Results of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+)

dc.bibliographicCitation.firstPage2283
dc.bibliographicCitation.issue7
dc.bibliographicCitation.journalTitleThe Cryosphereeng
dc.bibliographicCitation.lastPage2301
dc.bibliographicCitation.volume14
dc.contributor.authorCornford, Stephen L.
dc.contributor.authorSeroussi, Helene
dc.contributor.authorAsay-Davis, Xylar S.
dc.contributor.authorGudmundsson, G. Hilmar
dc.contributor.authorArthern, Rob
dc.contributor.authorBorstad, Chris
dc.contributor.authorChristmann, Julia
dc.contributor.authordos Santos, Thiago Dias
dc.contributor.authorFeldmann, Johannes
dc.contributor.authorGoldberg, Daniel
dc.contributor.authorHoffman, Matthew J.
dc.contributor.authorHumbert, Angelika
dc.contributor.authorKleiner, Thomas
dc.contributor.authorLeguy, Gunter
dc.contributor.authorLipscomb, William H.
dc.contributor.authorMerino, Nacho
dc.contributor.authorDurand, Gaël
dc.contributor.authorMorlighem, Mathieu
dc.contributor.authorPollard, David
dc.contributor.authorRückamp, Martin
dc.contributor.authorWilliams, C. Rosie
dc.contributor.authorYu, Hongju
dc.date.accessioned2022-12-09T07:11:18Z
dc.date.available2022-12-09T07:11:18Z
dc.date.issued2020
dc.description.abstractWe present the result of the third Marine Ice Sheet Model Intercomparison Project, MISMIP+. MISMIP+ is intended to be a benchmark for ice-flow models which include fast sliding marine ice streams and floating ice shelves and in particular a treatment of viscous stress that is sufficient to model buttressing, where upstream ice flow is restrained by a downstream ice shelf. A set of idealized experiments first tests that models are able to maintain a steady state with the grounding line located on a retrograde slope due to buttressing and then explore scenarios where a reduction in that buttressing causes ice stream acceleration, thinning, and grounding line retreat. The majority of participating models passed the first test and then produced similar responses to the loss of buttressing. We find that the most important distinction between models in this particular type of simulation is in the treatment of sliding at the bed, with other distinctions - notably the difference between the simpler and more complete treatments of englacial stress but also the differences between numerical methods - taking a secondary role. © 2020 Wolters Kluwer Medknow Publications. All rights reserved.eng
dc.description.versionpublishedVersion
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/10565
dc.identifier.urihttp://dx.doi.org/10.34657/9601
dc.language.isoeng
dc.publisherKatlenburg-Lindau : Copernicus
dc.relation.doihttps://doi.org/10.5194/tc-14-2283-2020
dc.relation.essn1994-0416
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subject.ddc550
dc.subject.otherfull-stokes modeleng
dc.subject.othergrounding-lineeng
dc.subject.otherhigher-ordereng
dc.subject.otherbasal frictioneng
dc.subject.otheradaptive mesheng
dc.subject.otherfloweng
dc.subject.otherglaciereng
dc.subject.otherperformanceeng
dc.subject.otherapproximationeng
dc.subject.othersimulationseng
dc.titleResults of the third Marine Ice Sheet Model Intercomparison Project (MISMIP+)eng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccess
wgl.contributorPIK
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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