Precipitation-Driven Land Cover Dynamics in Türkiye: A Multi-Dataset Assessment Using CHIRPS, TerraClimate, and TRMM

dc.authoridhttps://orcid.org/0000-0002-7729-6650
dc.authoridhttps://orcid.org/0000-0002-9746-1772
dc.authoridhttps://orcid.org/0000-0003-2104-9746
dc.contributor.authorÇelik, Mehmet Ali
dc.contributor.authorBilik, Adile
dc.contributor.authorAkpınar, Figen
dc.contributor.authorPaşa, Yasin
dc.date.accessioned2026-09-11T13:12:26Z
dc.date.issued2026
dc.departmentMühendislik ve Mimarlık Fakültesi
dc.description.abstractThis study investigates the spatiotemporal dynamics of Land Use/Land Cover (LULC) along precipitation gradients across Türkiye by integrating high-resolution satellite-based precipitation datasets (CHIRPS, TerraClimate, and TRMM) with the European Space Agency (ESA) WorldCover (10 m) product and multi-sensor Normalized Difference Vegetation Index (NDVI) composites (Landsat, MODIS, Sentinel-2). Türkiye’s heterogeneous climate, characterized by a sharp contrast between humid coastal belts and semi-arid interiors, serves as a natural laboratory to assess ecosystem responses to moisture availability. The results reveal a systematic and non-linear transformation of LULC classes as precipitation increases. In low-rainfall zones (200–400 mm), agricultural activities and bare surfaces predominate, reflecting human-induced land management in water-constrained environments. A critical ecological threshold was identified between 400 mm and 700 mm, where grassland areas expand rapidly, becoming the dominant class. Beyond the 900 mm isohyet, forest cover exhibits a sharp increase, approaching nearly 100% dominance in regions exceeding 1200 mm, effectively displacing other LULC categories. Comparative analysis of precipitation products shows that while all datasets capture the “coastal-wet/inland-dry” pattern, TRMM tends to overestimate winter precipitation (exceeding 100 mm), whereas CHIRPS and TerraClimate provide more conservative estimates (75–80 mm). Overlay analyses between seasonal NDVI and precipitation confirm a pronounced “time-lag effect” in vegetation phenology. Despite peak precipitation occurring in winter (~75 mm), NDVI reaches its minimum (~0.03) due to thermal limitations and dormancy. Conversely, vegetation greenness peaks during the dry summer months (NDVI ~0.14 to 0.40), utilizing antecedent soil moisture stored during the spring recharge. High-resolution Sentinel-2 data proved superior in delineating micro-topographic vegetation responses compared to Landsat and MODIS. These findings provide a scientific baseline for sustainable land management and climate adaptation strategies, highlighting that precipitation thresholds are the primary determinants of Türkiye’s ecological boundaries.
dc.identifier.citationÇelik, M. A., Bilik, A., Akpınar, F., & Paşa, Y. (2026). Precipitation-Driven Land Cover Dynamics in Türkiye: A Multi-Dataset Assessment Using CHIRPS, TerraClimate, and TRMM. Earth, 7(4), 130. https://doi.org/10.3390/earth7040130
dc.identifier.doi10.3390/earth7040130
dc.identifier.issn2673-4834
dc.identifier.issue4
dc.identifier.scopus2-s2.0-105048594266
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://hdl.handle.net/11363/12583
dc.identifier.volume7
dc.indekslendigikaynakScopus
dc.institutionauthorPaşa, Yasin
dc.institutionauthoridhttps://orcid.org/0000-0003-2104-9746
dc.language.isoen
dc.publisherMultidisciplinary Digital Publishing Institute (MDPI)
dc.relation.ispartofEarth (Switzerland)
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectLULC dynamics
dc.subjectprecipitation gradients
dc.subjectNDVI
dc.subjectremote sensing
dc.subjecteco-climatology
dc.subjectTürkiye
dc.titlePrecipitation-Driven Land Cover Dynamics in Türkiye: A Multi-Dataset Assessment Using CHIRPS, TerraClimate, and TRMM
dc.typeArticle

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