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- Baroclinity
- Bernoulli's principle
- Blasius boundary layer
- Coriolis acceleration in local Earth coordinates
- Couette flow with a slipping lower wall
- Cylindrical magnetostatic equilibrium
- Darcy law
- Depth independence of hydrostatic shallow-water flow
- Dynamic viscosity
- Effective permeability of complementary wedges
- Flat-plate boundary-layer traverse experiment
- Fluid
- Fluid mechanics
- Friction-induced instability of a collapsible-tube flow
- Fully developed flow
- Hartmann number
- Hydrostatic balance
- Hydrostatic pressure
- Kinematic viscosity
- Momentum thickness
- Oscillatory channel flux of a linear Maxwell fluid
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- Permeability of a porous medium
- Planar Poiseuille flow with equal wall slip
- Pressure compatibility at a no-slip wall
- Reynolds pipe-and-dye experiment
- Shear and pipe flow of an affine linear PTT fluid
- Stokes flow
- Strict geostrophic balance
- Thermodynamic equilibrium
- Two-layer plane Poiseuille flow with unequal viscosities
- Viscous stress tensor
- Vorticity
- Zero-flux Couette-Poiseuille flow
- Z-pinch
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A pressure gradient refers to the rate of change of pressure in a fluid (which can be a liquid or gas) over a specific distance. In simpler terms, it indicates how pressure varies from one point to another within a given space. The pressure gradient is a critical concept in various fields, including meteorology, fluid dynamics, and engineering.