Dynamic Large Eddy Simulations of the Ekman Layer Based on Stochastic Analysis

被引:10
|
作者
Kazemi, Ehsan [1 ]
Heinz, Stefan [1 ]
机构
[1] Univ Wyoming, Dept Math, 1000 East Univ Ave, Laramie, WY 82071 USA
关键词
large eddy simulation; dynamic subgrid-scale modeling; Ekman layer; DIRECT NUMERICAL-SIMULATION; TURBULENT REACTING FLOWS; FOKKER-PLANCK EQUATIONS; DENSITY-FUNCTION; REALIZABILITY; MODELS; CLOSURE; RANS; LES;
D O I
10.1515/ijnsns-2015-0049
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
Large eddy simulation (LES) of the neutrally stratified turbulent Ekman layer is performed. In particular, we compare three LES models with direct numerical simulation (DNS), which was validated against existing DNS. The models considered are a standard nondynamic LES model, the Smagorinsky model (SM), a standard dynamic LES model, the stabilized dynamic Smagorinsky model (DSM), and a new linear dynamic model (LDM), which was derived from a realizable stochastic turbulence model. The following conclusions are obtained. The SM does not represent an appropriate model for the flow considered. Mean velocity and turbulence intensities are poorly predicted. With respect to instantaneous fields, the SM provides a tilting of turbulence structures in the opposite direction as seen in DNS. The stabilized DSM also suffers from significant shortcomings. First, its behavior depends on the wall distance. Close to the wall, it produces acceptable turbulence structures. Away from the wall, it suffers from the same shortcomings as the SM. Second, it incorrectly describes the effect of grid coarsening. The new LDM is free from the disadvantages of the SM and stabilized DSM. Its predictions of both mean and instantaneous velocity fields agree very well with DNS. The relevant conclusion is the following. The use of a dynamic LES method represents a mean for correctly simulating large-scale structures (means and stresses), but it does not ensure a correct simultaneous simulation of small-scale structures. Our results indicate that a dynamic method designed in consistency with a realizable stress model can correctly simulate both large-scale and small-scale structures.
引用
收藏
页码:77 / 98
页数:22
相关论文
共 50 条
  • [21] Large eddy simulations of erosion of a stratified layer by a buoyant jet
    Sarikurt, Fatih S.
    Hassan, Yassin A.
    INTERNATIONAL JOURNAL OF HEAT AND MASS TRANSFER, 2017, 112 : 354 - 365
  • [22] Wall-layer models for large-eddy simulations
    Piomelli, Ugo
    PROGRESS IN AEROSPACE SCIENCES, 2008, 44 (06) : 437 - 446
  • [23] Large eddy simulations of mixed layer instabilities and sampling strategies
    Oezgoekmen, Tamay M.
    Poje, Andrew C.
    Fischer, Paul F.
    Haza, Angelique C.
    OCEAN MODELLING, 2011, 39 (3-4) : 311 - 331
  • [24] An Intercomparison of Large-Eddy Simulations of the Stable Boundary Layer
    Robert J. Beare
    Malcolm K. Macvean
    Albert A. M. Holtslag
    Joan Cuxart
    Igor Esau
    Jean-Christophe Golaz
    Maria A. Jimenez
    Marat Khairoutdinov
    Branko Kosovic
    David Lewellen
    Thomas S. Lund
    Julie K. Lundquist
    Anne Mccabe
    Arnold F. Moene
    Yign Noh
    Siegfried Raasch
    Peter Sullivan
    Boundary-Layer Meteorology, 2006, 118 : 247 - 272
  • [25] Wall-layer models for large-eddy simulations
    Piomelli, U
    Balaras, E
    ANNUAL REVIEW OF FLUID MECHANICS, 2002, 34 : 349 - 374
  • [26] STOCHASTIC BACKSCATTER IN LARGE-EDDY SIMULATIONS OF BOUNDARY-LAYERS
    MASON, PJ
    THOMSON, DJ
    JOURNAL OF FLUID MECHANICS, 1992, 242 : 51 - 78
  • [27] Large eddy simulations
    Piomelli, Ugo
    INTERNATIONAL JOURNAL OF COMPUTATIONAL FLUID DYNAMICS, 2010, 24 (10) : 391 - 391
  • [28] Large eddy simulations of stratified turbulence: the dynamic Smagorinsky model
    Khani, Sina
    Waite, Michael L.
    JOURNAL OF FLUID MECHANICS, 2015, 773 : 327 - 344
  • [29] An improved Ekman layer approximation for smooth eddy diffusivity profiles
    Parmhed, O
    Kos, I
    Grisogono, B
    BOUNDARY-LAYER METEOROLOGY, 2005, 115 (03) : 399 - 407
  • [30] A generalized Ekman layer profile with gradually varying eddy diffusivities
    Grisogono, B.
    Royal Meteorological Society. Quarterly Journal, 1600, 121 (522/B):