Nighttime mesospheric hydroxyl enhancements during SEP events and accompanying geomagnetic storms: Ionization rate modeling and Aura satellite observations

Autor(en): Verkhoglyadova, O. P.
Wissing, J. M.
Wang, S.
Kallenrode, M. -B.
Zank, G. P.
Stichwörter: Astronomy & Astrophysics; ENERGETIC PARTICLE EVENTS; hydroxyl; INTERPLANETARY SHOCKS; magnetic storms; mesosphere; MIDDLE ATMOSPHERE; MLS; NORTHERN-HEMISPHERE; OCTOBER-NOVEMBER 2003; ODD HYDROGEN; PRECIPITATION; SEP; SOLAR PROTON EVENTS; TERTIARY OZONE MAXIMUM
Erscheinungsdatum: 2016
Herausgeber: AMER GEOPHYSICAL UNION
Enthalten in: JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
Band: 121
Ausgabe: 7
Startseite: 6017
Seitenende: 6030
Zusammenfassung: 
We quantify the effects of combined precipitating solar protons and magnetospheric electrons on nighttime odd hydrogen density enhancements during two solar energetic particle (SEP) events accompanied by strong geomagnetic storms. We perform detailed modeling of ionization rates for 7-17 November 2004 and 20-30 August 2005 intervals with improved version 1.6 of the Atmospheric Ionization Module Osnabruck model. Particle measurements from Geostationary Operational Environmental Satellites and Polar Orbiting Environmental Satellites are sorted and combined in 2h intervals to create realistic particle precipitation maps that are used as the modeling input. We show that modeled atmospheric ionization rates and estimated peak odd hydrogen (primarily hydroxyl) production from 0.001hPa to 0.1hPa atmospheric pressure levels during these intervals are consistent with enhancements in nighttime averaged zonal odd hydrogen densities derived from newly reprocessed and improved data set of Microwave Limb Sounder instrument on board Aura satellite. We show that both precipitating SEPs and magnetospheric electrons contribute to mesospheric ionization and their relative contributions change throughout the intervals. Our event-based modeling results underline the importance of the combined ionization sources for odd hydrogen chemistry in the middle atmosphere.
ISSN: 21699380
DOI: 10.1002/2015JA022217

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