A "unit hydrograph" (UH) is the hypothetical unit response of a watershed (in terms of runoff volume and timing) to a unit input of rainfall. It can be defined as the "direct runoff hydrograph" (DRH) resulting from one unit (e.g., one cm or one inch) of "effective rainfall" occurring uniformly over that watershed at a uniform rate over a unit period of time. As a UH is applicable only to the direct runoff component of a hydrograph (i.e., surface runoff), a separate determination of the baseflow component is required.