Implementing the Linear Adaptive False Discovery Rate Procedure for Spatiotemporal Trend Testing.

dc.centroFacultad de Filosofía y Letrases_ES
dc.contributor.authorGutiérrez-Hernández, Oliver
dc.contributor.authorGarcía, Luis V.
dc.date.accessioned2025-11-17T08:04:23Z
dc.date.available2025-11-17T08:04:23Z
dc.date.issued2025-11-12
dc.departamentoGeografíaes_ES
dc.description.abstractStatistical inference in spatiotemporal trend analysis often involves testing separate hypotheses for each pixel in datasets containing thousands of observations. A pixel is considered significant if its p-value falls below a rejection threshold (α). However, this uncorrected approach ignores the large number of simultaneous tests and greatly increases the risk of false positives. This issue, known as multiple testing or multiplicity, can be addressed by controlling the false discovery rate (FDR), defined as the expected proportion of false positives (i.e., false discoveries) among all rejected hypotheses, at a pre-specified control level q. This study implements the linear adaptive two-stage Benjamini–Krieger–Yekutieli (BKY) procedure for FDR control in spatiotemporal trend testing and compares it with two alternatives: the uncorrected significance approach and the original non-adaptive Benjamini–Hochberg (BH) procedure. The BKY method empirically estimates the number of true null hypotheses (m0) and adaptively relaxes the rejection threshold when many true alternatives are present, thereby increasing statistical power without compromising FDR control. Results indicate that the BKY procedure is a recommended approach for large-scale trend testing using spatiotemporal environmental data, particularly in gridded-data-intensive fields such as environmental remote sensing, climatology, and hydrology. To foster reproducibility, R code is provided to apply the BKY procedure and compare it with the uncorrected raw p-values and the BH approach on any gridded dataset.es_ES
dc.identifier.citationGutiérrez-Hernández, O., & García, L. V. (2025). Implementing the Linear Adaptive False Discovery Rate Procedure for Spatiotemporal Trend Testing. Mathematics, 13(22), 3630. https://doi.org/10.3390/math13223630es_ES
dc.identifier.doi10.3390/math13223630
dc.identifier.urihttps://hdl.handle.net/10630/40766
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.accessRightsopen accesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectGeomáticaes_ES
dc.subjectMeteorologíaes_ES
dc.subjectModelos matemáticoses_ES
dc.subjectMétodos de simulaciónes_ES
dc.subjectClimatologíaes_ES
dc.subjectTeledetecciónes_ES
dc.subjectMedio ambiente - Teledetecciónes_ES
dc.subject.otherFDR controles_ES
dc.subject.otherMultiple testinges_ES
dc.subject.otherType I errores_ES
dc.subject.otherReplicabilityes_ES
dc.subject.otherEnvironmental remote sensinges_ES
dc.subject.otherMeteorologyes_ES
dc.subject.otherHydroclimatologyes_ES
dc.subject.otherSpatiotemporal gridded dataes_ES
dc.titleImplementing the Linear Adaptive False Discovery Rate Procedure for Spatiotemporal Trend Testing.es_ES
dc.typejournal articlees_ES
dc.type.hasVersionVoRes_ES
dspace.entity.typePublication

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