The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ...
We investigate the influence of Middle Range Energy Electrons (MEE; typically 30-300 keV) precipitation on the atmosphere using the SOCOL3-MPIOM chemistry-climate model with coupled ocean. Model simulations cover the 2002-2010 period for which ionization rates from the AIMOS dataset and atmospheric...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000115871 http://hdl.handle.net/20.500.11850/115871 |
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ftdatacite:10.3929/ethz-b-000115871 2024-04-28T08:36:38+00:00 The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... Arsenovic, Pavle Rozanov, Eugene Stenke, Andrea Funke, B. Wissing, J. M. Mursula, K. Tummon, Fiona Peter, Thomas 2016 application/pdf https://dx.doi.org/10.3929/ethz-b-000115871 http://hdl.handle.net/20.500.11850/115871 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 Atmospheric Chemistry Climate Mesosphere Middle Energy Electrons Ozone infoeu-repo/classification/ddc/550 infoeu-repo/classification/ddc/520 Earth sciences Astronomy, cartography article-journal Text ScholarlyArticle Journal Article 2016 ftdatacite https://doi.org/10.3929/ethz-b-000115871 2024-04-02T12:33:25Z We investigate the influence of Middle Range Energy Electrons (MEE; typically 30-300 keV) precipitation on the atmosphere using the SOCOL3-MPIOM chemistry-climate model with coupled ocean. Model simulations cover the 2002-2010 period for which ionization rates from the AIMOS dataset and atmospheric composition observations from MIPAS are available. Results show that during geomagnetically active periods MEE significantly increase the amount of NOy and HOx in the polar winter mesosphere, in addition to other particles and sources, resulting in local ozone decreases of up to 35%. These changes are followed by an intensification of the polar night jet, as well as mesospheric warming and stratospheric cooling. The contribution of MEE also substantially enhances the difference in the ozone anomalies between geomagnetically active and quiet periods. Comparison with MIPAS NOy observations indicates that the additional source of NOy from MEE improves the model results, however substantial underestimation above 50 km ... : Journal of Atmospheric and Solar-Terrestrial Physics, 146 ... Article in Journal/Newspaper polar night DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Atmospheric Chemistry Climate Mesosphere Middle Energy Electrons Ozone infoeu-repo/classification/ddc/550 infoeu-repo/classification/ddc/520 Earth sciences Astronomy, cartography |
spellingShingle |
Atmospheric Chemistry Climate Mesosphere Middle Energy Electrons Ozone infoeu-repo/classification/ddc/550 infoeu-repo/classification/ddc/520 Earth sciences Astronomy, cartography Arsenovic, Pavle Rozanov, Eugene Stenke, Andrea Funke, B. Wissing, J. M. Mursula, K. Tummon, Fiona Peter, Thomas The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
topic_facet |
Atmospheric Chemistry Climate Mesosphere Middle Energy Electrons Ozone infoeu-repo/classification/ddc/550 infoeu-repo/classification/ddc/520 Earth sciences Astronomy, cartography |
description |
We investigate the influence of Middle Range Energy Electrons (MEE; typically 30-300 keV) precipitation on the atmosphere using the SOCOL3-MPIOM chemistry-climate model with coupled ocean. Model simulations cover the 2002-2010 period for which ionization rates from the AIMOS dataset and atmospheric composition observations from MIPAS are available. Results show that during geomagnetically active periods MEE significantly increase the amount of NOy and HOx in the polar winter mesosphere, in addition to other particles and sources, resulting in local ozone decreases of up to 35%. These changes are followed by an intensification of the polar night jet, as well as mesospheric warming and stratospheric cooling. The contribution of MEE also substantially enhances the difference in the ozone anomalies between geomagnetically active and quiet periods. Comparison with MIPAS NOy observations indicates that the additional source of NOy from MEE improves the model results, however substantial underestimation above 50 km ... : Journal of Atmospheric and Solar-Terrestrial Physics, 146 ... |
format |
Article in Journal/Newspaper |
author |
Arsenovic, Pavle Rozanov, Eugene Stenke, Andrea Funke, B. Wissing, J. M. Mursula, K. Tummon, Fiona Peter, Thomas |
author_facet |
Arsenovic, Pavle Rozanov, Eugene Stenke, Andrea Funke, B. Wissing, J. M. Mursula, K. Tummon, Fiona Peter, Thomas |
author_sort |
Arsenovic, Pavle |
title |
The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
title_short |
The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
title_full |
The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
title_fullStr |
The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
title_full_unstemmed |
The influence of Middle Range Energy Electrons on atmospheric chemistry and regional climate ... |
title_sort |
influence of middle range energy electrons on atmospheric chemistry and regional climate ... |
publisher |
ETH Zurich |
publishDate |
2016 |
url |
https://dx.doi.org/10.3929/ethz-b-000115871 http://hdl.handle.net/20.500.11850/115871 |
genre |
polar night |
genre_facet |
polar night |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution Non Commercial No Derivatives 4.0 International https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000115871 |
_version_ |
1797568349292462080 |