Abstract
A two-dimensional, nonlinear, nonhydrostatic model is described which allows the calculation of moist airflow in mountainous terrain. The model is compressible, uses a terrain-following co-ordinate system, and employs lateral and upper boundary conditions which minimize wave reflections.-from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2341-2361 |
| Number of pages | 21 |
| Journal | Monthly Weather Review |
| Volume | 111 |
| Issue number | 12 |
| DOIs | |
| State | Published - 1983 |