Vertical transport of turbulent kinetic energy in the surface layer over a paddy field
โ Scribed by T. Maitani
- Publisher
- Springer
- Year
- 1977
- Tongue
- English
- Weight
- 935 KB
- Volume
- 12
- Category
- Article
- ISSN
- 0006-8314
No coin nor oath required. For personal study only.
โฆ Synopsis
Turbulent kinetic energy and its vertical flux were measured at two heights over a paddy field. The vertical transport of turbulent kinetic energy was always downward right above the paddy field and was frequently downward at higher levels within a few metres above the crop. Contributions to the downward transport arise mainly from the turbulent kinetic energy of horizontal wind velocity components. It is shown from the analysis of probability distributions that appreciable transport takes place intermittently in a few large downward bursts and that these downdrafts are efficient for downward energy transport.
In the budget of turbulent kinetic energy, the flux divergence term and the energy dissipation term are the main loss terms under unstable conditions. These terms increase in magnitude with increasing instability. Buoyant production is insufficient to balance these losses. The imbalance term involving the pressure-work term is probably one of the main energy sources in unstable conditions.
๐ SIMILAR VOLUMES
From measurements in the atmospheric surface layer over a paddy field, the Kolmogorov constants for CO, and longitudinal wind velocity were obtained. In this study, the nondimensional dissipation rate & = (1-16~,)-'/2forC0,varianceand~~= (l-16i,)-'I"-i, for turbulent energy were used, assuming the e
Turbulence statistics, including higher order moments, in the surface layer over plant canopies were compared with those observed over several different surfaces, using a nondimensional height (zd)/z(,. The values of (zd)/z,, extend over a very wide range from 10" over plant canopies to 10' over the