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dc.contributor.authorSchuler, Thomas Vikhamar
dc.contributor.authorKohler, Jack
dc.contributor.authorElagina, Nelly
dc.contributor.authorHagen, Jon Ove Methlie
dc.contributor.authorHodson, Andrew
dc.contributor.authorJania, Jacek A.
dc.contributor.authorKääb, Andreas Max
dc.contributor.authorLuks, Bartłomiej
dc.contributor.authorMałecki, Jakub
dc.contributor.authorMoholdt, Geir
dc.contributor.authorPohjola, Veijo A.
dc.contributor.authorSobota, Ireneusz
dc.contributor.authorVan Pelt, Ward J. J.
dc.coverage.spatialSvalbarden_US
dc.date.accessioned2021-02-02T14:37:58Z
dc.date.available2021-02-02T14:37:58Z
dc.date.created2020-08-05T12:33:04Z
dc.date.issued2020
dc.identifier.citationSchuler, T. V., Kohler, J., Elagina, N., Hagen, J. O. M., Hodson, A. J., Jania, J. A., … Van Pelt, W. J. J. (2020). Reconciling Svalbard glacier mass balance. Frontiers in Earth Science, 8.en_US
dc.identifier.issn2296-6463
dc.identifier.urihttps://hdl.handle.net/11250/2725878
dc.description.abstractSince the first estimates of Svalbard-wide glacier mass balance were made in the early 2000s, there has been great progress in remote sensing and modeling of mass balance, existing field records have been extended, field records at new locations have been added, and there has been considerable environmental change. There is a wide spread in the available estimates of both total mass balance and surface or climatic mass balance, but there is overall agreement that the glaciers on Svalbard have been losing mass since the 1960s, with a tendency toward more negative mass balance since 2000. We define criteria to select data that are representative and of high credibility; this subset shows a more coherent evolution and reduced spread. In addition, we combine individual field mass balance records collected by different groups into a single dataset that samples glaciers across Svalbard and a range of different size classes. We find a close relationship between measured specific surface mass balance and size of the glacier, in such a way that smaller glaciers experience more negative surface mass balances. A qualitatively similar relationship between the accumulation area ratio and glacier area is found for all glaciers in the Svalbard, suggesting that the relation derived from glaciological records is not only an artifact caused by the limited number of samples (n = 12). We apply this relation to upscale measured surface mass balance for a new estimate for all glaciers of Svalbard. Our reconciled estimates are −7 ± 4 Gt a–1 (2000–2019) for the climatic mass balance, and −8 ± 6 Gt a–1 for the total mass balance. The difference between the two represents the sum of frontal ablation and the combined uncertainty, which together amount to ca. −2 ± 7 Gt a–1. While this is consistent with a previous estimate of Svalbard-wide frontal ablation, the uncertainties are large. Furthermore, several large and long-lasting surges have had considerable and multi-year impact on the total mass balance, and in particular on calving rates, emphasizing the need for better-resolved and more frequently updated estimates of frontal ablation.en_US
dc.language.isoengen_US
dc.publisherFrontiers Media S.A.en_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectArctic glaciersen_US
dc.subjectglacier mass balanceen_US
dc.subjectmass balance modelingen_US
dc.subjectglaciological mass balanceen_US
dc.subjectgeodetic mass balanceen_US
dc.subjectglacier gravimetryen_US
dc.titleReconciling Svalbard Glacier Mass Balanceen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright © 2020 Schuler, Kohler, Elagina, Hagen, Hodson, Jania, Kääb, Luks, Małecki, Moholdt, Pohjola, Sobota and Van Pelten_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Kvartærgeologi, glasiologi: 465en_US
dc.source.pagenumber16en_US
dc.source.volume8en_US
dc.source.journalFrontiers in Earth Scienceen_US
dc.identifier.doi10.3389/feart.2020.00156
dc.identifier.cristin1821769
dc.relation.projectNorges forskningsråd: 251658en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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