Runoff is the water that is pulled by gravity across land’s surface, replenishing groundwater and surface water as it percolates into an aquifer or moves into a river, stream or watershed. It comes from unabsorbed water from rain, snowmelt, irrigation or other sources, comprising a significant element of the water cycle as well as the water supply when it drains into a watershed. Runoff is also a major contributor to the erosion which carves out canyons, gorges and related landforms.
The type, intensity and distribution of precipitation affects runoff, as does the slope, vegetation and topography of the land over which it travels.
Urbanization has changed the dynamics of runoff by impacting the land itself. Infrastructure reduces the amount of permeable land into which water can absorb, causing more stormwater to pass over the surface, necessitating drainage systems to prevent flooding. The connection between wildfires and subsequent flooding has been attributed to the increased runoff which is unable to absorb into the scorched earth. Additionally, more pollutants like pesticides can be introduced as runoff flows over contaminated areas.
Runoff is a combination of surface runoff, interflow and baseflow.
Surface runoff comes from overland flow and saturation excess overland flow. Overland flow is from urban sources like roofs or pavement, while saturation excess overland flow is from precipitation or melted snow which could simply not be absorbed into the ground. Surface runoff – from both of these sources – is driven downhill by gravity.
Interflow usually comes about after a large amount of precipitation. It travels horizontally below the surface but above the water table, in an area called the “zone of aeration” or “vadose zone,”
Baseflow (aka Groundwater Runoff)
Baseflow is the direct seepage from groundwater into surface water, which can bring whatever chemicals the groundwater has collected for more than thousands of years moving beneath the earth’s surface.