Articles | Volume 16, issue 5
https://doi.org/10.5194/hess-16-1305-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-16-1305-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
08 May 2012
Research article |
| 08 May 2012
Hydrological heterogeneity in Mediterranean reclaimed slopes: runoff and sediment yield at the patch and slope scales along a gradient of overland flow
L. Merino-Martín
Departamento de Ecología, Universidad de Alcalá, Alcalá de Henares, 28871 Madrid, España
M. Moreno-de las Heras
Departamento de Ecología, Universidad de Alcalá, Alcalá de Henares, 28871 Madrid, España
Faculty of Engineering and Built Environment, University of Newcastle, Callaghan, NSW 2308, Australia
S. Pérez-Domingo
Departamento de Ecología, Universidad de Alcalá, Alcalá de Henares, 28871 Madrid, España
T. Espigares
Departamento de Ecología, Universidad de Alcalá, Alcalá de Henares, 28871 Madrid, España
J. M. Nicolau
Departamento de Agricultura y Economía agraria, Escuela Politécnica Superior, Universidad de Zaragoza, Huesca, España
Related subject area
Subject: Hillslope hydrology | Techniques and Approaches: Theory development
Morphological controls on surface runoff: an interpretation of steady-state energy patterns, maximum power states and dissipation regimes within a thermodynamic framework
Soil moisture: variable in space but redundant in time
A history of the concept of time of concentration
Are dissolved organic carbon concentrations in riparian groundwater linked to hydrological pathways in the boreal forest?
The influence of diurnal snowmelt and transpiration on hillslope throughflow and stream response
Slope–velocity equilibrium and evolution of surface roughness on a stony hillslope
Assessment of land use impact on hydraulic threshold conditions for gully head cut initiation
Technical note: Inference in hydrology from entropy balance considerations
Ecohydrological effects of stream–aquifer water interaction: a case study of the Heihe River basin, northwestern China
Hillslope-scale experiment demonstrates the role of convergence during two-step saturation
Impacts of climate variability on wetland salinization in the North American prairies
Resolving structural errors in a spatially distributed hydrologic model using ensemble Kalman filter state updates
Runoff formation from experimental plot, field, to small catchment scales in agricultural North Huaihe River Plain, China
Addressing secondary school students' everyday ideas about freshwater springs in order to develop an instructional tool to promote conceptual reconstruction
Effect of hydraulic parameters on sediment transport capacity in overland flow over erodible beds
Large-scale runoff generation – parsimonious parameterisation using high-resolution topography
Estimating surface fluxes over middle and upper streams of the Heihe River Basin with ASTER imagery
Seasonal evaluation of the land surface scheme HTESSEL against remote sensing derived energy fluxes of the Transdanubian region in Hungary
Analysis of surface soil moisture patterns in agricultural landscapes using Empirical Orthogonal Functions
Modelling field scale water partitioning using on-site observations in sub-Saharan rainfed agriculture
Evaluation of alternative formulae for calculation of surface temperature in snowmelt models using frequency analysis of temperature observations
Growth of a high-elevation large inland lake, associated with climate change and permafrost degradation in Tibet
Selection of an appropriately simple storm runoff model
Spatial mapping of leaf area index using hyperspectral remote sensing for hydrological applications with a particular focus on canopy interception
Use of satellite-derived data for characterization of snow cover and simulation of snowmelt runoff through a distributed physically based model of runoff generation
A contribution to understanding the turbidity behaviour in an Amazon floodplain
Global spatial optimization with hydrological systems simulation: application to land-use allocation and peak runoff minimization
Implementing small scale processes at the soil-plant interface – the role of root architectures for calculating root water uptake profiles
Uncertainty in the determination of soil hydraulic parameters and its influence on the performance of two hydrological models of different complexity
Modelling the inorganic nitrogen behaviour in a small Mediterranean forested catchment, Fuirosos (Catalonia)
Soil bioengineering for risk mitigation and environmental restoration in a humid tropical area
Climate and terrain factors explaining streamflow response and recession in Australian catchments
Soil moisture active and passive microwave products: intercomparison and evaluation over a Sahelian site
Characteristics of 2-D convective structures in Catalonia (NE Spain): an analysis using radar data and GIS
The contribution of groundwater discharge to the overall water budget of two typical Boreal lakes in Alberta/Canada estimated from a radon mass balance
Actual daily evapotranspiration estimated from MERIS and AATSR data over the Chinese Loess Plateau
Calibration analysis for water storage variability of the global hydrological model WGHM
