Rate at which water is removed by flowing over the soil surface. This rate is determined by the texture of the soil, slope, climate, and land use cover (e.g. paved surface, grass, forest, bare soil). (Source: LANDY)



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van Langenhove G, de Bruine B, Rukira L, Hatutale A 1996. Flow régime changes in Namibian rivers: patterns, effects and possible causes.
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Flow regime changes in Namibian rivers.pdf 4.39 MB
Hughes DA, Andersson L, Wilk J, Savenije HHG 2006. Regional calibration of the Pitman model for the Okavango River. Journal of Hydrology 331 (1-2) 30-42
Symeonakis E, Drake N 2004. Monitoring deserti?cation and land degradation over sub-Saharan Africa. International Journal of Remote Sensing 25 (3) 573-592
van Rensburg HJ 1971. Range Management in Botswana. Botswana Notes and Records 3 112-130
Hernandez M, Miller SN, Goodrich DC, Kepner WG, Edmonds CM, Jones KB 2000. Modeling runoff response to land cover and rainfall spatial variability in semi-arid watersheds. Environmental Monitoring and Assessment 64 285-298
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modellingrunoff.pdf 174.68 KB