Articles | Volume 18, issue 2
https://doi.org/10.5194/acp-18-1115-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-18-1115-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Jan 2018
Research article |
| 29 Jan 2018
NOy production, ozone loss and changes in net radiative heating due to energetic particle precipitation in 2002–2010
Miriam Sinnhuber
CORRESPONDING AUTHOR
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Uwe Berger
Leibniz-Institut für Atmosphärenphysik, Kühlungsborn, Germany
Bernd Funke
Istituto de Astrofisica de Andalucia, Granada, Spain
Holger Nieder
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Thomas Reddmann
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Gabriele Stiller
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Stefan Versick
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Thomas von Clarmann
Institute of Meteorology and Climate Research, Karlsruhe Institute
of Technology, Karlsruhe, Germany
Jan Maik Wissing
University of Osnabrück,
Osnabrück, Germany
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- Climate, Variability, and Climate Sensitivity of “Middle Atmosphere” Chemistry Configurations of the Community Earth System Model Version 2, Whole Atmosphere Community Climate Model Version 6 (CESM2(WACCM6)) N. Davis et al. 10.1029/2022MS003579
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- Ionization effect in the Earth’s atmosphere due to cosmic rays during the GLE#71 on 17 May 2012 S. Pätsi & A. Mishev 10.1016/j.asr.2022.02.008
- Quantifying uncertainties of climate signals in chemistry climate models related to the 11-year solar cycle – Part 1: Annual mean response in heating rates, temperature, and ozone M. Kunze et al. 10.5194/acp-20-6991-2020
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- Impact of the Major Ssws of February 2018 and January 2019 on the Middle Atmospheric Nitric Oxide Abundance K. Pérot & Y. Orsolini 10.2139/ssrn.3980612
- Application of the global neutron monitor network for assessment of spectra and anisotropy and the related terrestrial effects of strong SEPs A. Mishev 10.1016/j.jastp.2023.106021
- Observational Validation of Cutoff Models as Boundaries of Solar Proton Event Impact Area E. Heino & N. Partamies 10.1029/2020JA027935
- Impact of the major SSWs of February 2018 and January 2019 on the middle atmospheric nitric oxide abundance K. Pérot & Y. Orsolini 10.1016/j.jastp.2021.105586
- Long-term mesospheric record of EPP-IE NO measured by Odin/SMR F. Grieco et al. 10.1016/j.jastp.2022.105997
- HEPPA III Intercomparison Experiment on Electron Precipitation Impacts: 1. Estimated Ionization Rates During a Geomagnetic Active Period in April 2010 H. Nesse Tyssøy et al. 10.1029/2021JA029128
- Heavenly lights: An exploratory review of auroral ecosystem services and disservices J. Broome et al. 10.1016/j.ecoser.2024.101626
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- Influence of Enhanced Planetary Wave Activity on the Polar Vortex Enhancement Related to Energetic Electron Precipitation T. Asikainen et al. 10.1029/2019JD032137
- Comparing the effects of solar-related and terrestrial drivers on the northern polar vortex A. Salminen et al. 10.1051/swsc/2020058
- Ionization effect in the Earth’s atmosphere during the sequence of October–November 2003 Halloween GLE events A. Mishev & P. Velinov 10.1016/j.jastp.2020.105484
- Heppa III Intercomparison Experiment on Electron Precipitation Impacts: 2. Model‐Measurement Intercomparison of Nitric Oxide (NO) During a Geomagnetic Storm in April 2010 M. Sinnhuber et al. 10.1029/2021JA029466
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- Long‐Term Prediction of Sudden Stratospheric Warmings With Geomagnetic and Solar Activity M. Vokhmyanin et al. 10.1029/2022JD037337
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Latest update: 11 Jul 2025
Short summary
Results from global models are used to analyze the impact of energetic particle precipitation on the middle atmosphere (10–80 km). Model results agree well with observations, and show strong enhancements of NOy, long-lasting ozone loss, and a net heating in the uppermost stratosphere (~35–45 km) during polar winter which changes sign in spring. Energetic particle precipitation therefore has the potential to impact atmospheric dynamics, starting from a warmer winter-time upper stratosphere.
Results from global models are used to analyze the impact of energetic particle precipitation on...
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