2003
DOI: 10.1046/j.1365-2486.2003.00690.x
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Detection of process‐related changes in plant patterns at extended spatial scales during early dryland desertification

Abstract: Arid and semiarid shrublands occupy extensive land areas over the world, are susceptible to desertification by anthropic use and can contribute to regional climate change. These prompt the interest to monitor and evaluate these lands adequately in order to detect early stages of degradation. Evaluation topics must refer to biology‐relevant characteristics of these systems, while simultaneously satisfying sampling consistency over extended landscape areas. We present an analysis of process‐relevant parameters r… Show more

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Cited by 40 publications
(40 citation statements)
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References 42 publications
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“…It builds on previous results obtained by Ares et al (2003) indicating that early desertification processes involve modifications of the overland flow patterns and its distribution among the various vegetation life forms in the Patagonian Monte (Argentina). Here, an experimental protocol is presented of the field plot experiments and coupled simulation model to estimate infiltration and overland flow parameters in the Monte environment.…”
Section: Introductionsupporting
confidence: 85%
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“…It builds on previous results obtained by Ares et al (2003) indicating that early desertification processes involve modifications of the overland flow patterns and its distribution among the various vegetation life forms in the Patagonian Monte (Argentina). Here, an experimental protocol is presented of the field plot experiments and coupled simulation model to estimate infiltration and overland flow parameters in the Monte environment.…”
Section: Introductionsupporting
confidence: 85%
“…Surface flow redistribution may also occur on flat ground if the presence of vegetation patches creates contrasts in infiltration rate between dry soil and water saturated areas. Changes in the pattern of surface water re-distribution occur during early stages of desertification (Ares et al, 2003). Several studies indicate that the horizontal movements of the naturally scarce rainfall water on the surface soil in arid regimes contribute to define the spatial pattern of woody and herbaceous vegetation forms as well as the extent of bare soil patches (Aguiar and Sala, 1999;Ares et al, 2003;Borgogno et al, 2009;Dunkerley, 2002).…”
Section: Introductionmentioning
confidence: 99%
“…To discriminate the slight differences among sites located close to watering point, more quantitative measurements of grazing disturbance such as the scale of heterogeneity of shrub patches, which is positively related to grazing disturbance, are necessary (Bisigato et al, 2005). The scale of heterogeneity is derived from the spatial arrangement of shrubs, which shows considerable less temporal variation than other variables based on seasonally fluctuating herbaceous forms, such as plant cover (Ares et al, 2003b). In addition, it is relatively easily measured in high-resolution aerial photographs, whereas plant cover measurements in the field are time consuming and, depending on the sampling protocol, subjective.…”
Section: Discussionmentioning
confidence: 99%
“…This study does not include sites located at intermediate distances from watering points, which would fill the big gap in scales of heterogeneity between ''far'' and ''close'' sites. The inclusion of these sites, which present intermediate spatial patterns between those of ''far'' and ''close'' sites (Ares et al, 2003b), would help to define a range of scales of heterogeneity where internal remobilisation of resources begins. However, this range should be close to 3 m, because the site F2 (the site with the highest scale of heterogeneity among sites located far from watering points) presents several characteristics in common with sites C1 and C3, such as autocorrelation in soil-N and covariance between shrub cover and soil mounds (Fig.…”
Section: Discussionmentioning
confidence: 99%
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