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Figure 5 reveals that this evaporative moistening works in opposition to the drying by subsidence and horizontal advection. Vertical dashed lines indicate local noon. This diurnal cycle is manifest in a daytime growth of cumulus clouds in both depth and areal coverage in response to oceanic diurnal warm layers, which drive a daytime increase of the air—sea fluxes of heat and moisture. The relatively bottom-heavy heating implies that convective inflow i. This daytime surface warming drives an increase in surface fluxes, which invigorates moist convection by reducing convective inhibition Fig. Cotturone, : Multiscale variability of the atmospheric mixed layer over the western Pacific warm pool.

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