Dawn/Dusk Asymmetry of the Martian UltraViolet Terminator Observed Through Suprathermal Electron Depletions. Issue 8 (21st August 2019)

• Record Type: Journal Article
• Authors: Steckiewicz, M.; Garnier, P.; Lillis, R.; Toublanc, D.; Leblanc, F.; Mitchell, D. L.; Andersson, L.; Mazelle, C.
• Is Part Of: Journal of geophysical research. Volume 124:Issue 8(2019)
• Page Start: 7283
• Page End: 7300
• Publication Date: 2019-08-21
• Subjects: Mars -- MAVEN mission -- nightside suprathermal electron depletions -- UV terminator; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1029/2018JA026336
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: Suprathermal electron depletions are structures of the nightside ionosphere of Mars resulting from an equilibrium between electron loss and creation processes. Photoionization of oxygen and carbon dioxide by UV and EUV photons is the main ionization process of the Martian atmosphere. The observation of suprathermal electron depletions is strongly unexpected in the portion of the Martian environment where photoionization can occur. This region is delimited by the UltraViolet (UV) terminator, behind which no UV ionizing photons are detected. In this study suprathermal electron depletions are used to determine the position of the UV terminator thanks to MAVEN observations. The MAVEN spacecraft is now in its fourth year of data recording and has already covered more than one Martian year, a large range of latitude, local time, and solar zenith angle in the nightside down to 110‐km altitude. This coverage enables us to determine the approximate position of the UV terminator over one Martian year. We then investigate the variation of its position on the dawnside and duskside and depending on seasons. Our results are compared with models of the Martian atmosphere and in situ data of the atmospheric composition which all highlight an asymmetry between the duskside and the dawnside at equinox. However, models show an inversion in the position of the dusk and the dawn UV terminator at perihelion and aphelion, which cannot yet be confirmed or disproved by the data. Key Points: The approximate position of the UltraViolet terminator can be determined thanks to suprathermal electron depletions The UV terminator is at a mean altitude of 123 km above the optical terminator over one Martian year The UV terminator is higher on the duskside than on the dawnside at equinox and models predict an inversion at aphelion and perihelion