Skip to main content
. Author manuscript; available in PMC: 2020 Aug 4.
Published in final edited form as: NPJ Clim Atmos Sci. 2020 Jan 17;3(1):2. doi: 10.1038/s41612-020-0106-4

Fig. 4. Evaluation of the assumption of identical or variable INP surface area (ISA) per droplet for isothermal freezing experiment, ISO3.

Fig. 4

a Experimentally derived and simulated unfrozen fraction of isothermal freezing experiment with 5th and 95th percentiles given by shading applying lognormally distributed ISA per droplet. Data in a are taken from Fig. 3a. b Calculated Jhet using lognormally distributed ISA per droplet referred to as Jhetactual. The shading is the range of the upper and lower fiducial limits following Poission statistics at the 0.999 confidence level. Simulation results in b are taken from Fig. 4a. c Experimentally derived and recalculated Jhet assuming identical ISA per droplet equal to measured mean BET values, termed Jhetapparent, are shown as open circles and shading, respectively. Jhetapparent derived from the model was calculated from the modeled UnF in a. The red solid lines are mean model values.