Hortonian Runoff
Hortonian Runoff is a type of surface runoff process in hydrology whereby overland flow is generated when rainfall intensity exceeds the infiltration capacity of the soil, leading to the accumulation and downslope movement of water on the land surface.
56
Publications
3.3K
Citations
153
Authors
91
Institutions
Publications per year
2017–2026
6
Variants
Infiltration-excess Overland Flow
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Laboratoire d'étude des Interactions Sol - Agrosystème - Hydrosystème, France
3 publications · 294 citations
3
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3
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1–5 of 153
91

Cornell University
Ithaca, United States
5 h-index
16 publications
725 citations
Institut de Recherche pour le Développement
Marseille, France
4 h-index
13 publications
509 citations
KU Leuven
Leuven, Belgium
3 h-index
6 publications
265 citations
Desert Research Institute
Reno, United States
3 h-index
3 publications
113 citations

Delft University of Technology
Delft, The Netherlands
2 h-index
2 publications
79 citations
Lancaster University
Lancaster, United Kingdom
2 h-index
2 publications
76 citations

Institut Agro Montpellier
Montpellier, France
2 h-index
5 publications
729 citations
Laboratoire d'étude des Interactions Sol - Agrosystème - Hydrosystème
Montpellier, France
2 h-index
5 publications
213 citations
1–8 of 91
15 publications · 1.1K citations
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6 publications · 359 citations
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6 publications · 545 citations
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5 publications · 182 citations
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3 publications · 167 citations
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