Fig. 7: Example experiment of a perfect ice-active particle population following the time-independent description. | npj Climate and Atmospheric Science

Fig. 7: Example experiment of a perfect ice-active particle population following the time-independent description.

From: Stochastic nucleation processes and substrate abundance explain time-dependent freezing in supercooled droplets

Fig. 7

The green line in a and b shows the frozen fraction for a cooling rate experiment and the experimental temperature, T, profile over time, t, respectively. The characteristic temperature at which all ice-active sites on particles nucleate ice, Tc, is indicated. Note that b is enlarged to show a longer time period. Squares in a show the frozen fraction for a single nucleation site.31

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