Reljeefi profiilikõverus kontrollib sademevee äravoolu kiirust ja ainete edasikannet. Vee äravoolu suunas kumeratel reljeefivormidel on profiilikõverus positiivne ja vool kiirenev; nõgusatel nõlvadel on profiilikõverus negatiivne javool aeglustuv.
Two optional output curvature types are possible: the profile curvature is in the direction of the maximum slope, and the plan curvature is perpendicular to the direction of the maximum slope.
Slope curvature amplifies penetration intensity and flow-path diversity until a threshold (δ ≈ 2–4), beyond which pool-riffle geometry becomes the dominant control.
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