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== Dissipation rate estimation ==
[[File:Arnaud Pic.jpg|thumb|Arnaud Le Boyer - Project Scientist in the MOD group at the Scripps Institution of Oceanography ]]
I am a seagoing physical oceanographer and part of the Multiscale Ocean Dynamics group at SIO/UCSD. I am tracking the energy path from internal wave sources all the way down to dissipation using long-term velocity times series and turbulence measurements.
The processing of shear-probe data can be divided into the following five major steps and these steps apply to data collected with any platform or vehicle. There are many sub-steps to these major steps. The major steps are;
To that end, I am leading the development of the EPSILOMETER, the one-and-only SCRIPPS micro-structure profiler, and get my hands “dirty” with software and the analog front end development, as well as probe fabrication.
# Conversion to physical units.
#:* [[Determine the speed of profiling]] of the shear-probe through the water.
#:* Determine the temperature of the water.
#:* Convert the shear-probe data samples into physical units
#:* Convert all other signals per the recommendations of the manufacturer of the sensor or instruments that produce these signals.
# Extract the profile defined in step 2.
# High-pass filter the shear-probe and (optionally) the vibration data.
http://www.mod.ucsd.edu/arnaud-le-boyer
# Identify each diss-length segment in the profile.
# De-spike the shear-probe data, and track the fraction of data affected by de-spiking within each diss-length segment. This will become a quality-control metric.
# Calculate the frequency spectra and cross-spectra of shear and vibrations for each diss-length segment using the method described here.
# Extract the original and the vibration-coherent clean shear-probe frequency spectra.
# Correct shear and vibration frequency spectra for the high-pass filter.
# Correct the cleaned frequency spectra for the bias induced by the Goodman algorithm.
# Convert the frequency spectra into wavenumber spectra using the mean speed for each diss-length segment.
# Correct the spectra of shear for the wavenumber response of the shear probe.
# Apply an iterative spectral integration algorithm to estimate the variance of shear, which is described here.
# Calculate the rate of dissipation by multiplying the shear variance by
Latest revision as of 17:41, 10 December 2021
Arnaud Le Boyer - Project Scientist in the MOD group at the Scripps Institution of Oceanography
I am a seagoing physical oceanographer and part of the Multiscale Ocean Dynamics group at SIO/UCSD. I am tracking the energy path from internal wave sources all the way down to dissipation using long-term velocity times series and turbulence measurements.
To that end, I am leading the development of the EPSILOMETER, the one-and-only SCRIPPS micro-structure profiler, and get my hands “dirty” with software and the analog front end development, as well as probe fabrication.
