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\ | |doi= 10.1175/1520-0485(1983)013{\l}2000:KOTCBA{\g}2.0.CO;2 | ||
}} | }} | ||
</ref> | </ref> | ||
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.
Here is expressed in rad/m and represents the velocities in direction . is the empirical Kolmogorov universal constant of C = 1.5 [1]. Amongst the three direction, the spectra deviates by the constant : [2]
- In the longitudinal direction, i.e., the direction of mean advection (j=1),
- In the other directions
Inertial subrange for flows influenced by surface waves
Need to add equations and figures from Lumley & Terray[3]
Notes
- ↑ {{#arraymap:K. R. Sreenivasan|,|x|x|, |and}}. 1995. On the universality of the Kolmogorov constant. Phys. Fluids. doi:10.1063/1.868656
- ↑ {{#arraymap:S.B Pope|,|x|x|, |and}}. 2000. Turbulent flows. Cambridge Univ. Press. doi:10.1017/CBO9780511840531
- ↑ {{#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

