When cold pools are removed from large-eddy simulations of trade cumulus, reduced precipitation keeps the boundary layer moister, cutting clear-sky longwave cooling and producing a 1.88 W/m2 top-of-atmosphere warming.
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Warming from cold pools: A pathway for mesoscale organization to alter Earth's radiation budget
When cold pools are removed from large-eddy simulations of trade cumulus, reduced precipitation keeps the boundary layer moister, cutting clear-sky longwave cooling and producing a 1.88 W/m2 top-of-atmosphere warming.