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Progress in Earth and Planetary Science
Fig. 6 | Progress in Earth and Planetary Science

Fig. 6

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

Fig. 6

a Domain-averaged high-cloud cover and b its response to a SST change in control simulations (CTRL) and simulations with a lower limit of pressure for the evaluation of the terminal velocity of ice particles (VTp440) and diffusivity of water vapour in air (KVp440). Differences in c high-cloud cover and d the responses between the control (CTRL) and sensitivity (SENS) simulations. From Ohno et al. (2021)

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