For a flow invariant in one horizontal direction, the volume flux per unit width is the velocity integrated across the flow depth. It has dimensions of area per unit time.
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- Benney equation
- Dupuit approximation
- Exner equation
- Forced filling similarity for power-law diffusion
- Gravity-driven ice flow on a conical slope
- Gravity film on an upward-moving wall
- Inclined porous gravity current
- Inverted falling film
- Line-source upstream reach under imposed shear
- Newtonian grounding-line flux
- Outlet layer in a deep unconfined aquifer
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- Sliding-plate flow through a parabolic gap
- Slowly opening Stokes wedge
- Square-root drainage boundary
- Steady friction-dominated grounding-line thickness relation
- Stream function
- Uniform gravity-driven Newtonian film
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