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Progress in Earth and Planetary Science
Fig. 8 | Progress in Earth and Planetary Science

Fig. 8

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

Fig. 8

Horizontal distribution of the mean 8 m s−1 radius (R08) on a 5º × 5º grid box for a the control experiment (CTL) and b the global warming experiment (GW), and c the difference between them (GW minus CTL). Panel d indicates the zonal mean of R08 in CTL (solid line) and GW (dashed line) for each ocean basin: the North Atlantic (70ºW–20ºW), the eastern North Pacific (180º–120ºW), the western North Pacific (140ºE–180º), the South Pacific (160ºW–120ºE), and the South Indian Ocean (50ºE–110ºE)

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