Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars

An algorithm has been developed to invert the solar wind parameters from the hydrogen energetic neutral atom (H-ENA) measured in near-Mars space. Supposing the H-ENA is produced by change exchange collision between protons that originated in the solar wind and neutrals in the exosphere, an H-ENA mod...

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Main Authors: Yiteng Zhang, Lei Li, Lianghai Xie, Linggao Kong, Wenya Li, Binbin Tang, Jijie Ma, Aibing Zhang
Format: Article
Language:English
Published: MDPI AG 2023-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/15/7/1721
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author Yiteng Zhang
Lei Li
Lianghai Xie
Linggao Kong
Wenya Li
Binbin Tang
Jijie Ma
Aibing Zhang
author_facet Yiteng Zhang
Lei Li
Lianghai Xie
Linggao Kong
Wenya Li
Binbin Tang
Jijie Ma
Aibing Zhang
author_sort Yiteng Zhang
collection DOAJ
description An algorithm has been developed to invert the solar wind parameters from the hydrogen energetic neutral atom (H-ENA) measured in near-Mars space. Supposing the H-ENA is produced by change exchange collision between protons that originated in the solar wind and neutrals in the exosphere, an H-ENA model is established based on the magnetohydrodynamic (MHD) simulation of the solar wind interaction with Mars, to study the H-ENA characteristics. It is revealed that the solar wind H-ENAs are high-speed, low-temperature beams, just like the solar wind, while the magnetosheath H-ENAs are slower and hotter, with broader energy distribution. Assuming Maxwellian velocity distribution, the solar wind H-ENA flux is best fitted by a Gaussian function, from which the solar wind velocity, density, and temperature can be retrieved. Further investigation, based on the ENA flux simulated by the H-ENA model, reveals that the accuracy of inversed solar wind parameters is related to the angular and energy resolutions of the ENA detector. Finally, the algorithm is verified using the H-ENA observations from the Tianwen-1 mission. The upstream solar wind velocity when inversed is close to that of the in situ plasma measurement. Our result suggests the solar wind parameters inversed from H-ENA observation could be an important supplement to the dataset supporting studies on the Martian space environment, where long-term continuous monitoring of the upstream SW condition is lacking.
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spelling doaj.art-80faa9fcc8cc498080cb90f6c90222072023-11-17T17:27:57ZengMDPI AGRemote Sensing2072-42922023-03-01157172110.3390/rs15071721Inversion of Upstream Solar Wind Parameters from ENA Observations at MarsYiteng Zhang0Lei Li1Lianghai Xie2Linggao Kong3Wenya Li4Binbin Tang5Jijie Ma6Aibing Zhang7State Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaNational Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaState Key Laboratory of Space Weather, National Space Science Center, Chinese Academy of Sciences, Beijing 100190, ChinaUniversity of Chinese Academy of Sciences, Beijing 100049, ChinaUniversity of Chinese Academy of Sciences, Beijing 100049, ChinaAn algorithm has been developed to invert the solar wind parameters from the hydrogen energetic neutral atom (H-ENA) measured in near-Mars space. Supposing the H-ENA is produced by change exchange collision between protons that originated in the solar wind and neutrals in the exosphere, an H-ENA model is established based on the magnetohydrodynamic (MHD) simulation of the solar wind interaction with Mars, to study the H-ENA characteristics. It is revealed that the solar wind H-ENAs are high-speed, low-temperature beams, just like the solar wind, while the magnetosheath H-ENAs are slower and hotter, with broader energy distribution. Assuming Maxwellian velocity distribution, the solar wind H-ENA flux is best fitted by a Gaussian function, from which the solar wind velocity, density, and temperature can be retrieved. Further investigation, based on the ENA flux simulated by the H-ENA model, reveals that the accuracy of inversed solar wind parameters is related to the angular and energy resolutions of the ENA detector. Finally, the algorithm is verified using the H-ENA observations from the Tianwen-1 mission. The upstream solar wind velocity when inversed is close to that of the in situ plasma measurement. Our result suggests the solar wind parameters inversed from H-ENA observation could be an important supplement to the dataset supporting studies on the Martian space environment, where long-term continuous monitoring of the upstream SW condition is lacking.https://www.mdpi.com/2072-4292/15/7/1721H-ENAMarssolar wind inversionTianwen-1MINPA
spellingShingle Yiteng Zhang
Lei Li
Lianghai Xie
Linggao Kong
Wenya Li
Binbin Tang
Jijie Ma
Aibing Zhang
Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
Remote Sensing
H-ENA
Mars
solar wind inversion
Tianwen-1
MINPA
title Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
title_full Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
title_fullStr Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
title_full_unstemmed Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
title_short Inversion of Upstream Solar Wind Parameters from ENA Observations at Mars
title_sort inversion of upstream solar wind parameters from ena observations at mars
topic H-ENA
Mars
solar wind inversion
Tianwen-1
MINPA
url https://www.mdpi.com/2072-4292/15/7/1721
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