Arabian Sea Dynamics
Abstract
The goal is to identify and understand the mechanisms which determine features of stratification and motion in the upper 200 m or so of mid-latitude oceans. This is the depth range over which surface fluxes of momentum and buoyancy have direct influence. Our interest is in the processes by which shear and stratification interact to change upper ocean structure.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 30, 1997
- Accession Number
- ADA627645
Entities
People
- Charles C. Eriksen
Organizations
- University of Washington