Basal freeze-on generates complex ice-sheet stratigraphy
Large, plume-like internal ice-layer-structures have been observed in radar images from both Antarctica and Greenland, rising from the ice-sheet base to up to half of the ice thickness. Their origins are not yet understood. Here, we simulate their genesis by basal freeze-on using numerical ice-flow...
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ftnerc:oai:nora.nerc.ac.uk:521446 2023-05-15T13:41:42+02:00 Basal freeze-on generates complex ice-sheet stratigraphy Leysinger Vieli, GJ-MC Martin, Carlos Hindmarsh, Richard Lüthi, MP 2018-11-07 text http://nora.nerc.ac.uk/id/eprint/521446/ https://nora.nerc.ac.uk/id/eprint/521446/1/10.1038_s41467-018-07083-3.pdf https://doi.org/10.1038/s41467-018-07083-3 en eng https://nora.nerc.ac.uk/id/eprint/521446/1/10.1038_s41467-018-07083-3.pdf Leysinger Vieli, GJ-MC; Martin, Carlos orcid:0000-0002-2661-169X Hindmarsh, Richard orcid:0000-0003-1633-2416 Lüthi, MP. 2018 Basal freeze-on generates complex ice-sheet stratigraphy. Nature Communications, 9 (4669). 13, pp. https://doi.org/10.1038/s41467-018-07083-3 <https://doi.org/10.1038/s41467-018-07083-3> cc_by_nc_4 CC-BY-NC Publication - Article PeerReviewed 2018 ftnerc https://doi.org/10.1038/s41467-018-07083-3 2023-02-04T19:47:20Z Large, plume-like internal ice-layer-structures have been observed in radar images from both Antarctica and Greenland, rising from the ice-sheet base to up to half of the ice thickness. Their origins are not yet understood. Here, we simulate their genesis by basal freeze-on using numerical ice-flow modelling and analyse the transient evolution of the emerging ice-plume and the surrounding ice-layer structure as a function of both freeze-on rate and ice flux. We find good agreement between radar observations, modelled ice-plume geometry and internal layer structure, and further show that plume height relates primarily to ice-flux and only secondarily to freeze-on. An in-depth analysis, performed for Northern Greenland of observed spatial plume distribution related to ice flow, basal topography and water availability supports our findings regarding ice flux and suggests freeze-on is controlled by ascending subglacial water flow. Our results imply that widespread basal freeze-on strongly affects ice stratigraphy and consequently ice-core interpretations. Article in Journal/Newspaper Antarc* Antarctica Greenland ice core Ice Sheet Natural Environment Research Council: NERC Open Research Archive Greenland Nature Communications 9 1 |
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Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
English |
description |
Large, plume-like internal ice-layer-structures have been observed in radar images from both Antarctica and Greenland, rising from the ice-sheet base to up to half of the ice thickness. Their origins are not yet understood. Here, we simulate their genesis by basal freeze-on using numerical ice-flow modelling and analyse the transient evolution of the emerging ice-plume and the surrounding ice-layer structure as a function of both freeze-on rate and ice flux. We find good agreement between radar observations, modelled ice-plume geometry and internal layer structure, and further show that plume height relates primarily to ice-flux and only secondarily to freeze-on. An in-depth analysis, performed for Northern Greenland of observed spatial plume distribution related to ice flow, basal topography and water availability supports our findings regarding ice flux and suggests freeze-on is controlled by ascending subglacial water flow. Our results imply that widespread basal freeze-on strongly affects ice stratigraphy and consequently ice-core interpretations. |
format |
Article in Journal/Newspaper |
author |
Leysinger Vieli, GJ-MC Martin, Carlos Hindmarsh, Richard Lüthi, MP |
spellingShingle |
Leysinger Vieli, GJ-MC Martin, Carlos Hindmarsh, Richard Lüthi, MP Basal freeze-on generates complex ice-sheet stratigraphy |
author_facet |
Leysinger Vieli, GJ-MC Martin, Carlos Hindmarsh, Richard Lüthi, MP |
author_sort |
Leysinger Vieli, GJ-MC |
title |
Basal freeze-on generates complex ice-sheet stratigraphy |
title_short |
Basal freeze-on generates complex ice-sheet stratigraphy |
title_full |
Basal freeze-on generates complex ice-sheet stratigraphy |
title_fullStr |
Basal freeze-on generates complex ice-sheet stratigraphy |
title_full_unstemmed |
Basal freeze-on generates complex ice-sheet stratigraphy |
title_sort |
basal freeze-on generates complex ice-sheet stratigraphy |
publishDate |
2018 |
url |
http://nora.nerc.ac.uk/id/eprint/521446/ https://nora.nerc.ac.uk/id/eprint/521446/1/10.1038_s41467-018-07083-3.pdf https://doi.org/10.1038/s41467-018-07083-3 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Greenland ice core Ice Sheet |
genre_facet |
Antarc* Antarctica Greenland ice core Ice Sheet |
op_relation |
https://nora.nerc.ac.uk/id/eprint/521446/1/10.1038_s41467-018-07083-3.pdf Leysinger Vieli, GJ-MC; Martin, Carlos orcid:0000-0002-2661-169X Hindmarsh, Richard orcid:0000-0003-1633-2416 Lüthi, MP. 2018 Basal freeze-on generates complex ice-sheet stratigraphy. Nature Communications, 9 (4669). 13, pp. https://doi.org/10.1038/s41467-018-07083-3 <https://doi.org/10.1038/s41467-018-07083-3> |
op_rights |
cc_by_nc_4 |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.1038/s41467-018-07083-3 |
container_title |
Nature Communications |
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9 |
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1 |
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1766154064208330752 |