Figure shows these cumulative distributions for the nucleation and solidification times. As expected, both increase with increasing storage temperature. For the nucleation times, this increase occurs over several orders of magnitude and we also find that the broadness of the distributions increases with temperature; for -8°C, the distributions span more than one order of magnitude in time, while close to none variability is observed at -40°C due to the more pronounced cooling. At -40°C, freezing occurs sequentially from the outside towards the core and the individual populations do not overlap; this is a direct consequence of operating in the cooling-limited regime. On the other hand, at -8°C, freezing takes place in the nucleation limited-regime, and significant overlap between the populations is observed.