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Cloud droplets in a bulk formulation and its application to buoyancy reversal instability
Author(s) -
de Lozar A.,
Mellado J. P.
Publication year - 2013
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.2234
Subject(s) - buoyancy , mechanics , instability , evaporation , diffusion , sedimentation , large eddy simulation , condensation , mixing (physics) , length scale , eulerian path , physics , materials science , thermodynamics , turbulence , geology , lagrangian , paleontology , quantum mechanics , sediment , mathematical physics
Abstract Mixing processes at the boundary of clouds often include typical length‐scales of several metres. Such length‐scales are too large for current Lagrangian models but they are also poorly resolved by typical Eulerian‐based large‐eddy simulations. Here, a bulk formulation is introduced for direct numerical simulations. Two main assumptions sustain this approach: the continuum approximation and the liquid‐phase diffusion approximation. The formulation includes the small‐scale features that originate from microscopic droplet dynamics: sedimentation, finite‐time condensation/evaporation, inertial effects and the low diffusion of liquid droplets with respect to vapour. The methodology is applied to the study of the buoyancy reversal instability that occurs at the top of stratocumulus clouds as a consequence of evaporative cooling. The inclusion of sedimentation, low liquid‐phase diffusion and finite‐time evaporation have a negative impact on instability when compared with the equilibrium formulation. The combined effect of all these small‐scale features reduces mixing at the cloud top by at least 90%. This strong reduction is explained by a condensate‐free middle layer, which emerges when droplets leave the cloud interface due to sedimentation.