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dc.contributor.authorZdanowicz, Christian
dc.contributor.authorGallet, Jean-Charles
dc.contributor.authorSalvatori, Rosamaria
dc.contributor.authorMalnes, Eirik
dc.contributor.authorIsaksen, Ketil
dc.contributor.authorHübner, Christiane E.
dc.contributor.authorJones, Eleanor
dc.contributor.authorLihavainen, Heikki
dc.date.accessioned2024-09-17T13:39:20Z
dc.date.available2024-09-17T13:39:20Z
dc.date.created2024-01-29T08:31:48Z
dc.date.issued2023
dc.identifier.citationPolar Research. 2023, 42 .en_US
dc.identifier.issn0800-0395
dc.identifier.urihttps://hdl.handle.net/11250/3152804
dc.description.abstractThe Arctic region is warming at over twice the mean rate of the Northern Hemisphere and nearly four times faster than the globe since 1979. The local rate of warming is even higher in the European archipelago of Svalbard. This warming is transforming the terrestrial snow cover, which modulates surface energy exchanges with the atmosphere, accounts for most of the runoff in Arctic catchments and is also a transient reservoir of atmospherically deposited compounds, including pollutants. Improved observations, understanding and modelling of changes in Arctic snow cover are needed to anticipate the effects these changes will have on the Arctic climate, atmosphere, terrestrial ecosystems and socioeconomic factors. Svalbard has been an international hub of polar research for many decades and benefits from a well-developed science infrastructure. Here, we present an agenda for the future of snow research in Svalbard, jointly developed by a multidisciplinary community of experts. We review recent trends in snow research, identify key knowledge gaps, prioritize future research efforts and recommend supportive actions to advance our knowledge of present and future snow conditions pertaining to glacier mass balance, permafrost, surface hydrology, terrestrial ecology, the cycling and fate of atmospheric contaminants, and remote sensing of snow cover. This perspective piece addresses issues relevant to the circumpolar North and could be used as a template for other national or international Arctic research plans.en_US
dc.language.isoengen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectBreens masse balanseen_US
dc.subjectGlacier mass balanceen_US
dc.subjectRemote Sensingen_US
dc.subjectFjernmålingen_US
dc.subjectØkosystemen_US
dc.subjectEcosystemen_US
dc.titleAn agenda for the future of Arctic snow research: the view from Svalbarden_US
dc.title.alternativeAn agenda for the future of Arctic snow research: the view from Svalbarden_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.rights.holder© 2023 C. Zdanowicz et alen_US
dc.description.versionpublishedVersionen_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doi10.33265/polar.v42.8827
dc.identifier.cristin2236405
dc.source.journalPolar Researchen_US
dc.source.volume42en_US
dc.source.pagenumber20en_US
dc.relation.projectNorges forskningsråd: 245638en_US
dc.relation.projectMeteorologisk institutt: 103600en_US
dc.relation.projectNorges forskningsråd: 269927en_US
dc.relation.projectNorges forskningsråd: 291644en_US
dc.relation.projectNorsk romsenter: 74CO2116en_US
dc.subject.nsiVDP::Geofag: 450en_US
dc.subject.nsiVDP::Geosciences: 450en_US


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