The Propagation of a Cold-Dome Meander: A Conceptual Model,
Abstract
The Model makes two assumptions. First we assume the cold water giving form to the dome is not trapped within the dome. We envisage a systematic vertical mass exchange: upwelling mass in the forward region replacing downwelling mass in the rear. Second, to attain the observed vertical coherence of the meander we assume the warm water overlying the dome to shrink or stretch in direct opposition to the stretching or shrinking within the dome. The model provides a new perspective, and the encouraging agreement found suggests that further study of the model could yield new insights into the dynamics of meandering.
Document Details
- Document Type
- Technical Report
- Publication Date
- Apr 01, 1982
- Accession Number
- ADP001043
Entities
People
- David A. Brooks
- Frank Chew
- John M. Bane Jr.
Organizations
- National Oceanic and Atmospheric Administration