Homogeneity Analysis of Turkish Rainfall Intensity Series
Yazarlar (2)
Doç. Dr. Utku ZEYBEKOĞLU Sinop Üniversitesi, Türkiye
Doç. Dr. Aslı Ülke Ondokuz Mayıs Üniversitesi, Türkiye
Makale Türü Açık Erişim Özgün Makale (Diğer hakemli uluslarası dergilerde yayınlanan tam makale)
Dergi Adı Sürdürülebilir Mühendislik Uygulamaları ve Teknolojik Gelişmeler Dergisi
Dergi ISSN 2651-3544
Dergi Tarandığı Indeksler Rootindexing, Eurasian Scientific Journal Index, Asos İndeks, İdeal Online, Google Scholar, ROAD, DRJI
Makale Dili İngilizce Basım Tarihi 01-2022
Kabul Tarihi 03-08-2022 Yayınlanma Tarihi 31-12-2022
Cilt / Sayı / Sayfa – / 2 / – DOI 10.51764/smutgd.1097444
Makale Linki https://doi.org/10.51764/smutgd.1097444
UAK Araştırma Alanları
Hidroloji Su Kaynakları ve Su Yapıları
Özet
In this study, homogeneity checking the annual maximum rainfall intensity series for periods ranging from 30 to 78 years were obtained from 103 stations operated by the Turkish State Meteorological Service. Absolute homogeneity tests namely Standard Normal Homogeneity Test (SNHT), Buishand Range Test (BRT), Pettitt Test (PT), and Von Neumann Ratio Test (VNRT) were applied at a confidence level of 95%. Stations were classified inhomogeneous if at least one of the standard durations data classified suspect or doubtful. Assuming that the factor destabilizing the homogeneity is the trend, a detrended methodology (DFA) was performed. After the implementation of DFA, absolute homogeneity tests were reapplied to the series of rainfall intensity. As a result of this study 49 of 103 stations called useful all 14 standard durations. 45 of the remaining 54 stations classified useful all standard durations after trend components separated from rainfall intensity series. As a result of the analysis, it was determined that the remaining 8 of 103 stations had inhomogeneous values after the trend components were separated.
Anahtar Kelimeler
BM Sürdürülebilir Kalkınma Amaçları
Atıf Sayıları
Google Scholar 1
Homogeneity Analysis of Turkish Rainfall Intensity Series

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