Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.

Detalhes bibliográficos
Autor(a) principal: GOTARDO, J. T.
Data de Publicação: 2016
Outros Autores: RODRIGUES, L. N., GOMES, B. M.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)
Texto Completo: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1051735
http://dx.doi.org/10.1590/1809-4430-Eng.Agric.v36n4p631-645/2016
Resumo: ABSTRACT: This study aimed to estimate the probability of climatological water deficit in an experimental watershed in the Cerrado biome, located in the central plateau of Brazil. For that, it was used a time series of 31 years (1982?2012). The probable climatological water deficit was calculated by the difference between rainfall and probable reference evapotranspiration, on a decennial scale. The reference evapotranspiration (ET0) was estimated by the standard FAO-56 Penman-Monteith method. To estimate water deficit, it was used gamma distribution, time series of rainfall and reference evapotranspiration. The adherence of the estimated probabilities to the observed data was verified by the Kolmogorov-Smirnov nonparametric test, with significance level (a-0.05), which presented a good adjustment to the distribution models. It was observed a climatological water deficit, in greater or lesser intensity, between the annual decennials 2 and 32.
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spelling Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.Distribuição gamaPenman-MonteithPrecipitação pluviométricaDéficit hídrico climatológicoBacia hidrográfica experimentalAgroclimatologiaCerradoEstimativaABSTRACT: This study aimed to estimate the probability of climatological water deficit in an experimental watershed in the Cerrado biome, located in the central plateau of Brazil. For that, it was used a time series of 31 years (1982?2012). The probable climatological water deficit was calculated by the difference between rainfall and probable reference evapotranspiration, on a decennial scale. The reference evapotranspiration (ET0) was estimated by the standard FAO-56 Penman-Monteith method. To estimate water deficit, it was used gamma distribution, time series of rainfall and reference evapotranspiration. The adherence of the estimated probabilities to the observed data was verified by the Kolmogorov-Smirnov nonparametric test, with significance level (a-0.05), which presented a good adjustment to the distribution models. It was observed a climatological water deficit, in greater or lesser intensity, between the annual decennials 2 and 32.JACKELINE T. GOTARDO, UNIOESTE; LINEU NEIVA RODRIGUES, CPAC; BENEDITO M. GOMES, UNIOESTE.GOTARDO, J. T.RODRIGUES, L. N.GOMES, B. M.2016-08-25T11:11:11Z2016-08-25T11:11:11Z2016-08-2520162017-02-13T11:11:11Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleEngenharia Agrícola, Jaboticabal, v. 36, n. 4, p. 631-645, jul./ago. 2016.http://www.alice.cnptia.embrapa.br/alice/handle/doc/1051735http://dx.doi.org/10.1590/1809-4430-Eng.Agric.v36n4p631-645/2016enginfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice)instname:Empresa Brasileira de Pesquisa Agropecuária (Embrapa)instacron:EMBRAPA2017-08-16T03:04:04Zoai:www.alice.cnptia.embrapa.br:doc/1051735Repositório InstitucionalPUBhttps://www.alice.cnptia.embrapa.br/oai/requestcg-riaa@embrapa.bropendoar:21542017-08-16T03:04:04Repositório Institucional da EMBRAPA (Repository Open Access to Scientific Information from EMBRAPA - Alice) - Empresa Brasileira de Pesquisa Agropecuária (Embrapa)false
dc.title.none.fl_str_mv Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
title Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
spellingShingle Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
GOTARDO, J. T.
Distribuição gama
Penman-Monteith
Precipitação pluviométrica
Déficit hídrico climatológico
Bacia hidrográfica experimental
Agroclimatologia
Cerrado
Estimativa
title_short Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
title_full Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
title_fullStr Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
title_full_unstemmed Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
title_sort Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado.
author GOTARDO, J. T.
author_facet GOTARDO, J. T.
RODRIGUES, L. N.
GOMES, B. M.
author_role author
author2 RODRIGUES, L. N.
GOMES, B. M.
author2_role author
author
dc.contributor.none.fl_str_mv JACKELINE T. GOTARDO, UNIOESTE; LINEU NEIVA RODRIGUES, CPAC; BENEDITO M. GOMES, UNIOESTE.
dc.contributor.author.fl_str_mv GOTARDO, J. T.
RODRIGUES, L. N.
GOMES, B. M.
dc.subject.por.fl_str_mv Distribuição gama
Penman-Monteith
Precipitação pluviométrica
Déficit hídrico climatológico
Bacia hidrográfica experimental
Agroclimatologia
Cerrado
Estimativa
topic Distribuição gama
Penman-Monteith
Precipitação pluviométrica
Déficit hídrico climatológico
Bacia hidrográfica experimental
Agroclimatologia
Cerrado
Estimativa
description ABSTRACT: This study aimed to estimate the probability of climatological water deficit in an experimental watershed in the Cerrado biome, located in the central plateau of Brazil. For that, it was used a time series of 31 years (1982?2012). The probable climatological water deficit was calculated by the difference between rainfall and probable reference evapotranspiration, on a decennial scale. The reference evapotranspiration (ET0) was estimated by the standard FAO-56 Penman-Monteith method. To estimate water deficit, it was used gamma distribution, time series of rainfall and reference evapotranspiration. The adherence of the estimated probabilities to the observed data was verified by the Kolmogorov-Smirnov nonparametric test, with significance level (a-0.05), which presented a good adjustment to the distribution models. It was observed a climatological water deficit, in greater or lesser intensity, between the annual decennials 2 and 32.
publishDate 2016
dc.date.none.fl_str_mv 2016-08-25T11:11:11Z
2016-08-25T11:11:11Z
2016-08-25
2016
2017-02-13T11:11:11Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv Engenharia Agrícola, Jaboticabal, v. 36, n. 4, p. 631-645, jul./ago. 2016.
http://www.alice.cnptia.embrapa.br/alice/handle/doc/1051735
http://dx.doi.org/10.1590/1809-4430-Eng.Agric.v36n4p631-645/2016
identifier_str_mv Engenharia Agrícola, Jaboticabal, v. 36, n. 4, p. 631-645, jul./ago. 2016.
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/1051735
http://dx.doi.org/10.1590/1809-4430-Eng.Agric.v36n4p631-645/2016
dc.language.iso.fl_str_mv eng
language eng
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repository.mail.fl_str_mv cg-riaa@embrapa.br
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