Stratified Flow Over Topography and Internal Solitary Waves
Abstract
Our long term goal is to use measurements of time varying stratified flow past topography to develop robust models of the relevant processes, including establishment of the high drag state, the role of boundary layer separation, friction and entrainment, and the generation, propagation and dissipation of internal solitary waves.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 30, 2002
- Accession Number
- ADA626450
Entities
People
- David M. Farmer
- Svein Vagle
Organizations
- University of Rhode Island