measurements. Then we present measurements from four CIRBE orbits and demonstrate the applicability of the proposed technique to the investigation of nightside precipitation using CIRBE observations, enabling separation between precipitation induced by curvature scattering and EMIC waves in nearby regions. Our study underscores the feasibility of employing high-energy-resolution CIRBE measurements for detecting nightside precipitation of relativistic electrons. Additionally, we briefly discuss outstanding scientific questions about these precipitation patterns that could be addressed with CIRBE measurements.

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ELFIN 和 CIRBE 立方体卫星观测到的夜侧电子沉降模式
配备高能粒子探测器的低空立方体卫星群迅速扩大,为监测辐射带和近地等离子体层的动态带来了新的机遇。与 POES 卫星等传统任务相比,立方体卫星尽管体积小,却能携带最先进的仪器,以更精细的能量分辨率和更广泛的能量覆盖范围提供电子通量测量。最近发射的 CIRBE 立方体卫星以极高的能量分辨率测量 250-6,000 千伏电子,但 CIRBE 通常只能测量局部俘获的电子,无法直接测量析出电子。这项工作旨在开发一种技术,利用 CIRBE 立方体卫星的局域俘获电子测量值来识别夜边沉淀的迹象。这项研究侧重于夜侧沉淀的两种主要驱动因素:磁尾电流片中磁场线曲率的电子散射和与电磁离子回旋波共振的电子散射。利用低空ELFIN立方体卫星的能量和俯仰角分辨电子通量,我们仅根据局部捕获的通量测量结果,就揭示了区分这两种沉淀机制的特征。然后,我们介绍了来自四个 CIRBE 轨道的测量数据,并证明了所提出的技术适用于利用 CIRBE 观测数据调查夜侧降水,从而能够区分曲率散射引起的降水和附近区域的电磁波。我们的研究强调了利用高能分辨率 CIRBE 测量来探测相对论电子夜侧沉淀的可行性。此外,我们还简要讨论了有关这些沉淀模式的悬而未决的科学问题,这些问题可以通过 CIRBE 测量来解决。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
期刊最新文献
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