48
IRUS Total
Downloads
  Altmetric

Comparative study of the Martian suprathermal electron depletions based on Mars Global Surveyor, Mars Express and Mars Atmosphere and Volatile EvolutioN missions observations

File Description SizeFormat 
jgra53118.pdfAccepted version1.77 MBAdobe PDFView/Open
Title: Comparative study of the Martian suprathermal electron depletions based on Mars Global Surveyor, Mars Express and Mars Atmosphere and Volatile EvolutioN missions observations
Authors: Steckiewicz, M
Garnier, P
André, N
Mitchell, DL
Andersson, L
Penou, E
Beth, A
Fedorov, A
Sauvaud, J-A
Mazelle, C
Brain, DA
Espley, JR
McFadden, J
Halekas, JS
Larson, DE
Lillis, RJ
Luhmann, JG
Soobiah, Y
Jakosky, BM
Item Type: Journal Article
Abstract: Nightside suprathermal electron depletions have been observed at Mars by three spacecraft to date: Mars Global Surveyor, Mars Express, and the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission. This spatial and temporal diversity of measurements allows us to propose here a comprehensive view of the Martian electron depletions through the first multispacecraft study of the phenomenon. We have analyzed data recorded by the three spacecraft from 1999 to 2015 in order to better understand the distribution of the electron depletions and their creation mechanisms. Three simple criteria adapted to each mission have been implemented to identify more than 134,500 electron depletions observed between 125 and 900 km altitude. The geographical distribution maps of the electron depletions detected by the three spacecraft confirm the strong link existing between electron depletions and crustal magnetic field at altitudes greater than ~170 km. At these altitudes, the distribution of electron depletions is strongly different in the two hemispheres, with a far greater chance to observe an electron depletion in the Southern Hemisphere, where the strongest crustal magnetic sources are located. However, the unique MAVEN observations reveal that below a transition region near 160–170 km altitude the distribution of electron depletions is the same in both hemispheres, with no particular dependence on crustal magnetic fields. This result supports the suggestion made by previous studies that these low-altitudes events are produced through electron absorption by atmospheric CO2.
Issue Date: 9-Jan-2017
Date of Acceptance: 18-Nov-2016
URI: http://hdl.handle.net/10044/1/43684
DOI: https://dx.doi.org/10.1002/2016JA023205
ISSN: 2169-9402
Publisher: American Geophysical Union
Start Page: 857
End Page: 873
Journal / Book Title: Journal of Geophysical Research: Space Physics
Volume: 122
Issue: 1
Copyright Statement: © 2017 American Geophysical Union. An edited version of this paper was published by AGU © 2017 American Geophysical Union. To view the published open abstract, go to http://dx.doi.org/10.1002/2016JA023205
Publication Status: Published
Appears in Collections:Space and Atmospheric Physics
Physics
Faculty of Natural Sciences