Processing your ADCP data using structure function techniques

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Revision as of 15:12, 30 May 2022 by Yuengdjern (talk | contribs)

To calculate the dissipation rate at a specific range bin and a specific time ensemble:

Schematic showing along-beam distance <math> r </math> and radial velocities.
  1. Extract or compute the along-beam bin center separation [<math>\delta r_0</math>] based on the instrument geometry
  2. Calculate the along-beam velocity fluctuation time-series in each bin <math>n</math>, where [<math>b’(n, t_s)</math>] from the along-beam velocity data that has met the QC criteria (i.e. the data in Level 2 of the netcdf file). Note <math> t_s </math> is the timeseries index within a segment.
  3. Select the maximum distance (<math>r_{max}</math>) over which to compute the structure function based on conditions of the flow (e.g., expected max overturn). The corresponding number of bins is [<math>n_{\text{rmax}} = r_{max} / \delta r_0</math>]
  4. Calculate the structure function <math>D_{ll}</math> for all possible bin separations <math>\delta</math> within <math>r_{max}</math> using either a bin-centred difference scheme or a forward-difference scheme.
  5. Perform a regression of <math>D_{ll}(n,\delta)</math> against <math>(\delta r)^{2/3}</math> for the appropriate range of bins and <math>\delta</math>r0 separation distances. Be aware of special considerations for forward-difference, center-difference schemes in setting up the regression calculation. The regression is typically done as a least-squares fit, either as:

    <math>D_{ll} = a_0 + a_1 (\delta r)^{2/3}</math>;
or as
<math>D_{ll} = a_0 + a_1 (\delta r)^{2/3}+a_3((\delta r)^{2/3})^3 </math>

the former being the canonical method that excludes non-turbulent velocity differences between bins, whereas the latter is a modified method that includes non-turbulent velocity differences between bins due to any oscillatory signal (e.g. surface waves, motion of the ADCP on a mooring).
  1. Use the coefficient <math>a_1</math> to calculate <math>\varepsilon</math> as

    <math>\varepsilon = \left(\frac{a_1}{C_2}\right)^{2/3}</math>

    where <math>C_2</math> is an empirical constant, typically taken as 2.0 or 2.1.



Next step: Apply quality-control on dissipation rates (QA2)

Previous step: Apply quality-control on velocity time series data (QA1)

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