THE EFFECT OF CLIMATE ON RADIAL GROWTH OF SCOTS PINE (Pinus sylvestris L.) IN A COASTAL MIXED STAND IN KAPISUYU, BARTIN, TURKEY

dc.contributor.authorÖzel, Halil Barış
dc.contributor.authorYaman, Barbaros
dc.contributor.authorVarol, Tuğrul
dc.contributor.authorVarol, Tuğrul
dc.contributor.authorÖzel, Halil Barış
dc.contributor.authorYaman, Barbaros
dc.date.accessioned2025-10-18T09:58:40Z
dc.date.created2021
dc.date.issued2021
dc.departmentFakülteler, Orman Fakültesi, Orman Endüstri Mühendisliği Bölümü
dc.departmentFakülteler, Orman Fakültesi, Orman Mühendisliği Bölümü
dc.description.abstractScots pine is geographically the most widespread pine species in the world, and it shows different growth responses to climate and environmental factors in diverse ecological sites. We studied both the stand dynamics and climate-growth relationships of Scots pine in isolated coastal stand (recently found) in the Western Black Sea Region of Turkey. The homogeneity index of this stand has varied between 1.92-3.56. In growth-ring analyses, after cross-dating of individual chronologies, COFECHA and ARSTAN software were used respectively for chronology quality control and standardization (detrend). In this way, a 58-year-long chronology (1959-2016) of Scots pine was constructed. In addition, DENDROCLIM software was used for investigating Scots pine's radial growth-climate relationships. Mean sensitivity changed from 0.163 to 0.331, with a mean of 0.183. Mean correlation among trees and signal to noise ratio were 0.389 and 7.012 respectively. In terms of the effect of precipitation on the radial growth of Scots pine in this site, the correlation coefficients were 0.43 (p<0.05) for December of the previous year and 0.41 (p<0.05) for July of the current year. For all the other months, precipitation had a non-significant effect. As for the maximum and mean air temperature, the correlation coefficients were 0.36 (p<0.05) and 0.40 (p<0.05) for February, and 0.40 (p<0.05) and 0.42 (p<0.05) for March, respectively. I Iowever, on the radial growth, while the maximum temperature in August had a negative effect (r= -0.26; p<0.05), minimum temperatures in February, March and July had a positive effect (r= 0.39, 0.40 and 0.34 respectively; p<0.05). It means while higher rains in July and higher temperatures in the late winter-early spring have caused the wider growth rings, the narrower growth rings have been formed in the years with higher maximum temperatures in August in the isolated coastal site of Scots pine.
dc.identifier.doi10.20886/ijfr.2021.8.2.187-197
dc.identifier.endpage197
dc.identifier.issn2355-7079
dc.identifier.issn2406-8195
dc.identifier.issue2
dc.identifier.orcidOZEL, Halil Baris/0000-0001-9518-3281
dc.identifier.scopus2-s2.0-85119178059
dc.identifier.scopusqualityQ4
dc.identifier.startpage187
dc.identifier.urihttps://doi.org/10.20886/ijfr.2021.8.2.187-197
dc.identifier.urihttps://hdl.handle.net/11772/19807
dc.identifier.volume8
dc.identifier.wosWOS:000713969000005
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherMinistry Environment & Forestry
dc.relation.ispartofIndonesian Journal of Forestry Research
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzWoS_20251016
dc.subjectClimate
dc.subjectHomogeneity Index
dc.subjectScots Pine
dc.subjectStand Dynamics
dc.subjectTree-Ring
dc.titleTHE EFFECT OF CLIMATE ON RADIAL GROWTH OF SCOTS PINE (Pinus sylvestris L.) IN A COASTAL MIXED STAND IN KAPISUYU, BARTIN, TURKEY
dc.typeArticle
dspace.entity.typePublication
relation.isAuthorOfPublication5c514123-1af3-473c-bb7e-e407592706f0
relation.isAuthorOfPublication24fb5839-125b-4241-9106-db7266b40340
relation.isAuthorOfPublication5115f1b0-2078-47f0-a522-d643e92b6629
relation.isAuthorOfPublication.latestForDiscovery5c514123-1af3-473c-bb7e-e407592706f0

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