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. Author manuscript; available in PMC: 2020 Aug 17.
Published in final edited form as: J Geophys Res Atmos. 2016 Apr 6;121(11):6299–6320. doi: 10.1002/2015JD024267

Table 2:

Numerical experiments performed in this study. “P” and “T” stand for the PRESTORM and TOGA COARE cases, respectively. “low” and “high” stand for low and high CCN concentration, respectively. “Warm” is for warm rain only, and “evap” indicates reduced evaporative cooling.

Case Name Description Domain mean rainfall (mm)
P-low PRESTORM continental case clean/background CCN over land 58.4
P-high 10 times CCN concentration as P-low 40.7
P-low-warm Same as P-low except for all ice microphysics are off 60.7
P-high-warm Same as P-high except for all ice microphysics are off 61.8
P-low-evap Same as P-low except for evaporation is turned off from the surface to 3km, between 1 and 3 hours 51.0
T-low TOGA-COARE maritime case clean/background CCN over ocean 19.0
T-high 10 times CCN concentration as T-low 33.0
T-low-warm Same as T-low except for all ice microphysics are off 18.0
T-high-warm Same as T-high except for all ice microphysics are off 24.7
T-high-evap Same as T-high except for evaporation is turned off from the surface to 4km, between 0 and 1.5 hours 26.4