Titlebook: Boundary-Layer Meteorology 25th Anniversary Volume, 1970–1995; Invited Reviews and J. R. Garratt,P. A. Taylor Book 1996 Springer Science+B

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Experimental Micrometeorology in an Era of Turbulence Simulation,x budgets, surface-exchange relations, and the universal functions of Monin—Obukhov similarity within the “constant-flux” layer. More recently, the growth in supercomputers and computational fluid dynamics has stimulated micrometeorological applications of large-eddy simulation (LES). LES uses a dif

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产生

Deference

大吃大喝

Frontal Substructures Within the Planetary Boundary Layer,e of the Planetary Boundary Layer (PBL) for the development and the substructures of two different types of cold fronts. The effects of turbulent friction, large-scale (geostrophic) forcing and the diurnal variation of the terms of the surface energy balance (SEB) equation on the frontal development

CLAMP

Review of Lagrangian Stochastic Models for Trajectories in the Turbulent Atmosphere,y their application to calculate dispersion in the principal types of atmospheric turbulence (stratified, vertically-inhomogeneous, Gaussian or non-Gaussian turbulence in the surface layer and above), and show that they are especially suitable for some problems (e.g., quantifying ground emissions).

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figment

Review of Some Basic Characteristics of the Atmospheric Surface Layer,.32 to 0.65 have been reported. Most of the data are, however, found in a rather narrow range between 0.39 and 0.41. Plotting all available atmospheric data against the so-called roughness Reynolds number, Reo = ..../. or against the surface Rossby number, Ro. = ./... gives no clear indication of sy

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malign