Nomenclature: Difference between revisions

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|
|
| W/kg
| W/kg
|-
| <math>Ri</math>
| Richardson number
| <math> Ri = \frac{N^2}{S^2}</math>
|
|-
| <math>Ri_f</math>
| Flux gradient Richardson number
| <math> \frac{B}{P} </math> or Ivey & Immerger?
|
|-
| <math>\kappa</math>
| Turbulent diffusivity
| <math> \kappa = \Gamma \epsilon N^{-2} </math>
| m<math>^2</math>s<math>^{-1}</math>
|}
== Fluid properties and background gradients for turbulence calculations ==
{| class="wikitable"
|- Style="font-weight:bold; "
! Symbol
! Description
! Eqn
! Units
|-
| <math>S</math>
| Background velocity shear
| <math> S = \frac{\partial |U|}{\partial z}</math>
| s<math>^{-1}</math>
|-
|-
| <math>\nu</math>
| <math>\nu</math>
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|-
|-
| <math>N</math>
| <math>N</math>
| Buoyancy frequency
| Background stratification, i.e buoyancy frequency
| <math> N = \sqrt{\frac{-g}{\bar{\rho}} \frac{\partial\bar{\rho}}{\partial z}}</math>
| <math> N = \sqrt{\frac{-g}{\bar{\rho}} \frac{\partial\bar{\rho}}{\partial z}}</math>
| rad/s
| rad/s
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| <math>L_E</math>
| <math>L_E</math>
| Ellison length scale (limit of vertical displacement without irreversible mixing)
| Ellison length scale (limit of vertical displacement without irreversible mixing)
| <math>L_E=\frac {\langle \rho'^2\rangle^{1/2}}{\partial \overbar{\rho}/\partial z}</math>
| <math>L_E=\frac {\langle \rho'^2\rangle^{1/2}}{\partial \overline{\rho}/\partial z}</math>
| m  
| m  
|-
|-

Revision as of 14:11, 31 March 2021

Frame of reference

  • Define frame of reference, and notation. Use u,v,w and x,y, and z?
  • Dumping a sketch would be useful


Reynold's Decomposition

  • Variable names for Decomposition of total, mean, turbulent and waves.


Turbulence properties

Symbol Description Eqn Units
ϵ Turbulent kinetic energy dissipation W/kg
Ri Richardson number Ri=N2S2
Rif Flux gradient Richardson number BP or Ivey & Immerger?
κ Turbulent diffusivity κ=ΓϵN2 m 2s 1

Fluid properties and background gradients for turbulence calculations

Symbol Description Eqn Units
S Background velocity shear S=|U|z s 1
ν Viscosity of water for seawater at 35psu and 20 oC 1×106 m2/s
N Background stratification, i.e buoyancy frequency N=gρ¯ρ¯z rad/s

Theoretical Length and Time Scales

Symbol Description Eqn Units
τN Buoyancy timescale τN=2πN s
LE Ellison length scale (limit of vertical displacement without irreversible mixing) LE=ρ'21/2ρ/z m
Lρ Density length scale Lρ m
LS Corssin length scale LS=ϵ/S3 m
η Kolmogorov length scale (smallest overturns) η=(ν3ϵ)1/4=12πk^K m
Lo Ozmidov length scale, measure of largest overturns in a stratified fluid Lo=(ϵN3)1/2 m

Turbulence Spectrum

Taylor's Frozen Turbulence for converting temporal to spatial measurements (u¯1x=t)


  • Missing the y-axi variable. CEB proposes:
    • Ψvariable for model/theoretical spectrum of variable e.g., du/dx or u
    • Φvariable for observed spectrum of variable e.g., du/dx or u
  • Lowest frequency and wavenumber resolvable
Symbol Description Eqn Units
Δt Sampling interval 1fs s
Δs Sampling volume dimension m
f Frequency ω2π Hz
fn Nyquist frequency fn=0.5fs Hz
fs Sampling frequency fs=1Δt Hz
k Wavenumbers (angular) k=fu¯=2πk^ rad/m
k^ Wavenumbers k^=k2π cpm
k^Δ Nyquist wavenumber, based on sampling volume's size Δl k^Δ=0.5Δl cpm
k^n Nyquist wavenumber, via Taylor's hypothesis (temporal measurements) k^n=fnu cpm
ω Angular frequency 2πf rad/s

Test