Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland
Discharge and water temperature measurements in the Skaftá river and measurements of the lowering of the ice over the subglacial lake at the western Skaftá cauldron, Vatnajökull, Iceland, were made during a rapidly rising glacial outburst flood (jökulhlaup) in September 2006. Outflow from the lake,...
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Cambridge University Press
2017
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Online Access: | https://doi.org/10.1017/jog.2017.33 https://doaj.org/article/a9f555123fd64d2e81bd744ae91796bf |
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ftdoajarticles:oai:doaj.org/article:a9f555123fd64d2e81bd744ae91796bf 2023-05-15T16:21:41+02:00 Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland BERGUR EINARSSON TÓMAS JÓHANNESSON THORSTEINN THORSTEINSSON ERIC GAIDOS THOMAS ZWINGER 2017-08-01T00:00:00Z https://doi.org/10.1017/jog.2017.33 https://doaj.org/article/a9f555123fd64d2e81bd744ae91796bf EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143017000338/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.33 0022-1430 1727-5652 https://doaj.org/article/a9f555123fd64d2e81bd744ae91796bf Journal of Glaciology, Vol 63, Pp 670-682 (2017) glacier hydrology jökulhlaups (GLOFs) subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2017.33 2023-03-12T01:30:59Z Discharge and water temperature measurements in the Skaftá river and measurements of the lowering of the ice over the subglacial lake at the western Skaftá cauldron, Vatnajökull, Iceland, were made during a rapidly rising glacial outburst flood (jökulhlaup) in September 2006. Outflow from the lake, flood discharge at the glacier terminus and the transient subglacial volume of floodwater during the jökulhlaup are derived from these data. The 40 km long initial subglacial path of the jökulhlaup was mainly formed by lifting and deformation of the overlying ice, induced by water pressure in excess of the ice overburden pressure. Melting of ice due to the heat of the floodwater from the subglacial lake and frictional heat generated by the dissipation of potential energy in the flow played a smaller role. Therefore this event, like other rapidly rising jökulhlaups, cannot be explained by the jökulhlaup theory of Nye (1976). Instead, our observations indicate that they can be explained by a coupled subglacial-sheet–conduit mechanism where essentially all of the initial flood path is formed as a sheet by the propagation of a subglacial pressure wave. Article in Journal/Newspaper glacier Iceland Journal of Glaciology Vatnajökull Directory of Open Access Journals: DOAJ Articles Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420) Skaftá ENVELOPE(-17.933,-17.933,63.783,63.783) Journal of Glaciology 63 240 670 682 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier hydrology jökulhlaups (GLOFs) subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
glacier hydrology jökulhlaups (GLOFs) subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 BERGUR EINARSSON TÓMAS JÓHANNESSON THORSTEINN THORSTEINSSON ERIC GAIDOS THOMAS ZWINGER Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
topic_facet |
glacier hydrology jökulhlaups (GLOFs) subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Discharge and water temperature measurements in the Skaftá river and measurements of the lowering of the ice over the subglacial lake at the western Skaftá cauldron, Vatnajökull, Iceland, were made during a rapidly rising glacial outburst flood (jökulhlaup) in September 2006. Outflow from the lake, flood discharge at the glacier terminus and the transient subglacial volume of floodwater during the jökulhlaup are derived from these data. The 40 km long initial subglacial path of the jökulhlaup was mainly formed by lifting and deformation of the overlying ice, induced by water pressure in excess of the ice overburden pressure. Melting of ice due to the heat of the floodwater from the subglacial lake and frictional heat generated by the dissipation of potential energy in the flow played a smaller role. Therefore this event, like other rapidly rising jökulhlaups, cannot be explained by the jökulhlaup theory of Nye (1976). Instead, our observations indicate that they can be explained by a coupled subglacial-sheet–conduit mechanism where essentially all of the initial flood path is formed as a sheet by the propagation of a subglacial pressure wave. |
format |
Article in Journal/Newspaper |
author |
BERGUR EINARSSON TÓMAS JÓHANNESSON THORSTEINN THORSTEINSSON ERIC GAIDOS THOMAS ZWINGER |
author_facet |
BERGUR EINARSSON TÓMAS JÓHANNESSON THORSTEINN THORSTEINSSON ERIC GAIDOS THOMAS ZWINGER |
author_sort |
BERGUR EINARSSON |
title |
Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
title_short |
Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
title_full |
Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
title_fullStr |
Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
title_full_unstemmed |
Subglacial flood path development during a rapidly rising jökulhlaup from the western Skaftá cauldron, Vatnajökull, Iceland |
title_sort |
subglacial flood path development during a rapidly rising jökulhlaup from the western skaftá cauldron, vatnajökull, iceland |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/jog.2017.33 https://doaj.org/article/a9f555123fd64d2e81bd744ae91796bf |
long_lat |
ENVELOPE(-16.823,-16.823,64.420,64.420) ENVELOPE(-17.933,-17.933,63.783,63.783) |
geographic |
Vatnajökull Skaftá |
geographic_facet |
Vatnajökull Skaftá |
genre |
glacier Iceland Journal of Glaciology Vatnajökull |
genre_facet |
glacier Iceland Journal of Glaciology Vatnajökull |
op_source |
Journal of Glaciology, Vol 63, Pp 670-682 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143017000338/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.33 0022-1430 1727-5652 https://doaj.org/article/a9f555123fd64d2e81bd744ae91796bf |
op_doi |
https://doi.org/10.1017/jog.2017.33 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
240 |
container_start_page |
670 |
op_container_end_page |
682 |
_version_ |
1766009675895013376 |