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. Author manuscript; available in PMC: 2019 Sep 18.
Published in final edited form as: Atmos Chem Phys. 2018;18:1065–1078. doi: 10.5194/acp-18-1065-2018

Figure 5.

Figure 5.

Simulated changes in (a) Rei and (b) ice crystal number concentration (Ni) and the fraction of ice crystal number produced by heterogeneous nucleation (het.) as a function of the total aerosol number concentration. Simulations are conducted for two initial water vapor mass mixing ratios (pv), an indicator of available water amount for ice formation. The ratios of externally mixed dust (deposition INP), coated dust (immersion INP), and sulfate (not INP) are prescribed values of 0.75 : 0.25 : 10000 in all experiments.