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Solar and Solar Wind Energy Drivers for O+ and O2+ Ion Escape at Mars
Journal article   Open access   Peer reviewed

Solar and Solar Wind Energy Drivers for O+ and O2+ Ion Escape at Mars

N. R. Schnepf, Y. Dong, D. Brain, K. G. Hanley, W. K. Peterson, R. J. Strangeway, E. M. B. Thiemann, J. S. Halekas, J. R. Espley, F. Eparvier, …
Journal of geophysical research. Space physics, Vol.129(5), e2023JA032053
05/2024
DOI: 10.1029/2023JA032053
url
https://doi.org/10.1029/2023JA032053View
Published (Version of record) Open Access

Abstract

Mars once had a dense atmosphere enabling liquid water existing on its surface, however, much of that atmosphere has since escaped to space. We examine how incoming solar and solar wind energy fluxes drive escape of atomic and molecular oxygen ions (O+ and (Formula presented.)) at Mars. We use MAVEN data to evaluate ion escape from 1 February 2016 through 25 May 2022. We find that Martian O+ and (Formula presented.) both have increased escape flux with increased solar wind kinetic energy flux and this relationship is generally logarithmic. Increased solar wind electromagnetic energy flux also corresponds to increased O+ and (Formula presented.) escape flux, however, increased solar wind electromagnetic energy flux seems to first dampen ion escape until a threshold level is reached, at which point ion escape increases with increasing electromagnetic energy flux. Increased solar irradiance (both total and ionizing) does not obviously increase escape of O+ and (Formula presented.). Our results suggest that the solar wind electromagnetic energy flux should be considered along with the kinetic energy flux as an important driver of ion escape, and that other parameters should be considered when evaluating solar irradiance's impact on O+ and (Formula presented.) escape.
atmosphere loss ion escape Mars

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