Abstract
A three dimensional linear model of orographically forced gravity waves (mountain waves) using realistic topography is used to simulate a high altitude (20 km) ER‐2 encounter with a large mountain wave over Alexander Island (72° W, 69° −72° S). Reasonable agreement between the linear model and observations is obtained if the effects of low‐level flow blocking are taken into account.
| Original language | English |
|---|---|
| Pages (from-to) | 81-84 |
| Number of pages | 4 |
| Journal | Geophysical Research Letters |
| Volume | 17 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jan 1990 |