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Experimental observation of transient 18 O interaction between snow and advective airflow under various temperature gradient conditions

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Table 1. Morphological properties and flow characteristics of the experimental runs: µCT measured snow density (ρ), porosity (ε), specificsurface area per unit mass (SSA), mean pore space diameter (dmean), superficial velocity in snow (uD), corresponding Reyn
Figure 2. Temporal isotopic composition offor each of the experimental runs. The spikes in the δ18O of the outflow δ18O were dueto small temperature changes in the cold laboratory (Ebner et al.,2014)

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