DOE PAGES title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain

Abstract

A challenge to simulating turbulent flow in multiscale atmospheric applications is the efficient generation of resolved turbulence motions over an area of interest. One approach is to apply small perturbations to flow variables near the inflow planes of turbulence-resolving simulation domains nested within larger mesoscale domains. While this approach has been examined in numerous idealized and simple terrain cases, its efficacy in complex terrain environments has not yet been fully explored. Here, we examine the benefits of the stochastic cell perturbation method (CPM) over real complex terrain using data from the 2017 Perdigão field campaign, conducted in an approximately 2-km wide valley situated between two nearly parallel ridges. Following a typical configuration for multiscale simulation using nested domains within the Weather Research and Forecasting (WRF) model to downscale from the mesoscale to a large-eddy simulation (LES), we apply the CPM on a domain with horizontal grid spacing of 150 m. At this resolution, spurious coherent structures are often observed under unstable atmospheric conditions with moderate mean wind speeds. Results from such an intermediate resolution grid are often nested down for finer, more detailed LES, where these spurious structures adversely affect the development of turbulence on the subsequent finer grid nest.more » We therefore examine the impacts of the CPM on the representation of turbulence within the nested LES domain under moderate mean flow conditions in three different stability regimes: weakly convective, strongly convective, and weakly stable. In addition, two different resolutions of the underlying terrain are used to explore the role of the complex topography itself in generating turbulent structures. We demonstrate that the CPM improves the representation of turbulence within the LES domain, relative to the use of high-resolution complex terrain alone. During the convective conditions, the CPM improves the rate at which smaller-scales of turbulence form, while also accelerating the attenuation of the spurious numerically generated roll structures near the inflow boundary. During stable conditions, the coarse mesh spacing of the intermediate LES domain used herein was insufficient to maintain resolved turbulence using CPM as the flow develops downstream, highlighting the need for yet higher resolution under even weakly stable conditions, and the importance of accurate representation of flow on intermediate LES grids.« less

Authors:
ORCiD logo [1];  [2];  [1];  [3]; ORCiD logo [4];  [1]
  1. Univ. of California, Berkeley, CA (United States)
  2. Univ. of California, Berkeley, CA (United States); Univ. of Twente, Enschede (Netherlands)
  3. Univ. of Twente, Enschede (Netherlands)
  4. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Publication Date:
Research Org.:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Org.:
USDOE National Nuclear Security Administration (NNSA); National Science Foundation (NSF)
OSTI Identifier:
1866158
Report Number(s):
LLNL-JRNL-818072
Journal ID: ISSN 2073-4433; 1028491
Grant/Contract Number:  
AC52-07NA27344; AGS-1565483
Resource Type:
Accepted Manuscript
Journal Name:
Atmosphere (Basel)
Additional Journal Information:
Journal Name: Atmosphere (Basel); Journal Volume: 12; Journal Issue: 1; Journal ID: ISSN 2073-4433
Publisher:
MDPI
Country of Publication:
United States
Language:
English
Subject:
17 WIND ENERGY; 58 GEOSCIENCES; 54 ENVIRONMENTAL SCIENCES; large-eddy simulation; complex terrain; weather research and forecasting model; turbulence generation; cell perturbation method; the Perdigão

