Modeling the Magnetospheric 3D X-Ray Emission From SWCX Using a Cusp-Magnetosheath Emissivity Model

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2025-02-06 DOI:10.1029/2024JA033307
S. J. Wharton, J. A. Carter, S. Sembay, Y. Soobiah, S. Nitti, T. R. Sun
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Abstract

A major challenge in solar-terrestrial physics is to understand the large-scale dynamics of planetary magnetospheres, such as the motion of the Earth's magnetopause. Currently, a combination of in situ measurements and numerical modeling has been used to address this challenge, but no global imaging has been available. The discovery of soft X-rays by the solar wind charge exchange (SWCX) process offers an opportunity to image the emitted X-ray photons. The SMILE mission, due for launch in late 2025, will carry a wide field of view soft X-ray telescope designed to observe emission from the magnetosheath and cusps. As no emission is expected from within the magnetosphere, it is expected that the magnetopause boundary will be observable from changes in X-ray intensity across the boundary. Extracting the 3D magnetopause boundary from the 2D X-ray images is a challenging task and several methods have been developed to model it. One method is to create a 3D emissivity model and adjust its parameters to fit the 2D X-ray image. In this paper, we develop a Cusp and Magnetosheath Emissivity Model (CMEM) and compare its performance to a previous model that did not include the cusps. We find CMEM has an improved fit to emissivity simulations for a wide range of solar wind densities, but that a poor choice of initial parameters can generate unphysical fits in both models. We propose and verify a method to resolve this that uses the upstream solar wind density to constrain some of the initial parameters.

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利用尖-磁鞘辐射率模型模拟SWCX的磁层三维x射线发射
日地物理学的一个主要挑战是了解行星磁层的大规模动力学,例如地球磁层顶的运动。目前,原位测量和数值模拟的结合已被用于解决这一挑战,但没有全球成像可用。通过太阳风电荷交换(SWCX)过程发现的软x射线为发射的x射线光子成像提供了机会。计划于2025年底发射的SMILE任务将携带一个宽视场软x射线望远镜,用于观测磁鞘和尖端的发射。由于预计在磁层内没有发射,预计将从磁层顶边界的x射线强度变化中观测到磁层顶边界。从二维x射线图像中提取三维磁层顶边界是一项具有挑战性的任务,已经开发了几种方法来模拟它。一种方法是建立三维发射率模型,并调整其参数以适应二维x射线图像。在本文中,我们建立了一个尖头和磁鞘发射率模型(CMEM),并将其性能与先前不包括尖头的模型进行了比较。我们发现CMEM对大范围太阳风密度的发射率模拟有更好的拟合,但初始参数的选择不当会在两个模型中产生非物理拟合。我们提出并验证了一种利用上游太阳风密度约束一些初始参数的方法来解决这个问题。
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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
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