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Please use this identifier to cite or link to this item: http://dspace.ucuenca.edu.ec/handle/123456789/39568
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dc.contributor.authorRomán Dañobeytia, Francisco-
dc.contributor.authorMosquera Rojas, Giovanny Mauricio-
dc.contributor.authorMarin Molina, Franklin Geovanny-
dc.contributor.authorStern, Margaret-
dc.contributor.authorBonnesoeur, Vivien-
dc.contributor.authorCrespo Sanchez, Patricio Javier-
dc.contributor.authorOchoa Tocachi, Boris Fernando-
dc.date.accessioned2022-08-03T20:00:27Z-
dc.date.available2022-08-03T20:00:27Z-
dc.date.issued2022-
dc.identifier.issn0048-9697-
dc.identifier.urihttp://dspace.ucuenca.edu.ec/handle/123456789/39568-
dc.identifier.urihttps://www.scopus.com/record/display.uri?eid=2-s2.0-85114748975&origin=inward&txGid=05d478f0373acc81ee59ec14f50d32f9&featureToggles=FEATURE_NEW_DOC_DETAILS_EXPORT:1,FEATURE_EXPORT_REDESIGN:0-
dc.description.abstractHigh-elevation grasslands worldwide provide essential hydrological services including water provision, flow regulation, and erosion control. Despite their importance, hydrological research of grasslands in montane regions is usually scarce and disperse, limiting the capacity to improve water resource management. We present a systematic literature review of the hydrological function of high Andean grasslands under conserved, degraded, and restored conditions in ecosystems situated above the tree line in the tropical Andes (paramos, punas, and jalcas). Most hydrological research on these grasslands has been developed in paramos (92%), especially in Ecuador, while research in punas is scarce (6%) despite being the largest grassland extent in the region. For paramos, published literature highlights the importance of conserving grasslands to facilitate water infiltration to soils, which in turn reduces erosive processes. Water-vegetation relations for conserved paramos are well understood, indicating that about 50% of water inputs return to the atmosphere via evapotranspiration, but knowledge about hydrological functions of conserved punas and jalcas is virtually non-existent. Under changing land use, afforestation of grassland ecosystems with exotic tree species, especially pines, reduces soil water storage as well as water yield and flow regulation capacity. Impacts of grazing and agriculture on the hydrological function of paramo grasslands strongly depend on historical land management and current land use practices and are not generalizable. Short-term restoration studies indicate that more than two years are necessary to recover the hydrological function of degraded grasslands, therefore medium and long-term studies are required to determine efficient restoration periods. These knowledge gaps limit the ability to extrapolate and regionalize findings. Future directions aimed to fill them are proposed, and methods successfully used to investigate the hydrology of high Andean grasslands are highlighted. This research not only enlightens what is known about the hydrology of high Andean grasslands, but also seeks to guide future hydrological evaluations to fill identified geographical and topical knowledge gaps precluding improved management of water resources in the tropical Andes. (c) 2021 Elsevier B.V. All rights reserved.-
dc.language.isoes_ES-
dc.sourceScience of the Total Environment-
dc.subjectTussock grass-
dc.subjectEcosystem services-
dc.subjectLand cover-
dc.subjectAlpine grassland-
dc.subjectEcohydrology-
dc.subjectLand use-
dc.subjectAlpine grassland-
dc.subjectEcohydrology-
dc.subjectEcosystem services-
dc.subjectLand cover-
dc.subjectLand use-
dc.subjectTussock grass-
dc.subjectEnvironmental chemistry-
dc.subjectEnvironmental engineering-
dc.subjectPollution-
dc.subjectWaste management and disposal-
dc.titleProgress in understanding the hydrology of high-elevation andean grasslands under changing land use-
dc.typeARTÍCULO-
dc.ucuenca.idautor0105365589-
dc.ucuenca.idautor0105802375-
dc.ucuenca.idautor0104450911-
dc.ucuenca.idautor0102572773-
dc.ucuenca.idautor0000-0002-2194-3652-
dc.ucuenca.idautor0000-0001-8208-5017-
dc.ucuenca.idautor0000-0001-6990-4460-
dc.identifier.doi10.1016/j.scitotenv.2021.150112-
dc.ucuenca.versionVersión publicada-
dc.ucuenca.areaconocimientounescoamplio05 - Ciencias Físicas, Ciencias Naturales, Matemáticas y Estadísticas-
dc.ucuenca.afiliacionOchoa, B., Iniciativa Regional de Monitoreo Hidrológico de Ecosistemas Andinos (iMHEA), Lima, Peru-
dc.ucuenca.afiliacionMarin, F., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador-
dc.ucuenca.afiliacionMosquera, G., Universidad San Francisco de Quito, Quito , Ecuador-
dc.ucuenca.afiliacionRomán, F., Consorcio para el Desarrollo Sostenible de la Ecorregión Andina (CONDESAN), Lima, Peru-
dc.ucuenca.afiliacionBonnesoeur, V., Iniciativa Regional de Monitoreo Hidrológico de Ecosistemas Andinos (iMHEA), Lima, Peru-
dc.ucuenca.afiliacionCrespo, P., Universidad de Cuenca, Departamento de Recursos Hídricos y Ciencias Ambientales, Cuenca, Ecuador; Crespo, P., Iniciativa Regional de Monitoreo Hidrológico de Ecosistemas Andinos (iMHEA), Lima, Peru-
dc.ucuenca.afiliacionStern, M., Iniciativa Regional de Monitoreo Hidrológico de Ecosistemas Andinos (iMHEA), Lima, Peru-
dc.ucuenca.volumenVolumen 804-
dc.ucuenca.indicebibliograficoSCOPUS-
dc.ucuenca.factorimpacto1.806-
dc.ucuenca.cuartilQ1-
dc.ucuenca.numerocitaciones0-
dc.ucuenca.areaconocimientofrascatiamplio1. Ciencias Naturales y Exactas-
dc.ucuenca.areaconocimientofrascatiespecifico1.5 Ciencias de la Tierra y el Ambiente-
dc.ucuenca.areaconocimientofrascatidetallado1.5.10 Recursos Hídricos-
dc.ucuenca.areaconocimientounescoespecifico052 - Medio Ambiente-
dc.ucuenca.areaconocimientounescodetallado0521 - Ciencias Ambientales-
dc.ucuenca.urifuentehttps://www.sciencedirect.com/journal/science-of-the-total-environment/vol/804/suppl/C-
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