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.

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Autores principales:	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
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/0a70821dadac4d4c8cbf60fe810ae850
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spelling	oai:doaj.org-article:0a70821dadac4d4c8cbf60fe810ae8502021-12-02T16:58:23ZIce stream motion facilitated by a shallow-deforming and accreting bed10.1038/ncomms107232041-1723https://doaj.org/article/0a70821dadac4d4c8cbf60fe810ae8502016-02-01T00:00:00Zhttps://doi.org/10.1038/ncomms10723https://doaj.org/toc/2041-1723Ice 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.Matteo SpagnoloEmrys PhillipsJan A. PiotrowskiBrice R. ReaChris D. ClarkChris R. StokesSimon J. CarrJeremy C. ElyAdriano RiboliniWojciech WysotaIzabela SzumanNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-11 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q 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
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.
format	article
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
title	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_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_sort	ice stream motion facilitated by a shallow-deforming and accreting bed
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/0a70821dadac4d4c8cbf60fe810ae850
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Ice stream motion facilitated by a shallow-deforming and accreting bed

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