In this note the forcing of cumulus cloud clearing over and downwind f
rom lakes during the warm season is evaluated conceptually by modeling
and observational approaches. It is suggested that drying by dynamica
lly induced subsidence and suppression of the CBL over the lake mutual
ly contribute to the cloud clearing. The effect of background flow spe
ed and the extent of potential clearing area is illustrated. Various i
mplications of the cloud clearing are discussed.