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Robert Wood

maintains the cloud layer (e.g., Nicholls 1984 ; Bretherton and Wyant 1997 ), and controls the development of mesoscale organization ( Shao and Randall 1996 ; Atkinson and Zhang 1996 ; Jonker et al. 1999 ; de Roode et al. 2004 ). Latent heating in the upward branches of the convective elements and evaporation in downdrafts, provides an additional source of turbulence that strengthens the convection (e.g., Moeng et al. 1992 ). Thus, stratocumulus clouds frequently exert first-order effects upon

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