Earth's Critical Zone and hydropedology: concepts, characteristics, and advances
Reducing scale dependence in TOPMODEL using a dimensionless topographic index
Spatial variation in soil active-layer geochemistry across hydrologic margins in polar desert ecosystems
Nitrogen retention in natural Mediterranean wetland-streams affected by agricultural runoff
Recent trends in groundwater levels in a highly seasonal hydrological system: the Ganges-Brahmaputra-Meghna Delta
Water availability, demand and reliability of in situ water harvesting in smallholder rain-fed agriculture in the Thukela River Basin, South Africa
Variability of the groundwater sulfate concentration in fractured rock slopes: a tool to identify active unstable areas
Copula based multisite model for daily precipitation simulation
Solid phase evolution in the Biosphere 2 hillslope experiment as predicted by modeling of hydrologic and geochemical fluxes
Deriving a global river network map and its sub-grid topographic characteristics from a fine-resolution flow direction map
Surface water acidification and critical loads: exploring the F-factor
Modelling runoff at the plot scale taking into account rainfall partitioning by vegetation: application to stemflow of banana (Musa spp.) plant
Dying to find the source – the use of rhodamine WT as a proxy for soluble point source pollutants in closed pipe surface drainage networks
Samuel Schroers, Olivier Eiff, Axel Kleidon, Ulrike Scherer, Jan Wienhöfer, and Erwin Zehe
Hydrol. Earth Syst. Sci., 26, 3125–3150, https://doi.org/10.5194/hess-26-3125-2022, https://doi.org/10.5194/hess-26-3125-2022, 2022
Short summary
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In hydrology the formation of landform patterns is of special interest as changing forcings of the natural systems, such as climate or land use, will change these structures. In our study we developed a thermodynamic framework for surface runoff on hillslopes and highlight the differences of energy conversion patterns on two related spatial and temporal scales. The results indicate that surface runoff on hillslopes approaches a maximum power state.
Mirko Mälicke, Sibylle K. Hassler, Theresa Blume, Markus Weiler, and Erwin Zehe
Hydrol. Earth Syst. Sci., 24, 2633–2653, https://doi.org/10.5194/hess-24-2633-2020, https://doi.org/10.5194/hess-24-2633-2020, 2020
Short summary
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We could show that distributed soil moisture time series bear a considerable amount of information about dynamic changes in soil moisture. We developed a new method to describe spatial patterns and analyze their persistency. By combining uncertainty propagation with information theory, we were able to calculate the information content of spatial similarity with respect to measurement uncertainty. This does help to understand when and why the soil is drying in an organized manner.
Keith J. Beven
Hydrol. Earth Syst. Sci., 24, 2655–2670, https://doi.org/10.5194/hess-24-2655-2020, https://doi.org/10.5194/hess-24-2655-2020, 2020
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The concept of time of concentration in the analysis of catchment responses dates back over 150 years. It is normally discussed in terms of the velocity of flow of a water particle from the furthest part of a catchment to the outlet. This is also the basis for the definition in the International Glossary of Hydrology, but this is in conflict with the way in which it is commonly used. This paper provides a clarification of the concept and its correct useage.
Stefan W. Ploum, Hjalmar Laudon, Andrés Peralta-Tapia, and Lenka Kuglerová
Hydrol. Earth Syst. Sci., 24, 1709–1720, https://doi.org/10.5194/hess-24-1709-2020, https://doi.org/10.5194/hess-24-1709-2020, 2020
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Near-stream areas, or riparian zones, are important for the health of streams and rivers. If these areas are disturbed by forestry or other anthropogenic activity, the water quality and all life in streams may be at risk. We examined which riparian areas are particularly sensitive. We found that only a few wet areas bring most of the rainwater from the landscape to the stream, and they have a unique water quality. In order to maintain healthy streams and rivers, these areas should be protected.
Brett Woelber, Marco P. Maneta, Joel Harper, Kelsey G. Jencso, W. Payton Gardner, Andrew C. Wilcox, and Ignacio López-Moreno
Hydrol. Earth Syst. Sci., 22, 4295–4310, https://doi.org/10.5194/hess-22-4295-2018, https://doi.org/10.5194/hess-22-4295-2018, 2018
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The hydrology of high-elevation headwaters in midlatitudes is typically dominated by snow processes, which are very sensitive to changes in energy inputs at the top of the snowpack. We present a data analyses that reveal how snowmelt and transpiration waves induced by the diurnal solar cycle generate water pressure fluctuations that propagate through the snowpack–hillslope–stream system. Changes in diurnal energy inputs alter these pressure cycles with potential ecohydrological consequences.
