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dc.contributor.authorZabaleta Lopetegui, Ane
dc.contributor.authorAntigüedad Auzmendi, Ignacio
dc.date.accessioned2014-02-07T17:18:01Z
dc.date.available2014-02-07T17:18:01Z
dc.date.issued2013
dc.identifier.citationHydrology and Earth System Sciences 17(1) : 211-223 (2013)es
dc.identifier.issn1027-5606
dc.identifier.urihttp://hdl.handle.net/10810/11386
dc.description.abstractThe hydrological response of a catchment to rainfall on different timescales is result of a complex system involving a range of physical processes which may operate simultaneously and have different spatial and temporal influences. This paper presents the analysis of streamflow response of a small humid-temperate catchment (Aixola, 4.8 km(2)) in the Basque Country on different timescales and discusses the role of the controlling factors. Firstly, daily time series analysis was used to establish a hypothesis on the general functioning of the catchment through the relationship between precipitation and discharge on an annual and multiannual scale (2003-2008). Second, rainfall-runoff relationships and relationships among several hydrological variables, including catchment antecedent conditions, were explored at the event scale (222 events) to check and improve the hypothesis. Finally, the evolution of electrical conductivity (EC) during some of the monitored storm events (28 events) was examined to identify the time origin of waters. Quick response of the catchment to almost all the rainfall events as well as a considerable regulation capacity was deduced from the correlation and spectral analyses. These results agree with runoff event scale data analysis; however, the event analysis revealed the non-linearity of the system, as antecedent conditions play a significant role in this catchment. Further, analysis at the event scale made possible to clarify factors controlling (precipitation, precipitation intensity and initial discharge) the different aspects of the runoff response (runoff coefficient and discharge increase) for this catchment. Finally, the evolution of EC of the waters enabled the time origin (event or pre-event waters) of the quickflow to be established; specifically, the conductivity showed that pre-event waters usually represent a high percentage of the total discharge during runoff peaks. The importance of soil waters in the catchment is being studied more deeply.es
dc.description.sponsorshipThe authors wish to thank the Environment and Land Management Department of the Gipuzkoa Provincial Council, the University of the Basque Country (UFI 11/26), and the Basque Government (Consolidated Group IT516-10 and the K-Egokitzen project-ETORTEK IE10-277) for supporting this research.es
dc.language.isoenges
dc.publisherCopernicus Gesellschaftes
dc.rightsinfo:eu-repo/semantics/openAccesses
dc.subjectcoefficientses
dc.subjectcross spectral analysises
dc.subjectrunoff generation processeses
dc.subjectsoil moisturees
dc.subjecthydrological systemses
dc.subjecttime serieses
dc.subjecthydrograph separationes
dc.subjectauto-correlationes
dc.subjectpeak dischargees
dc.subjectstorm flowes
dc.titleStreamflow response of a small forested catchment on different timescaleses
dc.typeinfo:eu-repo/semantics/articlees
dc.rights.holder© Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.es
dc.relation.publisherversionhttp://www.hydrol-earth-syst-sci.net/17/211/2013/hess-17-211-2013.htmles
dc.identifier.doi10.5194/hess-17-211-2013
dc.departamentoesGeodinámicaes_ES
dc.departamentoeuGeodinamikaes_ES
dc.subject.categoriaEARTH AND PLANETARY SCIENCES
dc.subject.categoriaWATER SCIENCE AND TECHNOLOGY


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