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.
Main Authors: | , , , , , , , , , , |
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Format: | Article |
Language: | English |
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Nature Portfolio
2016-02-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/ncomms10723 |
_version_ | 1819194668845367296 |
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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. |
first_indexed | 2024-12-23T02:00:32Z |
format | Article |
id | doaj.art-0a70821dadac4d4c8cbf60fe810ae850 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-23T02:00:32Z |
publishDate | 2016-02-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
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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