Gulf of Tehuantepec Wind-Jet Response
Abstract
The objective of this study was to observe the response of the upper ocean to the strong (greater than 20 knots) wind jet that intermittently blows seaward over the Gulf of Tehuantepec (Pacific coast of southern Mexico) during winter. The jet results from atmospheric high pressure systems over the Gulf of Mexico being confined by the Sierra Madre mountain range (2 km high and extending for over 1000 km); the largest pass in the mountain range is just inland from the Gulf of Tehuantepec. The wind jet (Tehuantepecano) lasts for several days and extends 300 km seaward from the coast.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jan 01, 1990
- Accession Number
- ADA246636
Entities
People
- P. M. Kosro
- Robert L. Smith
Organizations
- Oregon State University