Synonyms
Effective snowmelt generation; Excess precipitation generation; Glacial melt runoff generation; Infiltration excess generation; Overland flow generation; Saturation excess generation; Surface runoff generation
Definition
Runoff. It is a major component of the hydrologic cycle and is generated when water from precipitation or snow and glacial melt flows over the land. It is often referred to as the surface runoff. It is the water that is not absorbed by the soil.
Introduction
Runoff is the portion of precipitation or snow and glacial melt that flows across the landscape until it reaches streams, rivers, and, ultimately, oceans. Surface runoff generation depends on rainfall or snowmelt characteristics (amount, duration, intensity, and time distribution) and landscape characteristics (vegetation, land use, topography, soil texture and structure, and antecedent soil moisture conditions).
Conditions of runoff generation
Runoff during non- or partially frozen ground conditions...
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Bibliography
Betson, R. P., 1964. What is watershed runoff? Journal of Geophysical Research, 69(8), 1541–1552.
Beven, K. J., 2001. Rainfall-runoff modelling: the primer. New York, NY: J. Wiley & Sons.
Dunne, T., and Black, R. D., 1970. Partial area contributions to storm runoff in a small New England watershed. Water Resources Research, 6(5), 1296–1311.
Hewlett, J. D., and Hibbert, A. R., 1967. Factors affecting the response of small watersheds to precipitation in humid areas. In: International Symposium on Forest Hydrological Processes. Pergamon, New York, NY, pp. 275–290.
Horton, R. E., 1933. The role of infiltration in the hydrologic cycle. Transactions of the Americal Geophysical Union, 14, 446–460.
Jansson, P., Hock, R., and Schneider, T., 2003. The concept of glacier storage: a review. Journal of Hydrology, 282, 116–129.
Kuchment, L. S., Gelfan, A. N., and Demidov, V. N., 2000. A distributed model of runoff generation in the permafrost regions. Journal of Hydrology, 240, 1–22.
Singh, P., and Singh, V. P., 2001. Snow and Glacier Hydrology. Dordrecht, The Netherlands: Kluwer Academic.
Sokolov, B. L., 1975. Naleds and River Runoff. Leningrad, Russian: Hydrometeorological Publication.
Tindall, J. A., and Kunkel, J. R., 1999. Unsaturated Zone Hydrology for Scientists and Engineers, Chapter 11. New Jersey, USA: Prentice Hall.
Woo, M-K., 1990. Permafrost hydrology. In: Prowse, T. D., Ommanney, C. S. L. (Eds.), Northern Hydrology: Canadian Perspectives, NHRI Science Rep. No. 1. National Hydrology Research Institute, Environment Canada, Saskatoon, Saskatchewan, pp. 63–76.
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Thompson, A.M., Misra, D., Daanen, R.P. (2011). Runoff Generation. In: Singh, V.P., Singh, P., Haritashya, U.K. (eds) Encyclopedia of Snow, Ice and Glaciers. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2642-2_457
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DOI: https://doi.org/10.1007/978-90-481-2642-2_457
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