Determine the speed of profiling: Difference between revisions

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The speed of profiling can be determined in a variety of different methods but it must be determined because it is required for the conversion of the shear-probe samples into physical units. Methods for determining the speed of profiling include, but are not limited to:
The speed of profiling can be determined with a variety of different methods.
It must be determined because it is required for the conversion of the shear-probe samples into physical units and for transforming frequency spectra into wavenumber spectra.
Methods for determining the speed of profiling include, but are not limited to:
# Using the rate-of-change of pressure for a vertical profiler.
# Using the rate-of-change of pressure for a vertical profiler.
# Using the rate-of-change of pressure, the pitch angle, and the angle of attack for a glider.
# Using the rate-of-change of pressure, the pitch angle, and the angle of attack for a glider.
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# Using an onboard current meter.
# Using an onboard current meter.
# Using a constant speed.
# Using a constant speed.
# Using the speed recorded by an independent instrument after such data have been carefully aligned in time with the shear-probe data.
# Using the speed recorded by an independent instrument after its record has been carefully aligned in time with the shear-probe data.

Revision as of 22:31, 14 July 2021

The speed of profiling can be determined with a variety of different methods. It must be determined because it is required for the conversion of the shear-probe samples into physical units and for transforming frequency spectra into wavenumber spectra. Methods for determining the speed of profiling include, but are not limited to:

  1. Using the rate-of-change of pressure for a vertical profiler.
  2. Using the rate-of-change of pressure, the pitch angle, and the angle of attack for a glider.
  3. Using a flight model for a glider.
  4. Using an onboard current meter.
  5. Using a constant speed.
  6. Using the speed recorded by an independent instrument after its record has been carefully aligned in time with the shear-probe data.
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