Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland
For 3 years, during a 4-year observation period (2007-2010), jokulhlaups were observed from a lake at the northern margin of Russells Gletscher. At a gauging station located on a bedrock sill near the outlet of Watson River into Sdr Stromfjord, discharge and sediment transport was monitored during t...
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Language: | English |
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ftdtupubl:oai:pure.atira.dk:publications/a8c341d7-c372-4ec3-9240-7cf53bde7183 2024-09-15T18:09:07+00:00 Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland Mikkelsen, A. B. Hasholt, Bent Knudsen, N. T. Nielsen, Morten Holtegaard 2013 https://orbit.dtu.dk/en/publications/a8c341d7-c372-4ec3-9240-7cf53bde7183 https://doi.org/10.2166/nh.2012.165 eng eng https://orbit.dtu.dk/en/publications/a8c341d7-c372-4ec3-9240-7cf53bde7183 info:eu-repo/semantics/restrictedAccess Mikkelsen , A B , Hasholt , B , Knudsen , N T & Nielsen , M H 2013 , ' Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland ' , Hydrology Research , vol. 44 , no. 1 , pp. 58-67 . https://doi.org/10.2166/nh.2012.165 Greenland Nearctic region Kangerlussuaq Nearctic region Russells Gletscher Nearctic region Watson River Nearctic region englacial drainage condition jokulhlaups transport maximum discharge sediment transport 52803 Soil science - Genesis morphology classification geology Environmental Sciences article 2013 ftdtupubl https://doi.org/10.2166/nh.2012.165 2024-07-29T23:50:17Z For 3 years, during a 4-year observation period (2007-2010), jokulhlaups were observed from a lake at the northern margin of Russells Gletscher. At a gauging station located on a bedrock sill near the outlet of Watson River into Sdr Stromfjord, discharge and sediment transport was monitored during the jokulhlaups. The stage rose up to 5.3 m and a maximum discharge of 1,430 m(3) s(-1) was recorded. The jokulhlaups were very different, indicating varying influences of weather and englacial drainage conditions. Although the jokulhlaups caused high discharge and sediment transport rates, their share of the annual discharge and sediment transport were less than 2%. Article in Journal/Newspaper Greenland Kangerlussuaq Technical University of Denmark: DTU Orbit Hydrology Research 44 1 58 67 |
institution |
Open Polar |
collection |
Technical University of Denmark: DTU Orbit |
op_collection_id |
ftdtupubl |
language |
English |
topic |
Greenland Nearctic region Kangerlussuaq Nearctic region Russells Gletscher Nearctic region Watson River Nearctic region englacial drainage condition jokulhlaups transport maximum discharge sediment transport 52803 Soil science - Genesis morphology classification geology Environmental Sciences |
spellingShingle |
Greenland Nearctic region Kangerlussuaq Nearctic region Russells Gletscher Nearctic region Watson River Nearctic region englacial drainage condition jokulhlaups transport maximum discharge sediment transport 52803 Soil science - Genesis morphology classification geology Environmental Sciences Mikkelsen, A. B. Hasholt, Bent Knudsen, N. T. Nielsen, Morten Holtegaard Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
topic_facet |
Greenland Nearctic region Kangerlussuaq Nearctic region Russells Gletscher Nearctic region Watson River Nearctic region englacial drainage condition jokulhlaups transport maximum discharge sediment transport 52803 Soil science - Genesis morphology classification geology Environmental Sciences |
description |
For 3 years, during a 4-year observation period (2007-2010), jokulhlaups were observed from a lake at the northern margin of Russells Gletscher. At a gauging station located on a bedrock sill near the outlet of Watson River into Sdr Stromfjord, discharge and sediment transport was monitored during the jokulhlaups. The stage rose up to 5.3 m and a maximum discharge of 1,430 m(3) s(-1) was recorded. The jokulhlaups were very different, indicating varying influences of weather and englacial drainage conditions. Although the jokulhlaups caused high discharge and sediment transport rates, their share of the annual discharge and sediment transport were less than 2%. |
format |
Article in Journal/Newspaper |
author |
Mikkelsen, A. B. Hasholt, Bent Knudsen, N. T. Nielsen, Morten Holtegaard |
author_facet |
Mikkelsen, A. B. Hasholt, Bent Knudsen, N. T. Nielsen, Morten Holtegaard |
author_sort |
Mikkelsen, A. B. |
title |
Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
title_short |
Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
title_full |
Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
title_fullStr |
Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
title_full_unstemmed |
Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland |
title_sort |
jokulhlaups and sediment transport in watson river, kangerlussuaq, west greenland |
publishDate |
2013 |
url |
https://orbit.dtu.dk/en/publications/a8c341d7-c372-4ec3-9240-7cf53bde7183 https://doi.org/10.2166/nh.2012.165 |
genre |
Greenland Kangerlussuaq |
genre_facet |
Greenland Kangerlussuaq |
op_source |
Mikkelsen , A B , Hasholt , B , Knudsen , N T & Nielsen , M H 2013 , ' Jokulhlaups and sediment transport in Watson River, Kangerlussuaq, West Greenland ' , Hydrology Research , vol. 44 , no. 1 , pp. 58-67 . https://doi.org/10.2166/nh.2012.165 |
op_relation |
https://orbit.dtu.dk/en/publications/a8c341d7-c372-4ec3-9240-7cf53bde7183 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.2166/nh.2012.165 |
container_title |
Hydrology Research |
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44 |
container_issue |
1 |
container_start_page |
58 |
op_container_end_page |
67 |
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1810446520637456384 |