Add to ORKGNon UBCUnreviewedAuthor affiliation: Massachusetts Institute of TechnologyPostdoctora
The redistribution and dissipation of internal wave energy arising from the conversion at mid-ocean ...
Internal or baroclinic tidal currents are generated by the interaction of the barotropic tidal curre...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...
Non UBCUnreviewedAuthor affiliation: Massachusetts Institute of TechnologyPostdoctora
Non UBCUnreviewedAuthor affiliation: Massachusetts Institute of TechnologyFacult
Our long-term goal is to understand how energy is supplied to the ocean, and how it subsequently cas...
International audienceMicrostructure and fine-scale measurements collected in the central Bay of Bis...
Thesis (Ph.D.)--University of Washington, 2014A collection of field experiments and model simulation...
Internal gravity waves are a key process linking the large-scale mechanical forcing of the oceans to...
Direct Numerical Simulation (DNS) and Large Eddy Simulation (LES) are used to investigate and quanti...
International audienceWe investigate the stability of stratified fluid layers undergoing homogeneous...
Several claims have been made about the efficiency of internal wave scattering from rough topography...
Different types of internal wave and tide motion occur in the strongly stratified Strait of Georgia....
The interaction of tidal currents with sea-floor topography generates internal gravity waves, called...
A numerical study is performed to investigate nonlinear processes during internal wave generation by...
The redistribution and dissipation of internal wave energy arising from the conversion at mid-ocean ...
Internal or baroclinic tidal currents are generated by the interaction of the barotropic tidal curre...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...
Non UBCUnreviewedAuthor affiliation: Massachusetts Institute of TechnologyPostdoctora
Non UBCUnreviewedAuthor affiliation: Massachusetts Institute of TechnologyFacult
Our long-term goal is to understand how energy is supplied to the ocean, and how it subsequently cas...
International audienceMicrostructure and fine-scale measurements collected in the central Bay of Bis...
Thesis (Ph.D.)--University of Washington, 2014A collection of field experiments and model simulation...
Internal gravity waves are a key process linking the large-scale mechanical forcing of the oceans to...
Direct Numerical Simulation (DNS) and Large Eddy Simulation (LES) are used to investigate and quanti...
International audienceWe investigate the stability of stratified fluid layers undergoing homogeneous...
Several claims have been made about the efficiency of internal wave scattering from rough topography...
Different types of internal wave and tide motion occur in the strongly stratified Strait of Georgia....
The interaction of tidal currents with sea-floor topography generates internal gravity waves, called...
A numerical study is performed to investigate nonlinear processes during internal wave generation by...
The redistribution and dissipation of internal wave energy arising from the conversion at mid-ocean ...
Internal or baroclinic tidal currents are generated by the interaction of the barotropic tidal curre...
Internal tides are a predominant source of high‐frequency variability and diapycnal mixing in the oc...