The mechanisms behind Jakobshavn Isbræ's acceleration and mass loss: A 3‐D thermomechanical model study
Supporting Files
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2017
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Details
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Journal Title:Geophysical Research Letters
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NOAA Program & Office:
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Description:ThemechanismscausingwidespreadflowaccelerationofJakobshavnIsbræ,WestGreenland, remainuncleardespiteanabundanceofobservationsandmodelingstudies.Herewesimulatetheglacier’s evolutionfrom1985to2016usingathree-dimensionalthermomechanicaliceflowmodel.Themodel capturesthetimingand90%oftheobservedchangesbyforcingthecalvingfront.Basaldraginthetroughislow,andlateraldragbalancestheicestream’sdrivingstress.Thecalvingfrontpositionisthedominant controlonchangesofJakobshavnIsbræsincetheiceviscosityintheshearmarginsinstantaneouslydrops inresponsetothestressperturbationcausedbycalvingfrontretreat,whichallowsforwidespreadflowacceleration.Gradualshearmarginwarmingcontribut es5to10%tothetotalacceleration.Oursimulations suggest that the glacier will contribute to eustatic sea level rise at a rate comparable to or higher
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Keywords:
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Source:Geophysical Research Letters, 44(12), 6252-6260
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DOI:
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ISSN:0094-8276 ; 1944-8007
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Rights Information:Other
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Compliance:Library
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Main Document Checksum:urn:sha256:146fa01c430d1a1b1bae6af57bc772f5bbdbebc833e19dc77abeccd8cc862d40
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