Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil

Detalhes bibliográficos
Autor(a) principal: Medeiros, Raimundo Mainar de
Data de Publicação: 2021
Outros Autores: Braga, Salatiel Ewen, França, Manoel Vieira de, Araújo, Wagner Rodolfo de, Saboya, Luciano Marcelo Fallé, Rolim Neto, Fernando Cartaxo, Holanda, Romildo Morant De, Pereira, Márcia Liana Freire
Tipo de documento: Artigo
Idioma: por
Título da fonte: Research, Society and Development
Texto Completo: https://rsdjournal.org/index.php/rsd/article/view/14752
Resumo: Knowing the local climate is a necessary factor for assessing water resources, as several meteorological elements are indispensable throughout the hydrological cycle. In this context, the objectives of this work are to estimate the maximum, minimum and annual evapotranspirations for the hydrographic basin of the Uruçuí Preto River, state of Piauí. The estimate of the minimum, maximum and annual evapotranspiration was made from the empirical equations for the estimation of the air temperature for the area of the basin under study. Historical series of monthly air temperature values were used, from uniform periods with 30 years of observations, for the 49 municipalities that encompass the study area. With the data from these series, equations were adjusted by the least squares method, obtaining multiple linear regression equations and tested the statistical method. With the average air temperature data estimated, evapotranspiration was estimated using the empirical method of Thornthwaite. Values for the average air temperature were estimated, estimated by the Estima_T software. The average evapotranspiration oscillation in the studied area occurs between 92.4 mm in February and 170.1 mm in October. Maximum evapotranspiration ranges from 111.3 to 202.8 mm. The minimum ETP ranges from 70.7 to 130.2 mm. The ETP estimates of the Uruçuí Preto - Piauí river basin are dependent on geographic positioning (latitude and longitude), and also on local orography. In average terms, the occurrence classes of 70 to 125 mm, 125 to 175 mm and the highest class above 200 mm stand out, which together make up 84.4% of the study area, representing a variation of 5.3 mm to 10.8 mm, in terms of average daily evapotranspiration, in practically the entire basin.
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spelling Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil Estudio de evapotranspiración máxima, mínima y anual en la cuenca del río Uruçuí Preto - Piauí, Brasil Estudo da evapotranspiração máxima, mínima e anual sobre a bacia hidrográfica do rio Uruçuí Preto - Piauí, Brasil Producción AgrícolaRiegoEquilibrio hídricoDemanda de aguaCambio climático.Agricultural ProductionIrrigationHydric balanceWater balanceWater demandClimate change.Produção AgrícolaIrrigaçãoBalanço hídricoDemanda hídricaMudanças climáticas.Knowing the local climate is a necessary factor for assessing water resources, as several meteorological elements are indispensable throughout the hydrological cycle. In this context, the objectives of this work are to estimate the maximum, minimum and annual evapotranspirations for the hydrographic basin of the Uruçuí Preto River, state of Piauí. The estimate of the minimum, maximum and annual evapotranspiration was made from the empirical equations for the estimation of the air temperature for the area of the basin under study. Historical series of monthly air temperature values were used, from uniform periods with 30 years of observations, for the 49 municipalities that encompass the study area. With the data from these series, equations were adjusted by the least squares method, obtaining multiple linear regression equations and tested the statistical method. With the average air temperature data estimated, evapotranspiration was estimated using the empirical method of Thornthwaite. Values for the average air temperature were estimated, estimated by the Estima_T software. The average evapotranspiration oscillation in the studied area occurs between 92.4 mm in February and 170.1 mm in October. Maximum evapotranspiration ranges from 111.3 to 202.8 mm. The minimum ETP ranges from 70.7 to 130.2 mm. The ETP estimates of the Uruçuí Preto - Piauí river basin are dependent on geographic positioning (latitude and longitude), and also on local orography. In average terms, the occurrence classes of 70 to 125 mm, 125 to 175 mm and the highest class above 200 mm stand out, which together make up 84.4% of the study area, representing a variation of 5.3 mm to 10.8 mm, in terms of average daily evapotranspiration, in practically the entire basin.Conocer el clima local es un factor necesario para evaluar los recursos hídricos, ya que varios elementos meteorológicos son indispensables en todo ciclo hidrológico. En este contexto, los objetivos de este trabajo son estimar las evapotranspiraciones máximas, mínimas y anuales para la cuenca hidrográfica del río Uruçuí Preto, estado de Piauí. La estimación de la evapotranspiración mínima, máxima y anual se realizó a partir de las