Abstract
An analytical model is presented that accommodates nonhydrostatic shearing stratified flow over an obstacle, and that can be modified to include a superposed stratosphere with constant wind and higher stability. A simulation code is used in parallel with the analytic calculations to demonstrate a methodology for determining the wavelength and magnitude of gravity wave energy reflected, and that transmitted, by the tropopause. -Authors
| Original language | English |
|---|---|
| Pages (from-to) | 3269-3281 |
| Number of pages | 13 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 44 |
| Issue number | 21 |
| DOIs | |
| State | Published - 1987 |