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dc.contributor.authorYoung, T. J.
dc.contributor.authorChristoffersen, P.
dc.contributor.authorDoyle, S. H.
dc.contributor.authorNicholls, K. W.
dc.contributor.authorStewart, C. L.
dc.contributor.authorHubbard, B.
dc.contributor.authorHubbard, A.
dc.contributor.authorLok, L. B.
dc.contributor.authorBrennan, P.
dc.contributor.authorBenn, D. I.
dc.contributor.authorLuckman, A.
dc.contributor.authorBougamont, M.
dc.identifier.citationYoung , T J , Christoffersen , P , Doyle , S H , Nicholls , K W , Stewart , C L , Hubbard , B , Hubbard , A , Lok , L B , Brennan , P , Benn , D I , Luckman , A & Bougamont , M 2019 , ' Physical conditions of fast glacier flow : 3. Seasonally-evolving ice deformation on Store Glacier, West Greenland ' , Journal of Geophysical Research - Earth Surface , vol. 124 , no. 1 , pp. 245-267 .
dc.identifier.otherPURE: 257340161
dc.identifier.otherPURE UUID: f98b7b44-abf5-4833-82d0-cfd7812572d9
dc.identifier.otherRIS: urn:EA35D6BE95891453D1C345FE8C393F32
dc.identifier.otherScopus: 85060968958
dc.identifier.otherWOS: 000458729900014
dc.identifier.otherORCID: /0000-0002-3604-0886/work/64697398
dc.identifier.otherORCID: /0000-0001-5865-3459/work/133187397
dc.descriptionThis research was funded by the University of Cambridge Fieldwork Funds, by UK National Environment Research Council grants NE/K006126 and NE/K0058871/1, and by an Aberystwyth University Capital Equipment grant to BH.en
dc.description.abstractTemporal variations in ice sheet flow directly impact the internal structure within ice sheets through englacial deformation. Large‐scale changes in the vertical stratigraphy within ice sheets have been previously conducted on centennial to millennial timescales; however, intra‐annual changes in the morphology of internal layers have yet to be explored. Over a period of two years, we use autonomous phase‐sensitive radio‐echo sounding (ApRES) to track the daily displacement of internal layers on Store Glacier, West Greenland to millimeter accuracy. At a site located ∼30 km from the calving terminus, where the ice is ∼600m thick and flows at ∼700m a−1, we measure distinct seasonal variations in vertical velocities and vertical strain rates over a two‐year period. Prior to the melt season (March–June), we observe increasingly non‐linear englacial deformation with negative vertical strain rates (i.e. strain thinning) in the upper half of the ice column of ∼‐0.03a−1, whereas the ice below thickens under vertical strain reaching up to 0.16a−1. Early in the melt season (June–July), vertical thinning gradually ceases as the glacier increasingly thickens. During late summer to midwinter (August–February), vertical thickening occurs linearly throughout the entire ice column, with strain rates averaging 0.016a−1. We show that these complex variations are unrelated to topographic setting and localized basal slip, and hypothesize that this seasonality is driven by far‐field perturbations in the glacier's force balance, in this case generated by variations in basal hydrology near the glacier's terminus and propagated tens of kilometers upstream through longitudinal coupling.
dc.relation.ispartofJournal of Geophysical Research - Earth Surfaceen
dc.rightsCopyright © 2019 The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en
dc.subjectIce Sheeten
dc.subjectGE Environmental Sciencesen
dc.titlePhysical conditions of fast glacier flow : 3. Seasonally-evolving ice deformation on Store Glacier, West Greenlanden
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. School of Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews. Bell-Edwards Geographic Data Instituteen
dc.description.statusPeer revieweden

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