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dc.contributor.authorElliott M. Sainsbury
dc.contributor.authorReinhard K. H. Schiemann
dc.contributor.authorKevin I. Hodges
dc.contributor.authorAlexander J. Baker
dc.contributor.authorLen C. Shaffrey
dc.contributor.authorKieran T. Bhatia
dc.date.accessioned2023-04-12T18:33:19Z
dc.date.available2023-04-12T18:33:19Z
dc.date.copyright2022/09/26
dc.date.issued2022
dc.identifier.otherMWR-D-22-0111.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289871
dc.description.abstractPost-tropical cyclones (PTCs) can bring high winds and extreme precipitation to Europe. Although the structure and intensity of observed Europe-impacting PTCs has been investigated in previous studies, a quantitative understanding of the factors important for PTCs to reach Europe has not been established. By tracking and identifying the full life cycle of tropical cyclones (TCs) in the ERA5 reanalysis, we investigate why some PTCs impact Europe and why others do not, using a composite analysis. We show that PTCs that impact Europe are typically ∼4–6 m s
dc.publisherAmerican Meteorological Society
dc.titleWhy Do Some Post-Tropical Cyclones Impact Europe?
dc.typeJournal Paper
dc.journal.volume150
dc.journal.issue10
dc.journal.titleMonthly Weather Review
dc.identifier.doi10.1175/MWR-D-22-0111.1
dc.journal.fristpage2553
dc.journal.lastpage2571
dc.page2553–2571
dc.treeMonthly Weather Review:;2022:;volume( 150 ):;issue: 010
dc.contenttypeFulltext


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