Titlebook: An Introduction to Boundary Layer Meteorology; Roland B. Stull Textbook 1988 Kluwer Academic Publishers 1988 Cloud.Fog.Meteorology.Profil.

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Boundary Conditions and Surface Forcings,m the surface modify the state of the boundary layer. The heat and moisture fluxes are driven, in turn, by the external forcings such as radiation from the sun or transpiration from plants. Forcings across the top of the boundary layer also alter mean characteristics within it.

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Convective Mixed Layer, 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 structur

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Boundary Layer Clouds,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

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Geographic Effects,ographic variations can modify the boundary-layer flow, and in some cases generate circulations in conjunction with diurnal heating cycles. We have already touched on a few such flows, such as the drainage winds at night within a stable boundary layer. In this chapter we examine both geographically-

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Zeitliche Verteilung der Sal abscheidungen,Spectrum analysis is a statistical tool that we can employ to probe further into the workings of turbulence. By decomposing a series of measurements into frequency or wavenumber components, we can discover how eddies of different time and space scales contribute to the overall turbulence state.

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