𝔖 Bobbio Scriptorium
✦   LIBER   ✦

Determination of vertical variation in eddy diffusivity in lower layers of the atmosphere

✍ Scribed by Greenfield, Harvey

Publisher
Springer
Year
1964
Tongue
English
Weight
702 KB
Volume
12
Category
Article
ISSN
0003-6994

No coin nor oath required. For personal study only.

πŸ“œ SIMILAR VOLUMES

The eddy diffusivity and the temperature
The eddy diffusivity and the temperature of the lower layers of the atmosphere
✍ T. G. Cowling; A. White; S. Chapman πŸ“‚ Article πŸ“… 2007 πŸ› John Wiley and Sons 🌐 English βš– 640 KB

## Abstract Methods of calculating the eddy diffusivity ΞΊ are discussed. It is shown that methods which assume that ΞΊ can be regarded as independent of the height, even through a shallow layer, lead to erroneous results: in consequence the frequent use in the literature of the approximate equation

Vertical diffusion in the lowest layers
Vertical diffusion in the lowest layers of the atmosphere
✍ E. L. Deacon πŸ“‚ Article πŸ“… 1949 πŸ› John Wiley and Sons 🌐 English βš– 741 KB

## Abstract A semi‐empirical treatment of the vertical diffusion of matter in the lowest layers of the atmosphere is given in the following and shown to be in good agreement with the results of carefully conducted field experiments made over two different types of natural land surface. The present

A parametric model of vertical eddy flux
A parametric model of vertical eddy fluxes in the atmosphere
✍ Jean-FranΓ§ois Louis πŸ“‚ Article πŸ“… 1979 πŸ› Springer 🌐 English βš– 800 KB

A scheme for the representation of the vertical eddy fluxes of heat, momentum and water vapour in a forecast model is presented. An important feature of the scheme is the dependence of the diffusion coefficients on the static stability of the atmosphere. Two tests are presented, using the scheme in

Turbulent diffusivity and diurnal variat
Turbulent diffusivity and diurnal variations in the atmospheric boundary layer
✍ Nobuhisa Yasuda πŸ“‚ Article πŸ“… 1988 πŸ› Springer 🌐 English βš– 625 KB

Diurnal variations of the vertical profiles of wind and temperature have been surveyed, and the diffusivity and the dimensionless gradient function in the atmospheric boundary layer have been estimated. Even in the middle of the atmospheric boundary layer (e.g., below a height of 442 m), the vertica