Potential of Sentinel-3 snow cover fraction data for improving hydrological simulations at the regional scale. [PDF]
Tanhapour M +7 more
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The impact of land use land cover (LULC) change and climate variability on infiltration/runoff evolution in the Dar Es Salaam coastal floodplain. [PDF]
De Filippi FM +7 more
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Linking moss structural and functional traits to soil water fluxes and soil erosion. [PDF]
Gall C +6 more
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Latitudinal divergence in runoff responses to global forestation due to forest-atmosphere feedbacks. [PDF]
Kan F +8 more
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The contribution rate of stem-leaf and root of alfalfa (<i>Medicago sativa L.</i>) with diverse spatial distribution patterns to sediment and runoff reduction on the Loess Plateau. [PDF]
Yao C +7 more
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Potential Release of Micro- and Nanoplastics from Stormwater Infrastructure. [PDF]
Doti B, Gray A, Strom K, Foroutan H.
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Applications of a surface runoff model with horton and dunne runoff for VIC
Advances in Atmospheric Sciences, 2003Surface runoff is mainly generated by two mechanisms, infiltration excess (Horton) runoff and saturation excess (Dunne) runoff; and the spatial variability of soil properties, antecedent soil moisture, topography, and rainfall will result in different surface runoff generation mechanisms.
Zhenghui Xie +2 more
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In most climates, soil erosion is governed by the surface runoff of water during excessive rainfalls. Thus, numerical models for the simulation of surface runoff provide a key to quantitative modeling of soil erosion.
St. Hergarten, G. Paul, H. J. Neugebauer
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Surface‐runoff and infiltration
Eos, Transactions American Geophysical Union, 1945The terms, “surface runoff” and “infiltration,” which form the title of this paper, are usually associated with a piece of land and the precipitation falling upon it. They suggest that this ground is porous, that part of the water will infiltrate into it while the rest runs off along the surface or evaporates.
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