TY - JOUR
T1 - Dynamic LES modeling of a diurnal cycle
AU - Basu, Sukanta
AU - Vinuesa, Jean François
AU - Swift, Adrew
N1 - Funding Information:
The author wishes to thank Mr M.J. Howarth and Mr G.A. Alcock of I.O.S. Bidston and Mr S. Ferguson of Liverpool University for providing the original data. Dr N.S. Heaps gave much advice and guidance during the work. Thanks are also due to,& R.A. Smith for preparing the diagrams. The work described in this paper was funded by a Consortium consisting of the Natural Environment Research Council, the Ministry of Agriculture, Fisheries and Food and the Departments of Energy and Industry.
PY - 2008
Y1 - 2008
N2 - The diurnally varying atmospheric boundary layer observed during the Wangara (Australia) case study is simulated using the recently proposed locally averaged scale-dependent dynamic subgrid-scale (SGS) model. This tuning-free SGS model enables one to dynamically compute the Smagorinsky coefficient and the subgrid-scale Prandtl number based on the local dynamics of the resolved velocity and temperature fields. It is shown that this SGS-model-based large-eddy simulation (LES) has the ability to faithfully reproduce the characteristics of observed atmospheric boundary layers even with relatively coarse resolutions. In particular, the development, magnitude, and location of an observed nocturnal low-level jet are depicted quite well. Some well-established empirical formulations (e.g., mixed layer scaling, spectral scaling) are recovered with good accuracy by this SGS parameterization. The application of this new-generation dynamic SGS modeling approach is also briefly delineated to address several practical wind-energy-related issues.
AB - The diurnally varying atmospheric boundary layer observed during the Wangara (Australia) case study is simulated using the recently proposed locally averaged scale-dependent dynamic subgrid-scale (SGS) model. This tuning-free SGS model enables one to dynamically compute the Smagorinsky coefficient and the subgrid-scale Prandtl number based on the local dynamics of the resolved velocity and temperature fields. It is shown that this SGS-model-based large-eddy simulation (LES) has the ability to faithfully reproduce the characteristics of observed atmospheric boundary layers even with relatively coarse resolutions. In particular, the development, magnitude, and location of an observed nocturnal low-level jet are depicted quite well. Some well-established empirical formulations (e.g., mixed layer scaling, spectral scaling) are recovered with good accuracy by this SGS parameterization. The application of this new-generation dynamic SGS modeling approach is also briefly delineated to address several practical wind-energy-related issues.
UR - http://www.scopus.com/inward/record.url?scp=57649165538&partnerID=8YFLogxK
U2 - 10.1175/2007JAMC1677.1
DO - 10.1175/2007JAMC1677.1
M3 - Article
AN - SCOPUS:57649165538
SN - 1558-8424
VL - 47
SP - 1156
EP - 1174
JO - Journal of Applied Meteorology and Climatology
JF - Journal of Applied Meteorology and Climatology
IS - 4
ER -