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dc.contributor.authorLi, Huan
dc.contributor.authorRenssen, Hans
dc.contributor.authorRoche, Didier M.
dc.contributor.authorMiller, Paul A.
dc.date.accessioned2020-01-15T13:49:52Z
dc.date.available2020-01-15T13:49:52Z
dc.date.created2020-01-07T13:26:46Z
dc.date.issued2019
dc.identifier.citationJournal of Quaternary Science. 2019, 34 (8), 650-661.nb_NO
dc.identifier.issn0267-8179
dc.identifier.urihttp://hdl.handle.net/11250/2636471
dc.descriptionThis is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.nb_NO
dc.description.abstractThe 8.2 ka bp cooling event is assumed to be the most clearly marked abrupt climate event in the Holocene at northern mid‐ to high latitudes. In this study, we simulate the vegetation responses to the 8.2 ka bp climate change event over Europe and Northern Africa. Our results show that all dominant plant functional types (PFTs) over Europe and North Africa respond to these climate changes, but the magnitude, timing and impact factor of their responses are different. Compared with pollen‐based vegetation reconstructions, our simulation generally captures the main features of vegetation responses to the 8.2 ka bp event. Interestingly, in Western Europe, the simulated vegetation after perturbation is different from its initial state, which is consistent with two high‐resolution pollen records. This different vegetation composition indicates the long‐lasting impact of abrupt climate change on vegetation through eco‐physiological and ecosystem demographic processes, such as plant competition. Moreover, our simulations suggest a latitudinal gradient in the magnitude of the event, with more pronounced vegetation responses to the severe cooling in the north and weaker responses to less severe cooling in the south.nb_NO
dc.language.isoengnb_NO
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleModelling the vegetation response to the 8.2 ka BP cooling event in Europe and Northern Africanb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionpublishedVersionnb_NO
dc.rights.holder© 2019 The Authors.nb_NO
dc.subject.nsiVDP::Økologi: 488nb_NO
dc.subject.nsiVDP::Ecology: 488nb_NO
dc.source.pagenumber650-661nb_NO
dc.source.volume34nb_NO
dc.source.journalJournal of Quaternary Sciencenb_NO
dc.source.issue8nb_NO
dc.identifier.doi10.1002/jqs.3157
dc.identifier.cristin1767708
cristin.unitcode222,58,1,0
cristin.unitnameInstitutt for natur, helse og miljø
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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