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Annual air–sea exchange of CO2 in Young Sound, NE Greenland was estimated using pCO2 surface‐water measurements during summer (2006–2009) and during an ice‐covered winter 2008. All surface pCO2 values were below atmospheric levels indicating an uptake of atmospheric CO2. During sea ice formation, dissolved inorganic carbon (DIC) content is reduced causing sea ice to be under saturated in CO2. Approximately...
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