Verification of the stationarity of flow series in the Iguaçu River basin

Bibliographic Details
Main Author: Tozzi,Bruna Kiechaloski Miró
Publication Date: 2020
Other Authors: Fill,Heinz Dieter Oskar August
Format: Report
Language: eng
Source: RBRH (Online)
Download full: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312020000100402
Summary: ABSTRACT The purpose of this technical note is to verify the stationarity of flows in the Iguaçu River Basin, considering 14 fluviometric stations. For this purpose, three sets of annual flow series were studied: mean flows, maximum flows and minimum flows of 7 days. Initially, the exploratory analysis of the data was performed, based on the establishment of two points of change of the characteristics of the flows and the accomplishment of statistical tests of equality of mean and variance, parametric and nonparametric. Finally, composite tests were used considering the basin divided into Upper and Lower Iguaçu. In the exploratory analysis of the data, it was concluded that there was apparently a change in the trend of flow rates, part in the 1970s, part in the 1980s. Therefore, the series were divided in two different ways, at the half and at the point suggested in the exploratory analysis. Regarding the statistical tests, the Mann-Whitney test was chosen because it did not depend on the underlying distribution of the flow series, and because the test was highly recommended by other authors. It was concluded that the flow change occurred in a relatively short interval of time, and could be treated as a non-stationarity per hop. In general, the most recent change was downstream of the Uniao da Vitória fluviometric station. A change in the behavior of the mean and maximum flows was evident, however, such phenomenon was not observed in the evaluation of the minimum flows.
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spelling Verification of the stationarity of flow series in the Iguaçu River basinParametricStatisticTestsABSTRACT The purpose of this technical note is to verify the stationarity of flows in the Iguaçu River Basin, considering 14 fluviometric stations. For this purpose, three sets of annual flow series were studied: mean flows, maximum flows and minimum flows of 7 days. Initially, the exploratory analysis of the data was performed, based on the establishment of two points of change of the characteristics of the flows and the accomplishment of statistical tests of equality of mean and variance, parametric and nonparametric. Finally, composite tests were used considering the basin divided into Upper and Lower Iguaçu. In the exploratory analysis of the data, it was concluded that there was apparently a change in the trend of flow rates, part in the 1970s, part in the 1980s. Therefore, the series were divided in two different ways, at the half and at the point suggested in the exploratory analysis. Regarding the statistical tests, the Mann-Whitney test was chosen because it did not depend on the underlying distribution of the flow series, and because the test was highly recommended by other authors. It was concluded that the flow change occurred in a relatively short interval of time, and could be treated as a non-stationarity per hop. In general, the most recent change was downstream of the Uniao da Vitória fluviometric station. A change in the behavior of the mean and maximum flows was evident, however, such phenomenon was not observed in the evaluation of the minimum flows.Associação Brasileira de Recursos Hídricos2020-01-01info:eu-repo/semantics/reportinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S2318-03312020000100402RBRH v.25 2020reponame:RBRH (Online)instname:Associação Brasileira de Recursos Hídricos (ABRH)instacron:ABRH10.1590/2318-0331.252020180171info:eu-repo/semantics/openAccessTozzi,Bruna Kiechaloski MiróFill,Heinz Dieter Oskar Augusteng2020-04-23T00:00:00Zoai:scielo:S2318-03312020000100402Revistahttps://www.scielo.br/j/rbrh/https://old.scielo.br/oai/scielo-oai.php||rbrh@abrh.org.br2318-03311414-381Xopendoar:2020-04-23T00:00RBRH (Online) - Associação Brasileira de Recursos Hídricos (ABRH)false
dc.title.none.fl_str_mv Verification of the stationarity of flow series in the Iguaçu River basin
title Verification of the stationarity of flow series in the Iguaçu River basin
spellingShingle Verification of the stationarity of flow series in the Iguaçu River basin
Tozzi,Bruna Kiechaloski Miró
Parametric
Statistic
Tests
title_short Verification of the stationarity of flow series in the Iguaçu River basin
title_full Verification of the stationarity of flow series in the Iguaçu River basin
title_fullStr Verification of the stationarity of flow series in the Iguaçu River basin
title_full_unstemmed Verification of the stationarity of flow series in the Iguaçu River basin
title_sort Verification of the stationarity of flow series in the Iguaçu River basin
author Tozzi,Bruna Kiechaloski Miró
author_facet Tozzi,Bruna Kiechaloski Miró
Fill,Heinz Dieter Oskar August
author_role author
author2 Fill,Heinz Dieter Oskar August
author2_role author
dc.contributor.author.fl_str_mv Tozzi,Bruna Kiechaloski Miró
Fill,Heinz Dieter Oskar August
dc.subject.por.fl_str_mv Parametric
Statistic
Tests
topic Parametric
Statistic
Tests
description ABSTRACT The purpose of this technical note is to verify the stationarity of flows in the Iguaçu River Basin, considering 14 fluviometric stations. For this purpose, three sets of annual flow series were studied: mean flows, maximum flows and minimum flows of 7 days. Initially, the exploratory analysis of the data was performed, based on the establishment of two points of change of the characteristics of the flows and the accomplishment of statistical tests of equality of mean and variance, parametric and nonparametric. Finally, composite tests were used considering the basin divided into Upper and Lower Iguaçu. In the exploratory analysis of the data, it was concluded that there was apparently a change in the trend of flow rates, part in the 1970s, part in the 1980s. Therefore, the series were divided in two different ways, at the half and at the point suggested in the exploratory analysis. Regarding the statistical tests, the Mann-Whitney test was chosen because it did not depend on the underlying distribution of the flow series, and because the test was highly recommended by other authors. It was concluded that the flow change occurred in a relatively short interval of time, and could be treated as a non-stationarity per hop. In general, the most recent change was downstream of the Uniao da Vitória fluviometric station. A change in the behavior of the mean and maximum flows was evident, however, such phenomenon was not observed in the evaluation of the minimum flows.
publishDate 2020
dc.date.none.fl_str_mv 2020-01-01
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dc.publisher.none.fl_str_mv Associação Brasileira de Recursos Hídricos
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dc.source.none.fl_str_mv RBRH v.25 2020
reponame:RBRH (Online)
instname:Associação Brasileira de Recursos Hídricos (ABRH)
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