Publication:
Climate change in Turkey for the last half century

dc.contributor.authorTAYANÇ, METE
dc.contributor.authorDOĞRUEL, MURAT
dc.contributor.authorsTayanc, Mete; Im, Ulas; Dogruel, Murat; Karaca, Mehmet
dc.date.accessioned2022-03-12T17:46:58Z
dc.date.accessioned2026-01-10T21:38:56Z
dc.date.available2022-03-12T17:46:58Z
dc.date.issued2009
dc.description.abstractClimate change and its urban-induced bias in selected Turkish cities is studied with a quality controlled temperature and precipitation data of Turkish stations in the period of 1950-2004. These stations are classified into two groups according to their populations; S1, including rural and suburban stations and S2, including large urban stations. Moving average signals, 365-day, and their digital low pass filtered versions are produced to eliminate the short term fluctuations and examine the possible trends or anomalies in climate data. Furthermore, 'relative difference' signals are introduced and applied to temperature and precipitation series to observe the actual local changes in the climate data independent from large-scale effects. Mann-Kendall test statistics are calculated for maximum, minimum, mean temperature and precipitation series and plotted on maps to determine any spatial trend patterns. Signal analysis show a cool period extending from early 1960s till 1993, generally with the lowest temperature values on 1992-1993 owing to the eruption of Mount Pinatubo. A last decade significant warming trend is observed in both of the series, S1 and S2, leading to 2000-2002 temperatures to be recorded as maximums in record history. The variability of urban precipitation series is generally larger than the rural ones, suggesting that urban stations can experience more frequent and severe droughts and floods. Though not significant, an increase in the urban precipitation compared to the rural one is also found. Spatial analysis resulted in significant warming in southern and southeastern parts of the country. Particularly, minimum temperature series show significant warming in almost all of the regions indicating the effect of urbanization. Significant decreases of precipitation amounts in the western parts of Turkey, such as Aegean and Trachea regions, are found. On the other hand, some Turkish northern stations show increases in precipitation of which some are significant.
dc.identifier.doi10.1007/s10584-008-9511-0
dc.identifier.eissn1573-1480
dc.identifier.issn0165-0009
dc.identifier.urihttps://hdl.handle.net/11424/229622
dc.identifier.wosWOS:000266079200016
dc.language.isoeng
dc.publisherSPRINGER
dc.relation.ispartofCLIMATIC CHANGE
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectREGIONAL CLIMATE
dc.subjectMOUNT-PINATUBO
dc.subjectTEMPERATURE
dc.subjectURBANIZATION
dc.subjectVARIABILITY
dc.subjectPATTERNS
dc.subjectERUPTION
dc.titleClimate change in Turkey for the last half century
dc.typearticle
dspace.entity.typePublication
oaire.citation.endPage502
oaire.citation.issue3-4
oaire.citation.startPage483
oaire.citation.titleCLIMATIC CHANGE
oaire.citation.volume94

Files