Simulation of the seasonal cycle in the tropical Atlantic Ocean with a multi‐level primitive equation numerical model yields remarkably realistic results including the separation of the Brazilian Current from the coast and the reversal of the Countercurrent. This paper is not subject to U.S. copyright.
|Original language||English (US)|
|Number of pages||3|
|Journal||Geophysical Research Letters|
|State||Published - Aug 1984|
All Science Journal Classification (ASJC) codes
- Earth and Planetary Sciences(all)