Intensity-Duration-Frequency Curves for Manicaragua city, Cuba

dc.contributor.affiliationUniversidad de Las Americas - Chile
dc.contributor.authorLopez Ferraz, Roberto Luis
dc.contributor.authorCastillo García, Carlos Lázaro
dc.contributor.authorDominguez Hurtado, Ismabel
dc.contributor.authorSolis, Jose Alejandro
dc.contributor.authorGonzález Rodríguez, Lisdelys
dc.date.accessioned2025-04-21T20:07:58Z
dc.date.available2025-04-21T20:07:58Z
dc.date.issued2024-06-26
dc.description.abstractThe Intensity-Duration-Frequency (IDF) curves are a way to visualize and represent extreme hydrometeorological rainfall events. In this article, an analysis of convective rainfall events recorded at the La Piedra Meteorological Station, Villa Clara, Cuba, was conducted. To develop IDF curves, the 2006- 2019 time series was analyzed. A partial duration series was generated, including intervals from 20 minutes to 4320 minutes, subjected to an outlier detection process. The series was divided into two categories: one for durations ≤ 720 minutes and another for durations > 720 minutes. The resulting series underwent nonparametric tests to assess their independence, randomness, homogeneity, and seasonality. Subsequently, they were fitted to the Generalized Pareto probability distribution and to a parametric equation of the Montana model, and then the curves were plotted for return periods of 10, 50 and 100. The Montana model led to obtaining correlation coefficients greater than 0.90 compared to the other methods used, significantly improving the quality of the fit in both categories. This research provides information to understand and plan the management of intense climatic phenomena and adequate risk management in an area where such studies are lacking, facilitating access to crucial data essential in the design and execution of hydraulic engineering projects in the region.
dc.description.sponsorshipThe authors would like to express their sincere gratitude to the Provincial Meteorological Center of Villa Clara for their invaluable collaboration in the development of this research. The support provided has been exceptional and deserves spe-cial recognition.
dc.format.mimetypeapplication/pdf
dc.identifier.citationENFOQUE UTE, 15(3), 49-58. https://doi.org/10.29019/enfoqueute.1046
dc.identifier.doihttps://doi.org/10.29019/enfoqueute.1046
dc.identifier.issn1390-9363
dc.identifier.orcidhttps://orcid.org/0009-0001-4756-6496
dc.identifier.orcidhttps://orcid.org/0000-0002-6430-2775
dc.identifier.orcidhttps://orcid.org/0000-0002-7841-8031
dc.identifier.orcidhttps://orcid.org/0009-0003-4777-605X
dc.identifier.orcidhttps://orcid.org/0000-0002-7892-4604
dc.identifier.researcheridJYQ-0867-2024
dc.identifier.researcheridNRY-8569-2025
dc.identifier.rorhttps://ror.org/0166e9x11
dc.identifier.urihttps://repositorio.udla.cl/handle/udla/1738
dc.language.isoeng
dc.publisherUniversidad UTE
dc.relation.isindexedbyWeb of Science
dc.relation.issn1390-9363
dc.rightsCreative Commons Attribution 3.0 International
dc.rights.accessrightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/
dc.sourceENFOQUE UTE
dc.source.urihttps://doi.org/10.29019/enfoqueute.1046
dc.subjectpartial duration series
dc.subjectrainfall intensity
dc.subjectthreshold
dc.subjectcurves
dc.subject.lcshCurvas
dc.titleIntensity-Duration-Frequency Curves for Manicaragua city, Cuba
dc.typejournal article
dc.type.coarhttp://purl.org/coar/resource_type/c_6501
dc.type.driverinfo:eu-repo/semantics/article
oaire.citation.endPage58
oaire.citation.issue3
oaire.citation.startPage49
oaire.citation.titleENFOQUE UTE
oaire.citation.volume15
udla.curacion.controljmvg
udla.oecd.area1 Ciencias Naturales
udla.oecd.discipline1.1.3 Estadísticas y Probabilidades
udla.oecd.subarea1.1 Matemáticas

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