Supplemental material for "The diffusion of convective activity by cold pools"

This dataset is supplemental material to the manuscript "The diffusion of convective activity by cold pools," which has been submitted to the Journal of the Atmospheric Sciences. Fig. S1: Comparison between the longwave radiative heating rate and surface sensible heating rate in cold pool regions, using the Ev=1 experiment at t=4 days + 1 hour and showing the 100 km x 100 km southwest corner of the domain. (a) The total radiative heating rate (shortwave plus longwave) vertically averaged from 0 to z=281.6 m (the lowest four model levels), which is roughly the cold pool height (half the mixed layer depth). The nonuniform vertical grid spacing is considered using a trapezoidal integral. The air density is assumed vertically uniform for simplicity. We find but do not show here that the lowest model level contributes a considerable positive longwave heating rate, but the 2-4th vertical levels contribute to negative longwave heating rate. (b) The effective sensible heating rate is calculated by dividing the surface sensible heat flux by z=281.6 m. In cold pool regions (where the surface sensible heating rate is anomalously high), the total radiative heating rate (~0.25 K/day) is much smaller than the effective sensible heating rate (~2 K/day). Ev_sub_X.zip: The CM1 output for experiments Ev=0.2, 0.5, 0.7, 1.0, 1.2, 1.5, 1.7, 2.0. Each zip file contains the .nc output file at t=2.5 days and t=4 days + 1 hour. postprocessing_codes.zip: The postprocessing codes. The script coldpool_size.m diagnoses the mean cold pool size and stores the result in R_array.mat. The script theory.m reads R_array.mat and calculates the cloud interaction length scale. If you have any questions, please contact Dr. Hao Fu: [e-mail]