Abstract

Abstract Lateral detrainment from cumulus updrafts and its effect on the properties of cumulus cloud populations (as determined from large-scale observations) are examined. This detrainment, which can be related to the cumulus life cycle, has been specified for a spectrum of cloud sizes by considering initially the character of detrainment for the two extremes of convection: deep cumulonimbi and shallow cumuli. The main purpose is to determine for some reasonable assumption of individual cloud detrainment to what extent diagnosed cloud ensemble properties differ from those given by applying a steady-state plume model for convective updrafts and downdrafts. Application of the model to tropical western Pacific data indicates, as earlier studies have shown, that in convectively disturbed situations a bimodal cloud population exists of predominantly deep and shallow cumuli. However, the contribution to the total cloud-base mass flux from deep cumuli is increased and from shallow cumuli decreased somewhat when...

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