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Can changes in land use in a semi-arid region of Brazil cause seasonal variation in energy partitioning and evapotranspiration?

dc.contributor.authorSantos, Wilma Roberta dos
dc.contributor.authorJardim, Alexandre Maniçoba da Rosa Ferraz [UNESP]
dc.contributor.authorSouza, Luciana Sandra Bastos de
dc.contributor.authorSouza, Carlos André Alves de
dc.contributor.authorMorais, José Edson Florentino de
dc.contributor.authorAlves, Cleber Pereira
dc.contributor.authorAraujo Júnior, George do Nascimento
dc.contributor.authorSilva, Marcelo José da
dc.contributor.authorSalvador, Kaique Renan da Silva
dc.contributor.authorSilva, Marcos Vinícius da
dc.contributor.authorMorellato, Leonor Patricia Cerdeira [UNESP]
dc.contributor.authorSilva, Thieres George Freire da
dc.contributor.institutionFederal Rural University of Pernambuco
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.contributor.institutionFederal University of Alagoas
dc.date.accessioned2025-04-29T19:33:22Z
dc.date.issued2024-09-01
dc.description.abstractChanges to forests due to deforestation, or their replacement by agricultural areas, alter evapotranspiration and the partitioning of available energy. This study investigated seasonal variations in the energy balance and evapotranspiration in landscapes under different levels of anthropogenic intervention in the semi-arid region of Brazil. Micrometeorological data was obtained from September 2020 to October 2022 for three areas of the semi-arid region: preserved Caatinga (CAA, native vegetation), Caatinga under regeneration (REGE) and a deforested area (DEFA). Here, we use the Bowen ratio energy balance method. Measurements were taken of global solar radiation, air temperature, relative humidity, vapour pressure deficit, rainfall, net radiation, latent heat flux, sensible heat flux, soil heat flux, evapotranspiration, volumetric soil water content and Normalised Difference Vegetation Index. Sensible heat flux was the dominant flux in both areas with 66% for preserved Caatinga vegetation, 63% for Caatinga under regeneration and 62% deforested area. The latent heat flux was equivalent to 28% of the net radiation for preserved Caatinga vegetation, Caatinga under regeneration and deforested area. The evapotranspiration in turn responded as a function of water availability, being higher during the rainy seasons, with average values of 1.82 mm day−1 for preserved Caatinga vegetation, 2.26 mm day−1 for Caatinga under regeneration and 1.25 mm day−1 for deforested area. The Bowen ratio presented values > 1 in deforested area, preserved Caatinga vegetation and Caatinga under regeneration. Thus, it can be concluded that the change in land use alters the energy balance components, promoting reductions in available energy and latent and sensible heat fluxes during the rainy-dry transition in the deforested area. In addition, the seasonality of energy fluxes depends on water availability in the environment.en
dc.description.affiliationPostgraduate Program in Plant Production Academic Unit of Serra Talhada Federal Rural University of Pernambuco, Pernambuco
dc.description.affiliationDepartment of Biodiversity Institute of Biosciences São Paulo State University—UNESP, Av. 24A, 1515, Rio Claro
dc.description.affiliationDepartment of Agricultural Engineering Federal Rural University of Pernambuco, Pernambuco
dc.description.affiliationCentre of Agrarian Science Federal University of Alagoas, Alagoas
dc.description.affiliationUnespDepartment of Biodiversity Institute of Biosciences São Paulo State University—UNESP, Av. 24A, 1515, Rio Claro
dc.description.sponsorshipCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
dc.description.sponsorshipFundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
dc.description.sponsorshipConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
dc.description.sponsorshipIdCAPES: 001
dc.description.sponsorshipIdFAPESP: 2023/05323-4
dc.description.sponsorshipIdCNPq: 309558/2021-2
dc.description.sponsorshipIdCNPq: 402622/2021-9
dc.identifierhttp://dx.doi.org/10.1016/j.jenvman.2024.121959
dc.identifier.citationJournal of Environmental Management, v. 367.
dc.identifier.doi10.1016/j.jenvman.2024.121959
dc.identifier.issn1095-8630
dc.identifier.issn0301-4797
dc.identifier.scopus2-s2.0-85199697438
dc.identifier.urihttps://hdl.handle.net/11449/303933
dc.language.isoeng
dc.relation.ispartofJournal of Environmental Management
dc.sourceScopus
dc.subjectDry forest
dc.subjectLand use
dc.subjectSurface energy budget
dc.subjectTurbulent heat fluxes
dc.titleCan changes in land use in a semi-arid region of Brazil cause seasonal variation in energy partitioning and evapotranspiration?en
dc.typeArtigopt
dspace.entity.typePublication
unesp.author.orcid0000-0001-7094-3635[2]
unesp.author.orcid0000-0003-1946-0421[4]
unesp.author.orcid0000-0001-9706-5983[8]
unesp.author.orcid0000-0002-1318-2320[10]
unesp.author.orcid0000-0001-5265-8988[11]
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Biociências, Rio Claropt

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