When an open channel contracts into a narrowed flume section, water surface elevation changes depending on whether upstream flow is subcritical or supercritical. For subcritical flow entering a contracted channel bed of reduced width $(b_2 < b_1),$ the specific energy remains constant (neglecting friction losses): $E_1 = y_1 + \frac{v_1^2}{2 \cdot g} = y_2 + \frac{v_2^2}{2 \cdot g} = E_2$ As width decreases, discharge per unit width $(q_2 = Q / b_2)$ increases. The minimum channel width $(b_{min})$ before choking occurs corresponds to flow reaching the critical state $(y_2 = y_c)$ at minimum specific energy $(E_{min}):$ $b_{min} = \sqrt{\frac{Q^2}{g \cdot \left(\frac{2}{3} \cdot E_1\right)^3}}$ If $b_2 < b_{min},$ flow chokes, forcing upstream water level to rise $(y_1 \to y_1')$ to provide the required specific energy to pass discharge $Q.$ Unintended flow choking at canal aqueduct entries causes localized overtopping along major irrigation conveyance networks across Pen...