Fig. 5From: Recent global nonhydrostatic modeling approach without using a cumulus parameterization to understand the mechanisms underlying cloud changes due to global warming© The American Geophysical Union. Used with permissionDomain-averaged vertical profiles of a the net, b positive, and c negative tendencies of ice clouds due to cloud microphysical processes at equilibrium states in radiative-convective equilibrium simulations with a SST of 300 or 304 K. From Ohno et al. (2021),Back to article page