1999
DOI: 10.1175/1520-0469(1999)056<3331:caeltc>2.0.co;2
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Can anE–lTurbulence Closure Simulate Entrainment in Radiatively Driven Convective Boundary Layers?

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Cited by 5 publications
(1 citation statement)
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“…The simple model here has been developed for mostly heuristic purposes. It can obviously be extended by considering analogous models for simulations of water clouds (for which case the total-water mixing ratio must exceed the saturation threshold before liquid water is produced and the layer becomes radiatively active), or by considering its effect given more realistic models of w e , or by considering similar effects associated with other processes (e.g., subsidence, C. S. Bretherton and H. Grenier 1998, personal communication;Lenderink et al 1999). A further interesting extension follows by supposing that the buoyancy flux scales with a radiatively based bulk Richardson number (e.g., Lock and MacVean 1999)…”
mentioning
confidence: 99%
“…The simple model here has been developed for mostly heuristic purposes. It can obviously be extended by considering analogous models for simulations of water clouds (for which case the total-water mixing ratio must exceed the saturation threshold before liquid water is produced and the layer becomes radiatively active), or by considering its effect given more realistic models of w e , or by considering similar effects associated with other processes (e.g., subsidence, C. S. Bretherton and H. Grenier 1998, personal communication;Lenderink et al 1999). A further interesting extension follows by supposing that the buoyancy flux scales with a radiatively based bulk Richardson number (e.g., Lock and MacVean 1999)…”
mentioning
confidence: 99%