Abstract
The effect of horizontal transports of momentum and heat by transient eddies (TE) on the time-mean flow is studied by examining the relevant terms in a local budget of quasi-geostrophic potential vorticity. Two long-term observational data sets are used, and results for the Northern Hemisphere winter are presented. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1972-1984 |
| Number of pages | 13 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 39 |
| Issue number | 9 |
| DOIs | |
| State | Published - 1982 |
| Externally published | Yes |
All Science Journal Classification (ASJC) codes
- Atmospheric Science