Structural and functional control of surface-patch to hillslope-scale runoff and sediment connectivity in Mediterranean-dry reclaimed slope systems
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Structural and functional control of surface-patch to hillslope-scale runoff and sediment connectivity in Mediterranean-dry reclaimed slope systems ; year:2020 ; pages:1-28
Hydrology and earth system sciences discussions ; (2020), 1-28
- Creator
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Moreno-de-las-Heras, Mariano
Merino-Martín, Luis
Saco, Patricia M.
Espigares, Tíscar
Gallart, Francesc
Nicolau, José M.
- DOI
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10.5194/hess-2019-572
- URN
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urn:nbn:de:101:1-2020011605384860188581
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 11:03 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Moreno-de-las-Heras, Mariano
- Merino-Martín, Luis
- Saco, Patricia M.
- Espigares, Tíscar
- Gallart, Francesc
- Nicolau, José M.
Other Objects (12)
Structural and functional control of surface-patch to hillslope runoff and sediment connectivity in Mediterranean dry reclaimed slope systems
Hydrological heterogeneity in Mediterranean reclaimed slopes: runoff and sediment yield at the patch and slope scales along a gradient of overland flow
Formation of runoff at the hillslope scale during intense precipitation
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Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale
Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale
Assessment of shallow subsurface characterisation with non-invasive geophysical methods at the intermediate hill-slope scale
Structural and functional control of surface-patch to hillslope runoff and sediment connectivity in Mediterranean dry reclaimed slope systems
Hydrological heterogeneity in Mediterranean reclaimed slopes: runoff and sediment yield at the patch and slope scales along a gradient of overland flow
Formation of runoff at the hillslope scale during intense precipitation
Reclaimed
Vectors of subsurface stormflow in a layered hillslope during runoff initiation
Slope–velocity equilibrium and evolution of surface roughness on a stony hillslope
Radically speaking : feminism reclaimed
Toward a Reclaimed Tarot
Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale
Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale
Assessment of shallow subsurface characterisation with non-invasive geophysical methods at the intermediate hill-slope scale
Structural and functional control of surface-patch to hillslope runoff and sediment connectivity in Mediterranean dry reclaimed slope systems
Hydrological heterogeneity in Mediterranean reclaimed slopes: runoff and sediment yield at the patch and slope scales along a gradient of overland flow
Formation of runoff at the hillslope scale during intense precipitation
Reclaimed
Vectors of subsurface stormflow in a layered hillslope during runoff initiation
Slope–velocity equilibrium and evolution of surface roughness on a stony hillslope
Radically speaking : feminism reclaimed
Toward a Reclaimed Tarot
Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale
Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
Stable water isotope tracing through hydrological models for disentangling runoff generation processes at the hillslope scale