Buoyancy is the dominant mechanism driving turbulence in a convective boundary layer. Such turbulence is not completely random, but is often organized into identifiable structures such as thermals and plumes (Young, 1988). Entertainment happens at a variety of scales: lateral entertainment by small eddies into the sides of thermals, and vertical entertainment on the thermal scale into the whole mixed layer. In this chapter we examine the structure and evolution of the convective boundary layer, and study the forcings acting on it.
CITATION STYLE
Stull, R. B. (1988). Convective Mixed Layer. In An Introduction to Boundary Layer Meteorology (pp. 441–497). Springer Netherlands. https://doi.org/10.1007/978-94-009-3027-8_11
Mendeley helps you to discover research relevant for your work.