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A model of airflow above changes in surface heat flux, temperature and roughness for neutral and unstable conditions

✍ Scribed by P. A. Taylor

Publisher
Springer
Year
1970
Tongue
English
Weight
781 KB
Volume
1
Category
Article
ISSN
0006-8314

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πŸ“œ SIMILAR VOLUMES

Airflow above changes in surface heat fl
Airflow above changes in surface heat flux, temperature and roughness; an extension to include the stable case
✍ P. A. Taylor πŸ“‚ Article πŸ“… 1971 πŸ› Springer 🌐 English βš– 790 KB

## OkE Non-dimensional absolute humidity gradient. OH Non-dimensional temperature gradient of heat flux. ObM Non-dimensional wind shear. ~b ~' = OM = H = WE, an assumption used in stable conditions. Q Air density. e, Absolute humidity. Qw Density of water. T Kinematic shear stress. Logarithmic hei

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