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LARGE EDDY SIMULATION Chin-Hoh Moeng NCAR OUTLINE WHAT IS LES? APPLICATIONS TO PBL FUTURE DIRECTION.

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Presentation on theme: "LARGE EDDY SIMULATION Chin-Hoh Moeng NCAR OUTLINE WHAT IS LES? APPLICATIONS TO PBL FUTURE DIRECTION."— Presentation transcript:

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2 LARGE EDDY SIMULATION Chin-Hoh Moeng NCAR

3 OUTLINE WHAT IS LES? APPLICATIONS TO PBL FUTURE DIRECTION

4 WHAT IS LES? A NUMERICAL TOOL FOR TURBULENT FLOWS

5 Turbulent Flows governing equations, known nonlinear term >> dissipation term no analytical solution highly diffusive smallest eddies ~ mm largest eddies --- depend on Re- number (U; L; )

6 Numerical methods of studying turbulence Reynolds-averaged modeling (RAN) model just ensemble statistics Direct numerical simulation (DNS) resolve for all eddies Large eddy simulation (LES) intermediate approach

7 LES turbulent flow Resolved large eddies Subfilter scale, small (not so important) (important eddies)

8 FIRST NEED TO SEPARATE THE FLOW FIELD Select a filter function G Define the resolved-scale (large-eddy): Find the unresolved-scale (SGS or SFS):

9 Examples of filter functions Top-hat Gaussian

10 Example: An 1-D flow field f Apply filter  large eddies

11 Reynolds averaged model (RAN) f Apply ensemble avg  non-turbulent

12 LES EQUATIONS SFS Apply filter G

13 Different Reynolds number turbulent flows Small Re flows: laboratory (tea cup) turbulence; largest eddies ~ O(m); RAN or DNS Medium Re flows: engineering flows; largest eddies ~ O(10 m); RAN or DNS or LES Large Re flows: geophysical turbulence; largest eddies > km; RAN or LES

14 Geophysical turbulence PBL (pollution layer) boundary layer in the ocean turbulence inside forest deep convection convection in the Sun …..

15 LES of PBL kmm mm resolved eddiesSFS eddies dissipationenergy input L inertial range,

16 Major difference between engineer and geophysical flows: near the wall Engineering flow: viscous layer Geophysical flow : inertial-subrange layer; need to use surface-layer theory

17 The premise of LES Large eddies, most energy and fluxes, explicitly calculated Small eddies, little energy and fluxes, parameterized, SFS model

18 The premise of LES Large eddies, most energy and fluxes, explicitly calculated Small eddies, little energy and fluxes, parameterized, SFS model LES solution is supposed to be insensitive to SFS model

19 Caution near walls, eddies small, unresolved very stable region, eddies intermittent cloud physics, chemical reaction… more uncertainties

20 A typical setup of PBL-LES 100 x 100 x 100 points grid sizes < tens of meters time step < seconds higher-order schemes, not too diffusive spin-up time ~ 30 min, no use simulation time ~ hours massive parallel computers

21 Different PBL Flow Regimes numerical setup large-scale forcing flow characteristics

22 Clear-air convective PBL Convective updrafts ~ 2 km

23 Horizontal homogeneous CBL

24 Local Time LIDAR Observation

25 Oceanic boundary layer Add vortex force for Langmuir flows McWilliam et al 1997

26 Oceanic boundary layer Add vortex force for Langmuir flows McWilliams et al 1997

27 Canopy turbulence Add drag force---leaf area index Patton et al 1997 < 100 m

28 observation LES Comparison with observation

29 Shallow cumulus clouds Add phase change---condensation/evaporation ~ 6 km ~3 km ~ 12 hr

30 COUPLED with SURFACE turbulence heterogeneous land turbulence ocean surface wave

31 Coupled with heterogeneous soil Surface model Wet soil Dry soil the ground LES model Land model

32 Coupled with heterogeneous soil wet soildry soil (Patton et al 2003)

33 Coupled with wavy surface stably stratified

34 U-field flat surfacestationary wave moving wave

35 So far, idealized PBLs Flat surface Periodic in x & y Shallow clouds

36 Future Direction of LES for PBL Research Realistic surface –complex terrain, land use, waves PBL under severe weather

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38 500 km 50 km LES domain mesoscale model domain

39 Computational challenge Massive parallel machines Resolve turbulent motion in Taipei basin ~ 1000 x 1000 x 100 grid points

40 Technical issues Inflow boundary condition SFS effect near irregular surfaces Proper scaling; representations of ensemble mean

41 ? How to describe a turbulent inflow?

42 What do we do with LES solutions? Understand turbulence behavior & diffusion property Develop/calibrate PBL models i.e. Reynolds average models

43 CLASSIC EXAMPLES Deardorff (1972; JAS) - mixed layer scaling Lamb (1978; atmos env) - plume dispersion

44 FUTURE GOAL Understand PBL in complex environment and improve its parameterization for regional and climate models –turbulent fluxes –air quality –cloud –chemical transport/reaction


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