نمایش مختصر رکورد

dc.contributor.authormalekian, A.en_US
dc.contributor.authorzinati, T.en_US
dc.contributor.authorKhalighi Sigaroudi, SH.en_US
dc.date.accessioned1399-07-09T11:00:14Zfa_IR
dc.date.accessioned2020-09-30T11:00:14Z
dc.date.available1399-07-09T11:00:14Zfa_IR
dc.date.available2020-09-30T11:00:14Z
dc.date.issued2009-11-01en_US
dc.date.issued1388-08-10fa_IR
dc.date.submitted2015-10-28en_US
dc.date.submitted1394-08-06fa_IR
dc.identifier.citationmalekian, A., zinati, T., Khalighi Sigaroudi, SH.. (2009). Statistical model of daily flow in arid and semi arid regions. Desert, 14(1), 53-62. doi: 10.22059/jdesert.2010.21747en_US
dc.identifier.issn2008-0875
dc.identifier.issn475-2345X
dc.identifier.urihttps://dx.doi.org/10.22059/jdesert.2010.21747
dc.identifier.urihttps://jdesert.ut.ac.ir/article_21747.html
dc.identifier.urihttps://iranjournals.nlai.ir/handle/123456789/393059
dc.description.abstractAbstract <br /> <br /> Stochastic model for synthetic data generation is not available for daily flows of intermittent streams. Such a model is required in the planning and operation of structures on an intermittent stream for purposes where short time flow fluctuations are important. In this study a model is developed for such a case. The model consists of four steps: determination of the days on which flow occurs, determination of the days on which a flow increment occurs, determination of the magnitude of the flow increment, and calculation of the flow decrement on days when the flow is reduced. The first two steps are modeled by Markov chain. In the third step, flow increments on the rising limb of the hydrograph are assumed to be gamma distributed. In the last step an exponential recession is used with two different coefficients. Parameters of the model are estimated from the observed daily stream flow data for each month of the year. The model is applied to a daily flow series of 20 years' length. It is seen that the model can preserve the short-term characteristics (The ascension and recession curves and peaks) of the hydrograph in addition to the long-term characteristics (mean, variance, skew ness, and zero flow percentage).en_US
dc.format.extent711
dc.format.mimetypeapplication/pdf
dc.languageEnglish
dc.language.isoen_US
dc.publisherUniversity of Tehranen_US
dc.relation.ispartofDeserten_US
dc.relation.isversionofhttps://dx.doi.org/10.22059/jdesert.2010.21747
dc.subjectDaily Flowsen_US
dc.subjectFiroozabad Basinen_US
dc.subjectHydrographen_US
dc.subjectIranen_US
dc.subjectKermanen_US
dc.subjectMarkov Chainsen_US
dc.subjectStochastic Modelingen_US
dc.titleStatistical model of daily flow in arid and semi arid regionsen_US
dc.typeTexten_US
dc.contributor.departmentInternational Research Center for Living with Desert, University of Tehranen_US
dc.contributor.departmentM. Sc. Graduate, University of Tehranen_US
dc.contributor.departmentFaculty of Natural Resources, University of Tehranen_US
dc.citation.volume14
dc.citation.issue1
dc.citation.spage53
dc.citation.epage62


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