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Intra-Annual Course of Canopy Parameters and Phenological Patterns for a Mixed and Diverse Deciduous Forest Ecosystem Along the Altitudinal Gradients Within a Dam Reservoir Landscape

dc.contributor.authorÖztürk, Melih
dc.contributor.authorBiricik, Turgay
dc.contributor.authorAğlarcı, Ali Vasfi
dc.date.accessioned2026-01-04T21:58:32Z
dc.date.issued2025-05-04
dc.description.abstractWithin a dam reservoir landscape in the Western Black Sea Region of Türkiye, a dense young-mature stand composed diversely of oriental beeches, European hornbeams, sessile oaks, and silver lindens was chosen as a study field to analyze canopy parameters and to determine phenological patterns along the altitudinal gradients. Referring to the air-soil temperature and precipitation data, intra-annual eco-physiological characteristics of that stand tree canopies, were aimed to be determined regarding those altitudinal gradients. For each of the 10 altitudinal gradients, the mixed deciduous stand canopy physiological characteristics were analyzed by hemispherical photographing. Canopy parameters were acquired from those digital hemispherical photographs, which were confirmed with secondary LAI data from the LAI-2200C. Leaf Area Index, Light Transmission, Canopy Openness, and Gap Fraction were obtained during a total of 21 study field visits throughout the monitoring year. Beginning from a theoretical leafless stage with 0.51 m2 m−2, average LAI increased to 0.89 m2 m−2 during budburst stage, and then gradually up to 3.60 m2 m−2 during climax leaf period, and then to 1.38 m2 m−2 during senescence period, and gradually down to 0.50 m2 m−2 during the next theoretical leafless stage. However, average LT (64%, 61%, 9%, 36%, 74%), CO (65%, 62%, 9%, 37%, 75%), and GF (18%, 14%, 1%, 8%, 14%) followed opposite patterns. Though no apparent trend was valid for those canopy parameters from the lowest to the highest altitudinal gradient, their obvious intra-annual patterns emerged as compatible with the annual air-soil temperature data course.
dc.description.urihttps://doi.org/10.3390/d17050331
dc.description.urihttps://doaj.org/article/d47e9c94039c4245989e5b3b49367557
dc.description.urihttps://hdl.handle.net/11772/20148
dc.identifier.doi10.3390/d17050331
dc.identifier.eissn1424-2818
dc.identifier.openairedoi_dedup___::03f605d9feb71bef1e42df32d3e3f083
dc.identifier.orcid0000-0001-8745-386x
dc.identifier.scopus2-s2.0-105006562945
dc.identifier.startpage331
dc.identifier.urihttps://hdl.handle.net/20.500.12597/42660
dc.identifier.volume17
dc.language.isoeng
dc.publisherMDPI AG
dc.relation.ispartofDiversity
dc.rightsOPEN
dc.subjectAir-Soil Temperature
dc.subjectlandscape ecology
dc.subjectTree Eco-Physiology
dc.subjectQH301-705.5
dc.subjectelevation zones
dc.subjectPr & Uuml
dc.subjectK & Ouml
dc.subjectLandscape Ecology
dc.subjectTree Diversity
dc.subjectKirazl & Imath
dc.subjectLai
dc.subjectLAI
dc.subjectair-soil temperature
dc.subjectDam Watershed
dc.subjecttree diversity
dc.subjecttree eco-physiology
dc.subjectElevation Zones
dc.subjectBiology (General)
dc.titleIntra-Annual Course of Canopy Parameters and Phenological Patterns for a Mixed and Diverse Deciduous Forest Ecosystem Along the Altitudinal Gradients Within a Dam Reservoir Landscape
dc.typeArticle
dspace.entity.typePublication
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Referring to the air-soil temperature and precipitation data, intra-annual eco-physiological characteristics of that stand tree canopies, were aimed to be determined regarding those altitudinal gradients. For each of the 10 altitudinal gradients, the mixed deciduous stand canopy physiological characteristics were analyzed by hemispherical photographing. Canopy parameters were acquired from those digital hemispherical photographs, which were confirmed with secondary LAI data from the LAI-2200C. Leaf Area Index, Light Transmission, Canopy Openness, and Gap Fraction were obtained during a total of 21 study field visits throughout the monitoring year. Beginning from a theoretical leafless stage with 0.51 m2 m−2, average LAI increased to 0.89 m2 m−2 during budburst stage, and then gradually up to 3.60 m2 m−2 during climax leaf period, and then to 1.38 m2 m−2 during senescence period, and gradually down to 0.50 m2 m−2 during the next theoretical leafless stage. 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