EMM EMUS Observations of FUV Aurora on Mars: Dependence on Magnetic Topology, Local Time, and Season

Author:

Chirakkil Krishnaprasad12ORCID,Lillis Robert J.3ORCID,Deighan Justin1ORCID,Chaffin Michael S.1ORCID,Jain Sonal K.1ORCID,Brain David A.1ORCID,Fillingim Matthew O.3ORCID,Susarla Raghuram12ORCID,Holsclaw Greg1ORCID,Fang Xiaohua1ORCID,Schneider Nick M.1ORCID,AlMazmi Hoor4ORCID,AlMatroushi Hessa5ORCID,Gacesa Marko6ORCID,El‐Kork Nayla26,Thiemann Ed1ORCID,Halekas Jasper S.7ORCID

Affiliation:

1. Laboratory for Atmospheric and Space Physics University of Colorado Boulder Boulder CO USA

2. Space and Planetary Science Center Khalifa University Abu Dhabi UAE

3. Space Sciences Laboratory University of California Berkeley CA USA

4. United Arab Emirates Space Agency Abu Dhabi UAE

5. Mohammed Bin Rashid Space Centre Dubai UAE

6. Department of Physics Khalifa University Abu Dhabi UAE

7. Department of Physics and Astronomy University of Iowa Iowa City IA USA

Abstract

AbstractWe present a comprehensive study of the nightside aurora phenomenon on Mars, utilizing observations from EMUS onboard Emirates Mars Mission. The oxygen emission at 130.4 nm is by far the brightest FUV auroral emission line observed at Mars. Our statistical analysis reveals geographic, solar zenith angle, local time, and seasonal dependencies of auroral occurrence. Higher occurrence of aurora is observed in regions of open magnetic topology, where crustal magnetic fields are either very weak or both strong and vertical. Aurora occurs more frequently closer to the terminator and is more likely on the dusk side than on the dawn side of the night hemisphere. A pronounced auroral feature appears close to midnight local times in the southern hemisphere, consistent with the spot of energetic electron fluxes previously identified in the Mars Global Surveyor data. This auroral spot is more frequent after midnight than before. Additionally, some regions on Mars are “aurora voids” where essentially no aurora occurs. Aurora exhibits a seasonal dependence, with a major enhancement near perihelion. Non–crustal field aurora additionally shows a secondary enhancement near Ls 30°. This seasonal variability is a combination of the variability in ionospheric photoelectrons and thermospheric atomic oxygen abundance. Auroral occurrence also shows an increase with the rise of Solar Cycle 25. The brightest auroral pixels are observed during space weather events such as Coronal Mass Ejections and Stream Interaction Regions. These observations not only shed light on where and when Martian aurora occurs, but also add to our understanding of Mars' magnetic environment and its interaction with the heliosphere.

Publisher

American Geophysical Union (AGU)

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