The two MJO events are depicted in Fig. View larger version 43K Fig. The systematic deepening of convective clouds prior to the active phase has led many to argue that the free-tropospheric moistening by the antecedent populations of cumulus and congestus clouds is important for preconditioning the environment for subsequent deep convection Johnson et al. While rainfall in the October period largely persists through night before tapering off in the morning Fig. Comparison between the unfiltered Eulerian tendency and the same term smoothed with a h running mean i. The 3-hourly Eulerian tendency is depicted red , and black is the same except smoothed using a h running mean. There are times when P 0 is slightly negative or departs measurably from TRMM rainfall, which could owe to any of several factors: observational sampling errors Mapes et al. Journal of the Atmospheric Sciences November , Vol.
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