For a fixed half-angle , a slow slender gravity current in a V-shaped channel has an almost horizontal free surface across each section. Its area is , and its axial volume flux is . Here is the integral of the dimensionless cross-sectional Poisson equation solution: , with zero velocity on the two rigid slopes and zero normal velocity derivative on the horizontal shear-free surface. Conservation of mass gives . This treats the full two-dimensional section and does not require a shallow V angle.
For a shallow V-channel with floor , , let the free surface be . Hydrostatic pressure gives . A vertical strip has thickness and, with no slip below and zero shear above, flux . Integrating across gives
Conservation of volume is , . Here is the wall slope to the horizontal, not the opening half-angle measured from the vertical in a general V-section. Vertical shear dominates transverse shear by the shallow-slope approximation.
The variable converts the shallow V-channel lubrication flux equation into a porous medium equation:
Indeed . Its fixed-mass source-type solution gives and support length proportional to . Integrating the similarity equation once gives , and hence . The constant-volume similarity in a V-shaped channel fixes from the positive integral : .
The symmetric similarity solution for a localized fixed volume in a V-shaped channel gravity current has . Integrating the similarity conservation of mass equation once gives , and vanishing thickness at the two noses gives the profile. Its volume fixes , where . At any fixed nonzero position, the thickness first rises after arrival and then falls; its maximum occurs when .

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