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Eurasian Journal of Mathematical and Computer Applications, 2018, Volume 6, Issue 3, Pages 34–44
DOI: https://doi.org/10.32523/2306-6172-2018-6-3-34-44 (Mi ejmca117) 		 
Stochastic model for calculation of maximum flood stage in Charysh river using the data of annual winter precipitation

V. P. Galakhova, O. V. Lovtskayaa, E. V. Mardasovab

a Institute for Water and Environmental Problems, Siberian Branch of the Russian Academy of Sciences (IWEP SB RAS), 1, Molodezhnaya St., Barnaul, 656038, Altai Krai, Russian Federation
b Altai State University,Altai Krai, Russian Federation, 61, Lenina av., Barnaul, 656049, Altai Krai, Russian Federation
Full-text PDF (9195 kB)
DOI: https://doi.org/10.32523/2306-6172-2018-6-3-34-44
Abstract: Using the mountain watershed of Charysh river as an example, a methodology for calculating maximum stage during the snowmelt period is considered. Maximum stage occurred due to the ice jams is not considered.
Keywords: Charysh river, flood, snowmelt period, maximum stage.
Funding agency Grant number
Russian Foundation for Basic Research 18-05-00007
18-45-220006
The research is carried out with a financial support from the RFBR (grants 18-05-00007, 18-45-220006).
Bibliographic databases:
Document Type: Article
MSC: 86A05, 62H20.
Language: English
Citation: V. P. Galakhov, O. V. Lovtskaya, E. V. Mardasova, “Stochastic model for calculation of maximum flood stage in Charysh river using the data of annual winter precipitation”, Eurasian Journal of Mathematical and Computer Applications, 6:3 (2018), 34–44
Citation in format AMSBIB
\Bibitem{GalLovMar18}
\by V.~P.~Galakhov, O.~V.~Lovtskaya, E.~V.~Mardasova
\paper Stochastic model for calculation of maximum flood stage in Charysh river using the data of annual winter precipitation
\jour Eurasian Journal of Mathematical and Computer Applications
\yr 2018
\vol 6
\issue 3
\pages 34--44
\mathnet{http://mi.mathnet.ru/ejmca117}
\crossref{https://doi.org/10.32523/2306-6172-2018-6-3-34-44}
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\scopus{https://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85055731190}
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