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Publication:
Decadal cyclone variability in the North Atlantic

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cris.virtual.author-orcid0000-0003-0176-0602
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dc.contributor.authorLuksch, Ute
dc.contributor.authorRaible, Christoph
dc.contributor.authorBlender, Richard
dc.contributor.authorFraedrich, Klaus
dc.date.accessioned2024-09-02T17:47:42Z
dc.date.available2024-09-02T17:47:42Z
dc.date.issued2005
dc.description.abstractThe unstable midlatitude ocean-atmosphere coupling motivates the definition of two decadal regimes with distinct implications for the North Atlantic cyclone variability. Phases with low (high) decadal variability of the North Atlantic Oscillation, which are connected with an annular (sectoral) spatial scale of the geopotential height teleconnection pattern, are identified as a hemispheric (regional) regime. In the hemispheric regime during a positive El Niño/Southern Oscillation (ENSO) index (warm event), the North Atlantic cyclones and the regions of enhanced precipitation shift southward while over northern Europe the cyclone activity and the rainfall are reduced. During the regional regime this impact of ENSO on the Atlantic storm track is extremely small and a clear interpretation over Europe is inhibited.
dc.description.numberOfPages7
dc.description.sponsorshipPhysikalisches Institut, Klima- und Umweltphysik (KUP)
dc.identifier.doi10.48350/158567
dc.identifier.publisherDOI10.1127/0941-2948/2005/0075
dc.identifier.urihttps://boris-portal.unibe.ch/handle/20.500.12422/43219
dc.language.isoen
dc.publisherBorntraeger
dc.relation.ispartofMeteorologische Zeitschrift
dc.relation.issn0941-2948
dc.relation.organizationDCD5A442BF29E17DE0405C82790C4DE2
dc.subject.ddc500 - Science::530 - Physics
dc.titleDecadal cyclone variability in the North Atlantic
dc.typearticle
dspace.entity.typePublication
oaire.citation.endPage753
oaire.citation.issue6
oaire.citation.startPage747
oaire.citation.volume14
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oairecerif.author.affiliationPhysikalisches Institut, Klima- und Umweltphysik (KUP)
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unibe.date.licenseChanged2021-10-21 09:55:22
unibe.description.ispublishedpub
unibe.eprints.legacyId158567
unibe.journal.abbrevTitleMETEOROL Z
unibe.refereedTRUE
unibe.subtype.articlejournal

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