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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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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.
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Articles | Volume 18, issue 2
Atmos. Chem. Phys., 18, 1115–1147, 2018
https://doi.org/10.5194/acp-18-1115-2018
Atmos. Chem. Phys., 18, 1115–1147, 2018
https://doi.org/10.5194/acp-18-1115-2018

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 et al.

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Latest update: 17 Jan 2021
Publications Copernicus
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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.
Citation
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