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    Investigation of Trends and Nonstationarity in Hydrologic Variables in the Western Black Sea Basin, Turkey

    Source: Journal of Hydrologic Engineering:;2022:;Volume ( 027 ):;issue: 008::page 05022007
    Author:
    Hasan Zaifoglu
    ,
    A. Melih Yanmaz
    ,
    Müsteyde Baduna Koçyiğit
    DOI: 10.1061/(ASCE)HE.1943-5584.0002182
    Publisher: ASCE
    Abstract: Changes in precipitation and flow regimes may cause more catastrophic floods in the future. This study examines the trends in a subbasin of Bartin Stream in the Western Black Sea Basin, Turkey, and questions the influence of non-stationarity by performing flood frequency analyses on one stationary and nine non-stationary models by incorporating the covariates of time and annual precipitation as a linear function of their location and scale parameters. In this context, variabilities in annual precipitation, (AP), mean annual flow (MAF), and maximum daily flow (MDF), of five precipitation gauging stations and four streamflow gauging stations were examined using the Mann-Kendall and modified Mann-Kendall tests, and Sen’s slope estimator. The breakpoints were identified in the series by employing homogeneity tests, and the relative changes before and after the shifts were analyzed. The modified Mann-Kendall showed a significantly increasing trend at Bartin precipitation station, with an increase of 0.69  mm/year, and significant decreasing trends at Cide and Ulus precipitation stations, with a rate of change 7.10  mm/year and 3.26  mm/year, respectively, at the 5% significance level. Moreover, significant downward trends were detected at Kocairmak station (MAF varied 0.33  m3/s/year and MDF varied 4.55  m3/s/year); at Kocanaz station (MAF varied 0.04  m3/s/year); and at Bayiryuzu station (MDF varied 1.49  m3/s/year). The greatest relative changes in MAF and MDF were found at Kocairmak station, which can be considered as an indicator of non-stationarity. Thus, a non-stationary frequency analysis of the MDF series at Kocairmak station was performed, and the best-fitting model was found to use the AP series as a covariate, the same as other streamflow stations in the basin. In all stations, the non-stationary design flood quantiles were estimated to be greater than the stationary ones by up to 30%, which should be taken into account, particularly for designing flood mitigation facilities.
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      Investigation of Trends and Nonstationarity in Hydrologic Variables in the Western Black Sea Basin, Turkey

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4286384
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    contributor authorHasan Zaifoglu
    contributor authorA. Melih Yanmaz
    contributor authorMüsteyde Baduna Koçyiğit
    date accessioned2022-08-18T12:18:08Z
    date available2022-08-18T12:18:08Z
    date issued2022/05/17
    identifier other%28ASCE%29HE.1943-5584.0002182.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4286384
    description abstractChanges in precipitation and flow regimes may cause more catastrophic floods in the future. This study examines the trends in a subbasin of Bartin Stream in the Western Black Sea Basin, Turkey, and questions the influence of non-stationarity by performing flood frequency analyses on one stationary and nine non-stationary models by incorporating the covariates of time and annual precipitation as a linear function of their location and scale parameters. In this context, variabilities in annual precipitation, (AP), mean annual flow (MAF), and maximum daily flow (MDF), of five precipitation gauging stations and four streamflow gauging stations were examined using the Mann-Kendall and modified Mann-Kendall tests, and Sen’s slope estimator. The breakpoints were identified in the series by employing homogeneity tests, and the relative changes before and after the shifts were analyzed. The modified Mann-Kendall showed a significantly increasing trend at Bartin precipitation station, with an increase of 0.69  mm/year, and significant decreasing trends at Cide and Ulus precipitation stations, with a rate of change 7.10  mm/year and 3.26  mm/year, respectively, at the 5% significance level. Moreover, significant downward trends were detected at Kocairmak station (MAF varied 0.33  m3/s/year and MDF varied 4.55  m3/s/year); at Kocanaz station (MAF varied 0.04  m3/s/year); and at Bayiryuzu station (MDF varied 1.49  m3/s/year). The greatest relative changes in MAF and MDF were found at Kocairmak station, which can be considered as an indicator of non-stationarity. Thus, a non-stationary frequency analysis of the MDF series at Kocairmak station was performed, and the best-fitting model was found to use the AP series as a covariate, the same as other streamflow stations in the basin. In all stations, the non-stationary design flood quantiles were estimated to be greater than the stationary ones by up to 30%, which should be taken into account, particularly for designing flood mitigation facilities.
    publisherASCE
    titleInvestigation of Trends and Nonstationarity in Hydrologic Variables in the Western Black Sea Basin, Turkey
    typeJournal Article
    journal volume27
    journal issue8
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)HE.1943-5584.0002182
    journal fristpage05022007
    journal lastpage05022007-13
    page13
    treeJournal of Hydrologic Engineering:;2022:;Volume ( 027 ):;issue: 008
    contenttypeFulltext
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