Sediments in arctic sea ice - entrainment, characterization and quantification ...
Sediments in Arctic sea ice are important for erosion and redistribution and consequently a factor for the sediment budget of the Arctic Ocean. The processes leading to the incorporation of sediments into the ice are not understood in detail yet. In the present study, experiments on the incorporatio...
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ftdatacite:10.1594/pangaea.693818 2024-09-15T17:53:54+00:00 Sediments in arctic sea ice - entrainment, characterization and quantification ... Thiede, Jörn Lindemann, Frank 1998 application/zip https://dx.doi.org/10.1594/pangaea.693818 https://doi.pangaea.de/10.1594/PANGAEA.693818 en eng PANGAEA https://dx.doi.org/10.2312/bzp_0283_1998 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Ice station ARK-XI/1 Transdrift-III Polarstern Kapitan Dranitsyn Quaternary Environment of the Eurasian North QUEEN article Collection Supplementary Publication Series of Datasets 1998 ftdatacite https://doi.org/10.1594/pangaea.69381810.2312/bzp_0283_1998 2024-07-03T13:10:33Z Sediments in Arctic sea ice are important for erosion and redistribution and consequently a factor for the sediment budget of the Arctic Ocean. The processes leading to the incorporation of sediments into the ice are not understood in detail yet. In the present study, experiments on the incorporation of sediments were therefore conducted in ice tanks of The Hamburg Ship Model Basin (HSVA) in winter 1996/1997, These experiments showed that on average 75 % of the artificial sea-ice sediments were located in the brine-channel system. The sediments were scavenged from the water column by frazil ice. Sediments functioning as a nucleus for the formation of frazil ice were less important for the incorporation. Filtration in grease ice during relatively calm hydrodynamic conditions was probably an effective process to enrich sediments in the ice. Wave fields did not play an important role for the incorporation of sediments into the artificial sea ice.During the expedition TRANSDRIFT III (TDIII, October 1995), ... : Supplement to: Lindemann, Frank (1998): Sedimente im arktischen Meereis - Eintrag, Charakterisierung und Quantifizierung (Sediments in arctic sea ice - entrainment, characterization and quantification). Berichte zur Polarforschung = Reports on Polar Research, 283, 124 pp ... Article in Journal/Newspaper Arctic Ocean Arktis* Sea ice DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Ice station ARK-XI/1 Transdrift-III Polarstern Kapitan Dranitsyn Quaternary Environment of the Eurasian North QUEEN |
spellingShingle |
Ice station ARK-XI/1 Transdrift-III Polarstern Kapitan Dranitsyn Quaternary Environment of the Eurasian North QUEEN Thiede, Jörn Lindemann, Frank Sediments in arctic sea ice - entrainment, characterization and quantification ... |
topic_facet |
Ice station ARK-XI/1 Transdrift-III Polarstern Kapitan Dranitsyn Quaternary Environment of the Eurasian North QUEEN |
description |
Sediments in Arctic sea ice are important for erosion and redistribution and consequently a factor for the sediment budget of the Arctic Ocean. The processes leading to the incorporation of sediments into the ice are not understood in detail yet. In the present study, experiments on the incorporation of sediments were therefore conducted in ice tanks of The Hamburg Ship Model Basin (HSVA) in winter 1996/1997, These experiments showed that on average 75 % of the artificial sea-ice sediments were located in the brine-channel system. The sediments were scavenged from the water column by frazil ice. Sediments functioning as a nucleus for the formation of frazil ice were less important for the incorporation. Filtration in grease ice during relatively calm hydrodynamic conditions was probably an effective process to enrich sediments in the ice. Wave fields did not play an important role for the incorporation of sediments into the artificial sea ice.During the expedition TRANSDRIFT III (TDIII, October 1995), ... : Supplement to: Lindemann, Frank (1998): Sedimente im arktischen Meereis - Eintrag, Charakterisierung und Quantifizierung (Sediments in arctic sea ice - entrainment, characterization and quantification). Berichte zur Polarforschung = Reports on Polar Research, 283, 124 pp ... |
format |
Article in Journal/Newspaper |
author |
Thiede, Jörn Lindemann, Frank |
author_facet |
Thiede, Jörn Lindemann, Frank |
author_sort |
Thiede, Jörn |
title |
Sediments in arctic sea ice - entrainment, characterization and quantification ... |
title_short |
Sediments in arctic sea ice - entrainment, characterization and quantification ... |
title_full |
Sediments in arctic sea ice - entrainment, characterization and quantification ... |
title_fullStr |
Sediments in arctic sea ice - entrainment, characterization and quantification ... |
title_full_unstemmed |
Sediments in arctic sea ice - entrainment, characterization and quantification ... |
title_sort |
sediments in arctic sea ice - entrainment, characterization and quantification ... |
publisher |
PANGAEA |
publishDate |
1998 |
url |
https://dx.doi.org/10.1594/pangaea.693818 https://doi.pangaea.de/10.1594/PANGAEA.693818 |
genre |
Arctic Ocean Arktis* Sea ice |
genre_facet |
Arctic Ocean Arktis* Sea ice |
op_relation |
https://dx.doi.org/10.2312/bzp_0283_1998 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.69381810.2312/bzp_0283_1998 |
_version_ |
1810430016546144256 |