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dc.contributor.authorCornish, S.B.
dc.contributor.authorJohnson, H.L.
dc.contributor.authorMallett, R.D.C.
dc.contributor.authorDörr, Jakob Simon
dc.contributor.authorKostov, Y.
dc.contributor.authorRichards, A.E.
dc.date.accessioned2023-01-20T14:11:51Z
dc.date.available2023-01-20T14:11:51Z
dc.date.created2023-01-02T17:04:06Z
dc.date.issued2022
dc.identifier.issn2041-1723
dc.identifier.urihttps://hdl.handle.net/11250/3045017
dc.description.abstractThe volume, extent and age of Arctic sea ice is in decline, yet winter sea ice production appears to have been increasing, despite Arctic warming being most intense during winter. Previous work suggests that further warming will at some point lead to a decline in ice production, however a consistent explanation of both rise and fall is hitherto missing. Here, we investigate these driving factors through a simple linear model for ice production. We focus on the Kara and Laptev seas-sometimes referred to as Arctic “ice factories” for their outsized role in ice production, and train the model on internal variability across the Community Earth System Model’s Large Ensemble (CESM-LE). The linear model is highly skilful at explaining internal variability and can also explain the forced rise-then-fall of ice production, providing insight into the competing drivers of change. We apply our linear model to the same climate variables from observation-based data; the resulting estimate of ice production over recent decades suggests that, just as in CESM-LE, we are currently passing the peak of ice production in the Kara and Laptev seas.en_US
dc.language.isoengen_US
dc.publisherSpringer Natureen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleRise and fall of sea ice production in the Arctic Ocean’s ice factoriesen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2022 the authorsen_US
dc.source.articlenumber7800en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1038/s41467-022-34785-6
dc.identifier.cristin2099112
dc.source.journalNature Communicationsen_US
dc.identifier.citationNature Communications. 2022, 13, 7800.en_US
dc.source.volume13en_US


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