Mark A. Nearing, Viktor O. Polyakov, Mary H. Nichols, Mariano Hernandez, Li Li, Ying Zhao, and Gerardo Armendariz
Hydrol. Earth Syst. Sci., 21, 3221–3229, https://doi.org/10.5194/hess-21-3221-2017, https://doi.org/10.5194/hess-21-3221-2017, 2017
Short summary
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This study presents novel scientific understanding about the way that hillslope surfaces form when exposed to rainfall erosion, and the way those surfaces interact with and influence runoff velocities during rain events. The data show that hillslope surfaces form such that flow velocities are independent of slope gradient and dependent on flow rates alone. This result represents a shift in thinking about surface water runoff.
Aliakbar Nazari Samani, Qiuwen Chen, Shahram Khalighi, Robert James Wasson, and Mohammad Reza Rahdari
Hydrol. Earth Syst. Sci., 20, 3005–3012, https://doi.org/10.5194/hess-20-3005-2016, https://doi.org/10.5194/hess-20-3005-2016, 2016
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We hypothesized that land use had important effects on hydraulic threshold conditions for gully head cut initiation. We investigated the effects using an experimental plot. The results indicated that the use of a threshold value of τcr = 35 dyne cm−2 and ωu = 0.4 Cm S−1 in physically based soil erosion models is susceptible to high uncertainty when assessing gully erosion.
Stefan J. Kollet
Hydrol. Earth Syst. Sci., 20, 2801–2809, https://doi.org/10.5194/hess-20-2801-2016, https://doi.org/10.5194/hess-20-2801-2016, 2016
Yujin Zeng, Zhenghui Xie, Yan Yu, Shuang Liu, Linying Wang, Binghao Jia, Peihua Qin, and Yaning Chen
Hydrol. Earth Syst. Sci., 20, 2333–2352, https://doi.org/10.5194/hess-20-2333-2016, https://doi.org/10.5194/hess-20-2333-2016, 2016
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In arid areas, stream–aquifer water exchange essentially sustains the growth and subsistence of riparian ecosystem. To quantify this effect for intensity and range, a stream–riverbank scheme was incorporated into a state-of-the-art land model, and some runs were set up over Heihe River basin, northwestern China. The results show that the hydrology circle is significantly changed, and the ecological system is benefitted greatly by the river water lateral transfer within a 1 km range to the stream.
A. I. Gevaert, A. J. Teuling, R. Uijlenhoet, S. B. DeLong, T. E. Huxman, L. A. Pangle, D. D. Breshears, J. Chorover, J. D. Pelletier, S. R. Saleska, X. Zeng, and P. A. Troch
Hydrol. Earth Syst. Sci., 18, 3681–3692, https://doi.org/10.5194/hess-18-3681-2014, https://doi.org/10.5194/hess-18-3681-2014, 2014
U. Nachshon, A. Ireson, G. van der Kamp, S. R. Davies, and H. S. Wheater
Hydrol. Earth Syst. Sci., 18, 1251–1263, https://doi.org/10.5194/hess-18-1251-2014, https://doi.org/10.5194/hess-18-1251-2014, 2014
J. H. Spaaks and W. Bouten
Hydrol. Earth Syst. Sci., 17, 3455–3472, https://doi.org/10.5194/hess-17-3455-2013, https://doi.org/10.5194/hess-17-3455-2013, 2013
S. Han, D. Xu, and S. Wang
Hydrol. Earth Syst. Sci., 16, 3115–3125, https://doi.org/10.5194/hess-16-3115-2012, https://doi.org/10.5194/hess-16-3115-2012, 2012
S. Reinfried, S. Tempelmann, and U. Aeschbacher
Hydrol. Earth Syst. Sci., 16, 1365–1377, https://doi.org/10.5194/hess-16-1365-2012, https://doi.org/10.5194/hess-16-1365-2012, 2012
M. Ali, G. Sterk, M. Seeger, M. Boersema, and P. Peters
Hydrol. Earth Syst. Sci., 16, 591–601, https://doi.org/10.5194/hess-16-591-2012, https://doi.org/10.5194/hess-16-591-2012, 2012
