Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics
Articles | Volume 19, issue 14
Articles | Volume 19, issue 14
Atmos. Chem. Phys., 19, 9485–9494, 2019
https://doi.org/10.5194/acp-19-9485-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 9485–9494, 2019
https://doi.org/10.5194/acp-19-9485-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 14
Research article
26 Jul 2019
Research article | 26 Jul 2019

Reactive nitrogen (NOy) and ozone responses to energetic electron precipitation during Southern Hemisphere winter

Pavle Arsenovic et al.

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Latest update: 18 May 2022
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Short summary
Low-energy electrons (LEE) are the dominant source of odd nitrogen, which destroys ozone, in the mesosphere and stratosphere in polar winter in the geomagnetically active periods. However, the observed stratospheric ozone anomalies can be reproduced only when accounting for both low- and middle-range energy electrons (MEE) in the chemistry-climate model. Ozone changes may induce further dynamical and thermal changes in the atmosphere. We recommend including both LEE and MEE in climate models.
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