Research Article

An MCV Nonhydrostatic Atmospheric Model with Height-Based Terrain following Coordinate: Tests of Waves over Steep Mountains

Figure 1

Numerical results of linear hydrostatic mountain waves. Numerical solution (a), semianalytical solution (b), and normalized momentum flux (c) are shown. The contour values vary from −0.005 to 0.005 with an interval of 0.0005. Negative values are denoted by dashed lines.
(a)
(b)
(c)