Basit öğe kaydını göster

dc.contributor.authorAKKEMİK, Ünal
dc.contributor.authorKopabayeva, Arailym
dc.contributor.authorMazarzhanova, Kuralay
dc.contributor.authorKÖSE, Nesibe
dc.date.accessioned2021-03-02T18:34:41Z
dc.date.available2021-03-02T18:34:41Z
dc.date.issued2020
dc.identifier.citationAKKEMİK Ü., KÖSE N., Kopabayeva A., Mazarzhanova K., "October to July precipitation reconstruction for Burabai region (Kazakhstan) since 1744", INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, cilt.64, ss.803-813, 2020
dc.identifier.issn0020-7128
dc.identifier.othervv_1032021
dc.identifier.otherav_a689debf-e50d-4790-a1d4-3e5f53eb93b1
dc.identifier.urihttp://hdl.handle.net/20.500.12627/5198
dc.identifier.urihttps://doi.org/10.1007/s00484-020-01870-8
dc.description.abstractThe history of climate is crucially important for any part of the world to understand the nature of climate change. In this context, precipitation reconstruction is still lacking in northern Kazakhstan. The purpose of this study is to present a reconstruction for the total precipitation of October of the previous year to July of the current year in northern Kazakhstan. Pinus sylvestris L. (Scots pine) forests in Burabai Region are quite important to collect samples to study the climate history. A regional chronology, covering the years of 1702-2014 of Pinus sylvestris constructed by using 289/466 trees/cores was used in the reconstruction. The gridded climate data for the years of 1950-2014 were used in the calibration and verification process. High and significant correlations were obtained between tree-ring widths and October to July precipitation in Burabai Region. Based on this significant relationship, reconstruction was performed for the years of 1744-2014. Adjusted R-2, F-value, sign test, and r value were found as 0.38, 39.7 (P <= 0.001), 47+/17, and 0.62 for reconstruction, respectively. The reconstruction showed that 43 dry and 42 wet years occurred during the years of 1744-2014. Only a one-time four-year duration of the wet period was determined covering the years 1978-1981. However, three of six very dry years occurred after the 1950s. As a conclusion, extremity in recent decades is getting an increase in Burabai region.
dc.language.isoeng
dc.subjectTarımsal Bilimler
dc.subjectAtmosfer Bilimleri ve Meteoroloji Mühendisliği
dc.subjectÇevre Mühendisliği
dc.subjectYaşam Bilimleri
dc.subjectTemel Bilimler
dc.subjectMühendislik ve Teknoloji
dc.subjectBİYOFİZİK
dc.subjectBiyoloji ve Biyokimya
dc.subjectYaşam Bilimleri (LIFE)
dc.subjectÇEVRE BİLİMLERİ
dc.subjectÇevre / Ekoloji
dc.subjectTarım ve Çevre Bilimleri (AGE)
dc.subjectMETEOROLOJİ VE ATMOSFER BİLİMLERİ
dc.subjectYerbilimleri
dc.subjectTemel Bilimler (SCI)
dc.subjectFİZYOLOJİ
dc.subjectTıp
dc.subjectSağlık Bilimleri
dc.subjectTemel Tıp Bilimleri
dc.subjectBiyofizik
dc.subjectBiyokimya
dc.subjectFizyoloji
dc.titleOctober to July precipitation reconstruction for Burabai region (Kazakhstan) since 1744
dc.typeMakale
dc.relation.journalINTERNATIONAL JOURNAL OF BIOMETEOROLOGY
dc.contributor.departmentİstanbul Üniversitesi-Cerrahpaşa , Orman Fakültesi , Orman Mühendisliği
dc.identifier.volume64
dc.identifier.issue5
dc.identifier.startpage803
dc.identifier.endpage813
dc.contributor.firstauthorID2280976


Bu öğenin dosyaları:

DosyalarBoyutBiçimGöster

Bu öğe ile ilişkili dosya yok.

Bu öğe aşağıdaki koleksiyon(lar)da görünmektedir.

Basit öğe kaydını göster