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| Registros recuperados : 181 | |
| 5. |  | LEIVAS, J. F.; TEIXEIRA, A. H. de C.; ANDRADE, R. G. Agrometeorologia. In: TÔSTO, S. G.; RODRIGUES, C. A. G.; BOLFE, E. L.; BATISTELLA, M. (Ed.). Geotecnologias e geoinformação. Brasília, DF: Embrapa, 2014. p. 107-118. (Coleção 500 Perguntas, 500 Respostas).| Biblioteca(s): Embrapa Territorial. |
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| 8. | | LEIVAS, J. F.; ANDRADE, R. G.; VICTORIA, D. de C.; BOLFE, E. L. Análise espaço-temporal do índice de vegetação em mesorregiões produtoras de milho safrinha. In: CONGRESSO BRASILEIRO DE AGROMETEOROLOGIA, 18., 2013, Belém, PA. Belém, PA: Sociedade Brasileira de Agrometeorologia, 2013. 6 p.| Biblioteca(s): Embrapa Territorial. |
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| 10. | | TEIXEIRA, A. H. DE C.; LEIVAS, J. F.; TAKEMURA, C. M.; GARCON, E. A. M. Aplicação do algoritmo SAFER para monitoramento da evapotranspiração nos Biomas brasileiros. In: SILVA, C. D. D. da; ROLIM, E. C. de A. (Org.). Aspectos e impactos ambientais: o que geram as atividades do homem? Ponta Grossa, PR: Atena, 2021. Publicado também em: TEIXEIRA, A. H. DE C.; LEIVAS, J. F.; TAKEMURA, C. M.; GARCON, E. A. M. Aplicação do algoritmo SAFER para monitoramento da evapotranspiração nos Biomas brasileiros. In: ENCONTRO DE RECURSOS HÍDRICOS EM SERGIPE,...| Biblioteca(s): Embrapa Territorial. |
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| 11. | | LEIVAS, J. F.; TEIXEIRA, A. H. de C.; SILVA, G. B. S. da. Aplicação de modelo agrometeorológico espectral no perímetro irrigado da bacia do São Francisco, utilizando imagens RAPIDEYE. In: SIMPÓSIO DA BACIA HIDROGRÁFICA DO RIO SÃO FRANCISCO, 1., 2016, Juazeiro, BA; Petrolina, PE. Anais... Juazeiro; Petrolina: CBHSF, 2016. 7 p.| Biblioteca(s): Embrapa Territorial. |
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| 17. | | LEIVAS, J. F.; TEIXEIRA, A. H. de C.; ANDRADE, R. G.; VICTORIA, D. de C. Estimativa da evapotranspiração, biomassa e produtividade da água em municípios produtores de trigo, no Rio Grande do Sul. In: SEMINÁRIO DA REDE AGROHIDRO, 2., 2014, Campinas. Impactos da agricultura e das mudanças climáticas nos recursos hídricos: anais... Campinas: Embrapa Informática Agropecuária, 2014. p. 126-130.| Biblioteca(s): Embrapa Trigo. |
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| 18. | | LEIVAS, J. F.; TEIXEIRA, A. H. de C.; ANDRADE, R. G.; VICTORIA, D. de C. Estimativa da evapotranspiração, biomassa e produtividade da água em municípios produtores de trigo, no Rio Grande do Sul. In: SEMINÁRIO DA REDE AGROHIDRO, 2., 2014, Campinas. Impactos da agricultura e das mudanças climáticas nos recursos hídricos: anais... Campinas: Embrapa Informática Agropecuária, 2014. p. 126-130.| Biblioteca(s): Embrapa Territorial. |
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| Registros recuperados : 181 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Territorial. |
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Data corrente: |
03/11/2023 |
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Data da última atualização: |
03/11/2023 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 2 |
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Autoria: |
FARIAS, F.; TEIXEIRA, A. H. de C.; SOUSA, I.; LEIVAS, J. F.; TAKEMURA, C. M.; GARCON, E. A. M. |
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Afiliação: |
FRANZONE FARIAS, UNIVERSIDADE FEDERAL DE SERGIPE; ANTONIO HERIBERTO DE C TEIXEIRA, UNIVERSIDADE DE SERGIPE; INAJÁ SOUSA, UNIVERSIDADE DE SERGIPE; JANICE FREITAS LEIVAS, CNPM; CELINA MAKI TAKEMURA, CNPM; EDLENE APARECIDA MONTEIRO GARCON, CNPM. |
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Título: |
Large-scale water balance modeling using remote sensing and weather data: Application in an agricultural growing region of the coastal northeast Brazil. |
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Ano de publicação: |
2023 |
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Fonte/Imprenta: |
Remote Sensing Applications: Society and Environment, v. 32, e101072, 2023. |
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ISSN: |
2352-9385 |
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DOI: |
https://doi.org/10.1016/j.rsase.2023.101072 |
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Idioma: |
Inglês |
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Conteúdo: |
ABSTRACT: The SAFER (Simple Algorithm for Evapotranspiration Retrieving) algorithm was applied to test water balance (WB) monitoring in the agricultural growing region of SEALBA, an acronym for the states Sergipe (SE), Alagoas (AL), and Bahia (BA), coastal Northeast Brazil, classifying the biomes Atlantic Forest and Caatinga. The MODIS MOD13Q1 reflectance product and meteorological data were used to calculate actual (ET) and reference (ET0 ) evapotranspiration at 16-day timescale along the years 2007?2021. The period with the highest precipitation (P) is in May, when the 16- day values are above 90 mm in Atlantic Forest and higher than 70 mm in Caatinga. For ET, the largest rates occur between July and September, when the 16-day average surpass 2.70 mm d −1 in the Atlantic Forest and 2.90 