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dc.contributor.authorMarcel, Nicolaus
dc.contributor.authorPerovich, Donald
dc.contributor.authorSpreen, Gunnar
dc.contributor.authorGranskog, Mats
dc.contributor.authorDivine, Dmitry
dc.contributor.authorGerland, Sebastian
dc.contributor.authorGradinger, Rolf Rudolf
dc.contributor.authorHøyland, Knut Vilhelm
dc.contributor.authorLange, Benjamin
dc.contributor.authorSalganik, Evgenii
dc.date.accessioned2022-11-30T09:02:00Z
dc.date.available2022-11-30T09:02:00Z
dc.date.created2022-02-07T10:08:38Z
dc.date.issued2022
dc.identifier.issn2325-1026
dc.identifier.urihttps://hdl.handle.net/11250/3034928
dc.description.abstractYear-round observations of the physical snow and ice properties and processes that govern the ice pack evolution and its interaction with the atmosphere and the ocean were conducted during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition of the research vessel Polarstern in the Arctic Ocean from October 2019 to September 2020. This work was embedded into the interdisciplinary design of the 5 MOSAiC teams, studying the atmosphere, the sea ice, the ocean, the ecosystem, and biogeochemical processes.The overall aim of the snow and sea ice observations during MOSAiC was to characterize the physical properties of the snow and ice cover comprehensively in the central Arctic over an entire annual cycle. This objective was achieved by detailed observations of physical properties and of energy and mass balance of snow and ice. By studying snow and sea ice dynamics over nested spatial scales from centimeters to tens of kilometers, the variability across scales can be considered. On-ice observations of in situ and remote sensing properties of the different surface types over all seasons will help to improve numerical process and climate models and to establish and validate novel satellite remote sensing methods; the linkages to accompanying airborne measurements, satellite observations, and results of numerical models are discussed. We found large spatial variabilities of snow metamorphism and thermal regimes impacting sea ice growth. We conclude that the highly variable snow cover needs to be considered in more detail (in observations, remote sensing, and models) to better understand snow-related feedback processes.The ice pack revealed rapid transformations and motions along the drift in all seasons. The number of coupled ice–ocean interface processes observed in detail are expected to guide upcoming research with respect to the changing Arctic sea ice.en_US
dc.language.isoengen_US
dc.publisherUniversity of California Pressen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectPolarekspedisjoneren_US
dc.subjectPolar expeditionsen_US
dc.subjectPolare områderen_US
dc.subjectPolar regionsen_US
dc.subjectSjøisen_US
dc.subjectSea iceen_US
dc.subjectSnøen_US
dc.subjectSnowen_US
dc.titleOverview of the MOSAiC expedition: Snow and sea iceen_US
dc.title.alternativeOverview of the MOSAiC expedition: Snow and sea iceen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.subject.nsiVDP::Geofag: 450en_US
dc.subject.nsiVDP::Geosciences: 450en_US
dc.subject.nsiVDP::Geofag: 450en_US
dc.subject.nsiVDP::Geosciences: 450en_US
dc.source.volume10en_US
dc.source.journalElementa: Science of the Anthropoceneen_US
dc.source.issue1en_US
dc.identifier.doi10.1525/elementa.2021.000046
dc.identifier.cristin1998408
dc.relation.projectNorges forskningsråd: 280292en_US
dc.relation.projectNorges forskningsråd: 280531en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal