Impacts of land use on the hydrological response of tropical Andean catchments

dc.contributor.authorB. F. Ochoa‐Tocachi
dc.contributor.authorWouter Buytaert
dc.contributor.authorBert De Bièvre
dc.contributor.authorRolando Célleri
dc.contributor.authorPatricio Crespo
dc.contributor.authorMarcos Villacís
dc.contributor.authorCarlos Llerena
dc.contributor.authorL. Acosta
dc.contributor.authorMauricio Villazón
dc.contributor.authorMario Guallpa
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T13:52:36Z
dc.date.available2026-03-22T13:52:36Z
dc.date.issued2016
dc.descriptionCitaciones: 150
dc.description.abstractAbstract Changes in land use and land cover are major drivers of hydrological alteration in the tropical Andes. However, quantifying their impacts is fraught with difficulties because of the extreme diversity in meteorological boundary conditions, which contrasts strongly with the lack of knowledge about local hydrological processes. Although local studies have reduced data scarcity in certain regions, the complexity of the tropical Andes poses a big challenge to regional hydrological prediction. This study analyses data generated from a participatory monitoring network of 25 headwater catchments covering three of the major Andean biomes ( páramo , jalca and puna ) and links their hydrological responses to main types of human interventions (cultivation, afforestation and grazing). A paired catchment setup was implemented to evaluate the impacts of change using a ‘trading space‐for‐time’ approach. Catchments were selected based on regional representativeness and contrasting land use types. Precipitation and discharge have been monitored and analysed at high temporal resolution for a time period between 1 and 5 years. The observed catchment responses clearly reflect the extraordinarily wide spectrum of hydrological processes of the tropical Andes. They range from perennially humid páramos in Ecuador and northern Peru with extremely large specific discharge and baseflows, to highly seasonal, flashy catchments in the drier punas of southern Peru and Bolivia. The impacts of land use are similarly diverse and their magnitudes are a function of catchment properties, original and replacement vegetation and management type. Cultivation and afforestation consistently affect the entire range of discharges, particularly low flows. The impacts of grazing are more variable but have the largest effect on the catchment hydrological regulation. Overall, anthropogenic interventions result in increased streamflow variability and significant reductions in catchment regulation capacity and water yield, irrespective of the hydrological properties of the original biome. Copyright © 2016 The Authors. Hydrological Processes . Published by John Wiley & Sons Ltd.
dc.identifier.doi10.1002/hyp.10980
dc.identifier.urihttps://doi.org/10.1002/hyp.10980
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/43237
dc.language.isoen
dc.publisherWiley
dc.relation.ispartofHydrological Processes
dc.sourceConsortium for Sustainable Development of the Andean Ecoregion
dc.subjectLand use
dc.subjectBiome
dc.subjectDrainage basin
dc.subjectEnvironmental science
dc.subjectLand cover
dc.subjectPrecipitation
dc.subjectAfforestation
dc.subjectCatchment hydrology
dc.subjectRange (aeronautics)
dc.subjectHydrology (agriculture)
dc.titleImpacts of land use on the hydrological response of tropical Andean catchments
dc.typearticle

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