| dc.contributor.author | Elliott M. Sainsbury | |
| dc.contributor.author | Reinhard K. H. Schiemann | |
| dc.contributor.author | Kevin I. Hodges | |
| dc.contributor.author | Alexander J. Baker | |
| dc.contributor.author | Len C. Shaffrey | |
| dc.contributor.author | Kieran T. Bhatia | |
| dc.date.accessioned | 2023-04-12T18:33:19Z | |
| dc.date.available | 2023-04-12T18:33:19Z | |
| dc.date.copyright | 2022/09/26 | |
| dc.date.issued | 2022 | |
| dc.identifier.other | MWR-D-22-0111.1.pdf | |
| dc.identifier.uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4289871 | |
| dc.description.abstract | Post-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.publisher | American Meteorological Society | |
| dc.title | Why Do Some Post-Tropical Cyclones Impact Europe? | |
| dc.type | Journal Paper | |
| dc.journal.volume | 150 | |
| dc.journal.issue | 10 | |
| dc.journal.title | Monthly Weather Review | |
| dc.identifier.doi | 10.1175/MWR-D-22-0111.1 | |
| dc.journal.fristpage | 2553 | |
| dc.journal.lastpage | 2571 | |
| dc.page | 2553–2571 | |
| dc.tree | Monthly Weather Review:;2022:;volume( 150 ):;issue: 010 | |
| dc.contenttype | Fulltext | |