If angular velocity is independent of height, integrating the viscous stress ρνrΩ′ gives ΣνˉrΩ′. Thus the surface density weighted average, rather than an unweighted height average, enters vertically averaged viscous disk equations.
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- Critical internal-wave reflection
- Darcy thermal-time Rayleigh number
- Ekman layer
- Hartmann number
- Linearized Boussinesq equations
- Magnetohydrodynamic momentum equation
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- Prandtl boundary-layer equation
- Prandtl number
- Square-root-radius diffusion transform
- Surface density of a steady photoevaporating disk
- Surface Ekman layer
- Taylor number
- Torque-dominated accretion disk
- Unbuttressed Newtonian grounding-line stress
- Vertically averaged alpha closure for a mixed-pressure layer
- Viscous attenuation of an internal-wave beam
- Viscous diffusion time
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