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A double continuum hydrological model for glacier applications

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dc.contributor.authorde Fleurian, B.
dc.contributor.authorGagliardini, O.
dc.contributor.authorZwinger, T.
dc.contributor.authorDurand, G.
dc.contributor.authorLe Meur, E.
dc.contributor.authorMair, D.
dc.contributor.authorRaback, P.
dc.contributor.institutionUniversity of Aberdeen.Geography & Environmenten
dc.date.accessioned2014-10-15T11:26:02Z
dc.date.available2014-10-15T11:26:02Z
dc.date.issued2014
dc.description.statusPeer revieweden
dc.format.extent17
dc.format.extent5007214
dc.identifier35560821
dc.identifierf782b309-857e-4a12-8280-1f21a6bd7999
dc.identifier000332317000010
dc.identifier84893073532
dc.identifier.citationde Fleurian, B, Gagliardini, O, Zwinger, T, Durand, G, Le Meur, E, Mair, D & Raback, P 2014, 'A double continuum hydrological model for glacier applications', The Cryosphere, vol. 8, no. 1, pp. 137-153. https://doi.org/10.5194/tc-8-137-2014en
dc.identifier.doi10.5194/tc-8-137-2014
dc.identifier.iss1en
dc.identifier.issn1994-0416
dc.identifier.urihttp://hdl.handle.net/2164/3724
dc.identifier.vol8en
dc.language.isoeng
dc.relation.ispartofThe Cryosphereen
dc.subjectsubglacial water-pressureen
dc.subjecthigh-velocity eventen
dc.subjectice-sheeten
dc.subjectdrainage systemen
dc.subjecttemperature glaciersen
dc.subjectseasonal-changesen
dc.subjectbasal motionen
dc.subjectSwitzerlanden
dc.subjectflowen
dc.subjectdarollaen
dc.subjectQE Geologyen
dc.subject.lccQEen
dc.titleA double continuum hydrological model for glacier applicationsen
dc.typeJournal articleen

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