Citation Formats

Connolly, Alex, van Veen, Leendert, Neher, James, Geurts, Bernard J., Mirocha, Jeff D., and Chow, Fotini Katopodes. Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain. United States: N. p., 2020. Web. doi:10.3390/atmos12010055.
Connolly, Alex, van Veen, Leendert, Neher, James, Geurts, Bernard J., Mirocha, Jeff D., & Chow, Fotini Katopodes. Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain. United States. https://doi.org/10.3390/atmos12010055
Connolly, Alex, van Veen, Leendert, Neher, James, Geurts, Bernard J., Mirocha, Jeff D., and Chow, Fotini Katopodes. Thu . "Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain". United States. https://doi.org/10.3390/atmos12010055. https://www.osti.gov/servlets/purl/1866158.
@article{osti_1866158,
title = {Efficacy of the Cell Perturbation Method in Large-Eddy Simulations of Boundary Layer Flow over Complex Terrain},
author = {Connolly, Alex and van Veen, Leendert and Neher, James and Geurts, Bernard J. and Mirocha, Jeff D. and Chow, Fotini Katopodes},
abstractNote = {A challenge to simulating turbulent flow in multiscale atmospheric applications is the efficient generation of resolved turbulence motions over an area of interest. One approach is to apply small perturbations to flow variables near the inflow planes of turbulence-resolving simulation domains nested within larger mesoscale domains. While this approach has been examined in numerous idealized and simple terrain cases, its efficacy in complex terrain environments has not yet been fully explored. Here, we examine the benefits of the stochastic cell perturbation method (CPM) over real complex terrain using data from the 2017 Perdigão field campaign, conducted in an approximately 2-km wide valley situated between two nearly parallel ridges. Following a typical configuration for multiscale simulation using nested domains within the Weather Research and Forecasting (WRF) model to downscale from the mesoscale to a large-eddy simulation (LES), we apply the CPM on a domain with horizontal grid spacing of 150 m. At this resolution, spurious coherent structures are often observed under unstable atmospheric conditions with moderate mean wind speeds. Results from such an intermediate resolution grid are often nested down for finer, more detailed LES, where these spurious structures adversely affect the development of turbulence on the subsequent finer grid nest. We therefore examine the impacts of the CPM on the representation of turbulence within the nested LES domain under moderate mean flow conditions in three different stability regimes: weakly convective, strongly convective, and weakly stable. In addition, two different resolutions of the underlying terrain are used to explore the role of the complex topography itself in generating turbulent structures. We demonstrate that the CPM improves the representation of turbulence within the LES domain, relative to the use of high-resolution complex terrain alone. During the convective conditions, the CPM improves the rate at which smaller-scales of turbulence form, while also accelerating the attenuation of the spurious numerically generated roll structures near the inflow boundary. During stable conditions, the coarse mesh spacing of the intermediate LES domain used herein was insufficient to maintain resolved turbulence using CPM as the flow develops downstream, highlighting the need for yet higher resolution under even weakly stable conditions, and the importance of accurate representation of flow on intermediate LES grids.},
doi = {10.3390/atmos12010055},
journal = {Atmosphere (Basel)},
number = 1,
volume = 12,
place = {United States},
year = {Thu Dec 31 00:00:00 EST 2020},
month = {Thu Dec 31 00:00:00 EST 2020}
}

Works referenced in this record:

Mixing efficiency in turbulent shear layers
journal, January 2001


Mesoscale to Microscale Simulations over Complex Terrain with the Immersed Boundary Method in the Weather Research and Forecasting Model
journal, January 2020

  • Wiersema, David J.; Lundquist, Katherine A.; Chow, Fotini Katopodes
  • Monthly Weather Review, Vol. 148, Issue 2
  • DOI: 10.1175/MWR-D-19-0071.1

Wind Flow Over Complex Terrain: A Historical Perspective and the Prospect for Large-Eddy Modelling
journal, August 2000


The Shuttle Radar Topography Mission
journal, January 2007

  • Farr, Tom G.; Rosen, Paul A.; Caro, Edward
  • Reviews of Geophysics, Vol. 45, Issue 2
  • DOI: 10.1029/2005RG000183

Long-term simulation of the boundary layer flow over the double-ridge site during the Perdigão 2017 field campaign
journal, January 2019

  • Wagner, Johannes; Gerz, Thomas; Wildmann, Norman
  • Atmospheric Chemistry and Physics, Vol. 19, Issue 2
  • DOI: 10.5194/acp-19-1129-2019

Toward Numerical Modeling in the “Terra Incognita”
journal, July 2004


Generation of Turbulent Inflow Data for Spatially-Developing Boundary Layer Simulations
journal, March 1998

  • Lund, Thomas S.; Wu, Xiaohua; Squires, Kyle D.
  • Journal of Computational Physics, Vol. 140, Issue 2
  • DOI: 10.1006/jcph.1998.5882

Bridging the Transition from Mesoscale to Microscale Turbulence in Numerical Weather Prediction Models
journal, August 2014

  • Muñoz-Esparza, Domingo; Kosović, Branko; Mirocha, Jeff
  • Boundary-Layer Meteorology, Vol. 153, Issue 3
  • DOI: 10.1007/s10546-014-9956-9

Resolved Turbulence Characteristics in Large-Eddy Simulations Nested within Mesoscale Simulations Using the Weather Research and Forecasting Model
journal, February 2014

  • Mirocha, Jeff; Kosović, Branko; Kirkil, Gokhan
  • Monthly Weather Review, Vol. 142, Issue 2
  • DOI: 10.1175/MWR-D-13-00064.1

