Definition
Run-off, also referred to as runoff or surface runoff, is the term used to refer to that part of precipitation in the water cycle that moves on the ground surface downslope or downstream away from the location where it first accumulated as rain or snow. Surface water run-off is part of the water cycle that also includes evaporation, infiltration, and storage (USGS 2016). Run-off is estimated from rainfall based on an empirical approach that is known as the rational method (Goyen et al. 2014)
where q is the peak unit discharge in m3/s from a drainage basin at a point of interest, C is a dimensionless coefficient that represents the amount of run-off as a decimal fraction of precipitation, A is the drainage basin area in m2 above the point of interest, and pis representative rainfall intensity in mm/hr for a meaningful duration and a desired return period. The duration for the rainfall intensity may be the time of concentration (the time required for...
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References
Goyen A, Phillips BC, Pathiraja S (2014) Project 13: urban rational method review. Australian rainfall & runoff report P13/S3/001, Engineers Australia. http://www.arr.org.au/wp-content/uploads/2013/Projects/ARR_Project_13_Stage3_report_DRAFT.pdf. Accessed May 2016
USGS (2016) The water cycle. U.S. Geological Survey webpage. http://water.usgs.gov/edu/watercycle.html. Accessed May 2016
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Keaton, J.R. (2018). Run-Off. In: Bobrowsky, P.T., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-73568-9_247
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