Model simulations of chemical effects of sprites in relation with observed HO<sub>2</sub> enhancements over sprite-producing thunderstorms
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Published:2021-05-19
Issue:10
Volume:21
Page:7579-7596
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Winkler HolgerORCID, Yamada TakayoshiORCID, Kasai Yasuko, Berger Uwe, Notholt Justus
Abstract
Abstract. Recently, measurements by the Superconducting Submillimeter-Wave
Limb Emission Sounder (SMILES) satellite instrument have been presented
which indicate an increase in mesospheric HO2 above sprite-producing thunderstorms.
The aim of this paper is to compare these observations to model simulations
of chemical sprite effects.
A plasma chemistry model in combination with a vertical transport module
was used to simulate the impact of a streamer discharge in the
altitude range 70–80 km, corresponding to one of the observed sprite events.
Additionally, a horizontal transport and dispersion model was used
to simulate advection and expansion of the sprite air masses.
The model simulations predict a production of hydrogen radicals
mainly due to reactions of proton hydrates formed after the electrical discharge.
The net effect is a conversion of water molecules into H+OH.
This leads to increasing HO2 concentrations a few hours
after the electric breakdown.
Due to the modelled long-lasting increase in HO2 after a sprite
discharge, an accumulation of HO2 produced by several sprites appears
possible.
However, the number of sprites needed to explain the
observed HO2 enhancements is unrealistically large.
At least for the lower measurement tangent heights, the
production mechanism of HO2 predicted by
the model might contribute to the observed enhancements.
Funder
Deutsche Forschungsgemeinschaft
Publisher
Copernicus GmbH
Subject
Atmospheric Science
Reference65 articles.
1. Arnone, E., Kero, A., Dinelli, B. M., Enell, C.-F., Arnold, N. F., Papandrea,
E., Rodger, C. J., Carlotti, M., Ridolfi, M., and Turunen, E.: Seeking
sprite-induced signatures in remotely sensed middle atmosphere NO2,
Geophys. Res. Lett., 35, L05807, https://doi.org/10.1029/2007GL031791, 2008. a 2. Arnone, E., Kero, A., Enell, C.-F., Carlotti, M., Rodger, C. J., Papandrea, E., Arnold, N. F., Dinelli, B. M., Ridolfi, M., and Turunen, E.: Seeking
sprite-induced signatures in remotely sensed middle atmosphere NO2:
latitude and time variations, Plasma Sources Sci. T., 18, 034014,
https://doi.org/10.1088/0963-0252/18/3/034014, 2009. a 3. Arnone, E., Smith, A. K., Enell, C.-F., Kero, A., and Dinelli, B. M.: WACCM
climate chemistry sensitivity to sprite perturbations, J. Geophys. Res.-Atmos., 119, 6958–6970, https://doi.org/10.1002/2013JD020825, 2014. a, b, c 4. Banerjee, A., Archibald, A. T., Maycock, A. C., Telford, P., Abraham, N. L., Yang, X., Braesicke, P., and Pyle, J. A.: Lightning NOx, a key chemistry–climate interaction: impacts of future climate change and consequences for tropospheric oxidising capacity, Atmos. Chem. Phys., 14, 9871–9881, https://doi.org/10.5194/acp-14-9871-2014, 2014. a 5. Banks, P. and Kockarts, G.: Aeronomy, Part 2, 1st edn., Academic Press, New York, USA, 372 pp., 1973. a
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