Velocity inertial subrange model: Difference between revisions

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{{DefineConcept
{{DefineConcept
|description=The inertial subrange separates the energy-containing production range from the viscous dissipation range.
|description=The inertial subrange separates the energy-containing production range from the viscous dissipation range.
|article_type=Concept
|article_type=Fundamentals
|instrument_type=Velocity point-measurements, Velocity profilers
|instrument_type=Velocity point-measurements, Velocity profilers
}}
}}
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== Inertial subrange for flows influenced by surface waves ==
== Inertial subrange for flows influenced by surface waves ==
Need to add equations and figures from Lumley & Terray
Need to add equations and figures from Lumley & Terray
== Notes ==
<references />

Revision as of 19:12, 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 may be discussed within the wiki.



Inertial subrange for steady-flows

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

ΨVj(k^)=ajCkε2/3k^5/3

Here k^ is expressed in rad/m and Vj represents the velocities V in direction j. Ck is the empirical Kolmogorov universal constant of C = 1.5 (see Sreenivasan 1995 for a review on the universality of this constant). Amongst the three direction, the spectra deviates by the constant aj:

  • In the longitudinal direction, i.e., the direction of mean advection (j=1), a1=1855
  • In the other directions a2=a3=43a1

Inertial subrange for flows influenced by surface waves

Need to add equations and figures from Lumley & Terray

Notes