Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments

While determining theoretical flood hydrographs, different methods of their construction are used depending on the needs of the problem or the scope of the project. It should be remembered that these methods differ mainly with the principle of the waveform averaging, which may be done either accordi...

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Main Authors: Gądek Wiesław, Tokarczyk Tamara, Środula Arkadiusz
Format: Article
Language:English
Published: Sciendo 2016-12-01
Series:Journal of Water and Land Development
Subjects:
Online Access:http://www.degruyter.com/view/j/jwld.2016.31.issue-1/jwld-2016-0035/jwld-2016-0035.xml?format=INT
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spelling doaj-0c09d270367844be98814266078551ce2020-11-24T21:35:07ZengSciendoJournal of Water and Land Development2083-45352016-12-01311435110.1515/jwld-2016-0035jwld-2016-0035Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchmentsGądek WiesławTokarczyk TamaraŚrodula ArkadiuszWhile determining theoretical flood hydrographs, different methods of their construction are used depending on the needs of the problem or the scope of the project. It should be remembered that these methods differ mainly with the principle of the waveform averaging, which may be done either according to the flow or time. The hydrographs may be divided into nonparametric (determining on the basis of registered floods) and parametric (using mathematical description of the flood course). One of the analytical methods is Strupczewski method which has two parameters: responsible for the waveform and specifies the base flow, the flow above which values of hydrograph are calculated. The functional description uses the Pearson type III density distribution.http://www.degruyter.com/view/j/jwld.2016.31.issue-1/jwld-2016-0035/jwld-2016-0035.xml?format=INTanalytical flood hydrographnonparametric hydrographparametric hydrographStrupczewski methodthe Cracow methodtypical hydrograph
collection DOAJ
language English
format Article
sources DOAJ
author Gądek Wiesław
Tokarczyk Tamara
Środula Arkadiusz
spellingShingle Gądek Wiesław
Tokarczyk Tamara
Środula Arkadiusz
Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
Journal of Water and Land Development
analytical flood hydrograph
nonparametric hydrograph
parametric hydrograph
Strupczewski method
the Cracow method
typical hydrograph
author_facet Gądek Wiesław
Tokarczyk Tamara
Środula Arkadiusz
author_sort Gądek Wiesław
title Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
title_short Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
title_full Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
title_fullStr Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
title_full_unstemmed Estimation of parametric flood hydrograph determined by means of Strupczewski method in the Vistula and Odra catchments
title_sort estimation of parametric flood hydrograph determined by means of strupczewski method in the vistula and odra catchments
publisher Sciendo
series Journal of Water and Land Development
issn 2083-4535
publishDate 2016-12-01
description While determining theoretical flood hydrographs, different methods of their construction are used depending on the needs of the problem or the scope of the project. It should be remembered that these methods differ mainly with the principle of the waveform averaging, which may be done either according to the flow or time. The hydrographs may be divided into nonparametric (determining on the basis of registered floods) and parametric (using mathematical description of the flood course). One of the analytical methods is Strupczewski method which has two parameters: responsible for the waveform and specifies the base flow, the flow above which values of hydrograph are calculated. The functional description uses the Pearson type III density distribution.
topic analytical flood hydrograph
nonparametric hydrograph
parametric hydrograph
Strupczewski method
the Cracow method
typical hydrograph
url http://www.degruyter.com/view/j/jwld.2016.31.issue-1/jwld-2016-0035/jwld-2016-0035.xml?format=INT
work_keys_str_mv AT gadekwiesław estimationofparametricfloodhydrographdeterminedbymeansofstrupczewskimethodinthevistulaandodracatchments
AT tokarczyktamara estimationofparametricfloodhydrographdeterminedbymeansofstrupczewskimethodinthevistulaandodracatchments
AT srodulaarkadiusz estimationofparametricfloodhydrographdeterminedbymeansofstrupczewskimethodinthevistulaandodracatchments
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