L. Gong, S. Halldin, and C.-Y. Xu
Hydrol. Earth Syst. Sci., 15, 2481–2494, https://doi.org/10.5194/hess-15-2481-2011, https://doi.org/10.5194/hess-15-2481-2011, 2011
W. Ma, Y. Ma, Z. Hu, Z. Su, J. Wang, and H. Ishikawa
Hydrol. Earth Syst. Sci., 15, 1403–1413, https://doi.org/10.5194/hess-15-1403-2011, https://doi.org/10.5194/hess-15-1403-2011, 2011
E. L. Wipfler, K. Metselaar, J. C. van Dam, R. A. Feddes, E. van Meijgaard, L. H. van Ulft, B. van den Hurk, S. J. Zwart, and W. G. M. Bastiaanssen
Hydrol. Earth Syst. Sci., 15, 1257–1271, https://doi.org/10.5194/hess-15-1257-2011, https://doi.org/10.5194/hess-15-1257-2011, 2011
W. Korres, C. N. Koyama, P. Fiener, and K. Schneider
Hydrol. Earth Syst. Sci., 14, 751–764, https://doi.org/10.5194/hess-14-751-2010, https://doi.org/10.5194/hess-14-751-2010, 2010
H. Makurira, H. H. G. Savenije, and S. Uhlenbrook
Hydrol. Earth Syst. Sci., 14, 627–638, https://doi.org/10.5194/hess-14-627-2010, https://doi.org/10.5194/hess-14-627-2010, 2010
C. H. Luce and D. G. Tarboton
Hydrol. Earth Syst. Sci., 14, 535–543, https://doi.org/10.5194/hess-14-535-2010, https://doi.org/10.5194/hess-14-535-2010, 2010
J. Liu, S. Kang, T. Gong, and A. Lu
Hydrol. Earth Syst. Sci., 14, 481–489, https://doi.org/10.5194/hess-14-481-2010, https://doi.org/10.5194/hess-14-481-2010, 2010
A. I. J. M. van Dijk
Hydrol. Earth Syst. Sci., 14, 447–458, https://doi.org/10.5194/hess-14-447-2010, https://doi.org/10.5194/hess-14-447-2010, 2010
H. H. Bulcock and G. P. W. Jewitt
Hydrol. Earth Syst. Sci., 14, 383–392, https://doi.org/10.5194/hess-14-383-2010, https://doi.org/10.5194/hess-14-383-2010, 2010
L. S. Kuchment, P. Romanov, A. N. Gelfan, and V. N. Demidov
Hydrol. Earth Syst. Sci., 14, 339–350, https://doi.org/10.5194/hess-14-339-2010, https://doi.org/10.5194/hess-14-339-2010, 2010
E. Alcântara, E. Novo, J. Stech, J. Lorenzzetti, C. Barbosa, A. Assireu, and A. Souza
Hydrol. Earth Syst. Sci., 14, 351–364, https://doi.org/10.5194/hess-14-351-2010, https://doi.org/10.5194/hess-14-351-2010, 2010
I.-Y. Yeo and J.-M. Guldmann
Hydrol. Earth Syst. Sci., 14, 325–338, https://doi.org/10.5194/hess-14-325-2010, https://doi.org/10.5194/hess-14-325-2010, 2010
C. L. Schneider, S. Attinger, J.-O. Delfs, and A. Hildebrandt
Hydrol. Earth Syst. Sci., 14, 279–289, https://doi.org/10.5194/hess-14-279-2010, https://doi.org/10.5194/hess-14-279-2010, 2010
G. Baroni, A. Facchi, C. Gandolfi, B. Ortuani, D. Horeschi, and J. C. van Dam
Hydrol. Earth Syst. Sci., 14, 251–270, https://doi.org/10.5194/hess-14-251-2010, https://doi.org/10.5194/hess-14-251-2010, 2010
C. Medici, S. Bernal, A. Butturini, F. Sabater, M. Martin, A. J. Wade, and F. Frances
Hydrol. Earth Syst. Sci., 14, 223–237, https://doi.org/10.5194/hess-14-223-2010, https://doi.org/10.5194/hess-14-223-2010, 2010
A. Petrone and F. Preti
Hydrol. Earth Syst. Sci., 14, 239–250, https://doi.org/10.5194/hess-14-239-2010, https://doi.org/10.5194/hess-14-239-2010, 2010
A. I. J. M. van Dijk
Hydrol. Earth Syst. Sci., 14, 159–169, https://doi.org/10.5194/hess-14-159-2010, https://doi.org/10.5194/hess-14-159-2010, 2010
C. Gruhier, P. de Rosnay, S. Hasenauer, T. Holmes, R. de Jeu, Y. Kerr, E. Mougin, E. Njoku, F. Timouk, W. Wagner, and M. Zribi
Hydrol. Earth Syst. Sci., 14, 141–156, https://doi.org/10.5194/hess-14-141-2010, https://doi.org/10.5194/hess-14-141-2010, 2010
M. Barnolas, T. Rigo, and M. C. Llasat
