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Large-Eddy Simulation of the Stable Atmospheric Boundary Layer using Dynamic Models with Different Averaging Schemes

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Abstract

Large-eddy simulation (LES) of a stable atmospheric boundary layer is performed using recently developed dynamic subgrid-scale (SGS) models. These models not only calculate the Smagorinsky coefficient and SGS Prandtl number dynamically based on the smallest resolved motions in the flow, they also allow for scale dependence of those coefficients. This dynamic calculation requires statistical averaging for numerical stability. Here, we evaluate three commonly used averaging schemes in stable atmospheric boundary-layer simulations: averaging over horizontal planes, over adjacent grid points, and following fluid particle trajectories. Particular attention is focused on assessing the effect of the different averaging methods on resolved flow statistics and SGS model coefficients. Our results indicate that averaging schemes that allow the coefficients to fluctuate locally give results that are in better agreement with boundary-layer similarity theory and previous LES studies. Even among models that are local, the averaging method is found to affect model coefficient probability density function distributions and turbulent spectra of the resolved velocity and temperature fields. Overall, averaging along fluid pathlines is found to produce the best combination of self consistent model coefficients, first- and second-order flow statistics and insensitivity to grid resolution.

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Authors and Affiliations

  1. Saint Anthony Falls Laboratory, Department of Civil Engineering, University of Minnesota, Minneapolis, 55414, MN, USA

    Rob Stoll & Fernando Porté-Agel

  2. National Center for Earth-Surface Dynamics, Minneapolis, 55414, MN, USA

    Rob Stoll & Fernando Porté-Agel

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  1. Rob Stoll
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  2. Fernando Porté-Agel
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Correspondence to Fernando Porté-Agel.

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Stoll, R., Porté-Agel, F. Large-Eddy Simulation of the Stable Atmospheric Boundary Layer using Dynamic Models with Different Averaging Schemes. Boundary-Layer Meteorol 126, 1–28 (2008). https://doi.org/10.1007/s10546-007-9207-4

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  • DOI: https://doi.org/10.1007/s10546-007-9207-4

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