The effect of the relative humidity and the specific humidity on the determination of the climate regions in Turkey

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dc.authorid0000-0002-7662-3250
dc.authorscopusid36005636900
dc.authorscopusid6603624190
dc.authorwosidSahin, Sinan/ABA-6198-2020
dc.contributor.authorŞahin, Sinan
dc.contributor.authorCığızoğlu, H. Kerem
dc.date.accessioned2022-05-11T14:26:37Z
dc.date.available2022-05-11T14:26:37Z
dc.date.issued2013
dc.departmentFakülteler, Çorlu Mühendislik Fakültesi, İnşaat Mühendisliği Bölümü
dc.description.abstractAll elements of climate that affect climatic events must be taken into account such that the climate regions are determined with exactitude. To this end, data on maximum temperature (Tx), minimum temperature (Tn), mean temperature (Tm), and precipitation (Pt) as well as local pressure (Ps), mean wind (WN), relative humidity (RH), and specific humidity (SH) have been investigated statistically and graphically. The specific humidity data calculated using Tm, Ps, and RH data and statistical comparisons have shown that there are no drawbacks to using SH in climatologic studies. According to principal component analysis, it was concluded that RH and SH should be used together with Tx, Tm, Tn, and Pt for the determination of the climate regions. Two cluster analysis methods, Ward's method and Kohonen neural network technique, were used to show the effect of RH and SH. A comparison of the cluster's stability between the limited and high number of stations shows that Ward's method and Kohonen neural network are very stable in both cases. It was also determined that RH does not change the outline of climate regions but that it affects the zones of climate transition. It was observed that clusters determined by using Tm, Pt, and RH provide relatively more distinctive clusters in the data space than clusters determined by using Tm, Pt, and SH.
dc.identifier.doi10.1007/s00704-012-0743-6
dc.identifier.endpage481
dc.identifier.issn0177-798X
dc.identifier.issn1434-4483
dc.identifier.issue45385en_US
dc.identifier.scopus2-s2.0-84876445448
dc.identifier.scopusqualityQ2
dc.identifier.startpage469
dc.identifier.urihttps://doi.org/10.1007/s00704-012-0743-6
dc.identifier.urihttps://hdl.handle.net/20.500.11776/6516
dc.identifier.volume112
dc.identifier.wosWOS:000318246300010
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorŞahin, Sinan
dc.language.isoen
dc.publisherSpringer Wien
dc.relation.ispartofTheoretical and Applied Climatology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectNorth-Atlantic Oscillation
dc.subjectRainfall Variations
dc.subjectPrecipitation
dc.subjectVariability
dc.titleThe effect of the relative humidity and the specific humidity on the determination of the climate regions in Turkey
dc.typeArticle

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