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dc.contributor.authorPérot, Kristell
dc.contributor.authorOrsolini, Yvan J.
dc.date.accessioned2021-04-20T08:02:34Z
dc.date.available2021-04-20T08:02:34Z
dc.date.created2021-04-09T09:55:37Z
dc.date.issued2021
dc.identifier.citationJournal of Atmospheric and Solar-Terrestrial Physics. 2021, 105586.en_US
dc.identifier.issn1364-6826
dc.identifier.urihttps://hdl.handle.net/11250/2738503
dc.description.abstractThe Arctic middle atmosphere was affected by major sudden stratospheric warmings (SSW) in February 2018 and January 2019, respectively. In this article, we report for the first time the impact of these two events on the middle atmospheric nitric oxide (NO) abundance. The study is based on measurements obtained during two dedicated observation campaigns, using the Sub-Millimetre Radiometer (SMR) aboard the Odin satellite, measuring NO globally since 2003. The SSW of February 2018 was similar to other, more dynamically quiet, Arctic winters in term of NO downward transport from the upper mesosphere–lower thermosphere to lower altitudes (referred to as energetic particle precipitation indirect effect EPP-IE). On the contrary, the event of January 2019 led to one of the strongest EPP-IE cases observed within the Odin operational period. Important positive NO anomalies were indeed observed in the lower mesosphere–upper stratosphere during the three months following the SSW onset, corresponding to NO volume mixing ratios more than 50 times higher than the climatological values. These different consequences on the middle atmospheric composition are explained by very different dynamical characteristics of these two SSW events.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleImpact of the major SSWs of February 2018 and January 2019 on the middle atmospheric nitric oxide abundanceen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2021 The Authors. Published by Elsevier Ltd.en_US
dc.source.volume218en_US
dc.source.journalJournal of Atmospheric and Solar-Terrestrial Physicsen_US
dc.identifier.doi10.1016/j.jastp.2021.105586
dc.identifier.cristin1903147
dc.relation.projectNorges forskningsråd: 255276en_US
dc.relation.projectNILU - Norsk institutt for luftforskning: 116104en_US
dc.source.articlenumber105586en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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