Discharge (hydrology)

This article needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Find sources: "Discharge" hydrology – news · newspapers · books · scholar · JSTOR (December 2023) (Learn how and when to remove this message)

In hydrology, discharge is the volumetric flow rate (volume per time, in units of m³/h or ft³/h) of a stream. It equals the product of average flow velocity (with dimension of length per time, in m/h or ft/h) and the cross-sectional area (in m² or ft²).^[1] It includes any suspended solids (e.g. sediment), dissolved chemicals like CaCO
₃(aq), or biologic material (e.g. diatoms) in addition to the water itself. Terms may vary between disciplines. For example, a fluvial hydrologist studying natural river systems may define discharge as streamflow, whereas an engineer operating a reservoir system may equate it with outflow, contrasted with inflow.