Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin

The return period of "7.26" rainstorm flood in 2017 in Wudinghe basin is analyzed by the method of P-III distribution. The Lijiahe and Dingjiagou stations with long rainfall observation data in the rainstorm area are selected, and the frequency curve of the annual maximum 24 hours rainfall...

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Main Authors: Jin Shuang-yan, Gao Wen-yong, Luo Si-wu, Gao Ya-jun
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:MATEC Web of Conferences
Online Access:https://doi.org/10.1051/matecconf/201824601105
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author Jin Shuang-yan
Gao Wen-yong
Luo Si-wu
Gao Ya-jun
author_facet Jin Shuang-yan
Gao Wen-yong
Luo Si-wu
Gao Ya-jun
author_sort Jin Shuang-yan
collection DOAJ
description The return period of "7.26" rainstorm flood in 2017 in Wudinghe basin is analyzed by the method of P-III distribution. The Lijiahe and Dingjiagou stations with long rainfall observation data in the rainstorm area are selected, and the frequency curve of the annual maximum 24 hours rainfall are established, and the recurrence period of rainfall stations in rainstorm area are estimated according to the parameters determined by the curve fitting method. The frequency curve of the annual maximum peak discharge of Baijiachuan hydrological stations and so on are established, and the return period are analyzed in combination with the historical survey floods. The results show that the return period of Zhaojiabian of heavy rainfall center is about 100 years, and which of the other stations over than 200mm in Wudinghe basin is about 30~90 years; while the return period of the peak discharge of Baijiachuan and Suide hydrological station is about 30 and 20 years respectively.
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spelling doaj.art-f124f6dfc5814e27bdf52adf88b97b0e2022-12-21T23:04:56ZengEDP SciencesMATEC Web of Conferences2261-236X2018-01-012460110510.1051/matecconf/201824601105matecconf_iswso2018_01105Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe BasinJin Shuang-yanGao Wen-yongLuo Si-wuGao Ya-junThe return period of "7.26" rainstorm flood in 2017 in Wudinghe basin is analyzed by the method of P-III distribution. The Lijiahe and Dingjiagou stations with long rainfall observation data in the rainstorm area are selected, and the frequency curve of the annual maximum 24 hours rainfall are established, and the recurrence period of rainfall stations in rainstorm area are estimated according to the parameters determined by the curve fitting method. The frequency curve of the annual maximum peak discharge of Baijiachuan hydrological stations and so on are established, and the return period are analyzed in combination with the historical survey floods. The results show that the return period of Zhaojiabian of heavy rainfall center is about 100 years, and which of the other stations over than 200mm in Wudinghe basin is about 30~90 years; while the return period of the peak discharge of Baijiachuan and Suide hydrological station is about 30 and 20 years respectively.https://doi.org/10.1051/matecconf/201824601105
spellingShingle Jin Shuang-yan
Gao Wen-yong
Luo Si-wu
Gao Ya-jun
Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
MATEC Web of Conferences
title Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
title_full Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
title_fullStr Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
title_full_unstemmed Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
title_short Analysis on the Return Period of “7.26” Rainstorm and Flood in 2017 in the Wudinghe Basin
title_sort analysis on the return period of 7 26 rainstorm and flood in 2017 in the wudinghe basin
url https://doi.org/10.1051/matecconf/201824601105
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AT luosiwu analysisonthereturnperiodof726rainstormandfloodin2017inthewudinghebasin
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