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Determining large scale actual evapotranspiration using agro-meteorological and remote sensing data in the Northwest of Sao Paulo state, Brazil

dc.contributor.authorHernandez, F. B.T. [UNESP]
dc.contributor.authorDe Teixeira, A. H.C.
dc.contributor.authorNeale, C. M.U.
dc.contributor.authorTaghvaeian, S.
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionEmpresa Brasileira de Pesquisa Agropecuária (EMBRAPA)
dc.contributor.institutionRemote Sensing Lab
dc.contributor.institutionColorado State University
dc.date.accessioned2018-12-11T16:37:47Z
dc.date.available2018-12-11T16:37:47Z
dc.date.issued2014-06-20
dc.description.abstractThe best irrigation management depends on accurate estimation of reference evapotranspiration (ET0) and then selection of the appropriate crop coefficient for each phenological stage. However, the evaluation of water productivity on a large scale can be done by using actual evapotranspiration (ETa), determined by coupling agrometeorological and remote sensing data. This paper describes methodologies used for estimating ETa for 20 centerpivots using three different approaches: the traditional FAO crop coefficient (Kc) method and two remote sensing algorithms, one called SEBAL and other named TEIXEIRA. The methods were applied to one Landsat 5 Thematic Mapper image acquired in July 2010 over the Northwest portion of the Sao Paulo State, Brazil. The corn, bean and sugar cane crops are grown under center pivot sprinkler irrigation. ET0was calculated by the Penman-Monteith method with data from one automated weather station close to the study site. The results showed that for the crops at effective full cover, SEBAL and TEIXEIRA's methods agreed well comparing with the traditional method. However, both remote sensing methods overestimated ETaaccording to the degree of exposed soil, with the TEIXEIRA method presenting closer ET avalues with those resulted from the traditional FAO K cmethod. This study showed that remote sensing algorithms can be useful tools for monitoring and establishing realistic Kc values to further determine ETaon a large scale. However, several images during the growing seasons must be used to establish the necessary adjustments to the traditional FAO crop coefficient method.en
dc.description.affiliationUNESP-Campus Ilha Solteira Hydraulics and Irrigation Division, Ilha Solteira, SP
dc.description.affiliationEmbrapa Monitoramento por Satélite, Sao Paulo, SP
dc.description.affiliationUtah State University Remote Sensing Lab, Logan, UT
dc.description.affiliationColorado State University, Fort Collins, CO
dc.description.affiliationUnespUNESP-Campus Ilha Solteira Hydraulics and Irrigation Division, Ilha Solteira, SP
dc.format.extent263-270
dc.identifierhttp://dx.doi.org/10.17660/ActaHortic.2014.1038.31
dc.identifier.citationActa Horticulturae, v. 1038, p. 263-270.
dc.identifier.doi10.17660/ActaHortic.2014.1038.31
dc.identifier.issn0567-7572
dc.identifier.scopus2-s2.0-84905054671
dc.identifier.urihttp://hdl.handle.net/11449/167649
dc.language.isoeng
dc.relation.ispartofActa Horticulturae
dc.relation.ispartofsjr0,198
dc.rights.accessRightsAcesso abertopt
dc.sourceScopus
dc.subjectCrop coefficient
dc.subjectWeather station
dc.titleDetermining large scale actual evapotranspiration using agro-meteorological and remote sensing data in the Northwest of Sao Paulo state, Brazilen
dc.typeTrabalho apresentado em eventopt
dspace.entity.typePublication
unesp.author.lattes7276242706611764[1]
unesp.author.orcid0000-0001-9241-243X[1]
unesp.campusUniversidade Estadual Paulista (UNESP), Faculdade de Engenharia, Ilha Solteirapt

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