The entrainment coefficient is the dimensionless constant in the Batchelor entrainment hypothesis, so the mean speed at which ambient fluid crosses a plume edge is α times the plume's characteristic axial speed.
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- Batchelor entrainment hypothesis
- Confined plume with compensating return flow
- Constant-speed entraining gravity current on a slope
- Entrainment velocity
- Forced-plume virtual-origin geometry
- Jet length
- Melting-driven saline wall plume
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- Two-sided top-hat line plume
- Unsteady Boussinesq triangular-profile line-plume balances
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