Priestly-Taylor Coefficient Evaluation for Konya Closed Basin

dc.authoridhttps://orcid.org/0000-0003-3632-2725en_US
dc.authoridhttps://orcid.org/0000-0002-5229-4018en_US
dc.authorscopusid36728602600en_US
dc.authorwosidG-2829-2015en_US
dc.contributor.authorCicibıyık, Alara
dc.contributor.authorŞarlak, Nermin
dc.contributor.authorÜstün, Deniz
dc.date.accessioned2024-07-31T10:39:40Z
dc.date.available2024-07-31T10:39:40Z
dc.date.issued2024en_US
dc.departmentFakülteler, Mühendislik Fakültesi, Bilgisayar Mühendisliği Bölümüen_US
dc.description.abstractMeasurement of evaporation in the field is difficult and expensive; thus, the empirical evaporation estimation methods have been developed. However, these estimation methods have both advantages and disadvantages. The main disadvantage is that their coefficients were determined by the climatic conditions of the study areas. One of these methods is Penman. The Penman method, accepted as a reference, has reached the closest estimations to the measurement of evaporation in the field of the different parts of the world. However, it needs lots of measured climatic data. The Priestley-Taylor method was derived to reduce the measured data needs of the Penman method. Priestly and Taylor represented the variables such as saturated and actual vapor pressures and wind speed with coefficient of 1.26. The researchers have continued to study on the calibration of the  coefficient for their studies’ area since this method has been known to underestimate evaporation value in areas where advection is effective. The present study consists of two stages. First, evaporation was tried to be estimated with these two methods by using the measured climatic data of five meteorological stations in the Konya Closed Basin. Estimated values were evaluated making comparison with the pan measurements. Although slightly higher values were estimated from the pan measurements with each method, the Penman method was found to be relatively more consistent on the basis of statistical indicators. Second,  coefficient was obtained as 1.28 for the study area by using three artificial intelligence-based optimization algorithms. The Penman method was used for comparison in this stage. It was concluded that there was no need for any calibration of the  coefficient and the original one was found to be valid for the study area as well.en_US
dc.identifier.citationCicibıyık, A., Şarlak, N., ve Üstün, D. (2024). Priestly-Taylor Coefficient Evaluation for Konya Closed Basin. Bilecik Şeyh Edebali Üniversitesi Fen Bilimleri Dergisi, 11(1), 26-36. Erişim adresi: https://doi.org/10.35193/bseufbd.1209924en_US
dc.identifier.endpage36en_US
dc.identifier.issue1en_US
dc.identifier.startpage26en_US
dc.identifier.urihttps://dergipark.org.tr/en/download/article-file/2793773
dc.identifier.urihttps://hdl.handle.net/20.500.13099/302
dc.identifier.volume11en_US
dc.institutionauthorÜstün, Deniz
dc.language.isoengen_US
dc.publisherBilecik Şeyh Edebali Üniversitesien_US
dc.relation.ispartofBilecik Şeyh Edebali Üniversitesi Fen Bilimleri Dergisien_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectPenmanen_US
dc.subjectPriestly-Tayloren_US
dc.subjectEvaporationen_US
dc.titlePriestly-Taylor Coefficient Evaluation for Konya Closed Basinen_US
dc.title.alternativeKonya Kapalı Havzası için Priestly-Taylor Katsayısı Değerlendirmesien_US
dc.typearticleen_US

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