Ice stream motion facilitated by a shallow-deforming and accreting bed

Ice streams are fundamental to ice sheet dynamics, but the mechanisms controlling their flow remain elusive. Here, the authors perform macro- and microscale analyses of mega-scale glacial lineations, which indicate a continuously accreting, shallow-deforming bed during ice stream flow.

Bibliographic Details
Main Authors: Matteo Spagnolo, Emrys Phillips, Jan A. Piotrowski, Brice R. Rea, Chris D. Clark, Chris R. Stokes, Simon J. Carr, Jeremy C. Ely, Adriano Ribolini, Wojciech Wysota, Izabela Szuman
Format: Article
Language:English
Published: Nature Portfolio 2016-02-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/ncomms10723
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author Matteo Spagnolo
Emrys Phillips
Jan A. Piotrowski
Brice R. Rea
Chris D. Clark
Chris R. Stokes
Simon J. Carr
Jeremy C. Ely
Adriano Ribolini
Wojciech Wysota
Izabela Szuman
author_facet Matteo Spagnolo
Emrys Phillips
Jan A. Piotrowski
Brice R. Rea
Chris D. Clark
Chris R. Stokes
Simon J. Carr
Jeremy C. Ely
Adriano Ribolini
Wojciech Wysota
Izabela Szuman
author_sort Matteo Spagnolo
collection DOAJ
description Ice streams are fundamental to ice sheet dynamics, but the mechanisms controlling their flow remain elusive. Here, the authors perform macro- and microscale analyses of mega-scale glacial lineations, which indicate a continuously accreting, shallow-deforming bed during ice stream flow.
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spelling doaj.art-0a70821dadac4d4c8cbf60fe810ae8502022-12-21T18:03:59ZengNature PortfolioNature Communications2041-17232016-02-017111110.1038/ncomms10723Ice stream motion facilitated by a shallow-deforming and accreting bedMatteo Spagnolo0Emrys Phillips1Jan A. Piotrowski2Brice R. Rea3Chris D. Clark4Chris R. Stokes5Simon J. Carr6Jeremy C. Ely7Adriano Ribolini8Wojciech Wysota9Izabela Szuman10Department of Geography and Environment, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen AB243UF, UKBritish Geological SurveyDepartment of Geoscience, Aarhus University, DK-8000 Aarhus C, DenmarkDepartment of Geography and Environment, School of Geosciences, University of Aberdeen, Elphinstone Road, Aberdeen AB243UF, UKDepartment of Geography, University of SheffieldDepartment of Geography, Durham UniversitySchool of Geography, Queen Mary University of LondonDepartment of Geography, University of SheffieldDipartimento di Scienze della Terra, University of Pisa, 56126 Pisa, ItalyFaculty of Earth Sciences, Nicolaus Copernicus UniversityDepartment of Geomorphology, Adam Mickiewicz UniversityIce streams are fundamental to ice sheet dynamics, but the mechanisms controlling their flow remain elusive. Here, the authors perform macro- and microscale analyses of mega-scale glacial lineations, which indicate a continuously accreting, shallow-deforming bed during ice stream flow.https://doi.org/10.1038/ncomms10723
spellingShingle Matteo Spagnolo
Emrys Phillips
Jan A. Piotrowski
Brice R. Rea
Chris D. Clark
Chris R. Stokes
Simon J. Carr
Jeremy C. Ely
Adriano Ribolini
Wojciech Wysota
Izabela Szuman
Ice stream motion facilitated by a shallow-deforming and accreting bed
Nature Communications
title Ice stream motion facilitated by a shallow-deforming and accreting bed
title_full Ice stream motion facilitated by a shallow-deforming and accreting bed
title_fullStr Ice stream motion facilitated by a shallow-deforming and accreting bed
title_full_unstemmed Ice stream motion facilitated by a shallow-deforming and accreting bed
title_short Ice stream motion facilitated by a shallow-deforming and accreting bed
title_sort ice stream motion facilitated by a shallow deforming and accreting bed
url https://doi.org/10.1038/ncomms10723
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