Transient Lateral Flow
Transient Lateral Flow is a hydrological process denoting the temporary, downslope movement of water within the subsurface soil or regolith layer, driven by transient saturation conditions during and immediately following storm events.
25
Publications
829
Citations
58
Authors
45
Institutions
Publications per year
2017–2026
3
Parents
25
Cristiano Lanni, Marco Borga, Riccardo Rigon et al. · Hydrology and earth system sciences · 2012 · 67 citations · Full text
J. R. McAfee · Planetary and Space Science · 1967 · 63 citations
Steady‐state field‐aligned currents at Mercury
B. J. Anderson, C. L. Johnson, H. Korth et al. · Geophysical Research Letters · 2014 · 63 citations · Full text
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National Oceanic and Atmospheric Administration, United States
2 publications · 78 citations
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1
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Laboratoire de génie des procédés pour la bioraffinerie, les matériaux bio-sourcés et l’impression fonctionnelle
Grenoble, France
2 h-index
4 publications
76 citations
University of Houston
Houston, United States
2 h-index
4 publications
54 citations
University of Pittsburgh
Pittsburgh, United States
2 h-index
3 publications
93 citations
United States Geological Survey
Reston, United States
2 h-index
3 publications
87 citations

University of Trento
Trento, Italy
1 h-index
2 publications
134 citations
University of Tennessee at Knoxville
Knoxville, United States
1 h-index
1 publications
69 citations
Chuo University
Hachiōji, Japan
1 h-index
1 publications
60 citations

Heriot-Watt University
Edinburgh, United Kingdom
1 h-index
2 publications
38 citations
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3 publications · 110 citations
3
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2 publications · 78 citations
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2 publications · 62 citations
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ETFS · 1 publications · 22 citations
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1 publications · 16 citations
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