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Progress in Earth and Planetary Science
Fig. 17 | Progress in Earth and Planetary Science

Fig. 17

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

Fig. 17

© The Meteorological Society of Japan. Used with permission

Domain-averaged cloud cover for a total, b thin, c medium, and d thick high clouds for the simulations with and without an SGS condensation scheme for ice water condensate (labeled as ICE and NOICE, respectively) using SSTs of 300 (black) and 304 (red) K. e Cloud cover response to increasing SST for the total (purple), thin (green), medium (blue), and thick (orange) high clouds. High clouds were defined based on the International Satellite Cloud Climatology Project definition of cloud types (Rossow and Schiffer 1999). From Ohno et al. (2020),

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