Massive subsurface ice formed by refreezing of ice-shelf melt ponds

The influence of surface ponding on the interior of ice shelves is currently unknown. Here, the authors combine surface and borehole geophysics on the Larsen C Ice Shelf, Antarctica, with remote sensing and modelling and show how pond refreezing increases ice shelf density and temperature.

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Autores principales:	Bryn Hubbard, Adrian Luckman, David W. Ashmore, Suzanne Bevan, Bernd Kulessa, Peter Kuipers Munneke, Morgane Philippe, Daniela Jansen, Adam Booth, Heidi Sevestre, Jean-Louis Tison, Martin O’Leary, Ian Rutt
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/203a8531cede46309726ae68494c650a
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id	oai:doaj.org-article:203a8531cede46309726ae68494c650a
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spelling	oai:doaj.org-article:203a8531cede46309726ae68494c650a2021-12-02T14:38:56ZMassive subsurface ice formed by refreezing of ice-shelf melt ponds10.1038/ncomms118972041-1723https://doaj.org/article/203a8531cede46309726ae68494c650a2016-06-01T00:00:00Zhttps://doi.org/10.1038/ncomms11897https://doaj.org/toc/2041-1723The influence of surface ponding on the interior of ice shelves is currently unknown. Here, the authors combine surface and borehole geophysics on the Larsen C Ice Shelf, Antarctica, with remote sensing and modelling and show how pond refreezing increases ice shelf density and temperature.Bryn HubbardAdrian LuckmanDavid W. AshmoreSuzanne BevanBernd KulessaPeter Kuipers MunnekeMorgane PhilippeDaniela JansenAdam BoothHeidi SevestreJean-Louis TisonMartin O’LearyIan RuttNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-6 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Bryn Hubbard Adrian Luckman David W. Ashmore Suzanne Bevan Bernd Kulessa Peter Kuipers Munneke Morgane Philippe Daniela Jansen Adam Booth Heidi Sevestre Jean-Louis Tison Martin O’Leary Ian Rutt Massive subsurface ice formed by refreezing of ice-shelf melt ponds
description	The influence of surface ponding on the interior of ice shelves is currently unknown. Here, the authors combine surface and borehole geophysics on the Larsen C Ice Shelf, Antarctica, with remote sensing and modelling and show how pond refreezing increases ice shelf density and temperature.
format	article
author	Bryn Hubbard Adrian Luckman David W. Ashmore Suzanne Bevan Bernd Kulessa Peter Kuipers Munneke Morgane Philippe Daniela Jansen Adam Booth Heidi Sevestre Jean-Louis Tison Martin O’Leary Ian Rutt
author_facet	Bryn Hubbard Adrian Luckman David W. Ashmore Suzanne Bevan Bernd Kulessa Peter Kuipers Munneke Morgane Philippe Daniela Jansen Adam Booth Heidi Sevestre Jean-Louis Tison Martin O’Leary Ian Rutt
author_sort	Bryn Hubbard
title	Massive subsurface ice formed by refreezing of ice-shelf melt ponds
title_short	Massive subsurface ice formed by refreezing of ice-shelf melt ponds
title_full	Massive subsurface ice formed by refreezing of ice-shelf melt ponds
title_fullStr	Massive subsurface ice formed by refreezing of ice-shelf melt ponds
title_full_unstemmed	Massive subsurface ice formed by refreezing of ice-shelf melt ponds
title_sort	massive subsurface ice formed by refreezing of ice-shelf melt ponds
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/203a8531cede46309726ae68494c650a
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Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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