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A micrometeorological study of velocity profiles and surface drag in the region modified by a change in surface roughness

✍ Scribed by E. F. Bradley

Publisher
John Wiley and Sons
Year
1970
Tongue
English
Weight
91 KB
Volume
96
Category
Article
ISSN
0035-9009

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πŸ“œ SIMILAR VOLUMES

Relations between surface fluxes and mea
Relations between surface fluxes and mean profiles of velocity, temperature and concentration, downwind of a change in surface roughness
✍ P. J. Mulhearn πŸ“‚ Article πŸ“… 1977 πŸ› John Wiley and Sons 🌐 English βš– 790 KB

## Abstract Changes in surface fluxes (of momentum, heat, and mass) downwind of a surface roughness change, are related to changes in mean profiles (of velocity, temperature, and concentration). the theory assumes that changes in mean quantities are self‐preserving. At fetches sufficiently large fo

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✍ D. H. Wood πŸ“‚ Article πŸ“… 1978 πŸ› John Wiley and Sons 🌐 English βš– 583 KB

## Abstract The response of the boundary layer wind profile and the surface shear to a large step change in surface roughness is predicted by three calculation methods and the predictions are compared with measurements by Bradley. The first method, which assumes that local equilibrium exists everyw

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✍ Ulrich Schumann πŸ“‚ Article πŸ“… 1988 πŸ› Springer 🌐 English βš– 901 KB

A simple model is deduced for the surface layer of a convective boundary layer for zero mean wind velocity over homogeneous rough ground. The model assumes large-scale convective circulation driven by surface heat flux with a flow pattern as it would be obtained by conditional ensemble averages. The