Wintertime measurements of pCO2 in Arctic landfast sea ice
Recent work has described how gas exchange can occur through sea ice. First, carbon fluxes over sea ice surfaces have been measured. Second, sea ice brine has an elevated capacity over seawater to absorb CO2(g) due to its cold temperature and chemical equilibrium promoting carbon phase changes....
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| Format: | Others |
| Language: | en_US |
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2008
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| Online Access: | http://hdl.handle.net/1993/3093 |
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