Mountain Runoff Generation
Mountain Runoff Generation is a hydrological process denoting the production of surface and subsurface flow in mountainous terrain through the transformation of precipitation and meltwater into runoff, distinguished by the dominant influence of elevation-driven climate gradients, steep topography, and seasonal snow and ice dynamics.
53
Publications
2.6K
Citations
226
Authors
95
Institutions
Publications per year
2017–2026
20
Parents
53
Seasonal changes in runoff generation in a small forested mountain catchment
Daniele Penna, Ilja van Meerveld, Omar Oliviero et al. · Hydrological Processes · 2014 · 143 citations · Full text
1–5 of 53
226
3
h-index
3
h-index
2
h-index
2
h-index
2
h-index
1–5 of 226
95

Chinese Academy of Sciences
Beijing, China
9 h-index
49 publications
2.2K citations
Northwest Institute of Eco-Environment and Resources
Lanzhou, China
6 h-index
35 publications
1.5K citations
Northwest Normal University
Lanzhou, China
4 h-index
34 publications
980 citations
Norsk Hydro (Germany)
Grevenbroich, Germany
3 h-index
7 publications
376 citations
University of Zurich
Zurich, Switzerland
3 h-index
5 publications
243 citations

University of Freiburg
Freiburg im Breisgau, Germany
3 h-index
5 publications
250 citations
École Polytechnique Fédérale de Lausanne
Lausanne, Switzerland
2 h-index
5 publications
650 citations
University of California, Berkeley
Berkeley, United States
2 h-index
5 publications
578 citations
1–8 of 95
10 publications · 571 citations
9
h-index
8 publications · 608 citations
8
h-index
3 publications · 139 citations
3
h-index
3 publications · 106 citations
3
h-index
3 publications · 73 citations
3
h-index
1–5