uvi_01-20260114T1932-delayed
OxygèneSalinité de surfaceTempérature de surfaceCourants sous la surfaceSalinité sous la surfaceTempérature sous la surfaceCourants de surface
This research investigates how water masses are transformed as they flow through the Caribbean Sea, a region responsible for a quarter of the northern hemisphere's northward ocean heat transport and a vital component of the Atlantic Meridional Overturning Circulation (AMOC). The UVI glider will transit to 18 N 69 W, south of the Dominican Republic, and sample temperature, salinity, dissolved oxygen, and current velocity profiles from the surface to 900m depth southward along 69 W to just north of Curacao (12 24 N) – and return along the same path. The journey is expected to take a little over 3 months and will be repeated during hurricane season 2026. Delayed mode dataset.
Données et ressources
- Ce jeu de données n'a aucune ressource.
Informations supplémentaires
| DOI | https://doi.org/uvi_01-20260114T1932-delayed |
|---|---|
| Étendue temporelle | 2026-01-14 – 2026-04-08 |
| Étendue verticale | -964.8307 – 0.1419703 m |
| Date (publication) | 2026-09-30 |
| Date (creation) | 2026-11-04 |
| Statut | onGoing |
| Fréquence de mise à jour | asNeeded |
| Langue des métadonnées | en |
| Licence | This data may be redistributed and used without restriction. Data provided as is with no expressed or implied assurance of quality assurance or quality control |
| Métadonnées sources | ISO 19115 XML |
| Dernière mise à jour | 2026-11-04 |
| Créé | 2026-11-04 |
| API | package_show |