Abstract: he three-dimensional responses of a cyclonic ocean eddy (COE) for 1?2 months following a typhoon were investigated using altimeter data and numerical experiments. Two significant features were found: 1) the cyclonic eddy ...

Abstract: easurements of turbulence in the deep ocean, particularly close to the bottom, are extremely sparse because of the difficulty and operational risk of obtaining deep profiles near the seafloor. A newly developed expendable ...