Understanding run theory for evaluating hydrologic drought in the Wadi Mina Basin (Algeria): A historical analysis

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Drought is a natural disaster characterised as precipitation much lower than the precipitation reported in actual periods. Many studies characterized drought as meteorological, hydrological, agricultural, or socioeconomic. When there is a long-term shortage of precipitation, deficits in surface and ground waters occur. In this study, a hydrological drought analysis has been performed for Wadi Mina Basin (4900 km2), which is the biggest sub-basin in Cheliff Basin, using the Streamflow Drought Index (SDI) for the time scales of 3, 6, 9, and 12-month. Monthly mean streamflow records for 05 stations are obtained from the National Water Resources Agency. The obtained SDI values were subjected to Run analysis and drought duration and severity values were calculated. According to the analysis, it has been observed that the maximum (duration: 70 months, severity: 92.78) and average (duration: 31 months, severity: 31.28) droughts occurred at the Sidi AEK Djillali station on a 12-month time scale. The average drought severity was 6.34, with a maximum value of 56.71 on a monthly time scale. However, on a 12-month time scale, the average drought severity increased to 31.28, with a maximum value of 92.78. Therefore, it can be said that the drought severity has increased with the increase in the time scale. When the temporal changes of drought indices are evaluated, it is noteworthy that extraordinary droughts prevailed in the basin in 2000 and 2007. When the scatter diagrams of drought characteristics were examined, it was seen that there was a significant linear relationship between drought duration and severity. In addition, the highest correlation was observed at the 9-month time scale at Ain Hamara (R:0.964) and Oued Abtal (R:0.904) stations. In contrast, the highest correlation was observed at the 12-month time scale at Sidi AEK Djillali (R:0.980) and Takhmaret (R:0.969) stations. © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2024.

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https://rdlopen.rawdatalibrary.net/r/ebyu/11295Resmi atıflarda kullanılan kalıcı adres
DOI
https://doi.org/10.1007/s00704-024-05201-4Yayıncı resmi DOI adresi
Tam Kayıt
AlanDeğerDil
dc.contributor.authorAchite, Mohammed
dc.contributor.authorKatipoğlu, Okan Mert
dc.contributor.authorJehanzaib, Muhammad
dc.contributor.authorKartal, Veysi
dc.contributor.authorMansour, Hamidi
dc.date.accessioned2026-10-18T20:26:22.100169298Z
dc.date.available2026-10-18T20:26:22.100169298Z
dc.date.issued2024
dc.description.abstractDrought is a natural disaster characterised as precipitation much lower than the precipitation reported in actual periods. Many studies characterized drought as meteorological, hydrological, agricultural, or socioeconomic. When there is a long-term shortage of precipitation, deficits in surface and ground waters occur. In this study, a hydrological drought analysis has been performed for Wadi Mina Basin (4900 km2), which is the biggest sub-basin in Cheliff Basin, using the Streamflow Drought Index (SDI) for the time scales of 3, 6, 9, and 12-month. Monthly mean streamflow records for 05 stations are obtained from the National Water Resources Agency. The obtained SDI values were subjected to Run analysis and drought duration and severity values were calculated. According to the analysis, it has been observed that the maximum (duration: 70 months, severity: 92.78) and average (duration: 31 months, severity: 31.28) droughts occurred at the Sidi AEK Djillali station on a 12-month time scale. The average drought severity was 6.34, with a maximum value of 56.71 on a monthly time scale. However, on a 12-month time scale, the average drought severity increased to 31.28, with a maximum value of 92.78. Therefore, it can be said that the drought severity has increased with the increase in the time scale. When the temporal changes of drought indices are evaluated, it is noteworthy that extraordinary droughts prevailed in the basin in 2000 and 2007. When the scatter diagrams of drought characteristics were examined, it was seen that there was a significant linear relationship between drought duration and severity. In addition, the highest correlation was observed at the 9-month time scale at Ain Hamara (R:0.964) and Oued Abtal (R:0.904) stations. In contrast, the highest correlation was observed at the 12-month time scale at Sidi AEK Djillali (R:0.980) and Takhmaret (R:0.969) stations. © The Author(s), under exclusive licence to Springer-Verlag GmbH Austria, part of Springer Nature 2024.
dc.description.sponsorshipWe thank the National Agency of the Water Resources (ANRH) for the collected data and the General Directorate of Scientific Research and Technological Development of Algeria (DGRSDT).
dc.identifier.doi10.1007/s00704-024-05201-4
dc.identifier.eissn1434-4483
dc.identifier.endpage9688
dc.identifier.issn0177-798X
dc.identifier.issue11
dc.identifier.scopus2-s2.0-85206669986
dc.identifier.startpage9673
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/ebyu/11295
dc.identifier.volume155
dc.identifier.wosWOS:001329818200001
dc.language.isoen
dc.publisherSpringer
dc.relation.ispartofTheoretical and Applied Climatology
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectAlgeria
dc.subjectdrought
dc.subjecthistorical record
dc.subjectprecipitation (climatology)
dc.subjectstreamflow
dc.titleUnderstanding run theory for evaluating hydrologic drought in the Wadi Mina Basin (Algeria): A historical analysis
dc.typeArticle
dspace.entity.typePublication
rdl.citation.scopus10
rdl.citation.wos12
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)