is strikingly different – e.g., for CCA
evaporation, uLG (t‘) is at a minimum (maximum) value at
h 90 (see, in particular, Fig. 8 in Ref. [27]) – supporting that
while our steady-state experiments were designed for the coexistence
of both extreme modes of evaporation (i.e., CCR and CCA),
the results better represent dynamic CCR evaporation data in the
literature.