This dataset is associated to the NSF OCE/Physical Oceanography funded project “Laboratory Investigation of Turbulence Generation by Surface Waves”. There are three papers in preparation that will refer to data contained within this archive. The overarching goal of this project was to address a significant knowledge gap regarding the turbulent dissipation of non-breaking surface waves. To accomplish this, a comprehensive study in the SUrge-STructure-Atmosphere-INteraction (SUSTAIN) wind-wave laboratory at the University of Miami was conducted. A combination of established measurement approaches (Particle Image Velocimetry (PIV) and Vertical Microstructure Profiler (VMP)) and new technologies (Optical Turbulence Sensor (OTS)) have been used ...
Here we have determined the nature of turbulent flow associated with oceanic nonbreaking waves, whic...
Upper ocean turbulence is a very relevant process within the context of quantifying the exchange bet...
International audienceThe dissipation processes affecting short wind waves of centimeter and decimet...
Wave fields in the open ocean evolve according to the radiative transfer equation of wave energy or ...
This paper is dedicated to wave-induced turbulence unrelated to wave breaking. The existence of such...
Observations with a three-axis pulse-to-pulse coherent acoustic Doppler profiler and acoustic resona...
Wave-induced turbulence due to breaking in the absence of surface shear stresses is investigated exp...
To the best of our knowledge, one or more authors of this paper were federal employees when contribu...
Dissipation rate statistics in the near-surface layer of the ocean were obtained during the month-lo...
We have carried out an experimental study of the turbulence kinetic energy dissipation rate (e), tem...
Wave-induced turbulence due to breaking in the absence of surface shear stresses is investigated exp...
Observations of turbulent dissipation rates measured by two independent instruments are compared wit...
Here, for non-breaking short surface waves, we have experimentally determined the value of the turbu...
The ocean surface is a complex boundary where air-sea fluxes of mass, momentum and energy take place...
The ocean surface is a complex boundary where air-sea fluxes of mass, momentum and energy take place...
Here we have determined the nature of turbulent flow associated with oceanic nonbreaking waves, whic...
Upper ocean turbulence is a very relevant process within the context of quantifying the exchange bet...
International audienceThe dissipation processes affecting short wind waves of centimeter and decimet...
Wave fields in the open ocean evolve according to the radiative transfer equation of wave energy or ...
This paper is dedicated to wave-induced turbulence unrelated to wave breaking. The existence of such...
Observations with a three-axis pulse-to-pulse coherent acoustic Doppler profiler and acoustic resona...
Wave-induced turbulence due to breaking in the absence of surface shear stresses is investigated exp...
To the best of our knowledge, one or more authors of this paper were federal employees when contribu...
Dissipation rate statistics in the near-surface layer of the ocean were obtained during the month-lo...
We have carried out an experimental study of the turbulence kinetic energy dissipation rate (e), tem...
Wave-induced turbulence due to breaking in the absence of surface shear stresses is investigated exp...
Observations of turbulent dissipation rates measured by two independent instruments are compared wit...
Here, for non-breaking short surface waves, we have experimentally determined the value of the turbu...
The ocean surface is a complex boundary where air-sea fluxes of mass, momentum and energy take place...
The ocean surface is a complex boundary where air-sea fluxes of mass, momentum and energy take place...
Here we have determined the nature of turbulent flow associated with oceanic nonbreaking waves, whic...
Upper ocean turbulence is a very relevant process within the context of quantifying the exchange bet...
International audienceThe dissipation processes affecting short wind waves of centimeter and decimet...