at Google ScholarTitle data
Charuchittipan, Doojdao ; Wilson, J. D.:
Turbulent kinetic energy dissipation in the surface layer.
In: Boundary-Layer Meteorology.
Vol. 132
(2009)
Issue 2
.
- pp. 193-204.
ISSN 1573-1472
DOI: https://doi.org/10.1007/s10546-009-9399-x
Abstract in another language
We estimated the turbulent kinetic energy (TKE) dissipation rate (ϵ) for thirty-two 1-h intervals of unstable stratification covering the stability range 0.12 ≤ −z/L ≤ 43 (z/L is the ratio of instrument height to the Obukhov length), by fitting Kolmogorov’s inertial subrange spectrum to streamwise spectra observed over a desert flat. Estimated values are compatible with the existence of local equilibrium, in that the TKE dissipation rate approximately equalled the sum of shear and buoyant production rates. Only in the neutral limit was the turbulent transport term in the TKE budget measured to be small.
Further data
| Item Type: | Article in a journal |
|---|---|
| Refereed: | Yes |
| Additional notes: | BAYCEER73946 |
| Institutions of the University: | Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Former Professors > Professor Micrometeorology - Univ.-Prof. Dr. Thomas Foken Faculties Faculties > Faculty of Biology, Chemistry and Earth Sciences Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Former Professors |
| Result of work at the UBT: | Yes |
| DDC Subjects: | 500 Science |
| Date Deposited: | 21 Aug 2015 06:49 |
| Last Modified: | 26 Apr 2022 13:30 |
| URI: | https://eref.uni-bayreuth.de/id/eprint/18433 |