Ye Zhao, Zhi Yuan and Fan Chen Kent State University, Ohio, USA.

Slides:



Advertisements
Similar presentations
Magnetic Chaos and Transport Paul Terry and Leonid Malyshkin, group leaders with active participation from MST group, Chicago group, MRX, Wisconsin astrophysics.
Advertisements

Canopy Spectra and Dissipation John Finnigan CSIRO Atmospheric Research Canberra, Australia.
Proto-Planetary Disk and Planetary Formation
Introduction to Computational Fluid Dynamics
Vortex instability and the onset of superfluid turbulence
TURBULENCE MODELING A Discussion on Different Techniques used in Turbulence Modeling -Reni Raju.
University of Southampton Southampton, UK
Particle acceleration in a turbulent electric field produced by 3D reconnection Marco Onofri University of Thessaloniki.
Dynamics and Statistics of Quantum Turbulence at Low Temperatures
Boundary Layer Flow Describes the transport phenomena near the surface for the case of fluid flowing past a solid object.
THE PARAMETERIZATION OF STABLE BOUNDARY LAYERS BASED ON CASES-99 Zbigniew Sorbjan Marquette University, Milwaukee Zbigniew Sorbjan Marquette University,
Session: Computational Wave Propagation: Basic Theory Igel H., Fichtner A., Käser M., Virieux J., Seriani G., Capdeville Y., Moczo P.  The finite-difference.
Physical-Space Decimation and Constrained Large Eddy Simulation Shiyi Chen College of Engineering, Peking University Johns Hopkins University Collaborator:
Evolving Sub-Grid Turbulence for Smoke Animation Hagit Schechter Robert Bridson SCA 08.
Nanoflares and MHD turbulence in Coronal Loop: a Hybrid Shell Model Giuseppina Nigro, F.Malara, V.Carbone, P.Veltri Dipartimento di Fisica Università della.
Stationarity and Degree of Stationarity
Turbulent Scalar Mixing Revisiting the classical paradigm in variable diffusivity medium Gaurav Kumar Advisor: Prof. S. S. Girimaji Turbulence Research.
Modeling Generation and Nonlinear Evolution of Plasma Turbulence for Radiation Belt Remediation Center for Space Science & Engineering Research Virginia.
Nonlinear Evolution of Whistler Turbulence W.A. Scales, J.J. Wang, and O. Chang Center of Space Science and Engineering Research Virginia Tech L. Rudakov,
Quantitative Description of Particle Dispersal over Irregular Coastlines Tim Chaffey, Satoshi Mitarai, Dave Siegel.
0.1m 10 m 1 km Roughness Layer Surface Layer Planetary Boundary Layer Troposphere Stratosphere height The Atmospheric (or Planetary) Boundary Layer is.
DETECTION OF UPPER LEVEL TURBULENCE VIA GPS OCCULTATION METHODS Larry Cornman National Center for Atmospheric Research USA.
Eddy Viscosity Model Jordanian-German Winter Academy February 5 th -11 th 2006 Participant Name : Eng. Tareq Salameh Mechanical Engineering Department.
1 Physics of turbulence muna Al_khaswneh Dr.Ahmad Al-salaymeh.
L ehrstuhl für Modellierung und Simulation UNIVERSITY of ROSTOCK | CHAIR OF MODELLING AND SIMULATION Physics of turbulence Lecture 2.
Lagrangian dispersion of light solid particle in a high Re number turbulence; LES with stochastic process at sub-grid scales CNRS – UNIVERSITE et INSA.
1 KNOO Annual Meeting 2009 CFD analysis of Fuel Rod Bundles S. Rolfo D. Laurence School of Mechanical, Aerospace & Civil Engineering (MACE) The University.
LES of Turbulent Flows: Lecture 3 (ME EN )
Spectra of Gravity Wave Turbulence in a Laboratory Flume S Lukaschuk 1, P Denissenko 1, S Nazarenko 2 1 Fluid Dynamics Laboratory, University of Hull 2.
A LES-LANGEVIN MODEL B. Dubrulle Groupe Instabilite et Turbulence CEA Saclay Colls: R. Dolganov and J-P Laval N. Kevlahan E.-J. Kim F. Hersant J. Mc Williams.
Modeling, Simulating and Rendering Fluids Thanks to Ron Fediw et al, Jos Stam, Henrik Jensen, Ryan.
Motivation  Movie  Game  Engineering Introduction  Ideally  Looks good  Fast simulation  Looks good?  Look plausible  Doesn’t need to be exactly.
