Gulf Stream Boundary Interactions
Abstract
An array of subsurface current meter moorings was deployed for two years on the western slope of the Grand Banks to investigate the possibility that low frequency waves (Topographic Rossby Waves) were being radiated westward along the Rise and Slope by disturbances in the Gulf Stream to the south. Wave motions consistent with these dynamics were clearly evident in the data and their amplitude was found to be especially large at periods shorter than about 10 days. At longer periods there was no special enhancement, thus disagreeing with the prior expectations which were based on simple theoretical arguments.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jan 01, 2004
- Accession Number
- ADA435583
Entities
People
- Nelson G. Hogg
Organizations
- Woods Hole Oceanographic Institution