Abstract
The unstable normal modes of the barotropic vorticity equation, linearized around an observed zonally varying atmospheric flow, have been related to patterns of observed low-frequency variability. The sensitivity of this problem to changes in the model truncation and diffusion and to details of the basic state flow are examined. Normal modes that are highly sensitive to these changes are found to be of minimal relevance to the low-frequency variability of the atmosphere. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 2393-2410 |
| Number of pages | 18 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 48 |
| Issue number | 22 |
| DOIs | |
| State | Published - 1991 |