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Fig. 21 | Progress in Earth and Planetary Science

Fig. 21

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

Fig. 21

Relationships between horizontally averaged radar reflectivity (Zm) and optical depth from the cloud top (τd) for the case of thin clouds with polluted cloud condensate nuclei. Results are shown for a the bin scheme, b the bulk scheme with (νc, νr) = (1, − 1/3), c the bulk scheme with (νc, νr) = (− 1/3, 1). d–f are the same as a–c, respectively, but excluding droplets with a radius less than 8 μm from the calculation performed by the Joint Simulator. The flow of time is drawn in black, red, green and blue. From Kuba et al. (2020)

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