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dc.contributor.authorAkkemik, Unal
dc.contributor.authorGuner, H. Tuncay
dc.contributor.authorDalfes, H. Nuzhet
dc.contributor.authorGrissino-Mayer, Henri D.
dc.contributor.authorÖzeren, Mehmet Sinan
dc.contributor.authorKındap, Tayfun
dc.contributor.authorKose, Nesibe
dc.date.accessioned2021-03-04T14:35:25Z
dc.date.available2021-03-04T14:35:25Z
dc.date.issued2013
dc.identifier.citationKose N., Akkemik U., Guner H. T. , Dalfes H. N. , Grissino-Mayer H. D. , Özeren M. S. , Kındap T., "An improved reconstruction of May-June precipitation using tree-ring data from western Turkey and its links to volcanic eruptions", INTERNATIONAL JOURNAL OF BIOMETEOROLOGY, cilt.57, sa.5, ss.691-701, 2013
dc.identifier.issn0020-7128
dc.identifier.othervv_1032021
dc.identifier.otherav_82624a01-2d7c-4049-9ad2-7408d3d814c5
dc.identifier.urihttp://hdl.handle.net/20.500.12627/88801
dc.identifier.urihttps://doi.org/10.1007/s00484-012-0595-x
dc.description.abstractWe developed a high quality reconstruction of May-June precipitation for the interior region of southwestern Turkey using regional tree-ring data calibrated with meteorological data from Burdur. In this study, three new climate sensitive black pine chronologies were built. In addition to new chronologies, four previously published black pine chronologies were used for the reconstruction. Two separate reconstructions were developed. The first reconstruction used all site chronologies over the common interval AD 1813-2004. The second reconstruction used four of the chronologies with a common interval AD 1692-2004. R (2) values of the reconstructions were 0.64 and 0.51 with RE values of 0.63 and 0.51, respectively. During the period AD 1692-1938, 41 dry and 48 wet events were found. Very dry years occurred in AD 1725, 1814, 1851, 1887, 1916, and 1923, while very wet years occurred in AD 1736, 1780, 1788, 1803, and 1892. The longest dry period was 16 years long between 1860 and 1875. We then explored relationships between the reconstructed rainfall patterns and major volcanic eruptions, and discovered that wetter than normal years occurred during or immediately after the years with the largest volcanic eruptions.
dc.language.isoeng
dc.subjectTemel Bilimler
dc.subjectMühendislik ve Teknoloji
dc.subjectÇevre Mühendisliği
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.subjectTarımsal Bilimler
dc.subjectAtmosfer Bilimleri ve Meteoroloji Mühendisliği
dc.subjectYaşam Bilimleri
dc.titleAn improved reconstruction of May-June precipitation using tree-ring data from western Turkey and its links to volcanic eruptions
dc.typeMakale
dc.relation.journalINTERNATIONAL JOURNAL OF BIOMETEOROLOGY
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume57
dc.identifier.issue5
dc.identifier.startpage691
dc.identifier.endpage701
dc.contributor.firstauthorID58821


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