Design Process Supporting LWST 1.Deeper understanding of technical terms and issues 2.Linkage to enabling research projects and 3.Impact on design optimization.
Using synthetic turbulence as an inlet condition for large eddy simulations Thomas P. Lloyd 1,2*, Stephen R. Turnock 1 and Victor F. Humphrey 2 1 Fluid.
Theory of wind-driven sea by V.E. Zakharov S. Badulin A.Dyachenko V.Geogdjaev N.Ivenskykh A.Korotkevich A.Pushkarev In collaboration with:
0 Local and nonlocal conditional strain rates along gradient trajectories from various scalar fields in turbulence Lipo Wang Institut für Technische Verbrennung.
DEVELOPMENT AND VALIDATION OF MODEL FOR AEROSOLS TRANSPORTATION IN BOUNDARY LAYERS A.S. Petrosyan, K.V. Karelsky, I.Smirnov Space Research Institute Russian.
Simulations of Compressible MHD Turbulence in Molecular Clouds Lucy Liuxuan Zhang, CITA / University of Toronto, Chris Matzner,
Governing equations: Navier-Stokes equations, Two-dimensional shallow-water equations, Saint-Venant equations, compressible water hammer flow equations.
Reynolds-Averaged Navier-Stokes Equations -- RANS
Lecture 8 - Turbulence Applied Computational Fluid Dynamics
On the Instantaneous Dynamics of the Large- Scale Structures In The Impinging Round Jet J. W. Hall & D. Ewing Department of Mechanical Engineering, McMaster.
Turbulent properties: - vary chaotically in time around a mean value - exhibit a wide, continuous range of scale variations - cascade energy from large.
ON MULTISCALE THEORY OF TURBULENCE IN WAVELET REPRESENTATION M.V.Altaisky
Numerical simulations of thermal counterflow in the presence of solid boundaries Andrew Baggaley Jason Laurie Weizmann Institute Sylvain Laizet Imperial.
LES of Turbulent Flows: Lecture 2 (ME EN )
Introduction: Lattice Boltzmann Method for Non-fluid Applications Ye Zhao.
Turbulence in the magnetosphere studied with CLUSTER data : evidence of intermittency Lamy H. 1, Echim M. 1,2, Darrouzet F. 1, Lemaire J. 3, Décréau P.
George Angeli 26 November, 2001 What Do We Need to Know about Wind for GSMT?
On Describing Mean Flow Dynamics in Wall Turbulence J. Klewicki Department of Mechanical Engineering University of New Hampshire Durham, NH
The Stability of Laminar Flows - 2
APPLICATION OF STATISTICAL MECHANICS TO THE MODELLING OF POTENTIAL VORTICITY AND DENSITY MIXING Joël Sommeria CNRS-LEGI Grenoble, France Newton’s Institute,
Emerging symmetries and condensates in turbulent inverse cascades Gregory Falkovich Weizmann Institute of Science Cambridge, September 29, 2008 כט אלול.
1 LES of Turbulent Flows: Lecture 7 (ME EN ) Prof. Rob Stoll Department of Mechanical Engineering University of Utah Fall 2014.
P. Meunier M. Bosco, P-Y Passaggia, S. Le Dizès Institut de Recherche sur les Phénomènes Hors-Equilibre, Marseille, France Lee waves of a tilted object.
1 Zonal Boundary Conditions. 2 Some Basics The flow domain is divided into zones and grids are generated within each zone. The flow equations are solved.
Tree methods, and the detection of vortical structures in the vortex filament method Andrew Baggaley, Carlo Barenghi, Jason Laurie, Lucy Sherwin, Yuri.
November 2005 Center for Computational Visualization Institute of Computational and Engineering Sciences Department of Computer Sciences University of.
Katarzyna Otmianowska-Mazur (UJ, Poland)‏ Grzegorz Kowal (UW-Madison/UJ, Poland)‏ Alex Lazarian (UW-Madison, USA)‏ Ethan Vishniac (McMaster, Canada)‏ Effects.
Animating smoke with dynamic balance Jin-Kyung Hong Chang-Hun Kim 발표 윤종철.
Thermal explosion of particles with internal heat generation in turbulent temperature of surrounding fluid Igor Derevich, Vladimir Mordkovich, Daria Galdina.
Introduction to the Turbulence Models
Modeling Astrophysical Turbulence
Introduction to Symmetry Analysis
C. F. Panagiotou and Y. Hasegawa
Animation of Trees CS 658.
In situ particle detection
Heavy-Ion Acceleration and Self-Generated Waves in Coronal Shocks
Turbulent Kinetic Energy (TKE)
Turbulent properties:
Presentation transcript:

