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| Registros recuperados : 427 | |
| 161. |  | BRANDÃO. E. O.; MOURA, M. S. B. de; SOARES, J. M.; SOUZA, L. S. B.; SILVA, T. G. F. da. Cobertura plástica da videira: evolução do crescimento de ramos e cachos e da área foliar no Submédio São Francisco. In: CONGRESSO BRASILEIRO DE ENGENHARIA AGRICOLA, 38., 2009, Juazeiro, Petrolina. Planejamento da bacia hidrográfica e o desenvolvimento da agricultura: anais. Juazeiro, Petrolina: UNIVASF: Embrapa Semiárido: CEFET: SBEA, 2009. 1 CD-ROM.| Biblioteca(s): Embrapa Semiárido. |
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| 162. | | ANGELOTTI, F.; PETRERE, V. G.; TEIXEIRA, A. H. de C.; SA, I. B.; MOURA, M. S. B. de. Cenários de mudanças climáticas para o semiárido brasileiro. In: SA, I. B.; SILVA, P. C. G. da. (Ed.). Semiárido brasileiro: pesquisa, desenvolvimento e inovação. Petrolina: Embrapa Semiárido, 2010. cap. 5, p. 159-197. il.| Biblioteca(s): Embrapa Semiárido. |
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| 164. | | BRITO, L. T. de L.; PEREIRA, L. A.; MOURA, M. S. B. de; CAVALCANTI, N. de B. Características físicas e agroclimáticas de açudes da microbacia do Riacho Pontal, em Petrolina, PE. In: SIMPÓSIO BRASILEIRO DE CAPTAÇÃO E MANEJO DE ÁGUA DE CHUVA, 8., 2012, Campina Grande. Aproveitamento da água de chuva em diferentes setores e escalas: desafio da gestão integrada. Campina Grande: ABCMAC: INSA: UEPB: UFCG: IRPAA; Petrolina: Embrapa Semiárido, 2012. 1 CD-ROM.| Biblioteca(s): Embrapa Semiárido. |
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| 165. | | CARVALHO, H. F. de S.; MOURA, M. S. B. de; SILVA, T. G. F. da; RODRIGUES, C. T. A. Microclima em áreas de Caatinga preservada e cana-de-açúcar irrigada no Semiárido brasileiro. In: CONGRESSO BRASILEIRO DE AGROMETEOROLOGIA, 20; SIMPÓSIO DE MUDANÇAS CLIMÁTICAS E DESERTIFICAÇÃO NO SEMIÁRIDO BRASILEIRO, 5., 2017, Juazeiro, BA. A agrometeorologia na solução de problemas multiescala: anais. Petrolina: Embrapa Semiárido; Juazeiro: UNIVASF; Campinas: Sociedade Brasileira de Agrometeorologia, 2017. 1 CD-ROM.| Biblioteca(s): Embrapa Semiárido. |
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| 169. | | MOURA, M. S. B. de; SILVA, T. G. F. da; SOUZA, L. S. B. de; TAURA, T. A. Onde e quando plantar palma-forrageira. In: VOLTOLINI, T. V.; OLIVEIRA, A. R. de; SALVIANO, A. M.; MOURA, M. S. B. de; ARAÚJO, G. G. L. de (ed.). Sistema de produção de palma-forrageira para o Estado da Paraíba. Petrolina: Embrapa Semiárido, 2022. (Embrapa Semiárido. Sistema de Produção, 14).| Biblioteca(s): Embrapa Semiárido. |
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| 172. | | SOUZA, L. S. B.; MOURA, M. S. B. de; SEDIYAMA, G. C.; SILVA, T. G. F. da; BRANDÃO, E. O. Determinação do coeficiente de cultura do milho (Zea mays L.) sob condições de semiárido brasileiro. In: CONGRESSO BRASILEIRO DE METEOROLOGIA, 16., 2010, Belém, PA. A Amazônia e o clima global: anais. Belém, PA: SBMET, 2010. 1 CD-ROM.| Biblioteca(s): Embrapa Semiárido. |
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| 178. | | RAMOS, R. R. D.; MOURA, M. S. B. de; SILVA, T. G. F. da; GALVINCIO, J. D. Evapotranspiração da cana-de-açúcar utilizando o Simple Algorithm for Evapotranspiration Retrieving (SAFER) no Vale São Francisco. In: CONGRESSO BRASILEIRO DE AGROMETEOROLOGIA, 20; SIMPÓSIO DE MUDANÇAS CLIMÁTICAS E DESERTIFICAÇÃO NO SEMIÁRIDO BRASILEIRO, 5., 2017, Juazeiro, BA. A agrometeorologia na solução de problemas multiescala: anais. Petrolina: Embrapa Semiárido; Juazeiro: UNIVASF; Campinas: Sociedade Brasileira de Agrometeorologia, 2017. 1 CD-ROM.| Biblioteca(s): Embrapa Semiárido. |
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| Registros recuperados : 427 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Semiárido. |
|
Data corrente: |
18/11/2019 |
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Data da última atualização: |
01/10/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
MIRANDA, R. de Q.; NÓBREGA, R. L. B.; MOURA, M. S. B. de; RAGHAVANE, S.; GALVÍNCIO, J. D. |
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Afiliação: |
Rodrigo de Queiroga Miranda, UFPE; Rodolfo Luiz Bezerra Nóbrega, University of Reading, Reading, UK; MAGNA SOELMA BESERRA DE MOURA, CPATSA; Srinivasan Raghavane, Texas A&M University, College Station, TX, USA; Josiclêda Domiciano Galvíncio, UFPE. |
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Título: |
Realistic and simplified models of plant and leaf area indices for a seasonally dry tropical forest. |
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Ano de publicação: |
2020 |
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Fonte/Imprenta: |
International Journal of Applied Earth Observation and Geoinformation, v. 85, 2020. |
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DOI: |
10.1016/j.jag.2019.101992 |
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Idioma: |
Inglês |
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Conteúdo: |
