Abstract: The generation of internal tides can be ascribed to the action of a buoyancy force caused by the flow of the barotropic tide over topographic features. It is commonly assumed that the barotropic flow can be taken as ...

Abstract: he purpose of this paper is to resolve a confusion that may arise from two quite distinct definitions of ?Doppler shifts?: both are used in the oceanographic literature but they are sometimes conflated. One refers to the ...