Publication:
The Impacts of Arctic Oscillation and the North Sea Caspian Pattern on the Temperature and Precipitation Regime in Turkey

dc.authorscopusid57207685341
dc.authorscopusid14013469000
dc.contributor.authorSezen, C.
dc.contributor.authorPartal, Turgay
dc.date.accessioned2020-06-21T12:19:48Z
dc.date.available2020-06-21T12:19:48Z
dc.date.issued2019
dc.departmentOndokuz Mayıs Üniversitesien_US
dc.department-temp[Sezen] Cenk, Department of Civil Engineering, Ondokuz Mayis Üniversitesi, Samsun, Turkey; [Partal] Turgay, Department of Civil Engineering, Ondokuz Mayis Üniversitesi, Samsun, Turkeyen_US
dc.description.abstractArctic oscillation (AO) and the North Sea Caspian pattern (NCP) are atmospheric teleconnections that affect climate parameters such as precipitation, temperature and stream flow. The purpose of this study is to identify the relationship of the AO and NCP with Turkey’s mean temperature and precipitation totals. First, Pearson correlation coefficients between the AO and NCP and climate data were calculated and the results were assessed using Student’s t test. Although the results vary from region to region, highly negative correlation coefficients were observed between either the NCP or AO and the temperature, especially in the winter. Furthermore, the NCP and AO have a remarkably strong relationship with winter precipitation. Second, the NCP index (NCPI) and AO index were divided into negative and positive phases; then, the impacts of both phases on the climatic data were determined as annual and seasonal. Accordingly, the annual and seasonal mean temperature values under the effect of NCP (−) and AO (−) are higher than the annual and seasonal temperature values under the effect of NCP (+) and AO (+). In this context, the temperature differences are significant, especially in winter. The precipitation amount, under the effect of positive and negative phases of global indices, was also investigated in this study. Thus, substantial results were obtained, particularly for winter precipitation in Turkey’s western regions. Finally, scatter diagrams were also prepared to examine the relationship between negative and positive phases of the AO or NCP and the temperature or precipitation. © 2019, Springer-Verlag GmbH Austria, part of Springer Nature.en_US
dc.identifier.doi10.1007/s00703-019-00665-w
dc.identifier.endpage1696en_US
dc.identifier.issn0177-7971
dc.identifier.issn1436-5065
dc.identifier.issue6en_US
dc.identifier.scopus2-s2.0-85062718447
dc.identifier.scopusqualityQ3
dc.identifier.startpage1677en_US
dc.identifier.urihttps://doi.org/10.1007/s00703-019-00665-w
dc.identifier.volume131en_US
dc.identifier.wosWOS:000495568500004
dc.identifier.wosqualityQ3
dc.language.isoenen_US
dc.publisherSpringer-Verlag Wienen_US
dc.relation.ispartofMeteorology and Atmospheric Physicsen_US
dc.relation.journalMeteorology and Atmospheric Physicsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.titleThe Impacts of Arctic Oscillation and the North Sea Caspian Pattern on the Temperature and Precipitation Regime in Turkeyen_US
dc.typeArticleen_US
dspace.entity.typePublication

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