Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/38423
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dc.contributor.authorAchite, Mohammeden_UK
dc.contributor.authorTerzi, Tolga Barisen_UK
dc.contributor.authorPandey, Kusumen_UK
dc.contributor.authorJehanzaib, Muhammaden_UK
dc.contributor.authorCaloiero, Tommasoen_UK
dc.date.accessioned2026-10-31T01:00:27Z-
dc.date.available2026-10-31T01:00:27Z-
dc.date.issued2026-02-14en_UK
dc.identifier.other207en_UK
dc.identifier.urihttp://hdl.handle.net/1893/38423-
dc.description.abstractMeteorological drought is a major natural hazard in semi-arid regions, where high climate variability and strong dependence on precipitation intensify pressure on water resources and socio-economic systems. This study examined the spatiotemporal characteristics of meteorological drought in the Wadi Sly basin (northwestern Algeria) over the period 1967–2022, using long-term monthly precipitation records from seven meteorological stations. The Standardized Precipitation Index (SPI) was calculated at multiple time scales (1-, 3-, 6-, 9-, and 12-month) to characterize drought onset, severity, persistence, and temporal variability. In addition, drought severity probability and frequency analyses were conducted to evaluate the likelihood and recurrence of different drought classes. The results indicate pronounced inter-annual and decadal variability in drought conditions, with severe and prolonged drought episodes occurring during the mid-1980s, early-to-mid-1990s, and late 2010s. During these periods, SPI values frequently fell below −2.0, signifying extreme drought conditions. Spatial analysis reveals strong basin-wide synchronicity of drought events, suggesting the influence of large-scale atmospheric drivers, although localized variations in drought intensity remain evident. Overall, near-normal conditions dominate the record (accounting for approximately 60–70% of observations), while moderately dry conditions occur more frequently than moderately wet conditions at several stations. Drought characteristics exhibit strong scale dependence, with short-term droughts prevailing at shorter SPI time scales, while longer time scales emphasize drought persistence and accumulation. Overall, the findings indicate an increasing prominence of long-duration drought conditions in recent decades, as evidenced by recurrent low SPI values at longer aggregation scales. Such conditions may pose heightened risks to groundwater recharge processes and long-term water resource availability. Despite the limitations inherent in precipitation-based indices, this study provides a robust statistical framework for drought characterization and contributes valuable insights for improved drought monitoring, early warning systems, and climate-resilient water resource management in semi-arid basinsen_UK
dc.language.isoenen_UK
dc.publisherMDPI AGen_UK
dc.relationAchite M, Terzi TB, Pandey K, Jehanzaib M & Caloiero T (2026) Meteorological Drought Under Climate Variability in the Wadi Sly Basin, Algeria (1967–2022). <i>Atmosphere</i>, 17 (2), Art. No.: 207. https://doi.org/10.3390/atmos17020207en_UK
dc.rightsThis article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license.en_UK
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en_UK
dc.subjectmeteorlogical droughten_UK
dc.subjectWadi Sly basinen_UK
dc.subjectSPIen_UK
dc.subjectwater managementen_UK
dc.subjectAlgeriaen_UK
dc.titleMeteorological Drought Under Climate Variability in the Wadi Sly Basin, Algeria (1967–2022)en_UK
dc.typeJournal Articleen_UK
dc.identifier.doi10.3390/atmos17020207en_UK
dc.citation.jtitleAtmosphereen_UK
dc.citation.issn2073-4433en_UK
dc.citation.volume17en_UK
dc.citation.issue2en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusVoR - Version of Recorden_UK
dc.author.emailmuhammad.jehanzaib@stir.ac.uken_UK
dc.citation.date14/02/2026en_UK
dc.contributor.affiliationHassiba Benbouali University of Chlefen_UK
dc.contributor.affiliationKaradeniz Technical Universityen_UK
dc.contributor.affiliationGovind Ballabh Pant 'National Institute of Himalayan Environment'en_UK
dc.contributor.affiliationHanyang Universityen_UK
dc.contributor.affiliationResearch Institute for Geo-Hydrological Protectionen_UK
dc.identifier.isiWOS:001699791500001en_UK
dc.identifier.scopusid105031220441en_UK
dc.identifier.wtid2308132en_UK
dc.contributor.orcid0000-0001-6084-5759en_UK
dc.contributor.orcid0009-0003-7404-281Xen_UK
dc.contributor.orcid0009-0005-4888-6650en_UK
dc.contributor.orcid0000-0002-0393-4592en_UK
dc.date.accepted2026-02-11en_UK
dcterms.dateAccepted2026-02-11en_UK
dc.date.filedepositdate2026-10-27en_UK
rioxxterms.apcnot requireden_UK
rioxxterms.versionVoRen_UK
local.rioxx.authorAchite, Mohammed|0000-0001-6084-5759en_UK
local.rioxx.authorTerzi, Tolga Baris|0009-0003-7404-281Xen_UK
local.rioxx.authorPandey, Kusum|0009-0005-4888-6650en_UK
local.rioxx.authorJehanzaib, Muhammad|en_UK
local.rioxx.authorCaloiero, Tommaso|0000-0002-0393-4592en_UK
local.rioxx.projectInternal Project|University of Stirling|https://isni.org/isni/0000000122484331en_UK
local.rioxx.freetoreaddate2026-10-27en_UK
local.rioxx.licencehttp://creativecommons.org/licenses/by/4.0/|2026-10-27|en_UK
local.rioxx.filenameatmosphere-17-00207.pdfen_UK
local.rioxx.filecount1en_UK
local.rioxx.source2073-4433en_UK
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