作者: David A. Randall
DOI: 10.1175/1520-0469(1987)044<0850:TFOLWA>2.0.CO;2
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摘要: Abstract A simple convective mass flux model is used to derive expressions for the fluxes of liquid water and buoyancy in partly cloudy turbulent layers. The results differ radically from those suggested some previous studies. Physical interpretation given, examples are presented. Implications dynamics boundary layers discussed, aftermath cloud-top entrainment instability analyzed.