Variation of temperature increase rate in the Northern Hemisphere according to latitude, longitude and altitude: the Turkey example

dc.contributor.authorSevgin, Fatih
dc.contributor.authorOzturk, Ali
dc.date.accessioned2024-12-14T22:07:20Z
dc.date.available2024-12-14T22:07:20Z
dc.date.issued2024
dc.departmentMuş Alparslan Üniversitesien_US
dc.description.abstractGlobal climate change notably influences meteorological variables such as temperature, affecting regions and countries worldwide. In this study, monthly average temperature data spanning 73 years (1950-2022) were analyzed for 28 stations in the city centers across seven regions of Turkey. The station warming rates (SWR) were calculated for selected stations and the overall country using Singular Spectrum Analysis (SSA) and Least Square Polynomial Fit (LSPF) methods. The temperature trend in Turkey exhibited a decline until the late 1970s, followed by a continuous rise due to global warming. Between 1980 and 2022, the average SWR in Turkey was found to be 0.52 degrees C/decade. The SWR was determined to be the lowest in Antakya (0.28 degrees C/decade) and the highest in Erzincan (0.69 degrees C/decade). The relationship between SWR and latitude, longitude, altitude, and distance to Null Island (D2NI) was explored through linear regression analysis. Altitude and D2NI were found to be the most significant variables, influencing the SWR. For altitude, the correlation coefficient (R) was 0.39 with a statistically significant value (p) of 0.039. For D2NI, R, and p values were 0.39 and 0.038, respectively. Furthermore, in the multiple regression analysis involving altitude and D2NI, R and p values were determined to be 0.50 and 0.029, respectively. Furthermore, the collinearity analysis indicates no collinearity between altitude and D2NI, suggesting that their effects are separated in the multiple regression.en_US
dc.identifier.doi10.1038/s41598-024-68164-6
dc.identifier.issn2045-2322
dc.identifier.issue1en_US
dc.identifier.pmid39107378
dc.identifier.scopus2-s2.0-85200462338
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1038/s41598-024-68164-6
dc.identifier.urihttps://hdl.handle.net/20.500.12639/6558
dc.identifier.volume14en_US
dc.identifier.wosWOS:001285457700077
dc.identifier.wosqualityQ1
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.indekslendigikaynakPubMed
dc.language.isoen
dc.publisherNature Portfolioen_US
dc.relation.ispartofScientific Reportsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.snmzKA_20241214
dc.subjectGlobal warmingen_US
dc.subjectAir temperatureen_US
dc.subjectSingular spectrum analysis (SSA)en_US
dc.subjectLeast square polynomial fit (LSPF)en_US
dc.titleVariation of temperature increase rate in the Northern Hemisphere according to latitude, longitude and altitude: the Turkey exampleen_US
dc.typeArticle

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