ecuaciones empíricas para la estimación de la temperatura del aire para el área de la cuenca en estudio. Se utilizaron series históricas de valores de temperatura del aire mensuales, de períodos uniformes con 30 años de observaciones, para los 49 municipios que componen el área de estudio. Con los datos de estas series, las ecuaciones fueron ajustadas por el método de mínimos cuadrados, obteniendo ecuaciones de regresión lineal múltiple y probando el método estadístico. Con los datos de temperatura promedio del aire estimados, la evapotranspiración se estimó utilizando el método empírico de Thornthwaite. Se estimaron los valores de la temperatura media del aire, estimados por el software Estima_T. La oscilación de la evapotranspiración promedio en el área estudiada ocurre entre 92,4 mm en febrero y 170,1 mm en octubre. La evapotranspiración máxima varía de 111,3 a 202,8 mm. El ETP mínimo oscila entre 70,7 y 130,2 mm. Las estimaciones de ETP de la cuenca del río Uruçuí Preto - Piauí dependen del posicionamiento geográfico (latitud y longitud), y también de la orografía local. En términos promedio, se destacan las clases de ocurrencia de 70 a 125 mm, 125 a 175 mm y la clase más alta por encima de 200 mm, que en conjunto componen el 84,4% del área de estudio, lo que representa una variación de 5,3 mm a 10,8 mm, en términos de evapotranspiración media diaria, en prácticamente toda la cuenca.Conhecer o clima local é um fator necessário para avaliação dos recursos hídricos, pois vários elementos meteorológicos são indispensáveis em todo ciclo hidrológico. Nesse contexto, os objetivos deste trabalho consistem em se estimar as evapotranspirações máxima, mínima e anual para a bacia hidrografica do rio Uruçuí Preto, estado do Piauí. A estimativa da evapotranspiração mínima, máxima e anual foi efetuada a partir das equações empíricas para a estimativa da temperatura do ar para a área da bacia em estudo. Foram utilizadas séries históricas de valores mensais da temperatura do ar, de períodos uniformizados com 30 anos de observações, para os 49 municípios que englobam a área de estudo. Com os dados dessas séries, foram ajustadas equações pelo método dos mínimos quadrados, obtendo-se equações de regressão linear múltipla e testaram o método estatístico. Com os dados de temperatura média do ar estimados, procedeu-se à estimativa da evapotranspiração pelo método empírico de Thornthwaite. Foram elaborados valores da temperatura média do ar, estimados pelo software Estima_T. A oscilação da evapotranspiração média da área estudada ocorre entre 92,4 mm em fevereiro a 170,1 mm no mês de outubro. A evapotranspiração máxima oscila entre 111,3 a 202,8 mm. A ETP mínima oscila entre 70,7 a 130,2 mm. As estimativas de ETP da bacia hidrográfica do rio Uruçuí Preto – Piauí apresentam dependência do posicionamento geográfico (latitude e longitude), e também da orografia local. Em termos médios, se sobressaem as classes de ocorrência de 70 a 125 mm, 125 a 175 mm e a classe mais alta superior aos 200 mm que, juntas, totalizam 84,4% da área de estudo, representando uma variação de 5,3 mm a 10,8 mm, em termos de evapotranspiração média diária, em praticamente toda a bacia.Research, Society and Development2021-05-12info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://rsdjournal.org/index.php/rsd/article/view/1475210.33448/rsd-v10i5.14752Research, Society and Development; Vol. 10 No. 5; e42810514752Research, Society and Development; Vol. 10 Núm. 5; e42810514752Research, Society and Development; v. 10 n. 5; e428105147522525-3409reponame:Research, Society and Developmentinstname:Universidade Federal de Itajubá (UNIFEI)instacron:UNIFEIporhttps://rsdjournal.org/index.php/rsd/article/view/14752/13563Copyright (c) 2021 Raimundo Mainar de Medeiros; Salatiel Ewen Braga; Manoel Vieira de França; Wagner Rodolfo de Araújo; Luciano Marcelo Fallé Saboya; Fernando Cartaxo Rolim Neto; Romildo Morant De Holanda; Márcia Liana Freire Pereirahttps://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessMedeiros, Raimundo Mainar de Braga, Salatiel EwenFrança, Manoel Vieira de Araújo, Wagner Rodolfo de Saboya, Luciano Marcelo Fallé Rolim Neto, Fernando Cartaxo Holanda, Romildo Morant DePereira, Márcia Liana Freire 2021-05-17T18:20:49Zoai:ojs.pkp.sfu.ca:article/14752Revistahttps://rsdjournal.org/index.php/rsd/indexPUBhttps://rsdjournal.org/index.php/rsd/oairsd.articles@gmail.com2525-34092525-3409opendoar:2024-01-17T09:35:46.953621Research, Society and Development - Universidade Federal de Itajubá (UNIFEI)false
dc.title.none.fl_str_mv Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
Estudio de evapotranspiración máxima, mínima y anual en la cuenca del río Uruçuí Preto - Piauí, Brasil
Estudo da evapotranspiração máxima, mínima e anual sobre a bacia hidrográfica do rio Uruçuí Preto - Piauí, Brasil
title Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
spellingShingle Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
Medeiros, Raimundo Mainar de
Producción Agrícola
Riego
Equilibrio hídrico
Demanda de agua
Cambio climático.
