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Journal of the Meteorological Society of Japan
A new mathematical model of the two-dimensional atmospheric boundary layer over undulating terrain is presented. Neither the hydrostatic assumption nor the Bousinesque assumption need to be introduced in this model. The system of equation is described with orthogonal curvilinear coordinates, and one of the axes (*) coincides with the undulating ground surface. Then, the system of equations are expanded in the Fourier series of and the time, following the spectral method. In this way, thedoi:10.2151/jmsj1965.59.3_361 fatcat:dqyyay3jfbdhdltfpez4m5c4qe