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In reality, channel slopes and cross-sections change, causing the water depth to vary gradually over long distances. The book excels at explaining the dynamic equation of GVF and classifying water surface profiles (M-curves, S-curves, C-curves, A-curves, and H-curves). Engineers use these profiles to predict how backwater from a dam or weir will affect upstream lands. E. Rapidly Varied Flow (RVF) and the Hydraulic Jump This article explores the key aspects of Das's

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