dc.contributor.author | Matte, Dominic | |
dc.contributor.author | Christensen, Jens Hesselbjerg | |
dc.contributor.author | Ozturk, Tugba | |
dc.date.accessioned | 2024-06-21T11:49:58Z | |
dc.date.available | 2024-06-21T11:49:58Z | |
dc.date.created | 2022-02-05T15:00:05Z | |
dc.date.issued | 2021 | |
dc.identifier.citation | Climate Dynamics. 2021, . | en_US |
dc.identifier.issn | 0930-7575 | |
dc.identifier.uri | https://hdl.handle.net/11250/3135327 | |
dc.description.abstract | Using a sub-selection of regional climate models at 0.11° ( 12 km) grid resolution from the EURO-CORDEX ensemble, we investigate how the spatial extent of areas associated with the most intensive daily precipitation events changes as a consequence of global warming. We address this by analysing three different warming levels: 1 °C, 2 °C and 3 °C. We find that not only does the intensity of such events increase, but their size will also change as a function of the warming: larger systems becomes more frequent and larger, while systems of lesser extent are reduced in numbers. | en_US |
dc.language.iso | eng | en_US |
dc.rights | Navngivelse 4.0 Internasjonal | * |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | * |
dc.title | Spatial extent of precipitation events: when big is getting bigger | en_US |
dc.title.alternative | Spatial extent of precipitation events: when big is getting bigger | en_US |
dc.type | Journal article | en_US |
dc.type | Peer reviewed | en_US |
dc.rights.holder | © The Author(s) 2021 | en_US |
dc.description.version | publishedVersion | en_US |
cristin.ispublished | true | |
cristin.fulltext | original | |
cristin.qualitycode | 2 | |
dc.identifier.doi | 10.1007/s00382-021-05998-0 | |
dc.identifier.cristin | 1998093 | |
dc.source.journal | Climate Dynamics | en_US |
dc.source.pagenumber | 0 | en_US |
dc.relation.project | EC/H2020/776613 | en_US |