In this study, we explore the applicability of a wavelet-entropy based segmentation technique in reduction of motion-induced contaminations in time-domain from subsurface turbulence measurements made by a moving shear probe. After the quality screening of data, the Shannon entropy procedure is combined with a time-dependent adaptive wavelet thresholding method to split each 60-s long shear segment into a number of motion-reduced subblocks. The wavelet-entropy strategy leads to preventing the false detection effect caused by applying either wavelet de-noising or Shannon entropy alone for conditions where the turbulence (strongly) overlap with scales induced by waves or platform motions. The longest stationary subblock, with a size greater th...
Ocean turbulence dissipation rate is estimated either by means of microstructure shear measurements,...
High levels of turbulence have been proven to substantially increase the blade loadings on tidal tur...
We compare estimates of the turbulent dissipation rate, , obtained independently from coincident me...
In this study, we explore the applicability of a wavelet-entropy based segmentation technique in red...
An internally recording, autonomous instrument has been tested for measurements of ocean turbulence ...
Preliminary results are presented from a moored, autonomous instrument measuring the upper ocean tur...
Upper-ocean turbulence is central to the exchanges of heat, momentum, and gases across the air–sea i...
AbstractPreliminary results are presented from a moored, autonomous instrument measuring the upper o...
Upper-ocean turbulence is central to the exchanges of heat, momentum, and gases across the air–sea i...
The combination of acoustic Doppler current profilers and the structure function methodology provide...
Townsend's (1976) attached eddy hypothesis states that the turbulent structure in the constant ...
Dissipation rate statistics in the near-surface layer of the ocean were obtained during the month-lo...
The structure function method for estimating the dissipation rate of turbulent kinetic energy, previ...
ABSTRACT Transitional flow data from boundary layers subject to strong acceleration (K as high as 9x...
Observations of turbulent dissipation rates measured by two independent instruments are compared wit...
Ocean turbulence dissipation rate is estimated either by means of microstructure shear measurements,...
High levels of turbulence have been proven to substantially increase the blade loadings on tidal tur...
We compare estimates of the turbulent dissipation rate, , obtained independently from coincident me...
In this study, we explore the applicability of a wavelet-entropy based segmentation technique in red...
An internally recording, autonomous instrument has been tested for measurements of ocean turbulence ...
Preliminary results are presented from a moored, autonomous instrument measuring the upper ocean tur...
Upper-ocean turbulence is central to the exchanges of heat, momentum, and gases across the air–sea i...
AbstractPreliminary results are presented from a moored, autonomous instrument measuring the upper o...
Upper-ocean turbulence is central to the exchanges of heat, momentum, and gases across the air–sea i...
The combination of acoustic Doppler current profilers and the structure function methodology provide...
Townsend's (1976) attached eddy hypothesis states that the turbulent structure in the constant ...
Dissipation rate statistics in the near-surface layer of the ocean were obtained during the month-lo...
The structure function method for estimating the dissipation rate of turbulent kinetic energy, previ...
ABSTRACT Transitional flow data from boundary layers subject to strong acceleration (K as high as 9x...
Observations of turbulent dissipation rates measured by two independent instruments are compared wit...
Ocean turbulence dissipation rate is estimated either by means of microstructure shear measurements,...
High levels of turbulence have been proven to substantially increase the blade loadings on tidal tur...
We compare estimates of the turbulent dissipation rate, , obtained independently from coincident me...