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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Main Authors: Thiede, Jörn, Lindemann, Frank
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1998
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.693818
https://doi.pangaea.de/10.1594/PANGAEA.693818
id ftdatacite:10.1594/pangaea.693818
record_format openpolar
spelling 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
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