A Tutorial on Lateral Boundary Conditions as a Basic and Potentially Serious Limitation to Regional Numerical Weather Prediction
journal, November 1997


Characteristics of roll and cellular convection in a deep and wide semiarid valley: A large-eddy simulation study
journal, July 2019


Stratocumulus-capped mixed layers derived from a three-dimensional model
journal, June 1980

  • Deardorff, James W.
  • Boundary-Layer Meteorology, Vol. 18, Issue 4
  • DOI: 10.1007/BF00119502

A priori and a posteriori tests of inflow conditions for large-eddy simulation
journal, December 2004

  • Keating, Anthony; Piomelli, Ugo; Balaras, Elias
  • Physics of Fluids, Vol. 16, Issue 12
  • DOI: 10.1063/1.1811672

Using NOAA AVHRR and SPOT VGT data to estimate surface parameters: application to a mesoscale meteorological model
journal, January 2004


Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave
journal, July 1997

  • Mlawer, Eli J.; Taubman, Steven J.; Brown, Patrick D.
  • Journal of Geophysical Research: Atmospheres, Vol. 102, Issue D14
  • DOI: 10.1029/97JD00237

Computational modelling for wind energy assessment
journal, October 2008


Multi-Scale Simulation of Wind Farm Performance during a Frontal Passage
journal, February 2020

  • Arthur, Robert S.; Mirocha, Jeffrey D.; Marjanovic, Nikola
  • Atmosphere, Vol. 11, Issue 3
  • DOI: 10.3390/atmos11030245

The MATERHORN: Unraveling the Intricacies of Mountain Weather
journal, November 2015

  • Fernando, H. J. S.; Pardyjak, E. R.; Di Sabatino, S.
  • Bulletin of the American Meteorological Society, Vol. 96, Issue 11
  • DOI: 10.1175/BAMS-D-13-00131.1

Investigation of model parameters for high-resolution wind energy forecasting: Case studies over simple and complex terrain
journal, November 2014

  • Marjanovic, Nikola; Wharton, Sonia; Chow, Fotini K.
  • Journal of Wind Engineering and Industrial Aerodynamics, Vol. 134
  • DOI: 10.1016/j.jweia.2014.08.007

Thermodynamic Variability within the Convective Boundary Layer Due to Horizontal Convective Rolls
journal, May 1996


A Large-Eddy-Simulation Model for the Study of Planetary Boundary-Layer Turbulence
journal, July 1984


The Convective Boundary Layer in the Terra Incognita
journal, July 2014

  • Zhou, Bowen; Simon, Jason S.; Chow, Fotini K.
  • Journal of the Atmospheric Sciences, Vol. 71, Issue 7
  • DOI: 10.1175/JAS-D-13-0356.1

Inlet conditions for large eddy simulation: A review
journal, April 2010


An Improved Mellor–Yamada Level-3 Model: Its Numerical Stability and Application to a Regional Prediction of Advection Fog
journal, March 2006


Numerically induced high-pass dynamics in large-eddy simulation
journal, December 2005

  • Geurts, Bernard J.; van der Bos, Fedderik
  • Physics of Fluids, Vol. 17, Issue 12
  • DOI: 10.1063/1.2140022

High-Resolution Large-Eddy Simulations of Flow in a Steep Alpine Valley. Part I: Methodology, Verification, and Sensitivity Experiments
journal, January 2006

  • Chow, Fotini Katopodes; Weigel, Andreas P.; Street, Robert L.
  • Journal of Applied Meteorology and Climatology, Vol. 45, Issue 1
  • DOI: 10.1175/JAM2322.1

Comparison of Measured and Numerically Simulated Turbulence Statistics in a Convective Boundary Layer Over Complex Terrain
journal, November 2016


Convectively Induced Secondary Circulations in Fine-Grid Mesoscale Numerical Weather Prediction Models
journal, September 2014


Atmospheric modeling to assess wind dependence in tracer dilution method measurements of landfill methane emissions
journal, March 2018


Generation of Inflow Turbulence in Large-Eddy Simulations of Nonneutral Atmospheric Boundary Layers with the Cell Perturbation Method
journal, June 2018


Practical Considerations for Computing Dimensional Spectra from Gridded Data
journal, September 2017

  • Durran, Dale; Weyn, Jonathan A.; Menchaca, Maximo Q.
  • Monthly Weather Review, Vol. 145, Issue 9
  • DOI: 10.1175/MWR-D-17-0056.1