Scale disparity and spectral transfer in anisotropic numerical turbulence
 1994
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Institute for Computer Applications in Science and Engineering, NASA Langley Research Center, National Technical Information Service, distributor , Hampton, VA, [Springfield, Va
Statement  Ye Zhou, P.K. Yeung, James G. Brasseur. 
Series  ICASE report  no. 9464., NASA contractor report  194956., NASA contractor report  NASA CR194956. 
Contributions  Yeung, P. K., Brasseur, James G., Institute for Computer Applications in Science and Engineering. 
The Physical Object  

Format  Microform 
Pagination  1 v. 
ID Numbers  
Open Library  OL17001373M 
OCLC/WorldCa  32213490 
Scale disparity and spectral transfer in anisotropic numerical turbulence by the turbulence forcing scale. In such locally anisotropic turbulence, the particle pair dispersion depends on the. Get this from a library. Scale disparity and spectral transfer in anisotropic numerical turbulence.
[Ye Zhou; P K Yeung; James G Brasseur; Institute for Computer Applications in Science and Engineering.].
Details Scale disparity and spectral transfer in anisotropic numerical turbulence EPUB
PHYSICS OF FLU () The anisotropic structure of turbulence and its energy spectrum G. a1,a) c2 1Laboratory for Aero and Hydrodynamics, Delft University of Technology, CA Delft, The Netherlands 2Department of Mechanical Engineering, The University of Melbourne, VictoriaAustraliaFile Size: KB.
Direct numerical simulations (DNSs) [22,28,29,31,32,33] 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 The spectral energy transfer in isotropic decaying turbulence is examined using DNS and experiments.
The universal equilibrium range idea of Kolmogorov does not apply at the highest Reynolds numbers available. By contrast, the equilibrium similarity hypothesis of George is in Cited by: 2. The dynamics of spectral transfer in a model of drift wave turbulence with two nonlinearities D.
Newman and P. Terry Department of Physics, University of. Zhou, P. Yeung and James Scale disparity and spectral transfer in anisotropic numerical turbulence book Brasseur,"Scale disparity and spectral transfer in anisotropic numerical turbulence", Physics Review E, 53, (1), pp.
Lin, James G Brasseur, P. Pouderoux and P. Kahrilas,"The phrenic ampulla: Distal esophagus or potential hiatal hernia?", American Journal of Physiology  Gastrointestinal. grid turbulence were recently compared with results from a direct numerical simulation (DNS) of homogeneous isotropic turbulence [5].
The comparison highlighted the difﬁculty of specifying an adequate spatial domain for numerical and experimental studies so that an accurate determination of integral length is obtained. The scale properties of anisotropic and isotropic turbulence in the urban surface layer are investigated.
A dimensionless anisotropic tensor is introduced and the turbulent tensor anisotropic coefficient, defined as C, where \(C = 3d_{3}\,+\,1 (d_{3}\) is the minimum eigenvalue of the tensor) is used to characterize the turbulence anisotropy or by: 5.
Note that a “lowReynolds number” type wall correction is used for the spectral transfer coefficients in the current work that approaches the spectral transfer rates (C 1 = and C 2 = ) used for the decay of isotropic turbulence (Bolotnov et al., a) and uniform shear flow (Bolotnov et al., b).Cited by: 1.
Sukoriansky, S., B. Galperin and I. Staroselsky, A quasinormal scale elimination model of turbulent flows with stable stratification. Physics of Fluids, 17, –1–28, Sukoriansky, S., B.
Galperin, and V. Perov, Application of a new spectral theory of stably stratified. SmallScale Statistics and Structure of Turbulence – in the Light of High Resolution Direct Numerical Simulation Yukio Kaneda and Koji Morishita Introduction Fully developed turbulence is a phenomenon involving huge numbers of degrees of dynamical freedom.
The motions of a turbulent ﬂuid are sensitiveFile Size: KB. from anisotropic contributions and different anisotropic contributions among themselves.
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•Dynamical importance through the “foliation” mechanism of the eqs. of motion. •(i) Power law behaviour only in separated (j) sectors; (ii) intermittency also in anisotropic sectors, (iii). We experimentally investigate scaletoscale anisotropy from the integral to the dissipative scales in homogeneous turbulence.
We employ an apparatus in which two facing arrays of randomly actuated air jets generate turbulence with negligible mean flow and shear, over a volume several times larger than the energycontaining eddy by: 7.
mogeneous and anisotropic turbulence by direct numerical simulations of the Navier–Stokes equations in a periodic box. Previous numerical studies have been limited to either homogeneous and isotropic turbulence15,16 or to shell models of the energy cascade.
energytransfer spectra for some of the same flow fields are presented in figures 10 and Because turbulence is intermittent, one might expect some fluctuations in the timedependent spectra of a finite sample. In our simulations the turbulent length scale L (see eq.
