Large-scale characteristics of stratified wake turbulence at varying Reynolds number

被引:31
|
作者
Zhou, Qi [1 ]
Diamessis, Peter J. [2 ]
机构
[1] Univ Calgary, Dept Civil Engn, Calgary, AB T2N 1N4, Canada
[2] Cornell Univ, Sch Civil & Environm Engn, Ithaca, NY 14853 USA
来源
PHYSICAL REVIEW FLUIDS | 2019年 / 4卷 / 08期
基金
加拿大自然科学与工程研究理事会; 英国工程与自然科学研究理事会;
关键词
DIRECT NUMERICAL SIMULATIONS; ZIGZAG INSTABILITY; TOWED SPHERE; SIMILARITY; EVOLUTION; DYNAMICS; LAYER;
D O I
10.1103/PhysRevFluids.4.084802
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
We analyze a large-eddy simulation data set of wakes of a towed sphere of diameter D at speed U in a uniformly stratified Boussinesq fluid with buoyancy frequency N and kinematic viscosity nu. These temporally evolving wakes are simulated using a spectral multidomain penalty-method-based incompressible Navier-Stokes solver for Fr 2U/ND is an element of {4, 16, 64} and Re UD/nu is an element of {5 x 10(3),10(5), 4 x 10(5)}, enabling a systematic examination of stratified wakes at three different values of Re sufficiently separated in magnitude. As such, particular attention is paid to the effects of varying Re on the evolution of large-scale characteristics of stratified wake turbulence. We examine the evolution of horizontal and vertical integral length scales (l(h) and l(v)), horizontal and vertical fluctuation velocities (U and W), local vertical shear, as well as the resulting dimensionless parameters based on the above quantities. In particular, the vertical turbulent Froude number Fr-v* 2 pi U/Nl(v) is found to be of order unity, a signature of the dynamics in the strongly stratified regime where shear instabilities develop between anisotropic flow layers. The horizontal turbulent Reynolds number Re-h Ul(h)/nu stays approximately constant in time and the horizontal turbulent Froude number Fr-h U/Nlh decays in time as (Nt)(-1), consistent with scaling analysis of freely decaying turbulence. We characterize the transitions between distinct stratified flow regimes and examine the effects of body-based parameters Re and Fr on these transitions. The transition from the weakly to the strongly stratified regime, which is marked by Fr-v* decaying to unity, occurs when Fr-h similar or equal to O(0.01). We further show that the initial value of Re h at which the flow completes the above transition scales as Re Fr--(2/3), which provides a way to predict the possibility of accessing the strongly stratified regime for a wake of given Re and Fr. The analysis reported here constitutes an attempt to obtain the predictive capability of stratified wake turbulence in terms of Reynolds number Re, applying select elements of strongly stratified turbulence theory, so far typically utilized for homogeneous turbulence, to a canonical inhomogeneous turbulent free-shear flow.
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页数:30
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