Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution
Abstract The design and management of various hydraulic structures (such as stormwater drains, bridges and dams) require the estimation of rainfall with duration of a few minutes up to 24 h or more. Intensity-duration-frequency (IDF) curves links probability of occurrence to a given rainfall intensi...
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Language: | English |
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Sociedade Brasileira de Meteorologia
2022-07-01
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Series: | Revista Brasileira de Meteorologia |
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Online Access: | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862022005008201&lng=en&tlng=en |
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author | Wagner Alessandro Pansera Benedito Martins Gomes Eloy Lemos de Mello João Carlos Cury Saad |
author_facet | Wagner Alessandro Pansera Benedito Martins Gomes Eloy Lemos de Mello João Carlos Cury Saad |
author_sort | Wagner Alessandro Pansera |
collection | DOAJ |
description | Abstract The design and management of various hydraulic structures (such as stormwater drains, bridges and dams) require the estimation of rainfall with duration of a few minutes up to 24 h or more. Intensity-duration-frequency (IDF) curves links probability of occurrence to a given rainfall intensity. The procedure for obtaining IDF curves basically involves two steps: (i) frequency analysis for different durations and (ii) modeling of IDF curves. In the first step, this study aimed to adequately select the upper tail weight of the following distributions: generalized extreme value (GEV), generalized logistic (GLO) and generalized Pareto (GPA). In the second step, this study aimed to evaluate the performance of three models of IDF curves. The traditional model (M1) was compared with empirical model (M2) and a second-order polynomial model (M3). To perform this study, rainfall data from the city of Caraguatatuba (São Paulo state, Brazil) for the period between 1971 and 2001 were used, for time intervals between 10 and 1440 min. The main conclusions were: (i) GLO and GEV had heavy upper tail while GPA had light upper tail, impacting quantiles with T > 100 years; (ii) M3 presents errors lower than M1 for return periods greater than 100 years. |
first_indexed | 2024-04-13T22:39:39Z |
format | Article |
id | doaj.art-36af55b384644203833d629799c1f99a |
institution | Directory Open Access Journal |
issn | 1982-4351 |
language | English |
last_indexed | 2024-04-13T22:39:39Z |
publishDate | 2022-07-01 |
publisher | Sociedade Brasileira de Meteorologia |
record_format | Article |
series | Revista Brasileira de Meteorologia |
spelling | doaj.art-36af55b384644203833d629799c1f99a2022-12-22T02:26:38ZengSociedade Brasileira de MeteorologiaRevista Brasileira de Meteorologia1982-43512022-07-0110.1590/0102-77863710069Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the DistributionWagner Alessandro Panserahttps://orcid.org/0000-0002-6850-6775Benedito Martins GomesEloy Lemos de MelloJoão Carlos Cury SaadAbstract The design and management of various hydraulic structures (such as stormwater drains, bridges and dams) require the estimation of rainfall with duration of a few minutes up to 24 h or more. Intensity-duration-frequency (IDF) curves links probability of occurrence to a given rainfall intensity. The procedure for obtaining IDF curves basically involves two steps: (i) frequency analysis for different durations and (ii) modeling of IDF curves. In the first step, this study aimed to adequately select the upper tail weight of the following distributions: generalized extreme value (GEV), generalized logistic (GLO) and generalized Pareto (GPA). In the second step, this study aimed to evaluate the performance of three models of IDF curves. The traditional model (M1) was compared with empirical model (M2) and a second-order polynomial model (M3). To perform this study, rainfall data from the city of Caraguatatuba (São Paulo state, Brazil) for the period between 1971 and 2001 were used, for time intervals between 10 and 1440 min. The main conclusions were: (i) GLO and GEV had heavy upper tail while GPA had light upper tail, impacting quantiles with T > 100 years; (ii) M3 presents errors lower than M1 for return periods greater than 100 years.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862022005008201&lng=en&tlng=endesign rainfallextreme valuesLH moments |
spellingShingle | Wagner Alessandro Pansera Benedito Martins Gomes Eloy Lemos de Mello João Carlos Cury Saad Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution Revista Brasileira de Meteorologia design rainfall extreme values LH moments |
title | Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution |
title_full | Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution |
title_fullStr | Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution |
title_full_unstemmed | Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution |
title_short | Development of Intensity-Duration-Frequency Curves of Intense Rainfall With Emphasis on the Behavior of the Upper Tail of the Distribution |
title_sort | development of intensity duration frequency curves of intense rainfall with emphasis on the behavior of the upper tail of the distribution |
topic | design rainfall extreme values LH moments |
url | http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862022005008201&lng=en&tlng=en |
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