Effects of a Solar Flare on the Martian Hot O Corona and Photochemical Escape
Abstract
Here, we examine for the first time the flare–induced effects on the Martian hot O corona. The rapid ionospheric response to the increase in the soft X–ray flux (~800%) facilitates more hot O production at altitudes below the main ionospheric peak, but almost all of these atoms are thermalized before escape. In response to the increase in the extreme ultraviolet (EUV) flux (~170%), the overall upper ionospheric and thermospheric densities are enhanced, and the peak thermospheric responses are found ~1.5 hr later. The photochemical escape rate is predicted to increase by ~20% with the increases in the soft X–ray and EUV fluxes but decrease rapidly by ~13% about 2.5 hr later before recovering the preflare level. Since escaping hot O atoms are mostly produced at high altitudes where ionization by the EUV flux is the greatest, the main contributor to the 20% increase in escape rate is the enhancement in the EUV flux.
- Authors:
-
- NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States); GESTAR, Univ. Space Research Assoc., Columbia, MD (United States)
- Princeton Univ., Princeton, NJ (United States)
- Eastern Michigan Univ., Ypsilanti, MI (United States)
- Univ. of Colorado Boulder, Boulder, CO (United States)
- Univ. of Michigan, Ann Arbor, MI (United States)
- NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
- NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States); Univ. of Maryland, Baltimore, MD (United States)
- Publication Date:
- Research Org.:
- Princeton Plasma Physics Lab. (PPPL), Princeton, NJ (United States)
- Sponsoring Org.:
- This work was supported by NASA’s NGIMS/MAVEN investigation. Resources for all simulations were provided by NASA Center for Climate Simulation (NCCS).; USDOE
- OSTI Identifier:
- 1472014
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Geophysical Research Letters
- Additional Journal Information:
- Journal Volume: 45; Journal Issue: 14; Journal ID: ISSN 0094-8276
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 79 ASTRONOMY AND ASTROPHYSICS; Mars upper atmosphere; MAVEN mission; photochemical escape; hot O corona; solar flare; numerical simulation
Citation Formats
Lee, Yuni, Dong, Chuanfei, Pawlowski, Dave, Thiemann, Edward, Tenishev, Valeriy, Mahaffy, Paul, Benna, Mehdi, Combi, Michael, Bougher, Stephen, and Eparvier, Frank. Effects of a Solar Flare on the Martian Hot O Corona and Photochemical Escape. United States: N. p., 2018.
Web. doi:10.1029/2018GL077732.
Lee, Yuni, Dong, Chuanfei, Pawlowski, Dave, Thiemann, Edward, Tenishev, Valeriy, Mahaffy, Paul, Benna, Mehdi, Combi, Michael, Bougher, Stephen, & Eparvier, Frank. Effects of a Solar Flare on the Martian Hot O Corona and Photochemical Escape. United States. https://doi.org/10.1029/2018GL077732
Lee, Yuni, Dong, Chuanfei, Pawlowski, Dave, Thiemann, Edward, Tenishev, Valeriy, Mahaffy, Paul, Benna, Mehdi, Combi, Michael, Bougher, Stephen, and Eparvier, Frank. Tue .
"Effects of a Solar Flare on the Martian Hot O Corona and Photochemical Escape". United States. https://doi.org/10.1029/2018GL077732. https://www.osti.gov/servlets/purl/1472014.
@article{osti_1472014,
title = {Effects of a Solar Flare on the Martian Hot O Corona and Photochemical Escape},
author = {Lee, Yuni and Dong, Chuanfei and Pawlowski, Dave and Thiemann, Edward and Tenishev, Valeriy and Mahaffy, Paul and Benna, Mehdi and Combi, Michael and Bougher, Stephen and Eparvier, Frank},
abstractNote = {Here, we examine for the first time the flare–induced effects on the Martian hot O corona. The rapid ionospheric response to the increase in the soft X–ray flux (~800%) facilitates more hot O production at altitudes below the main ionospheric peak, but almost all of these atoms are thermalized before escape. In response to the increase in the extreme ultraviolet (EUV) flux (~170%), the overall upper ionospheric and thermospheric densities are enhanced, and the peak thermospheric responses are found ~1.5 hr later. The photochemical escape rate is predicted to increase by ~20% with the increases in the soft X–ray and EUV fluxes but decrease rapidly by ~13% about 2.5 hr later before recovering the preflare level. Since escaping hot O atoms are mostly produced at high altitudes where ionization by the EUV flux is the greatest, the main contributor to the 20% increase in escape rate is the enhancement in the EUV flux.},
doi = {10.1029/2018GL077732},
journal = {Geophysical Research Letters},
number = 14,
volume = 45,
place = {United States},
year = {Tue Jun 12 00:00:00 EDT 2018},
month = {Tue Jun 12 00:00:00 EDT 2018}
}
Web of Science
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