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dc.contributor.authorPearce, Danielle
dc.contributor.authorMair, Douglas
dc.contributor.authorRea, Brice
dc.contributor.authorLea, James
dc.contributor.authorSchofield, J. Edward
dc.contributor.authorKamenos, Nicholas
dc.contributor.authorSchoenrock, Kathryn
dc.date.accessioned2018-08-16T00:15:50Z
dc.date.available2018-08-16T00:15:50Z
dc.date.issued2018-02-08
dc.identifier.citationPearce , D , Mair , D , Rea , B , Lea , J , Schofield , J E , Kamenos , N & Schoenrock , K 2018 , ' The glacial geomorphology of upper Godthåbsfjord (Nuup Kangerlua) in south-west Greenland ' , Journal of Maps , vol. 14 , no. 2 , pp. 45-55 . https://doi.org/10.1080/17445647.2017.1422447
dc.identifier.issn1744-5647
dc.identifier.otherORCID: /0000-0002-6889-224X/work/62752115
dc.identifier.urihttp://hdl.handle.net/2299/20424
dc.description© 2018 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
dc.description.abstractThe Greenland Ice Sheet (GrIS) is known to have experienced widespread retreat over the last century. Information on outlet glacier dynamics, prior to this, are limited due to both a lack of observations and a paucity of mapped or mappable deglacial evidence which restricts our understanding of centennial to millennial timescale dynamics of the GrIS. Here we present glacial geomorphological mapping, for upper Godthåbsfjord, covering 5800 km 2 at a scale of 1:92,000, using a combination of ASTER GDEM V2, a medium-resolution DEM (error < 10 m horizontal and < 6 m vertical accuracy), panchromatic orthophotographs and ground truthing. This work provides a detailed geomorphological assessment for the area, compiled as a single map, comprising of moraines, meltwater channels, streamlined bedrock, sediment lineations, ice-dammed lakes, trimlines, terraces, gullied sediment and marine limits. Whilst some of the landforms have been previously identified, the new information presented here improves our understanding of ice margin behaviour and can be used for future numerical modelling and landform dating programmes. Data also form the basis for palaeoglaciological reconstructions and contribute towards understanding of the centennial to millennial timescale record of this sector of the GrIS.en
dc.format.extent11
dc.format.extent4478398
dc.language.isoeng
dc.relation.ispartofJournal of Maps
dc.subjectGeomorphology
dc.subjectGodthåbsfjord
dc.subjectGreenland Ice Sheet
dc.subjectLittle Ice Age
dc.subjectMoraine
dc.subjectTidewater glacier
dc.subjectGeography, Planning and Development
dc.subjectEarth and Planetary Sciences (miscellaneous)
dc.titleThe glacial geomorphology of upper Godthåbsfjord (Nuup Kangerlua) in south-west Greenlanden
dc.contributor.institutionSchool of Life and Medical Sciences
dc.contributor.institutionDepartment of Biological and Environmental Sciences
dc.contributor.institutionAgriculture and Environmental Management Research
dc.description.statusPeer reviewed
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85049065809&partnerID=8YFLogxK
rioxxterms.versionofrecord10.1080/17445647.2017.1422447
rioxxterms.typeJournal Article/Review
herts.preservation.rarelyaccessedtrue


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