Wavenumber response of the shear probe: Difference between revisions

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The probe-response correction depends on the dimensions of the shear probe. For a commonly used shear probe the spectrum is corrected for the spatial averaging of the shear probe by multiplying it by the factor correction <math>1+\left( \frac{k}{k_0} \right)^2</math> where <math>k_0</math> = 50 cpm and <math>k</math> is the wavenumber expressed in units of cpm (Macoun and Lueck, 2004). The correction reaches a factor of 10 at a wavenumber of 150 cpm, and it is not recommended to use spectral data beyond this wavenumber unless the probe is small and <math>k_0</math> is larger than 50 cpm.
The probe-response correction depends on the dimensions of the shear probe. For a commonly used shear probe the spectrum is corrected for the spatial averaging of the shear probe by multiplying it by the factor correction <math>1+\left( \frac{k}{k_0} \right)^2</math> where <math>k_0</math> = 50 cpm and <math>k</math> is the wavenumber expressed in units of cpm <ref>Macoun, P., & Lueck, R. (2004). Modeling the spatial response of the airfoil shear probe using different sized probes. Journal of Atmospheric and Oceanic Technology, 21(2), 284-297.</ref>. The correction reaches a factor of 10 at a wavenumber of 150 cpm, and it is not recommended to use spectral data beyond this wavenumber unless the probe is small and <math>k_0</math> is larger than 50 cpm.
 
==References==
<references />

Revision as of 16:08, 5 October 2021

The probe-response correction depends on the dimensions of the shear probe. For a commonly used shear probe the spectrum is corrected for the spatial averaging of the shear probe by multiplying it by the factor correction 1+(kk0)2 where k0 = 50 cpm and k is the wavenumber expressed in units of cpm [1]. The correction reaches a factor of 10 at a wavenumber of 150 cpm, and it is not recommended to use spectral data beyond this wavenumber unless the probe is small and k0 is larger than 50 cpm.

References

  1. Macoun, P., & Lueck, R. (2004). Modeling the spatial response of the airfoil shear probe using different sized probes. Journal of Atmospheric and Oceanic Technology, 21(2), 284-297.