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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

dc.contributor.authorGarcía Mayor, Ángeles Pilar
dc.contributor.authorBautista, Susana
dc.contributor.authorSmall, Eric
dc.contributor.authorDixon, Mike
dc.contributor.authorBellot, Juan
dc.date.accessioned2024-02-02T09:41:58Z
dc.date.available2024-02-02T09:41:58Z
dc.date.issued2008
dc.description.abstractThe connectivity of runoff sources is considered one of the main factors controlling the hydrology of sparsely vegetated landscapes. However, the empirical demonstration of this role is very limited, partly because of the scarcity of suitable connectivity metrics. In this work, we derived and tested a spatial metric, Flowlength, for quantifying the connectivity of runoff source areas considering both vegetation pattern and topography. Flowlength is calculated as the average of the runoff pathway lengths from all the cells in a raster‐based map of the target site. We evaluated the relationships between the connectivity of runoff sources, measured with Flowlength, and the runoff and sediment yields from six plots and three catchments in semiarid southeast Spain. Flowlength distinguished varying degrees of connectivity between differing vegetation patterns with similar vegetation cover. The connectivity increased with the grain size of the bare areas and was positively related to plot runoff and sediment yields. Flowlength also correctly ranked the three catchments according to total runoff yielded during the study period. The inclusion of microtopographic information in the quantification of Flowlength improved the relationships between the pattern of runoff sources and the measured fluxes, highlighting the importance of topographic features in the connectivity of surface flows. In general, the microtopography had a net decreasing effect on the connectivity, which was mainly attributed to an increase in the amount of runoff sink areas caused by the sediment terracettes developed upslope of plants. Our results confirm that the connectivity of runoff sources is a key factor controlling runoff and erosion in semiarid lands and support the potential of Flowlength as a surrogate for the hydrological functioning of ecosystems with patchy vegetation.
dc.description.departmentDepto. de Biodiversidad, Ecología y Evolución
dc.description.facultyFac. de Ciencias Biológicas
dc.description.refereedTRUE
dc.description.sponsorshipNational Science Foundation
dc.description.sponsorshipMinisterio de Ciencia y Educación (España)
dc.description.statuspub
dc.identifier.citationMayor, Ángeles G., et al. «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 Resources Research, vol. 44, n.o 10, octubre de 2008, p. 2007WR006367. https://doi.org/10.1029/2007WR006367.
dc.identifier.doi10.1029/2007wr006367
dc.identifier.essn1944-7973
dc.identifier.issn0043-1397
dc.identifier.officialurlhttps://doi.org/10.1029/2007WR006367
dc.identifier.urihttps://hdl.handle.net/20.500.14352/98131
dc.issue.number10
dc.journal.titleWater Resources Research
dc.language.isoeng
dc.page.final13
dc.page.initial1
dc.publisherWiley
dc.rights.accessRightsopen access
dc.subject.ucmCiencias
dc.subject.unesco24 Ciencias de la Vida
dc.titleMeasurement 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
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number44
dspace.entity.typePublication
relation.isAuthorOfPublication2548da49-358e-4555-b413-dec6bae3af5d
relation.isAuthorOfPublication.latestForDiscovery2548da49-358e-4555-b413-dec6bae3af5d

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