CO2 and CH4 in sea ice from a subarctic fjord under influence of riverine input

peer reviewed We present the CH4 concentration [CH4], the par- tial pressure of CO2 (pCO2) and the total gas content in bulk sea ice from subarctic, land-fast sea ice in the Kapisillit fjord, Greenland. Fjord systems are characterized by freshwater runoff and riverine input and based on $\delta$18O...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Crabeck, O., Delille, Bruno, Thomas, David, Geilfus, N.-X., Rysgaard, S., Tison, J.-L.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2014
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Online Access:https://orbi.uliege.be/handle/2268/176908
https://orbi.uliege.be/bitstream/2268/176908/1/Crabeck%20et%20al%202014%20BG.pdf
https://doi.org/10.5194/bg-11-6525-2014
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Summary:peer reviewed We present the CH4 concentration [CH4], the par- tial pressure of CO2 (pCO2) and the total gas content in bulk sea ice from subarctic, land-fast sea ice in the Kapisillit fjord, Greenland. Fjord systems are characterized by freshwater runoff and riverine input and based on $\delta$18O data, we show that >30\% of the surface water originated from periodic river input during ice growth. This resulted in fresher sea-ice layers with higher gas content than is typical from marine sea ice. The bulk ice [CH4] ranged from 1.8 to 12.1 nmolL−1, which corresponds to a partial pressure ranging from 3 to 28ppmv. This is markedly higher than the average atmo- spheric methane content of 1.9ppmv. Evidently most of the trapped methane within the icewas contained inside bubbles, and only a minor portion was dissolved in the brines. The bulk ice pCO2 ranged from 60 to 330ppmv indicating that sea ice at temperatures above −4 ◦C is undersaturated com- pared to the atmosphere (390 ppmv). This study adds to the few existing studies of CH4 and CO2 in sea ice, and we con- clude that subarctic seawater can be a sink for atmospheric CO2, while being a net source of CH4.