Please use this identifier to cite or link to this item: https://oa.tib.eu/renate/jspui/handle/123456789/6003
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dc.rights.licenseCC BY 4.0 Unporteden
dc.contributor.authorSchneidereit, A.-
dc.contributor.authorPeters, D.H.W.-
dc.date.accessioned2020-11-25T14:52:42Z-
dc.date.available2020-11-25T14:52:42Z-
dc.date.issued2018-
dc.identifier.urihttp://dx.doi.org/10.34657/4632-
dc.identifier.urihttps://oar.tib.eu/jspui/handle/123456789/6003
dc.description.abstractStrong zonally asymmetric ozone (ZAO) changes are observed in the boreal extratropics for winter. During the TOMS (Total Ozone Mapping Spectrometer) period (1979-1992) the decrease of zonally asymmetric total ozone (ZATO) was twice as large as the observed zonal mean total ozone trend over Europe in January mainly caused by ultra-long wave transport. Recent studies have demonstrated that the ozone evolution reveals three different quasi-bidecadal trend stages: (i) Decline, (ii) leveling, and (ii) healing. This study focuses on the ZAO structure in boreal extratropics and on ozone transport changes by ultra-long waves during winter months. ERA-Interim data together with a linearized transport model are used. During the healing stage ZATO increases significantly over the North Atlantic/European region for January. The ZATO increase (healing stage) and ZATO decrease (decline stage) are caused by different monthly mean ozone transport characteristics of ultra-long planetary waves over the North Atlantic/European region. Furthermore, the vertical advection (ageostrophic transport) of ozone versus its horizontal component dominates in the lower and middle stratosphere during the healing stage. It is hypothesized that these ageostrophic wind changes are mainly caused by a wave train directed northeastwards which seems to be directly linked to the Arctic warming. © 2018 by the authors.eng
dc.description.sponsorshipLeibniz_Fonds-
dc.language.isoeng-
dc.publisherBasel : MDPI AG-
dc.relation.ispartofseriesAtmosphere 9 (2018), 12en
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en
dc.subjectOzone transporteng
dc.subjectQuasi-bidecadal trendeng
dc.subjectTotal column ozone, zonally asymmetric ozoneeng
dc.subjectUltra-long planetary waveseng
dc.subjectHorizontal componentseng
dc.subjectOzone transporteng
dc.subjectPlanetary Waveseng
dc.subjectQuasi-bidecadal trendeng
dc.subjectTotal column ozoneeng
dc.subjectTotal ozone mapping spectrometereng
dc.subjectTransport modelingeng
dc.subjectVertical advectioneng
dc.subjectOzoneeng
dc.subjectageostrophic floweng
dc.subjectatmospheric chemistryeng
dc.subjectatmospheric transporteng
dc.subjectextratropical environmenteng
dc.subjectlong range transporteng
dc.subjectozoneeng
dc.subjectplanetary waveeng
dc.subjectstratosphereeng
dc.subjecttemporal variationeng
dc.subjecttrend analysiseng
dc.subjectwintereng
dc.subjectAtlantic Oceaneng
dc.subjectAtlantic Ocean (North)eng
dc.subjectEuropeeng
dc.subject.ddc550-
dc.titleLong-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016eng
dc.typearticle-
dc.typeText-
dc.description.versionpublishedVersioneng
local.accessRightsopenAccess-
wgl.contributorIAPger
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
dc.bibliographicCitation.firstPage468-
dc.bibliographicCitation.volume9-
dc.bibliographicCitation.issue12-
dc.relation.doihttps://doi.org/10.3390/atmos9120468-
dc.relation.issn2073-4433-
dcterms.bibliographicCitation.journalTitleAtmosphereen
local.identifier.doihttp://dx.doi.org/10.34657/4632-
Appears in Collections:Geowissenschaften

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Schneidereit, A. and D.H.W. Peters, 2018. Long-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016. 2018. Basel : MDPI AG
Schneidereit, A. and Peters, D. H. W. (2018) “Long-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016.” Basel : MDPI AG. doi: https://doi.org/10.3390/atmos9120468.
Schneidereit A, Peters D H W. Long-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016. Vol. 9. Basel : MDPI AG; 2018.
Schneidereit, A., & Peters, D. H. W. (2018). Long-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016 (Version publishedVersion, Vol. 9). Version publishedVersion, Vol. 9. Basel : MDPI AG. https://doi.org/https://doi.org/10.3390/atmos9120468
Schneidereit A, Peters D H W. Long-term wintertime trend of zonally asymmetric ozone in boreal extratropics during 1979-2016. 2018;9(12). doi:https://doi.org/10.3390/atmos9120468


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