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Open solid arrows depict vertical horizontal motion, with size proportional to magnitude. View larger version 99K Fig. Journal of the Atmospheric Sciences April , Vol. Black hashes near the top indicate time periods of missing data where the time gap between scans exceeded 23 min. Part I: Convective signals. Wakimoto, : Thermodynamic variability within the convective boundary layer due to horizontal convective rolls. View larger version 43K Fig. During this preonset stage of the MJO, the diurnal cycle is manifest in a pronounced daytime invigoration of convective clouds and cumulus moistening of the low—midtroposphere, fundamentally driven by oceanic diurnal warm layers. Figure 5 reveals that this evaporative moistening works in opposition to the drying by subsidence and horizontal advection.

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