Impact of Long-Term Drought on Surface Water and Water Balance Variations in Iran: Insights from Highland and Lowland Regions

dc.contributor.authorKazemi Garajeh, Mohammad
dc.contributor.authorAbdoli, Nastaran
dc.contributor.authorSeyedebrahimi, Ebrahim
dc.contributor.authorNaboureh, Amin
dc.contributor.authorKurdpour, Iamn
dc.contributor.authorBakhshi Lomer
dc.contributor.authorAmir Reza
dc.contributor.authorSadeqi, Amin
dc.contributor.authorMirzaei, Saham
dc.contributor.organizationfi=maantiede|en=Geography |
dc.contributor.organization-code1.2.246.10.2458963.20.17647764921
dc.converis.publication-id458267379
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/458267379
dc.date.accessioned2025-08-28T00:45:32Z
dc.date.available2025-08-28T00:45:32Z
dc.description.abstract<p>Droughts have a significant impact on surface water resources, especially in arid and semi-arid regions. Computational and data handling limitations have constrained previous time-series analyses. However, advances in cloud computing services and remote sensing technology allow for a more detailed examination. This study integrates multi-source satellite-derived data with a cloud computing platform to assess the impact of long-term drought on surface water and water balance in Iran from 2000 to 2021. Given the varying effects of drought on highlands and lowlands, the analysis was conducted at three levels: the entire country, the highlands, and the lowlands. The results of this study reveal imbalances between water balance from 2000 to 2021, with notable disparities observed during 2000–2007, 2009–2014, and 2016–2019. The results also show varying drought trends (e.g., −1.22 in 2000 and −0.73 in 2021), with severe conditions captured in 2008 (SPI: −1.92). Additionally, our analysis illustrated that lowlands were more impacted by droughts compared to highlands. Long-term drought and permanent surface water had correlation values of 0.33 across the country, 0.33 in the highlands, and 0.31 in the lowlands. For seasonal surface water, coefficients were 0.18 for the entire country, 0.16 for the highlands, and 0.18 for the lowlands. Overall, long-term drought had minimal effect on reducing surface water. These findings show that drought is only part of the explanation for the decrease in surface water resources.</p>
dc.identifier.eissn2072-4292
dc.identifier.olddbid206346
dc.identifier.oldhandle10024/189373
dc.identifier.urihttps://www.utupub.fi/handle/11111/45530
dc.identifier.urlhttps://www.mdpi.com/2072-4292/16/19/3636
dc.identifier.urnURN:NBN:fi-fe2025082787324
dc.language.isoen
dc.okm.affiliatedauthorSadeqi, Amin
dc.okm.discipline1172 Environmental sciencesen_GB
dc.okm.discipline1172 Ympäristötiedefi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherMDPI
dc.publisher.countrySwitzerlanden_GB
dc.publisher.countrySveitsifi_FI
dc.publisher.country-codeCH
dc.relation.articlenumber3636
dc.relation.doi10.3390/rs16193636
dc.relation.ispartofjournalRemote Sensing
dc.relation.issue19
dc.relation.volume16
dc.source.identifierhttps://www.utupub.fi/handle/10024/189373
dc.titleImpact of Long-Term Drought on Surface Water and Water Balance Variations in Iran: Insights from Highland and Lowland Regions
dc.year.issued2024

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