Fluid statics and pressure head
For still water of constant density, gauge pressure increases with vertical depth below its free surface. Pressure head is pressure/unit weight, measured in length units. Elevation head instead measures height above a chosen datum.
Check yourself: Does your depth measure a vertical distance below the free surface?
Continuity and mean velocity
Discharge Q equals flow area A times cross-sectional mean velocity V. Steady incompressible flow without lateral inflow or storage change conserves discharge between sections. A smaller area then means larger mean velocity, not water loss.
Check yourself: Have you used the wetted flow area rather than the channel's empty cross-section?
Open-channel geometry
Hydraulic depth D is flow area/free-surface top width T. Hydraulic radius is area/wetted perimeter. For rectangular channels, hydraulic depth equals water depth; wetted perimeter includes the bottom and submerged sidewalls but excludes the free surface.
Check yourself: Does the equation require area/top width or area/wetted perimeter?
Froude number and flow regime
In the one-dimensional shallow-water model, Fr = V/√(gD) compares mean velocity with gravity-wave speed. Below one means subcritical; above one means supercritical. Froude number does not classify turbulence, which involves Reynolds number instead.
Check yourself: Is the gravity term inside the square root, with D measured in metres?
Hydrology and rainfall volume
Uniform rainfall depth times catchment area gives rainfall volume. A supplied event runoff fraction converts this to runoff volume in a simplified model. Peak discharge requires additional information about timing and storage.
Check yourself: Are you calculating an event volume, a time-averaged rate, or a peak rate?