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dc.contributor.authorMartínez Fernández, José 
dc.contributor.authorGonzález Zamora, Ángel 
dc.contributor.authorSánchez Martín, Nilda 
dc.contributor.authorGumuzzio, Ángela
dc.date.accessioned2025-10-02T09:40:27Z
dc.date.available2025-10-02T09:40:27Z
dc.date.issued2015
dc.identifier.citationJ. Martínez-Fernández, A. González-Zamora, N. Sánchez, A. Gumuzzio, A soil water based index as a suitable agricultural drought indicator, Journal of Hydrology, Volume 522, 2015, Pages 265-273, ISSN 0022-1694, https://doi.org/10.1016/j.jhydrol.2014.12.051. (https://www.sciencedirect.com/science/article/pii/S0022169414010622)es_ES
dc.identifier.issn0022-1694
dc.identifier.urihttp://hdl.handle.net/10366/167261
dc.description.abstract[EN]Currently, the availability of soil water databases is increasing worldwide. The presence of a growing number of long-term soil moisture networks around the world and the impressive progress of remote sensing in recent years has allowed the scientific community and, in the very next future, a diverse group of users to obtain precise and frequent soil water measurements. Therefore, it is reasonable to consider soil water observations as a potential approach for monitoring agricultural drought. In the present work, a new approach to define the soil water deficit index (SWDI) is analyzed to use a soil water series for drought monitoring. In addition, simple and accurate methods using a soil moisture series solely to obtain soil water parameters (field capacity and wilting point) needed for calculating the index are evaluated. The application of the SWDI in an agricultural area of Spain presented good results at both daily and weekly time scales when compared to two climatic water deficit indicators (average correlation coefficient, R, 0.6) and to agricultural production. The long-term minimum, the growing season minimum and the 5th percentile of the soil moisture series are good estimators (coefficient of determination, R2, 0.81) for the wilting point. The minimum of the maximum value of the growing season is the best estimator (R2, 0.91) for field capacity. The use of these types of tools for drought monitoring can aid the better management of agricultural lands and water resources, mainly under the current scenario of climate uncertainty.es_ES
dc.format.mimetypeapplication/pdf
dc.language.isoenges_ES
dc.publisherELSEVIERes_ES
dc.subjectSoil Moisturees_ES
dc.subjectDroughtes_ES
dc.subjectAvailable Water Contentes_ES
dc.subjectField Capacityes_ES
dc.subjectWilting Pointes_ES
dc.titleA soil water based index as a suitable agricultural drought indicatores_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1016/j.jhydrol.2014.12.051es_ES
dc.identifier.doi10.1016/j.jhydrol.2014.12.051
dc.relation.projectIDAYA2012-39356-C05-05es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.journal.titleJournal of Hydrologyes_ES
dc.volume.number522es_ES
dc.page.initial265es_ES
dc.page.final273es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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