[2] Lin C L, Glendening J W. Large eddy simulation of an inhomogeneous atmospheric boundary layer under neutral conditions [J]. Journal of the Atmospheric Sciences, 2002, 59(16): 2479-2497.
[3] Dosio A, de Arellano J V G. Statistics of absolute and relative dispersion in the atmospheric convective boundary layer: A large-eddy simulation study [J]. Journal of the Atmospheric Sciences, 2006, 63(4): 1253-1272.
[4] Glendening J W, Lin C L. Large eddy simulation of internal boundary layers created by a change in surface roughness [J]. Journal of the Atmospheric Sciences, 2002, 59(10): 1697-1711.
[5] Kumar V., Kleissl J, Meneveau C, et al. Large-eddy simulation of a diurnal cycle of the atmospheric boundary layer: atmospheric stability and scaling issues [J]. Water Resources Research, 2006, 42(6): W06D09.1-W06D09.18
[18] Grisogono B. Wave drag effects in a mesoscale model with a higher-order closure turbulence scheme [J]. Journal of Applied Meteorology, 1995, 34(4): 941-954.
[19] Arola A. Parameterization of turbulent and mesoscale fluxes for heterogeneous surfaces [J]. Journal of the Atmospheric Sciences, 1999, 56(4): 584-598.
[20] Kang S L , Davis K J. The effects of mesoscale surface heterogeneity on the fair-weather convective atmospheric boundary layer [J]. Journal of the Atmospheric Sciences, 2008, 65(10): 3197-3213.
[21] Letzel M O, Raasch S. Large eddy simulation of thermally induced oscillations in the convective boundary layer [J]. Journal of the Atmospheric Sciences, 2003, 60(18): 2328-2341.