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> | ||
| | | 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 \ | | <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 |
---|---|---|---|
[math]\displaystyle{ \epsilon }[/math] | Turbulent kinetic energy dissipation | W/kg | |
[math]\displaystyle{ Ri }[/math] | Richardson number | [math]\displaystyle{ Ri = \frac{N^2}{S^2} }[/math] | |
[math]\displaystyle{ Ri_f }[/math] | Flux gradient Richardson number | [math]\displaystyle{ \frac{B}{P} }[/math] or Ivey & Immerger? | |
[math]\displaystyle{ \kappa }[/math] | Turbulent diffusivity | [math]\displaystyle{ \kappa = \Gamma \epsilon N^{-2} }[/math] | m[math]\displaystyle{ ^2 }[/math]s[math]\displaystyle{ ^{-1} }[/math] |
Fluid properties and background gradients for turbulence calculations
Symbol | Description | Eqn | Units |
---|---|---|---|
[math]\displaystyle{ S }[/math] | Background velocity shear | [math]\displaystyle{ S = \frac{\partial |U|}{\partial z} }[/math] | s[math]\displaystyle{ ^{-1} }[/math] |
[math]\displaystyle{ \nu }[/math] | Viscosity of water for seawater at 35psu and 20 oC | [math]\displaystyle{ 1\times 10^{-6} }[/math] | m2/s |
[math]\displaystyle{ N }[/math] | Background stratification, i.e buoyancy frequency | [math]\displaystyle{ N = \sqrt{\frac{-g}{\bar{\rho}} \frac{\partial\bar{\rho}}{\partial z}} }[/math] | rad/s |
Theoretical Length and Time Scales
Symbol | Description | Eqn | Units |
---|---|---|---|
[math]\displaystyle{ \tau_N }[/math] | Buoyancy timescale | [math]\displaystyle{ \tau_N = \frac{2\pi}{N} }[/math] | s |
[math]\displaystyle{ L_E }[/math] | Ellison length scale (limit of vertical displacement without irreversible mixing) | [math]\displaystyle{ L_E=\frac {\langle \rho'^2\rangle^{1/2}}{\partial \overline{\rho}/\partial z} }[/math] | m |
[math]\displaystyle{ L_\rho }[/math] | Density length scale | [math]\displaystyle{ L_\rho }[/math] | m |
[math]\displaystyle{ L_S }[/math] | Corssin length scale | [math]\displaystyle{ L_S = \sqrt{\epsilon/S^3} }[/math] | m |
[math]\displaystyle{ \eta }[/math] | Kolmogorov length scale (smallest overturns) | [math]\displaystyle{ \eta=\left(\frac{\nu^3}{\epsilon}\right)^{1/4}=\frac{1}{2\pi\hat{k}_K} }[/math] | m |
[math]\displaystyle{ L_o }[/math] | Ozmidov length scale, measure of largest overturns in a stratified fluid | [math]\displaystyle{ L_o=\left(\frac{\epsilon}{N^3}\right)^{1/2} }[/math] | m |
Turbulence Spectrum
Taylor's Frozen Turbulence for converting temporal to spatial measurements [math]\displaystyle{ \left(\bar{u}_1\frac{\partial }{\partial{x}} = \frac{\partial}{\partial{t}}\right) }[/math]
- Missing the y-axi variable. CEB proposes:
- [math]\displaystyle{ \Psi_{variable} }[/math] for model/theoretical spectrum of variable e.g., du/dx or u
- [math]\displaystyle{ \Phi_{variable} }[/math] for observed spectrum of variable e.g., du/dx or u
- Lowest frequency and wavenumber resolvable
Symbol | Description | Eqn | Units |
---|---|---|---|
[math]\displaystyle{ \Delta t }[/math] | Sampling interval | [math]\displaystyle{ \frac{1}{f_s} }[/math] | s |
[math]\displaystyle{ \Delta s }[/math] | Sampling volume dimension | m | |
[math]\displaystyle{ f }[/math] | Frequency | [math]\displaystyle{ \frac{\omega}{2\pi} }[/math] | Hz |
[math]\displaystyle{ f_n }[/math] | Nyquist frequency | [math]\displaystyle{ f_n=0.5f_s }[/math] | Hz |
[math]\displaystyle{ f_s }[/math] | Sampling frequency | [math]\displaystyle{ f_s=\frac{1}{\Delta t} }[/math] | Hz |
[math]\displaystyle{ k }[/math] | Wavenumbers (angular) | [math]\displaystyle{ k=\frac{f}{\bar{u}}=2\pi\hat{k} }[/math] | rad/m |
[math]\displaystyle{ \hat{k} }[/math] | Wavenumbers | [math]\displaystyle{ \hat{k}=\frac{k}{2\pi} }[/math] | cpm |
[math]\displaystyle{ \hat{k}_\Delta }[/math] | Nyquist wavenumber, based on sampling volume's size [math]\displaystyle{ \Delta l }[/math] | [math]\displaystyle{ \hat{k}_\Delta=\frac{0.5}{\Delta l} }[/math] | cpm |
[math]\displaystyle{ \hat{k}_n }[/math] | Nyquist wavenumber, via Taylor's hypothesis (temporal measurements) | [math]\displaystyle{ \hat{k}_n=\frac{f_n}{u} }[/math] | cpm |
[math]\displaystyle{ \omega }[/math] | Angular frequency | [math]\displaystyle{ 2\pi f }[/math] | rad/s |