Namely, the drying by large-scale circulation wanes as the low—midtroposphere humidifies and the convective cloud population is invigorated Fig. Vertical dashed lines indicate local noon. View larger version 69K Fig. Zuidema, : The mesoscale convection life cycle: Building block or prototype for large-scale tropical waves? SH and LH have been smoothed using a 1-h running mean. The diurnal cycle in SST relates to oceanic diurnal warm layers that form under light-wind, clear-sky conditions Halpern and Reed ; Matthews et al.
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