Articles | Volume 6, issue 1 
            
                
                    
            
            
            
        https://doi.org/10.5194/asr-6-155-2011
                    © Author(s) 2011. This work is distributed under the Creative Commons Attribution 3.0 License.
                Atmospheric boundary layer wind profile at a flat coastal site – wind speed lidar measurements and mesoscale modeling results
Cited articles
                        
                        Blackadar, A.: The vertical distribution of wind and turbulent exchange in a neutral atmosphere, J. Geophys. Res., 67, 3095–3102, 1962.
                    
                
                        
                        Chen, F. and Dudhia, J.: Coupling an advanced land surface-hydrology model with the Penn State-NCAR MM5 modeling system. Part I: Model implementation and sensitivity, Mon. Weather Rev., 129, 569–585, 2001.
                    
                
                        
                        Draxl, C., Hahmann, A., Pe{ñ}a, A., Nissen, J., and Giebel, G.: Validation of boundary-layer winds from WRF mesoscale forecasts with applications to wind energy forecasting, in: 19th Symposium on Boundary Layers and Turbulence, Keystone, Colorado, Paper 1B.1, 7 pp., 2010.
                    
                
                        
                        Gryning, S., Batchvarova, E., Br{ü}mmer, B., Jørgensen, H., and Larsen, S.: On the extension of the wind profile over homogeneous terrain beyond the surface boundary layer, Bound.-Lay. Meteorol., 124, 251–268, 2007.
                    
                
                        
                        Gryning, S., Batchvarova, E., Quante, M., and Matthias, V.: Evaluation of vertical profiles in mesoscale meteorological models based on observations for the COST728 study of winter 2003 PM episodes in Europe, in: Air Pollution Modeling and its Application, edited by: Steyn, D. and Trini-Casteli, S., Springer Science+Business Media B.V, Dordrecht, The Netherlands, in print, 2011.
                    
                 
 
             
             
             
            