|
  Reynolds' stress is a basic property of turbulence that can be measured
throughout the depth of the water column with an ADCP. When an ADCP measures velocity
data there are a variety of sampling modes that can be used and similarly there are
four different coordinate systems that can be used (beam, instrument, ship, and earth).
If data is recorded in beam coordinates (each of the four transducers just store their
velocity data in a seperate variable), a mean velocity and variance for each beam can be
computed, with which two components of the Reynolds' stress tensor can be computed
(namely u'w' and v'w'). There are issues with using this type of measurement scheme in
low energy environments with little turbulence. However, in energetic systems this
technique can provide a quantitative measure of turbulence over time throughout the water
column in the system.
|