Hydrol. Earth Syst. Sci., 14, 129–139, https://doi.org/10.5194/hess-14-129-2010, https://doi.org/10.5194/hess-14-129-2010, 2010
A. Schmidt, J. J. Gibson, I. R. Santos, M. Schubert, K. Tattrie, and H. Weiss
Hydrol. Earth Syst. Sci., 14, 79–89, https://doi.org/10.5194/hess-14-79-2010, https://doi.org/10.5194/hess-14-79-2010, 2010
R. Liu, J. Wen, X. Wang, L. Wang, H. Tian, T. T. Zhang, X. K. Shi, J. H. Zhang, and SH. N. Lv
Hydrol. Earth Syst. Sci., 14, 47–58, https://doi.org/10.5194/hess-14-47-2010, https://doi.org/10.5194/hess-14-47-2010, 2010
S. Werth and A. Güntner
Hydrol. Earth Syst. Sci., 14, 59–78, https://doi.org/10.5194/hess-14-59-2010, https://doi.org/10.5194/hess-14-59-2010, 2010
H. Lin
Hydrol. Earth Syst. Sci., 14, 25–45, https://doi.org/10.5194/hess-14-25-2010, https://doi.org/10.5194/hess-14-25-2010, 2010
A. Ducharne
Hydrol. Earth Syst. Sci., 13, 2399–2412, https://doi.org/10.5194/hess-13-2399-2009, https://doi.org/10.5194/hess-13-2399-2009, 2009
J. E. Barrett, M. N. Gooseff, and C. Takacs-Vesbach
Hydrol. Earth Syst. Sci., 13, 2349–2358, https://doi.org/10.5194/hess-13-2349-2009, https://doi.org/10.5194/hess-13-2349-2009, 2009
V. García-García, R. Gómez, M. R. Vidal-Abarca, and M. L. Suárez
Hydrol. Earth Syst. Sci., 13, 2359–2371, https://doi.org/10.5194/hess-13-2359-2009, https://doi.org/10.5194/hess-13-2359-2009, 2009
M. Shamsudduha, R. E. Chandler, R. G. Taylor, and K. M. Ahmed
Hydrol. Earth Syst. Sci., 13, 2373–2385, https://doi.org/10.5194/hess-13-2373-2009, https://doi.org/10.5194/hess-13-2373-2009, 2009
J. C. M. Andersson, A. J. B. Zehnder, G. P. W. Jewitt, and H. Yang
Hydrol. Earth Syst. Sci., 13, 2329–2347, https://doi.org/10.5194/hess-13-2329-2009, https://doi.org/10.5194/hess-13-2329-2009, 2009
S. Binet, L. Spadini, C. Bertrand, Y. Guglielmi, J. Mudry, and C. Scavia
Hydrol. Earth Syst. Sci., 13, 2315–2327, https://doi.org/10.5194/hess-13-2315-2009, https://doi.org/10.5194/hess-13-2315-2009, 2009
A. Bárdossy and G. G. S. Pegram
Hydrol. Earth Syst. Sci., 13, 2299–2314, https://doi.org/10.5194/hess-13-2299-2009, https://doi.org/10.5194/hess-13-2299-2009, 2009
K. Dontsova, C. I. Steefel, S. Desilets, A. Thompson, and J. Chorover
Hydrol. Earth Syst. Sci., 13, 2273–2286, https://doi.org/10.5194/hess-13-2273-2009, https://doi.org/10.5194/hess-13-2273-2009, 2009
D. Yamazaki, T. Oki, and S. Kanae
Hydrol. Earth Syst. Sci., 13, 2241–2251, https://doi.org/10.5194/hess-13-2241-2009, https://doi.org/10.5194/hess-13-2241-2009, 2009
L. Rapp and K. Bishop
Hydrol. Earth Syst. Sci., 13, 2191–2201, https://doi.org/10.5194/hess-13-2191-2009, https://doi.org/10.5194/hess-13-2191-2009, 2009
J.-B. Charlier, R. Moussa, P. Cattan, Y.-M. Cabidoche, and M. Voltz
Hydrol. Earth Syst. Sci., 13, 2151–2168, https://doi.org/10.5194/hess-13-2151-2009, https://doi.org/10.5194/hess-13-2151-2009, 2009
C. H. Mines, A. Ghadouani, and G. N. Ivey
Hydrol. Earth Syst. Sci., 13, 2169–2178, https://doi.org/10.5194/hess-13-2169-2009, https://doi.org/10.5194/hess-13-2169-2009, 2009
Cited articles
Arnau-Rosalen, E., Calvo-Cases, A., Boix-Fayos, C., Lavee, H., and Sarah, P.: Analysis of soil surface component patterns affecting runoff generation. An example of methods applied to mediterranean hillslopes in alicante (Spain), Geomorphology, 101, 595–606, https://doi.org/10.1016/j.geomorph.2008.03.001, 2008.
Bautista, S., Bellot, J., and Vallejo, V. R.: Mulching treatment for postfire soil conservation in a semiarid ecosystem, Arid Soil Res. Rehab., 10, 235–242, 1996.
