Waves, Turbulence and Boundary Layers
Abstract
The long-term goal is to develop a unified fully coupled ocean wave - circulation model. This has not been possible previously since the interaction terms (e.g., wave radiation stress terms) are, a priori, vertically integrated (Phillips 1977) and the non-wave induced velocities have been assumed to be vertically constant. Following Mellor (2002), I plan to develop theory and computations for turbulent bottom boundary layers to account for shallow water wave and streaming effects.
Document Details
- Document Type
- Technical Report
- Publication Date
- Sep 30, 2005
- Accession Number
- ADA572826
Entities
People
- George L. Mellor