dc.contributor.author | Zabaleta Lopetegui, Ane | |
dc.contributor.author | Antigüedad Auzmendi, Ignacio | |
dc.date.accessioned | 2014-02-07T17:18:01Z | |
dc.date.available | 2014-02-07T17:18:01Z | |
dc.date.issued | 2013 | |
dc.identifier.citation | Hydrology and Earth System Sciences 17(1) : 211-223 (2013) | es |
dc.identifier.issn | 1027-5606 | |
dc.identifier.uri | http://hdl.handle.net/10810/11386 | |
dc.description.abstract | The 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.sponsorship | The 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.iso | eng | es |
dc.publisher | Copernicus Gesellschaft | es |
dc.rights | info:eu-repo/semantics/openAccess | es |
dc.subject | coefficients | es |
dc.subject | cross spectral analysis | es |
dc.subject | runoff generation processes | es |
dc.subject | soil moisture | es |
dc.subject | hydrological systems | es |
dc.subject | time series | es |
dc.subject | hydrograph separation | es |
dc.subject | auto-correlation | es |
dc.subject | peak discharge | es |
dc.subject | storm flow | es |
dc.title | Streamflow response of a small forested catchment on different timescales | es |
dc.type | info:eu-repo/semantics/article | es |
dc.rights.holder | © Author(s) 2013. This work is distributed
under the Creative Commons Attribution 3.0 License. | es |
dc.relation.publisherversion | http://www.hydrol-earth-syst-sci.net/17/211/2013/hess-17-211-2013.html | es |
dc.identifier.doi | 10.5194/hess-17-211-2013 | |
dc.departamentoes | Geodinámica | es_ES |
dc.departamentoeu | Geodinamika | es_ES |
dc.subject.categoria | EARTH AND PLANETARY SCIENCES | |
dc.subject.categoria | WATER SCIENCE AND TECHNOLOGY | |