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Civil-Comp Proceedings
ISSN 1759-3433 CCP: 84
PROCEEDINGS OF THE FIFTH INTERNATIONAL CONFERENCE ON ENGINEERING COMPUTATIONAL TECHNOLOGY Edited by: B.H.V. Topping, G. Montero and R. Montenegro
Paper 100
A Three-Dimensional Mass Consistent Wind Model Using Terrain Adapted Tetrahedral Meshes E. Rodríguez, G. Montero, R. Montenegro, J.M. Escobar and J.M. González-Yuste
University Institute of Intelligent Systems and Numerical Applications in Engineering (IUSIANI), University of Las Palmas de Gran Canaria, Spain , "A Three-Dimensional Mass Consistent Wind Model Using Terrain Adapted Tetrahedral Meshes", in B.H.V. Topping, G. Montero, R. Montenegro, (Editors), "Proceedings of the Fifth International Conference on Engineering Computational Technology", Civil-Comp Press, Stirlingshire, UK, Paper 100, 2006. doi:10.4203/ccp.84.100
Keywords: wind modelling, mass consistent models, finite element method, tetrahedral meshes, parameter estimation.
Summary
Mass consistent models have been widely used in three-dimensional wind modelling by the finite element method. In general, these problems are defined over regions with complex terrain and variable roughness length, therefore a suitable discretization of the studied zone will be necessary. In addition, points often exist where more accuracy is required. We have used a method for constructing tetrahedral meshes which are simultaneously adapted to the terrain orography and the roughness length by using a refinement-derefinement process in a two-dimensional mesh corresponding to the terrain surface, following the technique proposed in [1,2,3]. In this two-dimensional mesh we include a local refinement around several points which are previously defined by the user. We further develop a technique for adapting the mesh to any contour that has an important role in the simulation, like shorelines or roughness length contours [4,5]. The final tetrahedral mesh is also constructed with a greater density of nodes near the terrain. The regions where a greater density of points is needed to obtain a more accurate solution, are locally refined with the procedure proposed in [6].
This wind model improves that proposed in [7,8]. The characterization of the atmospheric stability is carried out by means of the experimental measures of the intensities of turbulence. On the other hand, since several measures are often available at a same vertical line, we have constructed a least square optimization of such measures for developing a vertical profile of wind velocities from an optimum friction velocity. The three main parameters governing the model are estimated using genetic algorithms with a parallel implementation [8,9,10]. For a given episode, we periodically update these parameters. In order to test the model, some numerical experiments are presented, comparing the results with realistic measures. References
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