Clouds can fonn at the top of mixed layers. and at the bottom of stable boundary layers. The amount and distribution of short and long-wave radiative flux divergence in the boundary layer are altered by clouds. and these effects are emerging as important aspects of the climate-change problem. In addition. the radiative effects combine with latent heating to modulate BL dynamics. turbulence generation. and evolution. This chapter provides a brief review of cloud thennodynamics. radiative processes. the role of entrainment. and descriptions of fogs. cumulus and stratocumulus clouds.
CITATION STYLE
Stull, R. B. (1988). Boundary Layer Clouds. In An Introduction to Boundary Layer Meteorology (pp. 545–585). Springer Netherlands. https://doi.org/10.1007/978-94-009-3027-8_13
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