Temporal Dynamics of Ikaite in Experimental Sea Ice

Here we present evidence for highly dynamic ikaite precipitation and dissolution in sea ice grown at an outdoor pool of the Sea-ice Environmental Research Facility (SERF) in Manitoba, Canada. During the experiment, ikaite precipitated in sea ice when temperatures were below -4 Celsius, creating three distinct zones of ikaite concentrations: (1) a millimeter-to-centimeter-thin surface layer containing frost flowers and brine skim with bulk ikaite concentrations of > 2000 &#956;mol kg-1, (2) an internal layer with ikaite concentrations of 200-400 &#956;mol kg-1, and (3) a bottom layer with ikaite concentrations of < 100 &#956;mol kg-1. Snowfall events caused the sea ice to warm and ikaite crystals to dissolve. Manual removal of the snow cover allowed the sea ice to cool and brine salinities to increase, resulting in rapid ikaite precipitation. The observed ikaite concentrations were on the same order of magnitude as modeled by FREZCHEM, which further supports the notion that ikaite concentration in sea ice increases with decreasing temperature. Thus, varying snow conditions may play a key role in ikaite precipitation and dissolution in sea ice. This could have a major implication for CO2 exchange with the atmosphere and ocean that has not been accounted for previously.

Source https://www.polardata.ca/pdcsearch/PDCSearchDOI.jsp?doi_id=12169
Metadata Access http://www.polardata.ca/oai/provider?verb=GetRecord&metadataPrefix=fgdc&identifier=12169_fgdc
Creator Rysgaard, Søren
Publisher Canadian Cryospheric Information Network
Contributor Polar Data Catalogue
Publication Year 2015
Rights Research programs, CCIN, or ArcticNet take no liability for the use or transmission of this data
OpenAccess true
Contact rysgaard(at)umanitoba.ca; pdc(at)uwaterloo.ca
Language English
Format Computer file
Discipline Biogeochemistry;Chemistry
Spatial Coverage (-97.130W, 49.900S, -97.130E, 49.900N)
Temporal Coverage Begin 2013-01-10T00:00:00Z
Temporal Coverage End 2013-01-31T00:00:00Z