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dc.creatorStojković, Milan
dc.creatorProhaska, Stevan
dc.creatorPlavšić, Jasna
dc.date.accessioned2019-04-19T14:22:44Z
dc.date.available2019-04-19T14:22:44Z
dc.date.issued2014
dc.identifier.issn2217-5547
dc.identifier.urihttp://grafar.grf.bg.ac.rs/handle/123456789/642
dc.description.abstractThe internal structure of hydrologic processes is discussed in the paper. Time series of mean annual river discharges are assessed to determine their stationarity, trend and periodicity. The time series of annual discharges are determined to be non-stationary. The trend varies in different time segments, with changing trend intensity and direction. Hurst analysis shows that the time series of annual discharges have a long memory. Long-term periodicity of annual time series is considered, while macroperiods are determined and classified into four groups of mean values: 9.5, 13.5, 22.5 and 31.5 years. Secondary microperiodicity is found to exist in the interval from 3.6 to 4.9 years.en
dc.publisherSerbian Water Pollution Control Society, Belgrade
dc.relationinfo:eu-repo/grantAgreement/MESTD/Technological Development (TD or TR)/37005/RS//
dc.rightsopenAccess
dc.sourceWater research and management
dc.subjectmulti-temporal trend analysisen
dc.subjectMann-Kendall trend testen
dc.subjectmacroperiodicityen
dc.subjectBlackman-Tukey methoden
dc.titleInternal stochastic structure of annual discharge time series of Serbia’s large riversen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage13
dc.citation.issue2
dc.citation.other4(2): 3-13
dc.citation.rankM51
dc.citation.spage3
dc.citation.volume4
dc.identifier.rcubconv_694
dc.type.versionpublishedVersion


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