2007
DOI: 10.1002/esp.1531
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Modelling dynamic water redistribution patterns in arid catchments in the Negev Desert of Israel

Abstract: In arid climate regions, redistribution of runoff water is highly relevant for vegetation development. The process of water redistribution at catchment scale is studied with the landscape process model LAPSUS, mainly used for erosion and sedimentation modelling. LAPSUS, formerly applied in Mediterranean climates, is modified to deal with the arid climate of the Negev Desert of Israel. Daily event based model runs were used instead of yearly model runs, and the infiltration module was modified to better represe… Show more

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Cited by 27 publications
(24 citation statements)
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“…Third, studies or models for ESSs either cover a small area (O 'Farrell et al 2010;Egoh et al 2011) or are not spatially explicit (Costanza et al 1997;Alcamo et al 2005;MA 2005). Finally, the effects of spatial and biophysical structure of the landscape, important for erosion and pollination among others (Steffan-Dewenter and Tscharntke 1999; Buis and Veldkamp 2008), and the effects of soil and climate are often overlooked (Kienast et al 2009). …”
Section: Introductionmentioning
confidence: 99%
“…Third, studies or models for ESSs either cover a small area (O 'Farrell et al 2010;Egoh et al 2011) or are not spatially explicit (Costanza et al 1997;Alcamo et al 2005;MA 2005). Finally, the effects of spatial and biophysical structure of the landscape, important for erosion and pollination among others (Steffan-Dewenter and Tscharntke 1999; Buis and Veldkamp 2008), and the effects of soil and climate are often overlooked (Kienast et al 2009). …”
Section: Introductionmentioning
confidence: 99%
“…In the end, agricultural activities also results in large and small scale micro-forms depending on the method and direction of 15 tillage used: from ridges and furrows (SzabĂł, 2006;Buis and Veldkamp, 2008), ditches, ridges and berms (Li et al, 2009;Vieira and Dabney, 2011) to saucer shaped depressions (Darboux et al, 2002;PĂĄsztor et al, 2006;Li et al, 2009). These local scales morphological changes together with presence/absence of forest, wetlands or impervious surfaces significantly the hydrologic regime of the catchment and the observed HEF (Ryan et al, 2010).…”
Section: Anthropogenic Factors -Land Management Impacts On Surface Hymentioning
confidence: 99%
“…Up to now, modeling approaches to characterize wetlands are generally based upon slope (wetlands tend to have flat slopes) and water accumulation derived on the basis of contributing area (Buis and Veldkamp 2008). Digital elevation models (DEM) are readily accessible nowadays, and automated procedures exist to compute terrain derivatives (slope, curvature, topographic index, variance in slope, etc.)…”
Section: Introductionmentioning
confidence: 99%