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Short spatial mooring-tilt variations from deep Mediterranean observations
Hans van Haren
Interaction between energy-abundant mesoscale eddies and internal waves can lead to convection-turbulence generation and may prove important for deep-sea life and circulation. Howe…
Whipped and mixed warm clouds in the deep sea
Hans van Haren
Turbulence is indispensable to redistribute nutrients for all life forms larger than microbial, on land and in the ocean. Yet, the development of deep-sea turbulence was not studie…
Convection and intermittency noise in water temperature near a deep Mediterranean seafloor
Hans van Haren
Turbulent and internal wave motions are important for the exchange of momentum, heat and suspended matter in the deep-sea which is generally stably stratified in density. Turbulenc…
Estimates of the temperature flux-temperature gradient relation above a sea-floor
Andrea A. Cimatoribus, Hans van Haren
The relation between the flux of temperature (or buoyancy), the vertical temperature gradient and the height above the bottom, is investigated in an oceanographic context, using hi…
Temperature statistics above a deep-ocean sloping boundary
Andrea A. Cimatoribus, Hans van Haren
We present a detailed analysis of the temperature statistics in an oceanographic observational dataset. The data are collected using a moored array of thermistors, 100 m tall and s…
Comparison of Ellison and Thorpe scales from Eulerian ocean temperature observations
Andrea Cimatoribus, Hans van Haren, Louis Gostiaux
Ocean turbulence dissipation rate is estimated either by means of microstructure shear measurements, or by adiabatically reordering vertical profiles of density. The latter techniq…