Dynamics of subglacial floods

The Nye model of jökulhlaups is able to explain both their periodicity and even the detailed shape of the flood hydrograph. In this paper, we show how the model can be used to predict the shape of the hydrographs from the subglacial lake Grímsvötn beneath Vatnajökull in Iceland, and we comment on th...

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Published in:Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Author: Fowler, A.C.
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2009
Subjects:
Online Access:http://dx.doi.org/10.1098/rspa.2008.0488
https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2008.0488
https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2008.0488
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spelling crroyalsociety:10.1098/rspa.2008.0488 2024-09-30T14:37:12+00:00 Dynamics of subglacial floods Fowler, A.C. 2009 http://dx.doi.org/10.1098/rspa.2008.0488 https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2008.0488 https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2008.0488 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences volume 465, issue 2106, page 1809-1828 ISSN 1364-5021 1471-2946 journal-article 2009 crroyalsociety https://doi.org/10.1098/rspa.2008.0488 2024-09-17T04:34:45Z The Nye model of jökulhlaups is able to explain both their periodicity and even the detailed shape of the flood hydrograph. In this paper, we show how the model can be used to predict the shape of the hydrographs from the subglacial lake Grímsvötn beneath Vatnajökull in Iceland, and we comment on three particular issues that have proved contentious in the application of the Nye model: the role of water temperature; the shape of the flood channel; and the value of the bed roughness coefficient. Article in Journal/Newspaper Iceland Vatnajökull The Royal Society Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420) Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 465 2106 1809 1828
institution Open Polar
collection The Royal Society
op_collection_id crroyalsociety
language English
description The Nye model of jökulhlaups is able to explain both their periodicity and even the detailed shape of the flood hydrograph. In this paper, we show how the model can be used to predict the shape of the hydrographs from the subglacial lake Grímsvötn beneath Vatnajökull in Iceland, and we comment on three particular issues that have proved contentious in the application of the Nye model: the role of water temperature; the shape of the flood channel; and the value of the bed roughness coefficient.
format Article in Journal/Newspaper
author Fowler, A.C.
spellingShingle Fowler, A.C.
Dynamics of subglacial floods
author_facet Fowler, A.C.
author_sort Fowler, A.C.
title Dynamics of subglacial floods
title_short Dynamics of subglacial floods
title_full Dynamics of subglacial floods
title_fullStr Dynamics of subglacial floods
title_full_unstemmed Dynamics of subglacial floods
title_sort dynamics of subglacial floods
publisher The Royal Society
publishDate 2009
url http://dx.doi.org/10.1098/rspa.2008.0488
https://royalsocietypublishing.org/doi/pdf/10.1098/rspa.2008.0488
https://royalsocietypublishing.org/doi/full-xml/10.1098/rspa.2008.0488
long_lat ENVELOPE(-16.823,-16.823,64.420,64.420)
geographic Vatnajökull
geographic_facet Vatnajökull
genre Iceland
Vatnajökull
genre_facet Iceland
Vatnajökull
op_source Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
volume 465, issue 2106, page 1809-1828
ISSN 1364-5021 1471-2946
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rspa.2008.0488
container_title Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 465
container_issue 2106
container_start_page 1809
op_container_end_page 1828
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