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Progress in Earth and Planetary Science
Fig. 18 | Progress in Earth and Planetary Science

Fig. 18

From: Recent global nonhydrostatic modeling approach without using a cumulus parameterization to understand the mechanisms underlying cloud changes due to global warming

Fig. 18

Binned vertical profiles of the turbulent diffusivity K (color and white lines) and the ice condensate (black lines) calculated a with and b without the SGS ice condensation scheme in the turbulent closure scheme, sorted by the ice water path. K and ice water path were calculated using a snapshot dataset from the ICE simulation with an SST of 300 K. c and d are the same as (a) and (b), respectively, for the simulation with an SST of 304 K. From Ohno et al. (2020)

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