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Fig. 1 | Progress in Earth and Planetary Science

Fig. 1

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

Fig. 1

Schematic of the influence of convective aggregation on outgoing longwave radiation in cases where convection becomes (left) more aggregated and (right) less aggregated. Wavy upward arrows indicate longwave radiation. Longwave radiations with thick arrows in darker color and thin arrows in lighter color show those emitted from the earth’s surface and from high clouds, respectively

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