Bochet, E., Poesen, J., and Rubio, J. L.: Runoff and soil loss under individual plants of a semi-arid mediterranean shrubland: Influence of plant morphology and rainfall intensity, Earth Surf. Proc. Land., 31, 536–549, 2006.
Bochet, E., Garcia-Fayos, P., and Tormo, J.: How can we control erosion of roadslopes in semiarid Mediterranean areas? Soil improvement and native plant establishment, Land Degrad. Dev., 21, 110–121, https://doi.org/10.1002/ldr.911, 2010.
Boix-Fayos, C., Martinez-Mena, M., Calvo-Cases, A., Castillo, V., and Albaladejo, J.: Concise review of interrill erosion studies in SE Spain (alicante and murcia): Erosion rates and progress of knowledge from the 1980s, Land Degrad. Dev., 16, 517–528, 2005.
Boix-Fayos, C., Martinez-Mena, M., Arnau-Rosalen, E., Calvo-Cases, A., Castillo, V., and Albaladejo, J.: Measuring soil erosion by field plots: Understanding the sources of variation, Earth-Sci. Rev., 78, 267–285, https://doi.org/10.1016/j.earscirev.2006.05.005, 2006.
Bracken, L. J. and Croke, J.: The concept of hydrological connectivity and its contribution to understanding runoff-dominated geomorphic systems, Hydrol. Process., 21, 1749–1763, 2007.
Bracken, L. J. and Kirkby, M. J.: Differences in hillslope runoff and sediment transport rates within two semi-arid catchments in southeast Spain, Geomorphology, 68, 183–200, https://doi.org/10.1016/j.geomorph.2004.11.013, 2005.
Bradshaw, A. D.: The reconstruction of ecosystems: Presidential address to the british ecological society, December 1982, J. Appl. Ecol., 20, 1–17, 1983.
Bromley, J., Brouwer, J., Barker, A. P., Gaze, S. R., and Valentine, C.: The role of surface water redistribution in an area of patterned vegetation in a semi-arid environment, south-west Niger, J. Hydrol., 198, 1–29, 1997.
Calvo-Cases, A., Boix-Fayos, C., and Imeson, A. C.: Runoff generation, sediment movement and soil water behaviour on calcareous (limestone) slopes of some mediterranean environments in southeast Spain, Geomorphology, 50, 269–291, 2003.
Cammeraat, L. H.: A review of two strongly contrasting geomorphological systems within the context of scale, Earth Surf. Proc. Land., 27, 1201–1222, https://doi.org/10.1002/esp.421, 2002.
Cassel, D. K., Kachanoski, R. G., and Topp, G. C.: Practical considerations for using a tdr cable tester, Soil Technol., 7, 113–126, 1994.
Cerdà, A.: The effect of patchy distribution of stipa tenacissima L on runoff and erosion, J. Arid Environ., 36, 37–51, 1997.
Cerdà, A.: Soil aggregate stability under different Mediterranean vegetation types, Catena, 32, 73–86, 1998.
Davenport, D. W., Breshears, D. D., Wilcox, B. P., and Allen, C. D.: Viewpoint: Sustainability of pinon-juniper ecosystems – a unifying perspective of soil erosion thresholds, J. Range Manage., 51, 231–240, 1998.
De Baets, S., Poesen, J., Knapen, A., Barbera, G. G., and Navarro, J. A.: Root characteristics of representative mediterranean plant species and their erosion-reducing potential during concentrated runoff, Plant Soil, 294, 169–183, 2007.
Dunkerley, D. L. and Brown, K. J.: Runoff and runon areas in a patterned chenopod shrubland, arid western New-South-Wales, Australia – characteristics and origin, J. Arid. Environ., 30, 41–55, 1995.
Espigares, T., Moreno-de las Heras, M., and Nicolau, J. M.: Performance of vegetation in reclaimed slopes affected by soil erosion, Restor. Ecol., 19, 35–44, 2011.
Garcia-Estringana, P., Alonso-Blazquez, N., Marques, M. J., Bienes, R., and Alegre, J.: Direct and indirect effects of mediterranean vegetation on runoff and soil loss, Eur. J. Soil Sci., 61, 174–185, https://doi.org/10.1111/j.1365-2389.2009.01221.x, 2010.
Garner, W. and Steinberger, Y.: A proposed mechanism for the formation of fertile islands in the desert ecosystem, J. Arid Environ., 16, 257–262, 1989.
Gokbulak, F.: Comparison of growth performance of lolium perenne L., dactylis glomerata L. and agropyron elongatum (host.) P. Beauv., For erosion control in Turkey, J. Environ. Biol., 24, 45–53, 2003.
