M. Abreu, M. Fraga, L. Almeida, F. Silva, R. Cecílio, G. Lyra, R. Delgado
{"title":"在Sapucaí河流流域的流量,巴西:概率建模,参考流,和区划","authors":"M. Abreu, M. Fraga, L. Almeida, F. Silva, R. Cecílio, G. Lyra, R. Delgado","doi":"10.22541/au.162134118.84540536/v1","DOIUrl":null,"url":null,"abstract":"This work aims to study the streamflow statistic patterns in the Sapucaí\nRiver watershed, state of Minas Gerais, Brazil. This study embraces the\nstreamflow probabilistic modeling to determine the reference streamflow\nand, later, the streamflow regionalization to improve the water\nresources management. A 26-year-data series (1989 - 2014) of maximum,\naverage, and minimum streamflow were used. Probability density functions\nwere applied to the maximum and minimum daily streamflow to determine\nthe recurrence periods. Long-term average annual and monthly streamflow\nwere also calculated. Linear and non-linear regressions were adjusted\nfor the streamflow regionalization. The drainage area and the streamflow\nequivalent to the total rainfall (with and without abstractions) were\nused as predictor variables. The probability density functions that best\nadjusted the maximum streamflow data set were the Generalized Extreme\nValues, and for the minimum streamflow was the normal distribution.\nLinear and non-linear regressions were efficient (R²> 0.90\nand d Willmott> 0.97) in the regionalization process\nregardless of the predictor variables. However, a small statistical\nadvantage was found for the adjustment of non-linear regressions that\nused the predictor variables drainage area and the streamflow equivalent\nto the total rainfall (without abstractions).","PeriodicalId":302795,"journal":{"name":"Physics and Chemistry of the Earth, Parts A/B/C","volume":"50 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-05-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Streamflow In The Sapucaí River Watershed, Brazil: Probabilistic Modeling, Reference Streamflow, And Regionalization\",\"authors\":\"M. Abreu, M. Fraga, L. Almeida, F. Silva, R. Cecílio, G. Lyra, R. Delgado\",\"doi\":\"10.22541/au.162134118.84540536/v1\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"This work aims to study the streamflow statistic patterns in the Sapucaí\\nRiver watershed, state of Minas Gerais, Brazil. This study embraces the\\nstreamflow probabilistic modeling to determine the reference streamflow\\nand, later, the streamflow regionalization to improve the water\\nresources management. A 26-year-data series (1989 - 2014) of maximum,\\naverage, and minimum streamflow were used. Probability density functions\\nwere applied to the maximum and minimum daily streamflow to determine\\nthe recurrence periods. Long-term average annual and monthly streamflow\\nwere also calculated. Linear and non-linear regressions were adjusted\\nfor the streamflow regionalization. The drainage area and the streamflow\\nequivalent to the total rainfall (with and without abstractions) were\\nused as predictor variables. The probability density functions that best\\nadjusted the maximum streamflow data set were the Generalized Extreme\\nValues, and for the minimum streamflow was the normal distribution.\\nLinear and non-linear regressions were efficient (R²> 0.90\\nand d Willmott> 0.97) in the regionalization process\\nregardless of the predictor variables. However, a small statistical\\nadvantage was found for the adjustment of non-linear regressions that\\nused the predictor variables drainage area and the streamflow equivalent\\nto the total rainfall (without abstractions).\",\"PeriodicalId\":302795,\"journal\":{\"name\":\"Physics and Chemistry of the Earth, Parts A/B/C\",\"volume\":\"50 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-05-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Physics and Chemistry of the Earth, Parts A/B/C\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.22541/au.162134118.84540536/v1\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physics and Chemistry of the Earth, Parts A/B/C","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.22541/au.162134118.84540536/v1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Streamflow In The Sapucaí River Watershed, Brazil: Probabilistic Modeling, Reference Streamflow, And Regionalization
This work aims to study the streamflow statistic patterns in the Sapucaí
River watershed, state of Minas Gerais, Brazil. This study embraces the
streamflow probabilistic modeling to determine the reference streamflow
and, later, the streamflow regionalization to improve the water
resources management. A 26-year-data series (1989 - 2014) of maximum,
average, and minimum streamflow were used. Probability density functions
were applied to the maximum and minimum daily streamflow to determine
the recurrence periods. Long-term average annual and monthly streamflow
were also calculated. Linear and non-linear regressions were adjusted
for the streamflow regionalization. The drainage area and the streamflow
equivalent to the total rainfall (with and without abstractions) were
used as predictor variables. The probability density functions that best
adjusted the maximum streamflow data set were the Generalized Extreme
Values, and for the minimum streamflow was the normal distribution.
Linear and non-linear regressions were efficient (R²> 0.90
and d Willmott> 0.97) in the regionalization process
regardless of the predictor variables. However, a small statistical
advantage was found for the adjustment of non-linear regressions that
used the predictor variables drainage area and the streamflow equivalent
to the total rainfall (without abstractions).