Subglacial floods beneath ice sheets.

Subglacial floods (jökulhlaups) are well documented as occurring beneath present day glaciers and ice caps. In addition, it is known that massive floods have occurred from ice-dammed lakes proximal to the Laurentide ice sheet during the last ice age, and it has been suggested that at least one such...

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Published in:Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Evatt, G, Fowler, A, Clark, C, Hulton, N
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.1098/rsta.2006.1798
https://ora.ox.ac.uk/objects/uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc
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spelling ftuloxford:oai:ora.ox.ac.uk:uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc 2023-05-15T16:40:14+02:00 Subglacial floods beneath ice sheets. Evatt, G Fowler, A Clark, C Hulton, N 2016-07-28 https://doi.org/10.1098/rsta.2006.1798 https://ora.ox.ac.uk/objects/uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc eng eng doi:10.1098/rsta.2006.1798 https://ora.ox.ac.uk/objects/uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc https://doi.org/10.1098/rsta.2006.1798 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1098/rsta.2006.1798 2022-06-28T20:11:28Z Subglacial floods (jökulhlaups) are well documented as occurring beneath present day glaciers and ice caps. In addition, it is known that massive floods have occurred from ice-dammed lakes proximal to the Laurentide ice sheet during the last ice age, and it has been suggested that at least one such flood below the waning ice sheet was responsible for a dramatic cooling event some 8000 years ago. We propose that drainage of lakes from beneath ice sheets will generally occur in a time-periodic fashion, and that such floods can be of severe magnitude. Such hydraulic eruptions are likely to have caused severe climatic disturbances in the past, and may well do so in the future. Article in Journal/Newspaper Ice Sheet ORA - Oxford University Research Archive Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 364 1844 1769 1794
institution Open Polar
collection ORA - Oxford University Research Archive
op_collection_id ftuloxford
language English
description Subglacial floods (jökulhlaups) are well documented as occurring beneath present day glaciers and ice caps. In addition, it is known that massive floods have occurred from ice-dammed lakes proximal to the Laurentide ice sheet during the last ice age, and it has been suggested that at least one such flood below the waning ice sheet was responsible for a dramatic cooling event some 8000 years ago. We propose that drainage of lakes from beneath ice sheets will generally occur in a time-periodic fashion, and that such floods can be of severe magnitude. Such hydraulic eruptions are likely to have caused severe climatic disturbances in the past, and may well do so in the future.
format Article in Journal/Newspaper
author Evatt, G
Fowler, A
Clark, C
Hulton, N
spellingShingle Evatt, G
Fowler, A
Clark, C
Hulton, N
Subglacial floods beneath ice sheets.
author_facet Evatt, G
Fowler, A
Clark, C
Hulton, N
author_sort Evatt, G
title Subglacial floods beneath ice sheets.
title_short Subglacial floods beneath ice sheets.
title_full Subglacial floods beneath ice sheets.
title_fullStr Subglacial floods beneath ice sheets.
title_full_unstemmed Subglacial floods beneath ice sheets.
title_sort subglacial floods beneath ice sheets.
publishDate 2016
url https://doi.org/10.1098/rsta.2006.1798
https://ora.ox.ac.uk/objects/uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc
genre Ice Sheet
genre_facet Ice Sheet
op_relation doi:10.1098/rsta.2006.1798
https://ora.ox.ac.uk/objects/uuid:49da3789-7a60-4ecd-a9c3-3c85db87a7dc
https://doi.org/10.1098/rsta.2006.1798
op_rights info:eu-repo/semantics/embargoedAccess
op_doi https://doi.org/10.1098/rsta.2006.1798
container_title Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 364
container_issue 1844
container_start_page 1769
op_container_end_page 1794
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