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Estimates of ikaite export from sea ice to the underlying seawater in a sea ice–seawater mesocosm

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Figure

Figure 1. The Sea-ice Environmental Research Facility (Universityof Manitoba, Winnipeg, Canada) with thin sea ice covering the pondduring the 2013 experiment
Figure 2. Evolution of (a) air temperature (◦C) at 2 m height, (b) snow thickness (black shaded areas) and sea ice/seawater temperature (◦C),(c) bulk ice salinity, (d) brine volume content within sea ice and (e) seawater temperature (blue) and salinity (gr
Table 1. Seawater conditions on 11 January, before any sea ice formation (on 29 January, at the end of the experiment
Figure 5. Air–ice CO2 fluxes (mmolm−2 d−1). Positive air–iceCO2 flux means outgassing from the ice, and negative CO2 fluxmeans uptake of atmospheric CO2
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