Dimensionless Numbers: Difference between revisions

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<div id="Rossby Number"></div>
<div id="Rossby Number"></div>
;'''Rossby Number'''  
;'''Rossby Number'''  
* Definition: <math> Ro = \frac{U}{fL} </math>, where <math> U </math> is the characteristic velocity, and <math> f </math> is the Coriolis frequency, and <math> L </math> is the characteristic length scale.  
* Definition: <math> Ro = \frac{U}{fL} </math>, where <math> U </math> is the characteristic velocity, and <math> f </math> is the [[Glossary#Coriolis Frequency|Coriolis frequency]], and <math> L </math> is the characteristic length scale.  
* Interpretation: The ratio of the advective forces to the Coriolis pseudo-forces.
* Interpretation: The ratio of the advective forces to the Coriolis pseudo-forces.
* Analysis: When <math>Ro\ll 1</math>, Coriolis effects dominate and the system approaches [[Glossary#Geostrophic Balance|geostrophic balance]].  
* Analysis: When <math>Ro\ll 1</math>, Coriolis effects dominate and the system approaches [[Glossary#Geostrophic Balance|geostrophic balance]].  

Revision as of 11:30, 28 May 2015

Mach Number
  • Definition: , where is the characteristic velocity scale, and is the speed of sound.
  • Interpretation: The ratio of inertia force to compressibility force.
  • Analysis: Compressibility effects can be neglected if .
Prandtl Number
  • Definition: , where is the viscosity, and is the thermal diffusivity.
  • Interpretation: The ratio of momentum diffusivity (i.e. viscosity) to heat diffusivity.
  • Analysis: The typical Prandtl number for water is around 7 for water (At 20 degrees Celsius). See also Schmidt number.
Reynolds Number
  • Definition: , where and are the characteristic velocity and length scales, and is the dynamic viscosity.
  • Interpretation: The ratio of inertia force to viscous force.
  • Analysis: Small Reynolds numbers are often associated with viscous flows, whereas large Reynolds numbers are typically found in turbulent flows.
Richardson Number
  • Definition: , where is the buoyancy frequency, and is the background horizontal velocity.
  • Interpretation: The ratio between the strength of stratification and velocity shear. Also called the gradient Richardson number.
  • Analysis: A sufficient condition for the flow to be linearly stable is that the local Richardson number exceed 0.25 throughout the flow. However, does not mean the flow is necessarily unstable (the criterion is not sufficient). When the flow is not a parallel shear flow, the meaning of is not clear.
Rossby Number
  • Definition: , where is the characteristic velocity, and is the Coriolis frequency, and is the characteristic length scale.
  • Interpretation: The ratio of the advective forces to the Coriolis pseudo-forces.
  • Analysis: When , Coriolis effects dominate and the system approaches geostrophic balance.
Schmidt Number
  • Definition: , where is the viscosity, and is the mass diffusivity.
  • Interpretation: The ratio of momentum diffusivity (i.e. viscosity) to mass diffusivity.
  • Analysis: The typical Schmidt number for water is around 500, depending on the temperature and salinity. For direct numerical simulations, is commonly used in the literature. See also Prandtl number.