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Diverse landscapes beneath Pine Island Glacier influence ice flow

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dc.contributor.authorBingham, Robert
dc.contributor.authorVaughan, David
dc.contributor.authorKing, Edward
dc.contributor.authorDavies, Damon
dc.contributor.authorCornford, Stephen
dc.contributor.authorSmith, Andrew
dc.contributor.authorArthern, Robert
dc.contributor.authorBrisbourne, Alex
dc.contributor.authorDe Rydt, Jan
dc.contributor.authorGraham, Alastair
dc.contributor.authorSpagnolo, Matteo
dc.contributor.authorMarsh, Oliver
dc.contributor.authorShean, David E
dc.contributor.institutionUniversity of Aberdeen.The Northen
dc.contributor.institutionUniversity of Aberdeen.Energyen
dc.contributor.institutionUniversity of Aberdeen.Geography & Environmenten
dc.contributor.institutionUniversity of Aberdeen.Cryosphere and Climate Change Research Groupen
dc.date.accessioned2017-12-06T17:43:36Z
dc.date.available2017-12-06T17:43:36Z
dc.date.issued2017-11-20
dc.descriptionThis work was supported by funding from the UK Natural Environment Research Council (NERC) iSTAR Programme (Grants NE/J005665 and NE/K011189), NERC grants NE/B502287/1 and NE/J004766/1 and the British Antarctic Survey (BAS) Polar Science for Planet Earth Programme. D.E.S. was supported by a NASA NESSF fellowship (NNX12AN36H). Bathymetric data used for Fig. 2c and f were sourced from the Bolin Centre Database Oden Mapping Data (cruise OSO 0910; http://oden.geo.su.se/oso0910) and NSF/IEDA Marine Geoscience Data System (http://www.marine-geo.org/tools/search/Files.php?data_set_uid=20080) respectively, and we thank the lead authors M. Jakobsson and F.O. Nitsche for their lodging. All fieldwork was supported by the staff at BAS’s Rothera Research Station and members of the iSTAR Traverse. In particular, we thank James Wake, Tim Gee, Jonny Yates (2013/14), David Routledge (2010/11) and Feargal Buckley, Chris Griffiths and Julian Scott (2007/08) for their help with data acquisition. We thank three anonymous referees for thorough and constructive reviews, which improved the final form of the manuscript.en
dc.description.statusPeer revieweden
dc.format.extent9
dc.format.extent4022626
dc.identifier109249919
dc.identifierb3346e18-73e1-4922-ac8a-689f2f29b6de
dc.identifier85034638063
dc.identifier.citationBingham, R, Vaughan, D, King, E, Davies, D, Cornford, S, Smith, A, Arthern, R, Brisbourne, A, De Rydt, J, Graham, A, Spagnolo, M, Marsh, O & Shean, D E 2017, 'Diverse landscapes beneath Pine Island Glacier influence ice flow', Nature Communications, vol. 8, 1618. https://doi.org/10.1038/s41467-017-01597-yen
dc.identifier.doi10.1038/s41467-017-01597-y
dc.identifier.issn2041-1723
dc.identifier.otherORCID: /0000-0002-2753-338X/work/45204748
dc.identifier.urihttp://hdl.handle.net/2164/9694
dc.identifier.vol8en
dc.language.isoeng
dc.relation.ispartofNature Communicationsen
dc.subjectcryospheric scienceen
dc.subjectgeomorphologyen
dc.subjectgeophysicsen
dc.subjectQE Geologyen
dc.subjectNatural Environment Research Council (NERC)en
dc.subjectNE/J005665en
dc.subjectNE/K011189en
dc.subjectNE/B502287/1en
dc.subjectNE/J004766/1en
dc.subject.lccQEen
dc.titleDiverse landscapes beneath Pine Island Glacier influence ice flowen
dc.typeJournal articleen

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