Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?

Solar Wind (SW) electron precipitation is able to deposit a substantial amount of energy in the nightside Martian upper atmosphere, potentially exerting an influence on its thermal structure. This study serves as the first investigation of such an issue, with the aid of the simultaneous measurements...

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Main Authors: LongKang Dai, Jun Cui, DanDan Niu, Hao Gu, YuTian Cao, XiaoShu Wu, HaiRong Lai
Format: Article
Language:English
Published: Science Press 2021-01-01
Series:Earth and Planetary Physics
Subjects:
Online Access:http://www.eppcgs.org/article/doi/10.26464/epp2021012?pageType=en
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author LongKang Dai
Jun Cui
DanDan Niu
Hao Gu
YuTian Cao
XiaoShu Wu
HaiRong Lai
author_facet LongKang Dai
Jun Cui
DanDan Niu
Hao Gu
YuTian Cao
XiaoShu Wu
HaiRong Lai
author_sort LongKang Dai
collection DOAJ
description Solar Wind (SW) electron precipitation is able to deposit a substantial amount of energy in the nightside Martian upper atmosphere, potentially exerting an influence on its thermal structure. This study serves as the first investigation of such an issue, with the aid of the simultaneous measurements of both neutral density and energetic electron intensity made on board the recent Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft. We report that, from a statistical point of view, the existing measurements do not support a scenario of noticeable neutral heating via SW electron precipitation. However, during 3%−4% of the MAVEN orbits for which data are available, strong correlation between nightside temperature and electron intensity is observed, manifested as collocated enhancements in both parameters, as compared to the surrounding regions. In addition, our analysis also indicates that neutral heating via SW electron precipitation tends to be more effective at altitudes below 160 km for integrated electron intensities above 0.01 ergs·cm−2·s−1 over the energy range of 3−450 eV. The results reported here highlight the necessity of incorporating SW electron precipitation as a heat source in the nightside Martian upper atmosphere under extreme circumstances such as during interplanetary coronal mass ejections.
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spelling doaj.art-a1a1a48853ce4911af89ad987f14d06d2022-12-22T01:52:39ZengScience PressEarth and Planetary Physics2096-39552021-01-015111010.26464/epp2021012RA215-cuijun-F2Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?LongKang Dai0Jun Cui1DanDan Niu2Hao Gu3YuTian Cao4XiaoShu Wu5HaiRong Lai6Planetary Environmental and Astrobiological Research Laboratory (PEARL), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai Guangdong 519082, ChinaPlanetary Environmental and Astrobiological Research Laboratory (PEARL), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai Guangdong 519082, ChinaInstitute of Space Science and Applied Technology, Harbin Institute of Technology, Shenzhen Guangdong 518055, ChinaPlanetary Environmental and Astrobiological Research Laboratory (PEARL), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai Guangdong 519082, ChinaPlanetary Environmental and Astrobiological Research Laboratory (PEARL), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai Guangdong 519082, ChinaKey Laboratory of Lunar and Deep Space Exploration, National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100101, ChinaPlanetary Environmental and Astrobiological Research Laboratory (PEARL), School of Atmospheric Sciences, Sun Yat-sen University, Zhuhai Guangdong 519082, ChinaSolar Wind (SW) electron precipitation is able to deposit a substantial amount of energy in the nightside Martian upper atmosphere, potentially exerting an influence on its thermal structure. This study serves as the first investigation of such an issue, with the aid of the simultaneous measurements of both neutral density and energetic electron intensity made on board the recent Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft. We report that, from a statistical point of view, the existing measurements do not support a scenario of noticeable neutral heating via SW electron precipitation. However, during 3%−4% of the MAVEN orbits for which data are available, strong correlation between nightside temperature and electron intensity is observed, manifested as collocated enhancements in both parameters, as compared to the surrounding regions. In addition, our analysis also indicates that neutral heating via SW electron precipitation tends to be more effective at altitudes below 160 km for integrated electron intensities above 0.01 ergs·cm−2·s−1 over the energy range of 3−450 eV. The results reported here highlight the necessity of incorporating SW electron precipitation as a heat source in the nightside Martian upper atmosphere under extreme circumstances such as during interplanetary coronal mass ejections.http://www.eppcgs.org/article/doi/10.26464/epp2021012?pageType=enmarssolar windupper atmospheremaven
spellingShingle LongKang Dai
Jun Cui
DanDan Niu
Hao Gu
YuTian Cao
XiaoShu Wu
HaiRong Lai
Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
Earth and Planetary Physics
mars
solar wind
upper atmosphere
maven
title Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
title_full Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
title_fullStr Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
title_full_unstemmed Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
title_short Is Solar Wind electron precipitation a source of neutral heating in the nightside Martian upper atmosphere?
title_sort is solar wind electron precipitation a source of neutral heating in the nightside martian upper atmosphere
topic mars
solar wind
upper atmosphere
maven
url http://www.eppcgs.org/article/doi/10.26464/epp2021012?pageType=en
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