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dc.contributor.authorSlater, D. A.
dc.contributor.authorNienow, P. W.
dc.contributor.authorCowton, T. R.
dc.contributor.authorGoldberg, D. N.
dc.contributor.authorSole, A. J.
dc.date.accessioned2017-09-18T12:30:12Z
dc.date.available2017-09-18T12:30:12Z
dc.date.issued2015-05-15
dc.identifier.citationSlater , D A , Nienow , P W , Cowton , T R , Goldberg , D N & Sole , A J 2015 , ' Effect of near-terminus subglacial hydrology on tidewater glacier submarine melt rates ' , Geophysical Research Letters , vol. 42 , no. 8 , pp. 2861-2868 . https://doi.org/10.1002/2014GL062494en
dc.identifier.issn0094-8276
dc.identifier.otherPURE: 245779514
dc.identifier.otherPURE UUID: 852d6f90-2411-4161-9d55-d9f7e3c26d3b
dc.identifier.otherRIS: urn:C938608B7B38D614A0A5296FFF9D0EDA
dc.identifier.otherScopus: 84929508941
dc.identifier.otherORCID: /0000-0003-1668-7372/work/60427792
dc.identifier.otherWOS: 000354560800038
dc.identifier.otherORCID: /0000-0001-8394-6149/work/70619157
dc.identifier.urihttp://hdl.handle.net/10023/11684
dc.descriptionD. A. S is supported by a NERC PhD studentship. T. R. C is supported by NERC grant NE/K014609/1 awarded to P. W. N and A. J. S.en
dc.description.abstractSubmarine melting of Greenlandic tidewater glacier termini is proposed as a possible mechanism driving their recent thinning and retreat. We use a general circulation model, MITgcm, to simulate water circulation driven by subglacial discharge at the terminus of an idealized tidewater glacier. We vary the spatial distribution of subglacial discharge emerging at the grounding line of the glacier and examine the effect on submarine melt volume and distribution. We find that subglacial hydrology exerts an important control on submarine melting; under certain conditions a distributed system can induce a factor 5 more melt than a channelized system, with plumes from a single channel inducing melt over only a localized area. Subglacial hydrology also controls the spatial distribution of melt, which has the potential to control terminus morphology and calving style. Our results highlight the need to constrain near-terminus subglacial hydrology at tidewater glaciers if we are to represent ocean forcing accurately.
dc.language.isoeng
dc.relation.ispartofGeophysical Research Lettersen
dc.rights©2015. 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.subjectGreenland ice sheeten
dc.subjectIce-ocean interactionsen
dc.subjectModelingen
dc.subjectSubglacial hydrologyen
dc.subjectSubmarine meltingen
dc.subjectTidewater glaciersen
dc.subjectGE Environmental Sciencesen
dc.subject3rd-DASen
dc.subjectBDCen
dc.subjectR2Cen
dc.subject.lccGEen
dc.titleEffect of near-terminus subglacial hydrology on tidewater glacier submarine melt ratesen
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.identifier.doihttps://doi.org/10.1002/2014GL062494
dc.description.statusPeer revieweden
dc.identifier.urlhttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014GL062494#support-information-sectionen


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