Abstract
Abstract. In this paper, we simulate intermittent turbulence (also known as bursting events) in stably stratified open-channel flows using direct numerical simulation. Clear signatures of this intriguing phenomenon are observed for a range of stabilities. However, the spatio-temporal characteristics of intermittency are found to be strongly stability-dependent. In general, the bursting events are much more frequent near the bottom wall than in the upper-channel region. A steady coexistence of laminar and turbulent flows is detected at various horizontal planes in very stable cases. This spatially intermittent pattern is found to propagate downstream and strongly correlate with the temporal evolution of intermittency. Last, a long standing hypothesis by Blackadar, i.e., the strong connection between local stability and intermittent turbulence, is corroborated by this modeling study.
Funder
Air Force Office of Scientific Research
Division of Atmospheric and Geospace Sciences
Reference65 articles.
1. Ansorge, C. and Mellado, J. P.: Global intermittency and collapsing turbulence in the stratified planetary boundary layer, Bound.-Lay. Meteorol., 153, 89–116, 2014.
2. Armenio, V. and Sarkar, S.: An investigation of stably stratified turbulent channel flow using large-eddy simulation, J. Fluid Mech., 459, 1–42, 2002.
3. Barnard, J. C.: Intermittent turbulence in the very stable Ekman layer, PhD thesis, University of Washington, Washington, 2000.
4. Basu, S. and Porté-Agel, F.: Large-eddy simulation of stably stratified atmospheric boundary layer turbulence: a scale-dependent dynamic modeling approach, J. Atmos. Sci., 63, 2074–2091, 2006.
5. Blackadar, A.: High-resolution models of the planetary boundary layer, Adv. Environ. Sci. Eng., 1, 50–85, 1979.
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