Direct numerical simulation of intermittent turbulence under stably stratified conditions

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 spatiotemporal characteristics of intermi...

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Main Authors: P. He, S. Basu
Format: Article
Language:English
Published: Copernicus Publications 2015-07-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/22/447/2015/npg-22-447-2015.pdf
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author P. He
S. Basu
author_facet P. He
S. Basu
author_sort P. He
collection DOAJ
description 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 spatiotemporal 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. Lastly, a long standing hypothesis by Blackadar (1979), i.e., the strong connection between local stability and intermittent turbulence, is corroborated by this modeling study.
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spelling doaj.art-1c1dc9b19e8f47bfb90bf910e14a17792022-12-21T23:01:47ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462015-07-0122444747110.5194/npg-22-447-2015Direct numerical simulation of intermittent turbulence under stably stratified conditionsP. He0S. Basu1Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USADepartment of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USAIn 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 spatiotemporal 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. Lastly, a long standing hypothesis by Blackadar (1979), i.e., the strong connection between local stability and intermittent turbulence, is corroborated by this modeling study.http://www.nonlin-processes-geophys.net/22/447/2015/npg-22-447-2015.pdf
spellingShingle P. He
S. Basu
Direct numerical simulation of intermittent turbulence under stably stratified conditions
Nonlinear Processes in Geophysics
title Direct numerical simulation of intermittent turbulence under stably stratified conditions
title_full Direct numerical simulation of intermittent turbulence under stably stratified conditions
title_fullStr Direct numerical simulation of intermittent turbulence under stably stratified conditions
title_full_unstemmed Direct numerical simulation of intermittent turbulence under stably stratified conditions
title_short Direct numerical simulation of intermittent turbulence under stably stratified conditions
title_sort direct numerical simulation of intermittent turbulence under stably stratified conditions
url http://www.nonlin-processes-geophys.net/22/447/2015/npg-22-447-2015.pdf
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