Extended Abstract (72K)4.4
Turbulence and mixing in the nocturnal boundary layer over a slope—VTMX field program results
Marko Princevac, Arizona State University, Tempe, AZ; and P. Monti, H. J. S. Fernando, T. A. Kowalewski, and E. R. Pardyjak
Measurements were conducted on an eastern slope of the Salt Lake Basin (SLB) as a part of the Vertical Transport and Mixing eXperiment (VTMX) conducted in October 2000. The interest was the nocturnal boundary layer on a slope (in particular, katabatic flows) in the absence of significant synoptic influence. Extensive measurements of mean flow, turbulence and radiation were made, from which circulation patterns on the slope and the nature of stratified turbulence in katabatic winds were inferred. The results show that near the surface (< 25 – 50 m) the nocturnal flow is highly stratified and directed down-slope, but at higher levels winds strongly varied in magnitude and direction with height and time, implying the domination of upper levels by air intrusions. These intrusions may peal off from different slopes surrounding the SLB, have different densities and flow at their equilibrium density levels. The turbulence was generally weak and continuous, but sudden increases of turbulence levels were detected as the mean gradient Richardson number (Rig ) dropped to about unity. Rig fluctuated with a short time scale on the order of a few tens of seconds while modulating with a longer (along-slope internal waves sloshing) time scale of about half an hour. The mixing efficiency (or the flux Richardson number) of the flow was found to be a strong function of Rig , similar to that found in laboratory experiments with inhomogeneous stratified shear flows. The eddy diffusivities of momentum and heat were evaluated, and they showed a systematic variation with Rig when scaled with the shear length scale and the rms vertical velocity of turbulence.
Supplementary URL: http://www.eas.asu.edu/~pefdhome/
Session 4, Boundary Layer Turbulence and Diffusion
Monday, 17 June 2002, 4:15 PM-5:30 PM
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