Abstract
Fields of TOPEX-derived sea level anomalies are validated against and compared with fields of Tropical Ocean and Global Atmosphere-Tropical Atmosphere Ocean (TOGA-TAO) dynamic height anomalies. At periods longer than 35 days, TOPEX sea level anomalies compared extremely well with TOGA-TAO dynamic height anomalies throughout the whole basin. Zonal geostrophic current anomalies are then derived from both data sets and validated against in situ current meter measurements at the equator. Despite localized discrepancies, basin-wide TOGA-TAO geostrophic currents compare reasonably well with TOPEX-derived geostrophic currents. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 25,087-25,099 |
| Journal | Journal of Geophysical Research |
| Volume | 100 |
| Issue number | C12 |
| DOIs | |
| State | Published - 1995 |