Hancock, G. R. and Willgoose, G. R.: An experimental and computer simulation study of erosion on a mine tailings dam wall, Earth Surf. Proc. Land., 29, 457–475, https://doi.org/10.1002/esp.1045, 2004.
Hollander, M. and Wolfe, D. A.: Nonparametric statistical methods, 2nd Edn., John Wiley & Sons, Inc, New York, 1999.
Lavee, H., Imeson, A. C., and Sarah, P.: The impact of climate change on geomorphology and desertification along a mediterranean-arid transect, Land Degrad. Dev., 9, 407–422, 1998.
Ludwig, J. A. and Tongway, D. J.: Spatial-organization of landscapes and its function in semiarid woodlands, Australia, Landscape Ecol., 10, 51–63, 1995.
Ludwig, J. and Tongway, D.: Viewing rangelands as landscape systems, in: Rangeland desertification, edited by: Arnalds, O. and Archer, S., Advances in vegetation science, Kluwer Academic, Dordrecht, The Netherlands, 39–52, 2000.
Ludwig, J., Tongway, D., Freudenberger, D., Noble, J., and Hodgkinson, K.: Landscape ecology, function and management: Principles from australia's rangelands, CSIRO Publishing, Melbourne, Australia, 1997.
Ludwig, J. A., Wilcox, B. P., Breshears, D. D., Tongway, D. J., and Imeson, A. C.: Vegetation patches and runoff-erosion as interacting ecohydrological processes in semiarid landscapes, Ecology, 86, 288–297, 2005.
MAPA: Métodos oficiales de análisis, in: Tomo iii. Secretaría general de alimentación, Dirección general de política alimentária, Ministerio de agricultura, pesca y alimentación, Madrid, Spain, 1994.
Mayor, A. G., Bautista, S., Small, E. E., Dixon, M., and Bellot, J.: Measurement of the connectivity of runoff source areas as determined by vegetation pattern and topography: A tool for assessing potential water and soil losses in drylands, Water Resour. Res., 44, W10423, https://doi.org/10.1029/2007wr006367, 2008.
Mayor, Á. G., Bautista, S., and Bellot, J.: Factors and interactions controlling infiltration, runoff, and soil loss at the microscale in a patchy Mediterranean semiarid landscape, Earth Surf. Proc. Land., 34, 1702–1711, 2009.
McIvor, J. G., Williams, J., and Gardener, C. J.: Pasture management influences runoff and soil movement in the semiarid tropics, Aust. J. Exp. Agr., 35, 55–65, 1995.
Merino-Martín, L., Breshears, D. D., Moreno-de las Heras, M., Villegas, J. C., Pérez-Domingo, S., Espigares, T., and Nicolau, J. M.: Ecohydrological interrelationships between vegetation patches and soil hydrological properties along a disturbance gradient: How sources and sinks of runoff determine a restoration threshold, Restor. Ecol., 20, 360–368, https://doi.org/10.1111/j.1526-100X.2011.00776.x, 2011.
Molinillo, M., Lasanta, T., and GarciaRuiz, J. M.: Managing mountainous degraded landscapes after farmland abandonment in the Central Spanish Pyrenees, Environ. Manage., 21, 587–598, 1997.
Moreno-de las Heras, M., Nicolau, J. M., and Espigares, T.: Vegetation succession in reclaimed coal-mining slopes in a Mediterranean-dry environment, Ecol. Eng., 34, 168-178, 2008.
Moreno-de las Heras, M., Merino-Martín, L., and Nicolau, J. M.: Effect of vegetation cover on the hydrology of reclaimed mining soils under Mediterranean-continental climate, Catena, 77, 39–47, 2009.
Moreno-de las Heras, M., Nicolau, J. M., Merino-Martin, L., and Wilcox, B. P.: Plot-scale effects on runoff and erosion along a slope degradation gradient, Water Resour. Res., 46, W04503, https://doi.org/10.1029/2009wr007875, 2010.
Moreno-de las Heras, M., Espigares, T., Merino-Martín, L., and Nicolau, J. M.: Water-related ecological impacts of rill erosion processes in Mediterranean-dry reclaimed slopes, Catena, 84, 114–124, 2011.
Morgan, R. P. C.: Factors influencing erosion, in: Soil Erosion and Conservation, edited by: Morgan, R. P. C., Longman, Essex, UK, 26–39, 1995.
Nicolau, J. M.: Runoff generation and routing on artificial slopes in a Mediterranean-continental environment: The teruel coalfield, Spain, Hydrol. Process., 16, 631–647, 2002.
