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Progress in Earth and Planetary Science
Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

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

Fig. 10

Composite of future minus past precipitation amount averaged over all the oceanic extratropical cyclones (top row) and the intense oceanic extratropical cyclones (bottom row) for (left to right): 56 km, 28 km, and 14 km mesh models. Gray circles indicate the distance from the center of the extratropical cyclone in intervals of 500 km

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