Temperature, salinity and ikaite crystal characteristics in snow, slush and sea ice during R/V Lance cruise in April-May 2011

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Main Authors: Nomura, Daiki, Assmy, Philipp, Nehrke, Gernot, Granskog, Mats A, Fischer, Michael, Dieckmann, Gerhard S, Fransson, Agneta, Hu, Yubin, Schnetger, Bernhard
Format: Dataset Open Access
Language:en
Published: PANGAEA 2011
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author Nomura, Daiki
Assmy, Philipp
Nehrke, Gernot
Granskog, Mats A
Fischer, Michael
Dieckmann, Gerhard S
Fransson, Agneta
Hu, Yubin
Schnetger, Bernhard
author_facet Nomura, Daiki
Assmy, Philipp
Nehrke, Gernot
Granskog, Mats A
Fischer, Michael
Dieckmann, Gerhard S
Fransson, Agneta
Hu, Yubin
Schnetger, Bernhard
collection Datos científicos de ciencias marinas y ambientales
contents We identified ikaite crystals (CaCO3 · 6H2O) and examined their shape and size distribution in first-year Arctic pack ice, overlying snow and slush layers during the spring melt onset north of Svalbard. Additional measurements of total alkalinity (TA) were made for melted snow and sea-ice samples. Ikaite crystals were mainly found in the bottom of the snowpack, in slush and the surface layers of the sea ice where the temperature was generally lower and salinity higher than in the ice below. Image analysis showed that ikaite crystals were characterized by a roughly elliptical shape and a maximum caliper diameter of 201.0±115.9 µm (n = 918). Since the ice-melting season had already started, ikaite crystals may already have begun to dissolve, which might explain the lack of a relationship between ikaite crystal size and sea-ice parameters (temperature, salinity, and thickness of snow and ice). Comparisons of salinity and TA profiles for melted ice samples suggest that the precipitation/dissolution of ikaite crystals occurred at the top of the sea ice and the bottom of the snowpack during ice formation/melting processes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_848979
institution PANGAEA
language en
publishDate 2011
publisher PANGAEA
record_format pangaea
spellingShingle Temperature, salinity and ikaite crystal characteristics in snow, slush and sea ice during R/V Lance cruise in April-May 2011
Nomura, Daiki
Assmy, Philipp
Nehrke, Gernot
Granskog, Mats A
Fischer, Michael
Dieckmann, Gerhard S
Fransson, Agneta
Hu, Yubin
Schnetger, Bernhard
Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
We identified ikaite crystals (CaCO3 · 6H2O) and examined their shape and size distribution in first-year Arctic pack ice, overlying snow and slush layers during the spring melt onset north of Svalbard. Additional measurements of total alkalinity (TA) were made for melted snow and sea-ice samples. Ikaite crystals were mainly found in the bottom of the snowpack, in slush and the surface layers of the sea ice where the temperature was generally lower and salinity higher than in the ice below. Image analysis showed that ikaite crystals were characterized by a roughly elliptical shape and a maximum caliper diameter of 201.0±115.9 µm (n = 918). Since the ice-melting season had already started, ikaite crystals may already have begun to dissolve, which might explain the lack of a relationship between ikaite crystal size and sea-ice parameters (temperature, salinity, and thickness of snow and ice). Comparisons of salinity and TA profiles for melted ice samples suggest that the precipitation/dissolution of ikaite crystals occurred at the top of the sea ice and the bottom of the snowpack during ice formation/melting processes.
title Temperature, salinity and ikaite crystal characteristics in snow, slush and sea ice during R/V Lance cruise in April-May 2011
topic Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; SPP1158
url https://doi.org/10.1594/PANGAEA.848979