Velocity inertial subrange model: Difference between revisions

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|paper_or_booktitle=Kinematics of turbulence convected by a random wave field
|paper_or_booktitle=Kinematics of turbulence convected by a random wave field
|year=1983
|year=1983
|doi= 10.1175/1520-0485(1983)013\l2000:KOTCBA\g2.0.CO;2
|doi= 10.1175/1520-0485(1983)013{\l}2000:KOTCBA{\g}2.0.CO;2
}}
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Revision as of 20:07, 11 November 2021


Short definition of Velocity inertial subrange model
The inertial subrange separates the energy-containing production range from the viscous dissipation range.

This is the common definition for Velocity inertial subrange model, but other definitions maybe discussed within the wiki.

{{#default_form:DefineConcept}} {{#arraymap:Velocity point-measurements, Velocity profilers|,|x||}}

Inertial subrange for steady-flows

This theoretical model predicts the spectral shape of velocities in wavenumber space.

<math>\Psi_{Vj}(\hat{k})=a_jC_k\varepsilon^{2/3}\hat{k}^{-5/3}</math>

Here <math>\hat{k}</math> is expressed in rad/m and <math>Vj</math> represents the velocities <math>V</math> in direction <math>j</math>. <math>C_k</math> is the empirical Kolmogorov universal constant of C = 1.5 [1]. Amongst the three direction, the spectra deviates by the constant <math>a_j</math>: [2]

  • In the longitudinal direction, i.e., the direction of mean advection (j=1), <math>a_1=\frac{18}{55}</math>
  • In the other directions <math>a_2=a_3=\frac{4}{3}a_1</math>

Inertial subrange for flows influenced by surface waves

Need to add equations and figures from Lumley & Terray[3]

Notes

  1. {{#arraymap:K. R. Sreenivasan|,|x|x|, |and}}. 1995. On the universality of the Kolmogorov constant. Phys. Fluids. doi:10.1063/1.868656
  2. {{#arraymap:S.B Pope|,|x|x|, |and}}. 2000. Turbulent flows. Cambridge Univ. Press. doi:10.1017/CBO9780511840531
  3. {{#arraymap:J. Lumley and E. Terray|,|x|x|, |and}}. 1983. Kinematics of turbulence convected by a random wave field. J. Phys. Oceanogr. doi:10.1175/1520-0485(1983)013{\l}2000:KOTCBA{\g}2.0.CO;2