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Stechmann, : The skeleton of tropical intraseasonal oscillations. 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. Composite date ranges are a 7—13 Oct and b 11—16 Nov end dates are inclusive. The heating profile becomes progressively more top heavy as peak ascending motion shifts upward later in the active phase, indicating increasing stratiform rainfall. The afternoon invigoration of convection is driven by the afternoon peak in SST and air—sea fluxes, which owes to the influence of oceanic diurnal warm layers Figs. Budget terms are calculated as shown in 5 , with the Eulerian tendency black , horizontal advection red dotted—dashed , vertical advection red dotted , the sum of horizontal and vertical advection [SUM ADV ; red solid], and apparent sources green.

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