Research Article
An MCV Nonhydrostatic Atmospheric Model with Height-Based Terrain following Coordinate: Tests of Waves over Steep Mountains
Figure 3
Numerical results of case A3. Numerical solution (a), semianalytic solution (b), streamlines from 0 to half vertical wavelength height over an isolated mountain (c), and normalized momentum flux (d) are shown. Contour interval is 0.25 ms−1. All negative values are denoted by dashed lines.
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(d) |