Abstract
We report an unprecedented description of the latitudinal structure of tropical Pacific Ocean sea level variability for time scales between 3 and 100 days. A plot of calculated sea level variance latitude and frequency is described and exposes a rich variety of phenomena. We find signals due to the fortnightly tide, equatorial waves, zonal current instabilities, and atmospheric forcing.
| Original language | American English |
|---|---|
| Journal | Journal of Physical Oceanography |
| Volume | 17 |
| DOIs | |
| State | Published - Jan 1 1987 |
| Externally published | Yes |
Disciplines
- Life Sciences
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