Three-dimensional structure of the Martian nightside ionosphere: Predicted rates of impact ionization from Mars Global Surveyor magnetometer and electron reflectometer measurements of precipitating electrons

The nightside ionosphere of Mars is known to be highly variable: electron densities are below detection thresholds in certain regions and are almost comparable to the photoionization‐produced dayside ionosphere in others. The factors controlling its structure include thermospheric densities, tempera...

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Bibliographic Details
Published inJournal of Geophysical Research: Space Physics Vol. 116; no. A12
Main Authors Lillis, Robert J., Fillingim, Matthew O., Brain, David A.
Format Journal Article
LanguageEnglish
Published Washington Blackwell Publishing Ltd 01.12.2011
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Summary:The nightside ionosphere of Mars is known to be highly variable: electron densities are below detection thresholds in certain regions and are almost comparable to the photoionization‐produced dayside ionosphere in others. The factors controlling its structure include thermospheric densities, temperatures and winds, day‐night plasma transport, plasma temperatures, current systems, meteoroid ablation, solar and galactic energetic particle events, and magnetic field geometry‐topology and electron precipitation, none of which are adequately understood at present. Using a kinetic approach called Mars Monte Carlo Electron Transport, we model the dynamics of precipitating electrons on the nightside of Mars to study the impact of these last two listed factors (magnetic fields and electron precipitation) on ionospheric structure. As input, we use precipitating electron energy spectra and pitch angle distributions from the Mars Global Surveyor Magnetometer and Electron Reflectometer. We thus calculate ionization rate in three dimensions, both for specific observations and average cases. The very highest average rates are equivalent to photoionization rates on the dayside at high solar zenith angle. We predict complex geometrical patterns in the ionization and huge variability (∼4 orders of magnitude) in peak ionization rates, both on single orbits and between the averages for different geographic regions, and find a bimodal distribution of predicted ionization rates where the highest rates correlate with the most vertical magnetic fields. This model can be used as input to electrodynamic models of the Mars ionosphere, which can be compared with, and informed by, data from the upcoming 2013 Mars Atmosphere and Volatile Evolution Mission. Key Points Nightside ionization depends on crustal magnetic field topology Peak ionization rates vary by approximately 4 orders of magnitude Highest ionization rates correlate with the most vertical magnetic fields
Bibliography:istex:EE73DB2FEB06A1DFAB3FCE1E9EADE28DA82049E7
NASA - No. NNX11AI87G; No. NNX09AD43G; No. NNX08AK94G
ark:/67375/WNG-5FRKD46V-J
ArticleID:2011JA016982
Animation 1.. Animation of three-dimensional ionization rates on the Martian nightside: viewpoint 1. This animation consists of an extension of : a 31-frame movie (animated GIF) showing three-dimensional ionization rates on the Martian nightside up to and including 80 km, 90 km, 100 km, ..., 380 km. The planetary surface is shaded according to topography and colored according to the radial component of crustal magnetic field at 400 km. The color scales are the same as for .Animation 2. Animation of three-dimensional ionization rates on the Martian nightside: viewpoint 2. This animation consists of an extension of : a 31-frame movie (animated GIF) showing three-dimensional ionization rates on the Martian nightside up to and including 80 km, 90 km, 100 km, ..., 380 km. The planetary surface is shaded according to topography and colored according to the radial component of crustal magnetic field at 400 km. The color scales are the same as for .
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0148-0227
2169-9380
2156-2202
2169-9402
DOI:10.1029/2011JA016982