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.
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(b) |
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