CONTENTS
- Internal Waves on the Continental Shelf
- Observations of the Internal Tide on the Southern California Shelf
- Internal Wave Energetics at a Seamount on the California Continental Borderland
- Internal Wave Measurements in Mamala Bay, Oahu, Hawaii
- Mixing over Shelves and Slopes
- Modeling Internal Tide Generation and Evolution into Internal Solitary Waves on the Australian North West Shelf
- Internal Tide Generation at Open Ocean Topographies
- The Hawaii Ocean Mixing Experiment (HOME): Is the Abyssal Stratification Maintained by Tidalgenic Mixing?
- Numerical Simulations and Observations of the Internal Tide in a Submarine Canyon
- Baroclinic Wave Drag and Barotropic to Baroclinic Energy Transfer at Sills as Evidenced by Tidal Retardation, Seiche Damping and Diapycnal Mixing in Fjords
- Stratified Flow Over Topography and the Generation of Internal Solitary Waves
- Exact Solitary Wave Solutions in Shallow Water
- Internal Solitary Waves in Lakes--a Closure Problem for Hydrostatic Models
- Vertical Mixing Induced by Tidally Generated Internal Waves in the Kuril Straits
- A Rough Recipe for the Energy Balance of Quasi-Steady Internal Lee Waves
- 72 + 25 = 99 + 1, or Some of what we Still Don't Know: Wave Groups and Boundary Processes
- Mixing Generated by Internal Waves Interacting with Rough Topography
- Along-Slope Current Generation by Obliquely Incident Internal Waves
- Turbulent Properties in a Wave-Energized Benthic Boundary Layer
- On Redistributed Energy Fluxes in Topographic Scattering Problems
- A Comparison of Highly Nonlinear Gravity-wave Generation by Two and Three Dimensional Obstacles
- Short-Term Directional Variability of the Continuum Range in the Dep-OCean Internal Wave Field
- Observations of Low-Latitude, Near-Intertial Gravity Waves Forced by Westerly Wind Bursts
- Internal Wave Generation in the Equatorial Undercurrent
- Large-Eddy Simulation of Pressure Transport Below the Mixed Layer
- Near-Inertial Wave Generation on an Unsteady Ocean Current
- Model Predicted Distribution of Internal Wave Energy for Diapycnal Mixing Processes in the Deep Waters of the North Pacific
- What is the "Near-Inertial" Band and Why is it Different?
- The Role of Vertical Divergence in Internal Wave/Wave Interaction
- Observations of Fine-Scale Richardson Number, Strain, and Effective Strain Rate Conditions Accompanying Overturning Events in the Thermocline
- Waves, Turbulence, and Mixing Parameterizations
- Large Eddy Simulation of Oceanic Fine Structure
- Diapycnal Mixing and Internal Waves
This page was last updated Wednesday 14 August 2002.
Please send all comments to dhenders@hawaii.edu.
Thank you!