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The Impact of Energetic Particles on the Martian Ionosphere During a Full Solar Cycle of Radar Observations: Radar Blackouts

Title: The Impact of Energetic Particles on the Martian Ionosphere During a Full Solar Cycle of Radar Observations: Radar Blackouts
Authors: Lester, Mark; Sanchez-Cano, Beatriz; Potts, Daniel; Lillis, Rob; Cartacci, Marco; Bernardini, Fabrizio; Orosei, Roberto; Perry, Matthew; Putzig, Nathaniel; Campbell, Bruce; Blelly, Pierre-Louis; Milan, Steve; Opgenoorth, Hermann; Witasse, Olivier; Redrojo, Elena M. M.; Russell, Aaron
Contributors: Institut de recherche en astrophysique et planétologie (IRAP); Université Toulouse III - Paul Sabatier (UT3); Communauté d'universités et établissements de Toulouse (Comue de Toulouse)-Communauté d'universités et établissements de Toulouse (Comue de Toulouse)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Source: ISSN: 2169-9380.
Publisher Information: CCSD; American Geophysical Union/Wiley
Publication Year: 2022
Collection: Université Toulouse III - Paul Sabatier: HAL-UPS
Subject Terms: Mars reconnaissance orbiter; Mars express; the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission; radio sounding; solar energetic particles; Mars ionosphere; [SDU]Sciences of the Universe [physics]
Description: International audience ; We present the first long-term characterization of ionization layers in the lower ionosphere of Mars (below ∼90 km), a region inaccessible to orbital in-situ observations, based on an analysis of radar echo blackouts observed on Mars Express and the Mars Reconnaissance Orbiter from 2006 to 2017. A blackout occurs when the expected surface reflection is partly or totally attenuated for portions of an observation. Enhanced ionization at altitudes of 60-90 km, below the main ionospheric electron density peak, leads to increased absorption of the radar signal, resulting in the blackouts. We find that (a) MARSIS, operating at frequencies between 1.8 and 5 MHz, suffered more blackouts than SHARAD, which has a higher carrier frequency (20 MHz), (b) there is a clear correlation of blackout occurrence with solar cycle, (c) there is no apparent relationship between blackout occurrence and crustal magnetic fields, and (d) blackouts occur during both nightside and dayside observations, although the peak occurrence is deep on the nightside. Analysis of Mars Atmosphere and Volatile EvolutioN Solar Energetic Particle electron counts between 20 and 200 keV demonstrates that these electrons are likely responsible for attenuating the radar signals. We investigate the minimum SEP electron fluxes required to ionize the lower atmosphere and produce measurable attenuation. When both radars experience a blackout, the SEP electron fluxes are at their highest. Based on several case studies, we find that the average SEP spectrum responsible for a blackout is particularly enhanced at its higher energy end, that is, above 70 keV.
Document Type: article in journal/newspaper
Language: English
Relation: BIBCODE: 2022JGRA.12729535L
DOI: 10.1029/2021JA029535
Availability: https://insu.hal.science/insu-03672052; https://insu.hal.science/insu-03672052v1/document; https://insu.hal.science/insu-03672052v1/file/JGR%20Space%20Physics%20-%202022%20-%20Lester%20-%20The%20Impact%20of%20Energetic%20Particles%20on%20the%20Martian%20Ionosphere%20During%20a%20Full%20Solar%20Cycle.pdf; https://doi.org/10.1029/2021JA029535
Rights: https://creativecommons.org/licenses/by/4.0/ ; info:eu-repo/semantics/OpenAccess
Accession Number: edsbas.450615F2
Database: BASE