University of Oulu

Xu, W., Marshall, R. A., Kero, A., & Sousa, A. (2021). Chemical response of the upper atmosphere due to lightning-induced electron precipitation. Journal of Geophysical Research: Atmospheres, 126, e2021JD034914. https://doi.org/10.1029/2021JD034914

Chemical response of the upper atmosphere due to lightning-induced electron precipitation

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Author: Xu, Wei; Marshall, Robert A.1; Kero, Antti2;
Organizations: 1Ann and H. J. Smead Department of Aerospace Engineering Sciences, University of Colorado Boulder, Boulder, CO, USA
2Sodankylä Geophysical Observatory, University of Oulu, Oulu, Finland
Format: article
Version: published version
Access: embargoed
Persistent link: http://urn.fi/urn:nbn:fi-fe2021121360198
Language: English
Published: American Geophysical Union, 2021
Publish Date: 2022-02-26
Description:

Abstract

Terrestrial lightning frequently serves as a loss mechanism for energetic electrons in the Van Allen radiation belts, leading to lightning-induced electron precipitation (LEP). Regardless of the specific causes, energetic electron precipitation from the radiation belts in general has a significant influence on the ozone concentration in the stratosphere and mesosphere. The atmospheric chemical effects induced by LEP have been previously investigated using subionospheric VLF measurements at Faraday station, Antarctica (65.25°S, 64.27°W, L = 2.45). However, there exist large variations in the precipitation flux, ionization production, and occurrence rate of LEP events depending on the peak current of the parent lightning discharge, as well as the season, location, and intensity of the thunderstorm activity. These uncertainties motivate us to revisit the calculation of atmospheric chemical changes produced by LEP. In this study, we combine a well-validated LEP model and first-principles atmospheric chemical simulation, and investigate three intense storms in the year of 2013, 2015, and 2017 at the magnetic latitude of 50.9°, 32.1°, and 35.7°. Modeling results show that the LEP events in these storms can cumulatively drive significant changes in the NOₓ, HOₓ, and Oₓ concentration in the mesosphere. These changes are as high as ~156%, ~66%, and -5% at 75–85 km altitude, respectively, and comparable to the effects typically induced by other types of radiation belt electron precipitation events. Considering the high occurrence rate of thunderstorms around the globe, the long-term global chemical effects produced by LEP events need to be properly quantified.

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Series: Journal of geophysical research. Atmospheres
ISSN: 2169-897X
ISSN-E: 2169-8996
ISSN-L: 2169-897X
Volume: 126
Issue: 17
Article number: e2021JD034914
DOI: 10.1029/2021JD034914
OADOI: https://oadoi.org/10.1029/2021JD034914
Type of Publication: A1 Journal article – refereed
Field of Science: 115 Astronomy and space science
114 Physical sciences
Subjects:
Funding: This research was supported by the NSF MAG award AGS1732359. The work of A. Kero is funded by the Tenure Track Project in Radio Science at Sodankylä Geophysical Observatory/University of Oulu.
Copyright information: © 2021. American Geophysical Union.