Ye Zhao, Zhi Yuan and Fan Chen Kent State University, Ohio, USA

 “Turbulence is an irregular motion which in general makes its appearance in fluids, gaseous or liquid” ▪ Taylor and von Kármán 1937

 “Turbulence is an irregular motion which in general makes its appearance in fluids, gaseous or liquid” ▪ Taylor and von Kármán 1937  Model them ?

 Turbulent fluids are “very hard to predict” ▪ Taylor and von Kármán 1937  Very large degree of freedom  Reynolds number (Re) ▪ Kitchen faucet: Re =  Intrinsic fluctuation  Stochastic  Intermittent

 Pure direct numerical simulation  Not practical for high Re number  Limited computational resources  Wind tunnel used in real experiments  Simulation + Synthetic noise  U + u’

 Frequency domain (Fourier)  Stam and Fiume 93, Rasmussen et al. 03  Curl operation on  Perlin noise ▪ Narain et al. 08, Schechter et al. 08  Wavelet noise ▪ Kim et al. 08  Particles in artificial boundary layer  Pfaff et al. 09

 Define energy transport between octaves of noise fields following Kolmogorov 1941 theory (K41): energy cascade  Linear model ▪ Schechter et al. 08  Advection-reaction-diffusion PDE ▪ Narain et al. 08  Locally assembled wavelets ▪ Kim et al. 08  Decay of particles ▪ Pfaff et al. 09

 Relation between u ′ and U following K41  Advect gas by u ′ and U together ▪ Stam and Fiume 93, Rasmussen et al. 03  Artificial seeding ▪ Schechter et al. 08  Local kinetic energy ▪ Kim et al. 08  Viscous hypothesis ▪ Narain et al. 08, Pfaff et al. 09

 Consistent temporal evolution of u ′ with respect to U  Distortion detection ▪ Kim et al. 08  Empirical rotation scalar field ▪ Schechter et al. 08  Special noise particles ▪ Narain et al. 08  Vortex particles ▪ Pfaff et al. 09

 Noise synthesis  Direct Fourier domain generation  Following prescribed energy spectrum  Noise fields as random forces inside a turbulence integration module  Adding forces for animation control

 Divergence free in Fourier domain

 Energy spectrum defines parameter  Gaussian control of spectrum Large variation

 Multiple scale field Kolmogorov Style An arbitrary Choice

 Noise fields as forces so that they are  A small group of force fields is enough  Pre-computed  Randomly selected  Reusable  Introduced turbulence  Continuous energy injection  Model unresolved small-scale effects  Compensate loss in numerical computing

 Enabling a feedback control in the integration  Natural coupling  Control flexibility  Large q: turbulent results close to U  Small q: significant turbulence from U

 Force integration makes it easy  What: different scales and spectra  How: conditions from physical/artificial rules  Where: local, critical, interested regions  When: intermittency

 Determine force magnitude  Velocity condition  Strain rate  Distance to obstacles  Vorticity  Scalar density

 Alternations in time between nearly non- turbulent and chaotic behavior  Extremely hard by direct simulation  We use temporal control in forcing integration  With randomly varied time intervals

 Pros  Turbulence to coarse, existing, ongoing simulation  Natural integration with random forcing  No extra boundary handling  Adaptive, conditional turbulence  Use precomputed, reusable synthetic noise  Generally independent of solvers  Handful control for animators

 Cons.  Not physically exact in spectrum control ▪ Local force integration ▪ Gaussian function in noise scales  Forced integration ▪ Extra computing load ▪ Artificially provided parameters may not always appropriate

 More integration conditions  More noise synthesis schemes  Local random force generation

 U.S. National Science Foundation  Grant IIS  Anonymous reviewers  Theodore Kim and Nils Thuerey  Rama Hoetzlein  Nvidia  Paul Farrel