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For ungauged rivers, when there are no hydrological measurements and there is a lack of data on perennial flow rates, the latter one to be determined based on other hydrological data. The river Suhareka catchment represents a similar case. Since there is no data on Suhareka’s flow rates, the authors of this study aimed for the flow rate determination based on rainfall measurements. From the available data on annual precipitation (monthly sums) provided by the Kosovo Hydrometeorological Institute for the Suhareka hydrometric station, the observed monthly rainfall data for 30 years were analysed. Those gaps were initially filled by connecting the hydrometric station in Suhareka with those of Prishtina, Prizren and Ferizaj, and as a result a fairly good fit was ensured. Moreover, the intensity-duration-frequency curves were formed using the expression of Sokolovsky, as a mathematical model of the dependence I (T, P). For a transformation of rainfall into flow, the American method SCS was used. As a result, the equation for the Suhareka River basin was derived, which enabled the determination of maximum inflows, for different return periods. The results obtained through this paper, indicates that even for ungauged river basins the peak flows can be determined from available rainfall data.
Czasopismo
Rocznik
Tom
Strony
110--121
Opis fizyczny
Bibliogr. 12 poz., rys., tab.
Twórcy
autor
- Faculty of Civil Engineering, University of Pristina, Kosovo
autor
- Faculty of Civil Engineering, University of Pristina, Kosovo
autor
- Faculty of Civil Engineering, University of Pristina, Kosovo
autor
- Faculty of Civil Engineering, University of Pristina, Kosovo
Bibliografia
- 1. Baoyan L., Wang D., Fu S., Cao W. 2017. Estimation of peak flow rates for small drainage areas. Water Resources Management, 1635–1647.
- 2. Kolbjorn E., Alfredsen K. 2020. Hydrology and water resources management in a changing world. Hydrology Research, 143–145.
- 3. McMillan H., Westerberg I.K., Krueger T. 2018. Hydrological data uncertainty and its implications. Wiley Interdisciplinary Reviews Water. https://doi.org/10.3390/w10111669
- 4. Nam K.W., Shin M.J. 2018. Estimation of peak flow in ungauged catchments using relationship between runoff coefficient and curve number. Water.
- 5. Nearing G.S., Gupta H.V., Clark M.P., Tian Y., Harrison K.W., Weijs S.V. 2016. A philosophical basis for hydrological uncertainty. Hydrological Sciences Journal, 1666–1678.
- 6. Maniak U. 2010. Hydrologie und Wasserwirtschaft’; Eine einführung für Ingenieure, 6. neu bearbeitete Auflage. TU Braunschweig.
- 7. Ven T.C. 1962. Hydrologic determination of waterway areas for the design of drainage structures in small drainage basins. University of Illinois at Urbana-Champaign.
- 8. Husno H. 2007. Inẑenjerska Hidrologija. Sarajevo.
- 9. Babac P. 2006. Osnovi Hidrotehnike u šumarstvu primeri iz teorije i prakse. Beograd.
- 10. KHMI. 1984. Hydromeorological yearbooks of Kosovo 1954–1983.
- 11. Bektesh B. 2005. Statistika elementare Prishtinë.
- 12. Karakuş C. 2020. Istatistiksel analiz, olasɪlɪk ve rassal deǧişkenler.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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