mm d −1 in Caatinga. Larger P together with lower ET, concentrates the positive water balance - WB (P ? ET) from March to August in both biomes, bringing suitability for the rainfed agriculture. However, from July to December occur the negative WB values, indicating the need of irrigation for critical crop stages. Inferring the root-zone moisture conditions throughout the evaporative fraction values (ETf = ET/ET0 ) it is noticed that their highest values occur from April to October, evidencing a delay between the moment in which rainfall attend evapotranspiration with that in which the root-zone moisture recovers the optimum levels after the driest periods, what was also confirmed by the Pearson correlation coefficient values. The large-scale modelling carried out in SEALBA, presented viability to subsidize public policies regarding the water resources, with potential for replication of the methods in other regions. MenosABSTRACT: The SAFER (Simple Algorithm for Evapotranspiration Retrieving) algorithm was applied to test water balance (WB) monitoring in the agricultural growing region of SEALBA, an acronym for the states Sergipe (SE), Alagoas (AL), and Bahia (BA), coastal Northeast Brazil, classifying the biomes Atlantic Forest and Caatinga. The MODIS MOD13Q1 reflectance product and meteorological data were used to calculate actual (ET) and reference (ET0 ) evapotranspiration at 16-day timescale along the years 2007?2021. The period with the highest precipitation (P) is in May, when the 16- day values are above 90 mm in Atlantic Forest and higher than 70 mm in Caatinga. For ET, the largest rates occur between July and September, when the 16-day average surpass 2.70 mm d −1 in the Atlantic Forest and 2.90 mm d −1 in Caatinga. Larger P together with lower ET, concentrates the positive water balance - WB (P ? ET) from March to August in both biomes, bringing suitability for the rainfed agriculture. However, from July to December occur the negative WB values, indicating the need of irrigation for critical crop stages. Inferring the root-zone moisture conditions throughout the evaporative fraction values (ETf = ET/ET0 ) it is noticed that their highest values occur from April to October, evidencing a delay between the moment in which rainfall attend evapotranspiration with that in which the root-zone moisture recovers the optimum levels after the driest periods, what was also confirm... Mostrar Tudo |
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Palavras-Chave: |
Precipitation; SAFER; SEALBA. |
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Thesaurus NAL: |
Evapotranspiration; Water resources. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1157757/1/6174.pdf
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Marc: |
LEADER 02604naa a2200265 a 4500
001 2157757
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008 2023 bl uuuu u00u1 u #d
022 $a2352-9385
024 7 $ahttps://doi.org/10.1016/j.rsase.2023.101072$2DOI
100 1 $aFARIAS, F.
245 $aLarge-scale water balance modeling using remote sensing and weather data$bApplication in an agricultural growing region of the coastal northeast Brazil.$h[electronic resource]
260 $c2023
520 $aABSTRACT: The SAFER (Simple Algorithm for Evapotranspiration Retrieving) algorithm was applied to test water balance (WB) monitoring in the agricultural growing region of SEALBA, an acronym for the states Sergipe (SE), Alagoas (AL), and Bahia (BA), coastal Northeast Brazil, classifying the biomes Atlantic Forest and Caatinga. The MODIS MOD13Q1 reflectance product and meteorological data were used to calculate actual (ET) and reference (ET0 ) evapotranspiration at 16-day timescale along the years 2007?2021. The period with the highest precipitation (P) is in May, when the 16- day values are above 90 mm in Atlantic Forest and higher than 70 mm in Caatinga. For ET, the largest rates occur between July and September, when the 16-day average surpass 2.70 mm d −1 in the Atlantic Forest and 2.90 mm d −1 in Caatinga. Larger P together with lower ET, concentrates the positive water balance - WB (P ? ET) from March to August in both biomes, bringing suitability for the rainfed agriculture. However, from July to December occur the negative WB values, indicating the need of irrigation for critical crop stages. Inferring the root-zone moisture conditions throughout the evaporative fraction values (ETf = ET/ET0 ) it is noticed that their highest values occur from April to October, evidencing a delay between the moment in which rainfall attend evapotranspiration with that in which the root-zone moisture recovers the optimum levels after the driest periods, what was also confirmed by the Pearson correlation coefficient values. The large-scale modelling carried out in SEALBA, presented viability to subsidize public policies regarding the water resources, with potential for replication of the methods in other regions.
650 $aEvapotranspiration
650 $aWater resources
653 $aPrecipitation
653 $aSAFER
653 $aSEALBA
700 1 $aTEIXEIRA, A. H. de C.
700 1 $aSOUSA, I.
700 1 $aLEIVAS, J. F.
700 1 $aTAKEMURA, C. M.
700 1 $aGARCON, E. A. M.
773 $tRemote Sensing Applications: Society and Environment$gv. 32, e101072, 2023.
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