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Runoff Generation

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Encyclopedia of Snow, Ice and Glaciers

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

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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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Correspondence to Anita M. Thompson .

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© 2011 Springer Science+Business Media B.V.

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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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