Agricultural Production
Irrigation
Hydric balance
Water balance
Water demand
Climate change.
Produção Agrícola
Irrigação
Balanço hídrico
Demanda hídrica
Mudanças climáticas.
title_short Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
title_full Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
title_fullStr Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
title_full_unstemmed Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
title_sort Study of maximum, minimum and annual evapotranspiration on the watershed of rio Uruçuí Preto - Piauí, Brazil
author Medeiros, Raimundo Mainar de
author_facet Medeiros, Raimundo Mainar de
Braga, Salatiel Ewen
França, Manoel Vieira de
Araújo, Wagner Rodolfo de
Saboya, Luciano Marcelo Fallé
Rolim Neto, Fernando Cartaxo
Holanda, Romildo Morant De
Pereira, Márcia Liana Freire
author_role author
author2 Braga, Salatiel Ewen
França, Manoel Vieira de
Araújo, Wagner Rodolfo de
Saboya, Luciano Marcelo Fallé
Rolim Neto, Fernando Cartaxo
Holanda, Romildo Morant De
Pereira, Márcia Liana Freire
author2_role author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Medeiros, Raimundo Mainar de
Braga, Salatiel Ewen
França, Manoel Vieira de
Araújo, Wagner Rodolfo de
Saboya, Luciano Marcelo Fallé
Rolim Neto, Fernando Cartaxo
Holanda, Romildo Morant De
Pereira, Márcia Liana Freire
dc.subject.por.fl_str_mv Producción Agrícola
Riego
Equilibrio hídrico
Demanda de agua
Cambio climático.
Agricultural Production
Irrigation
Hydric balance
Water balance
Water demand
Climate change.
Produção Agrícola
Irrigação
Balanço hídrico
Demanda hídrica
Mudanças climáticas.
topic Producción Agrícola
Riego
Equilibrio hídrico
Demanda de agua
Cambio climático.
Agricultural Production
Irrigation
Hydric balance
Water balance
Water demand
Climate change.
Produção Agrícola
Irrigação
Balanço hídrico
Demanda hídrica
Mudanças climáticas.
description Knowing the local climate is a necessary factor for assessing water resources, as several meteorological elements are indispensable throughout the hydrological cycle. In this context, the objectives of this work are to estimate the maximum, minimum and annual evapotranspirations for the hydrographic basin of the Uruçuí Preto River, state of Piauí. The estimate of the minimum, maximum and annual evapotranspiration was made from the empirical equations for the estimation of the air temperature for the area of the basin under study. Historical series of monthly air temperature values were used, from uniform periods with 30 years of observations, for the 49 municipalities that encompass the study area. With the data from these series, equations were adjusted by the least squares method, obtaining multiple linear regression equations and tested the statistical method. With the average air temperature data estimated, evapotranspiration was estimated using the empirical method of Thornthwaite. Values for the average air temperature were estimated, estimated by the Estima_T software. The average evapotranspiration oscillation in the studied area occurs between 92.4 mm in February and 170.1 mm in October. Maximum evapotranspiration ranges from 111.3 to 202.8 mm. The minimum ETP ranges from 70.7 to 130.2 mm. The ETP estimates of the Uruçuí Preto - Piauí river basin are dependent on geographic positioning (latitude and longitude), and also on local orography. In average terms, the occurrence classes of 70 to 125 mm, 125 to 175 mm and the highest class above 200 mm stand out, which together make up 84.4% of the study area, representing a variation of 5.3 mm to 10.8 mm, in terms of average daily evapotranspiration, in practically the entire basin.
publishDate 2021
dc.date.none.fl_str_mv 2021-05-12
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format article
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dc.identifier.uri.fl_str_mv https://rsdjournal.org/index.php/rsd/article/view/14752
10.33448/rsd-v10i5.14752
url https://rsdjournal.org/index.php/rsd/article/view/14752
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rights_invalid_str_mv https://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
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dc.publisher.none.fl_str_mv Research, Society and Development
publisher.none.fl_str_mv Research, Society and Development
dc.source.none.fl_str_mv Research, Society and Development; Vol. 10 No. 5; e42810514752
Research, Society and Development; Vol. 10 Núm. 5; e42810514752
Research, Society and Development; v. 10 n. 5; e42810514752
2525-3409
reponame:Research, Society and Development
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