Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil

The purpose of this study was to adjust equations that establish relationships between rainfall events with different duration and data from weather stations in the state of Santa Catarina, Brazil. In this study, the relationships between different duration heavy rainfalls from 13 weather stations o...

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Main Authors: Álvaro José Back, José Luiz Rocha Oliveira, Alan Henn
Format: Article
Language:English
Published: Sociedade Brasileira de Ciência do Solo 2012-06-01
Series:Revista Brasileira de Ciência do Solo
Subjects:
Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000300031&lng=en&tlng=en
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spelling doaj-107cf4e88cae40ff9e1c864487ea7d792021-01-02T00:57:11ZengSociedade Brasileira de Ciência do SoloRevista Brasileira de Ciência do Solo1806-96572012-06-013631015102210.1590/S0100-06832012000300031S0100-06832012000300031Duration-frequency relationships of heavy rainfall in Santa Catarina, BrazilÁlvaro José BackJosé Luiz Rocha OliveiraAlan HennThe purpose of this study was to adjust equations that establish relationships between rainfall events with different duration and data from weather stations in the state of Santa Catarina, Brazil. In this study, the relationships between different duration heavy rainfalls from 13 weather stations of Santa Catarina were analyzed. From series of maximum annual rainfalls, and using the Gumbel-Chow distribution, the maximum rainfall for durations between 5 min and 24 h were estimated considering return periods from 2 to 100 years. The data fit to the Gumbel-Chow model was verified by the Kolmogorov-Smirnov test at 5 % significance. The coefficients of Bell's equation were adjusted to estimate the relationship between rainfall duration t (min) and the return period T (y) in relation to the maximum rainfall with a duration of 1 hour and a 10 year return period. Likewise, the coefficients of Bell's equation were adjusted based on the maximum rainfall with a duration of 1 day and a 10 year return period. The results showed that these relationships are viable to estimate short-duration rainfall events at locations where there are no rainfall records.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000300031&lng=en&tlng=enchuva de projetohidrologiadrenagem
collection DOAJ
language English
format Article
sources DOAJ
author Álvaro José Back
José Luiz Rocha Oliveira
Alan Henn
spellingShingle Álvaro José Back
José Luiz Rocha Oliveira
Alan Henn
Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
Revista Brasileira de Ciência do Solo
chuva de projeto
hidrologia
drenagem
author_facet Álvaro José Back
José Luiz Rocha Oliveira
Alan Henn
author_sort Álvaro José Back
title Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
title_short Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
title_full Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
title_fullStr Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
title_full_unstemmed Duration-frequency relationships of heavy rainfall in Santa Catarina, Brazil
title_sort duration-frequency relationships of heavy rainfall in santa catarina, brazil
publisher Sociedade Brasileira de Ciência do Solo
series Revista Brasileira de Ciência do Solo
issn 1806-9657
publishDate 2012-06-01
description The purpose of this study was to adjust equations that establish relationships between rainfall events with different duration and data from weather stations in the state of Santa Catarina, Brazil. In this study, the relationships between different duration heavy rainfalls from 13 weather stations of Santa Catarina were analyzed. From series of maximum annual rainfalls, and using the Gumbel-Chow distribution, the maximum rainfall for durations between 5 min and 24 h were estimated considering return periods from 2 to 100 years. The data fit to the Gumbel-Chow model was verified by the Kolmogorov-Smirnov test at 5 % significance. The coefficients of Bell's equation were adjusted to estimate the relationship between rainfall duration t (min) and the return period T (y) in relation to the maximum rainfall with a duration of 1 hour and a 10 year return period. Likewise, the coefficients of Bell's equation were adjusted based on the maximum rainfall with a duration of 1 day and a 10 year return period. The results showed that these relationships are viable to estimate short-duration rainfall events at locations where there are no rainfall records.
topic chuva de projeto
hidrologia
drenagem
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832012000300031&lng=en&tlng=en
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AT alanhenn durationfrequencyrelationshipsofheavyrainfallinsantacatarinabrazil
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