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

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 (α-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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Main Authors: GOTARDO,JACKELINE T., RODRIGUES,LINEU N., GOMES,BENEDITO M.
Format: Digital revista
Language:English
Published: Associação Brasileira de Engenharia Agrícola 2016
Online Access:http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-69162016000400631
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spelling oai:scielo:S0100-691620160004006312016-09-21Estimation of climatological water deficit in an experimental watershed in the brazilian cerradoGOTARDO,JACKELINE T.RODRIGUES,LINEU N.GOMES,BENEDITO M. gamma distribution Penman-Monteith rainfall 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 (α-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.info:eu-repo/semantics/openAccessAssociação Brasileira de Engenharia AgrícolaEngenharia Agrícola v.36 n.4 20162016-08-01info:eu-repo/semantics/articletext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-69162016000400631en10.1590/1809-4430-Eng.Agric.v36n4p631-645/2016
institution SCIELO
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country Brasil
countrycode BR
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libraryname SciELO
language English
format Digital
author GOTARDO,JACKELINE T.
RODRIGUES,LINEU N.
GOMES,BENEDITO M.
spellingShingle GOTARDO,JACKELINE T.
RODRIGUES,LINEU N.
GOMES,BENEDITO M.
Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado
author_facet GOTARDO,JACKELINE T.
RODRIGUES,LINEU N.
GOMES,BENEDITO M.
author_sort GOTARDO,JACKELINE T.
title Estimation of climatological water deficit in an experimental watershed in the brazilian cerrado
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
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 (α-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.
publisher Associação Brasileira de Engenharia Agrícola
publishDate 2016
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0100-69162016000400631
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AT gomesbeneditom estimationofclimatologicalwaterdeficitinanexperimentalwatershedinthebraziliancerrado
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