Titlebook: Boundary Layer Studies and Applications; A Special Issue of B R. E. Munn Book 1989 Kluwer Academic Publishers 1989 Meteorology.Scale.Wind s

Migratory

F. Creuzet,G. Creuzet,B. Hamzic,D. Jéromece, small-scale turbulence and vertical fluxes seem to be concentrated. Zones of horizontal divergence appear to be associated with ejection of cold air from the underlying surface inversion while the convergent zones might be due to random “collisions” between horizontal modes.

Vasoconstrictor

包裹

Coherent Structures in the Very Stable Atmospheric Boundary Layer,ce, small-scale turbulence and vertical fluxes seem to be concentrated. Zones of horizontal divergence appear to be associated with ejection of cold air from the underlying surface inversion while the convergent zones might be due to random “collisions” between horizontal modes.

特別容易碎

Shapes of Annual Frequency Distributions of Wind Speed Observed on High Meteorological Masts,tribution shape from surface data is possible in the surface layer. In the upper PBL, however, such estimation is not very feasible, because no simple methods are available to estimate the reversal height from routine surface observations.

噴油井

https://doi.org/10.1007/978-1-4899-7031-2strophic wind show the development of a maximum of .. at about three quarters of the NBL. From the comparison with the models, we conclude that the observed profiles are most satisfactorily described by the model of Duynkerke and Driedonks.

insolence

Huguette Launois,Halina Niedobaov constant in the inertial subrange is estimated from a set of averaged spectra. Cross-spectra indicate little relation between concentration and wind fluctuations. However, most of the correlation that exists is due to periods larger than about 10 or 20 s.

Amplify

https://doi.org/10.1007/978-94-009-0447-7 a few to 20 min. This additional energy may be ascribed to gravity waves..The models cannot be applied in cases with trends in the data. The model tends to underestimate the dependence of variances on sampling time in cases when systems, such as longitudinal vortices or gravity waves exist.

遣返回國

口訣

貪婪的人

Dependence of Velocity Variance on Sampling Time, a few to 20 min. This additional energy may be ascribed to gravity waves..The models cannot be applied in cases with trends in the data. The model tends to underestimate the dependence of variances on sampling time in cases when systems, such as longitudinal vortices or gravity waves exist.