Nicolau, J. M.: Trends in relief design and construction in opencast mining reclamation, Land Degrad. Dev., 14, 215–226, 2003.
Noy-Meir, I.: Desert ecosystems: Environment and producers, Ann. Rev. Ecol. System., 4, 25–51, 1973.
Papadakis, J.: Climates of the world and their agricultural potentialities, edited by: Papadakis, J., Buenos Aires, 1966.
Peña, J. L., Cuadrat, J. M., and Sanchez, M.: El clima de la provincia de teruel, in: Cartilla turolense, Instituto de Estudios Turolenses (CSIC), Teruel, 2002.
Puigdefábregas, J., Sole, A., Gutierrez, L., del Barrio, G., and Boer, M.: Scales and processes of water and sediment redistribution in drylands: Results from the Rambla Honda field site in southeast Spain, Earth-Sci. Rev., 48, 39–70, 1999.
Puigdefábregas, J.: The role of vegetation patterns in structuring runoff and sediment fluxes in drylands, Earth Surf. Proc. Land., 30, 133–147, 2005.
R_Development_Core_Team: R: A language and environment for statistical computing, in: R Foundation for Statistical Computing, Vienna, Austria, 2009.
Reid, K. D., Wilcox, B. P., Breshears, D. D., and MacDonald, L.: Runoff and erosion in a Pinon-Juniper woodland: Influence of vegetation patches, Soil Sci. Soc. Am. J., 63, 1869–1879, 1999.
Richards, L. A.: A pressure-membrane extraction apparatus for soil solution, Soil Sci., 51, 377–386, https://doi.org/10.1097/00010694-194105000-00005, 1941.
Sánchez, G. and Puigdefabregas, J.: Interactions of plant-growth and sediment movement on slopes in a semiarid environment, Geomorphology, 9, 243–260, 1994.
Scanlan, J., Pressland, A., and Myles, D.: Run-off and soil movement on mid-slopes in north-east Queensland [Australia] grazed woodlands, Rangeland J., 18, 33–46, https://doi.org/10.1071/RJ9960033, 1996.
Schlesinger, W. H., Reynolds, J. F., Cunningham, G. L., Huenneke, L. F., Jarrell, W. M., Virginia, R. A., and Whitford, W. G.: Biological feedbacks in global desertification, Science, 247, 1043–1048, 1990.
Seghieri, J., Galle, S., Rajot, J. L., and Ehrmann, M.: Relationships between soil moisture and growth of herbaceous plants in a natural vegetation mosaic in niger, J. Arid Environ., 36, 87–102, 1997.
Statsoft: Statistica, in: Data analysis software system, Tulsa, OK, 2001.
Tryon, R. C.: Cluster analysis, Edwards Brothers, Ann Arbor, Michigan, 1939.
Turnbull, L., Wainwright, J., and Brazier, R. E.: A conceptual framework for understanding semi-arid land degradation: Ecohydrological interactions across multiple-space and time scales, Ecohydrology, 1, 23–34, https://doi.org/10.1002/eco.4, 2008.
Turnbull, L., Wainwright, J., Brazier, R. E., and Bol, R.: Biotic and abiotic changes in ecosystem structure over a shrub-encroachment gradient in the southwestern USA, Ecosystems, 13, 1239–1255, https://doi.org/10.1007/s10021-010-9384-8, 2010.
Vasquez-Mendez, R., Ventura-Ramos, E., Oleschko, K., Hernandez-Sandoval, L., Parrot, J. F., and Nearing, M. A.: Soil erosion and runoff in different vegetation patches from semiarid Central Mexico, Catena, 80, 162–169, https://doi.org/10.1016/j.catena.2009.11.003, 2010.
Wainwright, J., Parsons, A. J., Schlesinger, W. H., and Abrahams, A. D.: Hydrology-vegetation interactions in areas of discontinuous flow on a semi-arid Bajada, Southern New Mexico, J. Arid Environ, 51, 319–338, 2002.
White, L. P.: Vegetation arcs in Jordan, J. Ecol., 57, 461–464, 1969.
Wilcox, B. P., Breshears, D. D., and Allen, C. D.: Ecohydrology of a resource-conserving semiarid woodland: Effects of scale and disturbance, Ecol. Monogr., 73, 223–239, 2003.
Zhou, Z. C. and Shangguan, Z. P.: The effects of ryegrass roots and shoots on loess erosion under simulated rainfall, Catena, 70, 350–355, https://doi.org/10.1016/j.catena.2006.11.002, 2007.
Zhou, Z. C. and Shangguan, Z. P.: Effect of ryegrasses on soil runoff and sediment control, Pedosphere, 18, 131–136, 2008.
