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Application of MODIS images for modelling the energy balance components in the semi-arid conditions of Brazil

dc.contributor.authorTeixeira, Antonio H. de C.
dc.contributor.authorScherer-Warren, Morris
dc.contributor.authorLopes, Helio L.
dc.contributor.authorHernandez, Fernando B. T. [UNESP]
dc.contributor.authorAndrade, Ricardo G.
dc.contributor.authorNeale, Christopher M. U.
dc.contributor.authorNeale, CMU
dc.contributor.authorMaltese, A.
dc.contributor.institutionEmpresa Brasileira de Pesquisa Agropecuária (EMBRAPA)
dc.contributor.institutionAgencia Nacl Aguas
dc.contributor.institutionUniv Vale Sao Francisco
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.contributor.institutionUtah State Univ
dc.date.accessioned2020-12-10T16:37:18Z
dc.date.available2020-12-10T16:37:18Z
dc.date.issued2013-01-01
dc.description.abstractIn the semi-arid areas of Petrolina municipality, Northeast Brazil, irrigated agriculture has replaced the natural vegetation, thus the quantification of the energy exchanges between the plants and the low atmosphere is important. MODIS satellite images and agro-meteorological data for the years of 2010 and 2011 were used together, for modelling the energy balance components under these conditions. Surface albedo (alpha(0)), NDVI and surface temperature (T-0) were the remote sensing parameters required to calculate the latent heat flux (lambda E) and the surface resistance to evapotranspiration (r(s)) on a large scale. The daily net radiation (R-n) was retrieved from alpha(0), air temperature (T-a) and transmissivity (tau(sw)), allowing the quantification of the sensible heat flux (H) by residual in the energy balance. With threshold values for r(s), it was possible to do a simplified vegetation classification. The incident solar radiation (RS down arrow) partitioned as R-n ranged from 0.40 to 0.51, corresponding respectively to periods after the rainy season and the driest conditions of the year, with the observed differences between irrigated crops and natural ecosystem not significant. Considering all periods along the year, the averaged fractions of R-n partitioned as H, were 31 and 78%, for irrigated crops and natural vegetation, respectively, while as lambda E the corresponding ratios were 69 and 22%. Heat advection from the dry areas surrounding irrigated plots was observed with lambda E exceeding R-n by 9% during the coldest periods. The models tested herein can be used for monitoring the energy exchanges in agro-ecosystems under conditions of land use and climate change.en
dc.description.affiliationEmbrapa Monitoramento Satelite, Sao Paulo, Brazil
dc.description.affiliationAgencia Nacl Aguas, Brasilia, DF, Brazil
dc.description.affiliationUniv Vale Sao Francisco, Pernambuco, Brazil
dc.description.affiliationUniv Estadual Paulista, Sao Paulo, Brazil
dc.description.affiliationUtah State Univ, Logan, UT 84322 USA
dc.description.affiliationUnespUniv Estadual Paulista, Sao Paulo, Brazil
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.description.sponsorshipFAC EPE
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.format.extent11
dc.identifierhttp://dx.doi.org/10.1117/12.2025388
dc.identifier.citationRemote Sensing For Agriculture, Ecosystems, And Hydrology Xv. Bellingham: Spie-int Soc Optical Engineering, v. 8887, 11 p., 2013.
dc.identifier.doi10.1117/12.2025388
dc.identifier.issn0277-786X
dc.identifier.urihttp://hdl.handle.net/11449/194776
dc.identifier.wosWOS:000328503200034
dc.language.isoeng
dc.publisherSpie-int Soc Optical Engineering
dc.relation.ispartofRemote Sensing For Agriculture, Ecosystems, And Hydrology Xv
dc.sourceWeb of Science
dc.subjectsurface albedo
dc.subjectsurface temperature
dc.subjectNDVI
dc.subjectlatent heat flux
dc.subjectsensible heat flux
dc.titleApplication of MODIS images for modelling the energy balance components in the semi-arid conditions of Brazilen
dc.typeTrabalho apresentado em evento
dcterms.rightsHolderSpie-int Soc Optical Engineering
dspace.entity.typePublication
unesp.author.lattes7276242706611764[4]
unesp.author.orcid0000-0002-7199-6410[6]
unesp.author.orcid0000-0001-9241-243X[4]

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