Submesoscale Structure of the California Current Near San Clements Island
Abstract
The purpose of the San Clemente Basin Experiment (SCBE) was to survey the upper ocean currents and temperature in a region southwest of San Clemente Island (SCI). To accomplish this, two cruises were made during which currents were measured by using a shipboard mounted Acoustic Doppler Current Profile (ADCP). Temperature was measured during the second cruise by deploying expendable bathythermographs. The first cruise took place during 17-21 July 1989 and the second one during 2-6 September 1989. Data indicate a variety of features. Two different flow patterns were observed: Strong poleward alongshore flow (about 40 cm/s) occurred 40-60 km west of SCI and small scale eddies were seen further offshore, i.e. farther than 60 km west of SCI. The alongshore flow intensified poleward, reaching 300 m depth. The smaller scale eddies have a length scale of about 10 km and are believed to be associated with larger scale horizontal shear due to the California Current. Keywords: Coastal circulation; Upper ocean currents; Nearshore eddies.
Document Details
- Document Type
- Technical Report
- Publication Date
- Apr 01, 1990
- Accession Number
- ADA221489
Entities
People
- Cheng‐Yu Tsai
- Curtis Collins
- Paul F. Jessen
- Peter Cheng Chu
Organizations
- Naval Postgraduate School