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Climate-Induced Vegetation Stress Detected Through Remote Sensing of Hydroclimatic Indicators

dc.contributor.authorBayazit, Esra
dc.contributor.authorKartal, Veysi
dc.contributor.authorSammen, Saad Sh.
dc.contributor.authorScholz, Miklas
dc.date.accessioned2026-10-23T18:13:30Z
dc.date.available2026-10-23T18:13:30Z
dc.date.issued2026
dc.departmentSiirt Üniversitesi
dc.description.abstractMaintaining agricultural viability and managing water resources under rising global temperatures requires understanding the complex relationship between climate variability and vegetation dynamics. This study investigated the effects of hydroclimatic variability and long-term trends on vegetation response in the Meri & ccedil;-Ergene Basin, one of T & uuml;rkiye's most agriculturally productive and climate-sensitive regions. The monthly precipitation (pr), average temperature (Tave), reference evapotranspiration (ET0), and soil moisture (SM) were analyzed for 1975-2024 while the land surface temperature (LST) and Normalized Difference Vegetation Index (NDVI) were assessed between 2001 and 2024. Seasonal anomaly analysis revealed negative SM anomalies and frequent positive anomalies in the Tave, LST, and ET0, especially in spring and summer. The NDVI anomalies were more favorable in the spring and autumn but constrained in summer. Trend analyses (ITA/IPTA) showed increasing trends in the Tave, LST, and ET0, and declining trends in the SM. Correlation results indicated strong positive ET0-LST-Tave relationships (r > 0.90) and strong negative ET0-SM correlations (as low as -0.83). The NDVI showed moderate correlations with the LST but weak associations with the pr and SM, indicating a shift toward temperature-driven vegetation behavior. The findings demonstrate that vegetation dynamics, as represented by NDVI, are progressively affected by temperature anomalies. Warming trends specifically increase evapotranspiration demand and expedite phenological processes, resulting in stronger correlations between NDVI and both Tave and LST. This transition toward temperature sensitivity signifies that vegetation greenness in the study area is increasingly influenced by thermal factors rather than being solely limited by precipitation. These findings underscore the basin's vulnerability to warming and drying, highlighting the need for climate-resilient agriculture, improved irrigation planning, and adaptive land use strategies.
dc.identifier.doi10.3390/su18052235
dc.identifier.issn2071-1050
dc.identifier.issue5
dc.identifier.orcid0000-0001-8390-0212
dc.identifier.scopus2-s2.0-105032699968
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.3390/su18052235
dc.identifier.urihttps://hdl.handle.net/20.500.12604/12018
dc.identifier.volume18
dc.identifier.wosWOS:001714560200001
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherMDPI
dc.relation.ispartofSustainability
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WOS_20261017
dc.subjectHydroclimatic Trend
dc.subjectQuality Of Life
dc.subjectClimate Change
dc.subjectNdvi
dc.subjectLst
dc.subjectVegetation Stress
dc.subjectAgricultural Resilience
dc.titleClimate-Induced Vegetation Stress Detected Through Remote Sensing of Hydroclimatic Indicators
dc.typeArticle

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