16b) is the size of the periodic box, so the sample size is veryFile Size: 1MB. Spectral structure of stratiﬁed turbulence: direct numerical simulations and predictions by large eddy simulation we propose a subgridscale turbulence model for large eddy simulations of stratiﬁed ﬂows based on the Adaptive Local Deconvolution Method (ALDM).
Turbulence in a box: quantification of largescale resolution effects in isotropic turbulence free decay  Volume  M. Meldi, P. Sagaut Skip to main content Accessibility help We use cookies to distinguish you from other users and to provide you with a better experience on our by: 8.
Statistical properties of decaying geostrophic turbulence 20 1 The operator J in (1) is the horizontal Jacobian, and it represents horizontal advection.
N(z) is the nondimensional BruntVaisala frequency (i.e. the vertical gradient of the mean density profile). t is the temporal coordinate.
The horizontal coordinates are x and y, their range isCited by: We found experimentally a dependence of the integral length scales of correlation functions measured in different directions in a turbulent flow on the velocity fluctuation anisotropy in those same directions.
We derive invariants for anisotropic turbulence that is locally isotropic, and so a relationship between the velocity and length scales. The results emphasize the importance of defining Cited by: mental and numerical anisotropic turbulence at ﬁnite Reynolds numbers with ﬁnite scale range (see, e.g., [1,2] and the references cited therein).
The small scale anisotropy in turbulence is a theoretical challenge. The detailed information on the anisotropic process of energy transfer, in particular that in the inertial subrange, should be.
Description Scale disparity and spectral transfer in anisotropic numerical turbulence EPUB
Definition of spectral nonequilibrium property in homogeneous isotropic turbulence Presently there exist different definitions of the nonequilibrium turbulence. Some researchers define nonequilibrium as the imbalance between the maximum nonlinear energy transfer and the dissipation [8], [12], [13], [14], for example the freedecaying Cited by: PHYSICS OF FLU () Constrained multiscale turnover Lagrangian map for anisotropic synthetic turbulence: A prioritests Yi Li1,a) and Carlos Rosales2,b) 1School of Mathematics and Statistics, University of Shefﬁeld, Shefﬁeld S3 7RH, United Kingdom 2Department of Mechanical Engineering, Universidad Tecnica Federico Santa Maria, Valparaiso, Chile.
basin will also contribute to and affect the largescale ﬂow structures. Numerical studies of 2D turbulence in square, rectangular, and circular domains are so far hampered by the computational costs.
Moreover, the statistical and spectral analysis is not straightforward due to anisotropy and inhomogeneity induced by the lateral by: 5. title = "Measuring anisotropy ellipse of atmospheric turbulence by intensity correlations of laser light", abstract = "An experimental study has been performed of a laser beam propagating horizontally through the nearground atmosphere above a grassy field at the University of Miami (UM) Coral Gables by: The influence of turbulence structure, parameterized by two point correlations, on the returntoisotropy process is examined under controlled conditions.
In order to determine the influence of structure, direct numerical simulations (DNS) of returntoisotropy in homogeneous, anisotropic turbulence is performed on meshes of and xxAuthor: Christopher J Zusi. Turbulence Kinetic Energy Specific Dissipation Rate Closure Coefficients and Auxilary Relations References.
Wilcox, D.C. (), "Reassessment of the scaledetermining equation for advanced turbulence models", AIAA Journal, vol. 26, no. 11, pp. Theoretical and experimental investigations have shown that the atmospheric turbulence exhibits both anisotropic and nonKolmogorov properties.
In this work, two theoretical atmosphere refractiveindex fluctuations spectral models are derived for optical waves propagating through anisotropic nonKolmogorov atmospheric turbulence. They consider simultaneously the finite turbulence inner and. The integral scale in homogeneous isotropic turbulence 0 5 10 15 20 25 30 k E time = Figure1.E(k) versus kfor the Wray () DNS data.
to be correct, then show that the measurements can be accounted for by considering the contribution of the largest scales which the experiments. transfer of energy is caused by the interaction of vortices with similar sizes. There is, however, no explicit length scale in the vorticity equation in physical space.
This suggests that a multiscale method based on transforms with basis functions that are localized both in Fourier space and physical space is required (e.g. Meneveau. vortex lines by the largescale field is allowed, which is not the case for the present model.
Evidence that structures of this type are characteristic of the small scales of isotropic turbulence is provided by the numerical simulations of Kerr,3 Ashurst et a1.,4 Vincent and Meneguzzi,5 and oth. Title: Anisotropy and nonuniversality in scaling laws of the large scale energy spectrum in rotating turbulence Authors: Amrik Sen, Pablo D.
Mininni, Duane Rosenberg, Annick pouquet (Submitted on 22 Mar (v1), last revised 5 Apr (this version, v2))Cited by: turbulence energy is mostly associated with the larger eddies. Turbulence Lengthscales and Spectra /12 13 / 18 Kolmogorov Model I Based on empirical observations and dimensional analysis, the Kolmogorov model allows us to derive some quantitative rela tions for the spectral densities of k and e.
I The model is based on the following File Size: KB.







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