Leaf Area Index (LAI) models that consider all phenological stages have not been developed for the Caatinga, the largest seasonally dry tropical forest in South America. LAI models that are currently used show moderate to high covariance when compared to in situ data, but they often lack accuracy in the whole spectra of possible values and do not consider the impact that the stems and branches have over LAI estimates, which is of great influence in the Caatinga. In this study, we develop and assess PAI (Plant Area Index) and LAI models by using ground-based measurements and satellite (Landsat) data. The objective of this study was to create and test new empirical models using a multi-year and multi-source of reflectance data. The study was based on measurements of photosynthetic photon flux density (PPFD) from above and below the canopy during the periods of 2011?2012 and 2016?2018. Through iterative processing, we obtained more than a million candidate models for estimating PAI and LAI. To clean up the small discrepancies in the extremes of each interpolated series, we smoothed out the dataset by fitting a logarithmic equation with the PAI data and the inverse contribution of WAI (Wood Area Index) to PAI, that is the portion of PAI that is actually LAI (LAIC). LAIC can be calculated as follows: LAIC = 1 (WAI/PAI)). We subtracted the WAI values from the PAI to develop our in situ LAI dataset that was used for further analysis. Our in situ dataset was also used as a reference to compare our models with four other models used for the Caatinga, as well as the MODIS-derived LAI products (MCD15A3H/A2H). Our main findings were as follows: (i) Six models use NDVI (Normalized Difference Vegetation Index), SAVI (Soil-Adjusted Vegetation Index) and EVI (Enhanced Vegetation Index) as input, and performed well, with r2 ranging from 0.77 to 0.79 (PAI) and 0.76 to 0.81 (LAI), and RMSE with a minimum of 0.41m2m?2 (PAI) and 0.40m2m?2 (LAI). The SAVI models showed values 20% and 32% (PAI), and 21% and 15% (LAI) smaller than those found for the models that use EVI and NDVI, respectively; (ii) the other models (ten) use only two bands, and in contrast to the first six models, these new models may abstract other physical processes and components, such as leaves etiolation and increasing protochlorophyll. The developed models used the near-infrared band, and they varied only in relation to the inclusion of the red, green, and blue bands. (iii) All previously published models and MODIS-LAI underperformed against our calibrated models. Our study was able to provide several PAI and LAI models that realistically represent the phenology of the Caatinga. MenosLeaf Area Index (LAI) models that consider all phenological stages have not been developed for the Caatinga, the largest seasonally dry tropical forest in South America. LAI models that are currently used show moderate to high covariance when compared to in situ data, but they often lack accuracy in the whole spectra of possible values and do not consider the impact that the stems and branches have over LAI estimates, which is of great influence in the Caatinga. In this study, we develop and assess PAI (Plant Area Index) and LAI models by using ground-based measurements and satellite (Landsat) data. The objective of this study was to create and test new empirical models using a multi-year and multi-source of reflectance data. The study was based on measurements of photosynthetic photon flux density (PPFD) from above and below the canopy during the periods of 2011?2012 and 2016?2018. Through iterative processing, we obtained more than a million candidate models for estimating PAI and LAI. To clean up the small discrepancies in the extremes of each interpolated series, we smoothed out the dataset by fitting a logarithmic equation with the PAI data and the inverse contribution of WAI (Wood Area Index) to PAI, that is the portion of PAI that is actually LAI (LAIC). LAIC can be calculated as follows: LAIC = 1 (WAI/PAI)). We subtracted the WAI values from the PAI to develop our in situ LAI dataset that was used for further analysis. Our in situ dataset was also used as a reference... Mostrar Tudo |
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Palavras-Chave: |
Índice de área arborizada; Índice de área foliar; Plant Area Index; Semiárido. |
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Thesagro: |
Caatinga; Fenologia; Floresta Tropical. |
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Thesaurus NAL: |
Landsat; Phenology; Tropical forests. |
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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/item/204857/1/Realistic-and-simplified-models-of-plant-2019.pdf
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Marc: |
LEADER 03602naa a2200301 a 4500
001 2114427
005 2021-10-01
008 2020 bl uuuu u00u1 u #d
024 7 $a10.1016/j.jag.2019.101992$2DOI
100 1 $aMIRANDA, R. de Q.
245 $aRealistic and simplified models of plant and leaf area indices for a seasonally dry tropical forest.$h[electronic resource]
260 $c2020
520 $aLeaf Area Index (LAI) models that consider all phenological stages have not been developed for the Caatinga, the largest seasonally dry tropical forest in South America. LAI models that are currently used show moderate to high covariance when compared to in situ data, but they often lack accuracy in the whole spectra of possible values and do not consider the impact that the stems and branches have over LAI estimates, which is of great influence in the Caatinga. In this study, we develop and assess PAI (Plant Area Index) and LAI models by using ground-based measurements and satellite (Landsat) data. The objective of this study was to create and test new empirical models using a multi-year and multi-source of reflectance data. The study was based on measurements of photosynthetic photon flux density (PPFD) from above and below the canopy during the periods of 2011?2012 and 2016?2018. Through iterative processing, we obtained more than a million candidate models for estimating PAI and LAI. To clean up the small discrepancies in the extremes of each interpolated series, we smoothed out the dataset by fitting a logarithmic equation with the PAI data and the inverse contribution of WAI (Wood Area Index) to PAI, that is the portion of PAI that is actually LAI (LAIC). LAIC can be calculated as follows: LAIC = 1 (WAI/PAI)). We subtracted the WAI values from the PAI to develop our in situ LAI dataset that was used for further analysis. Our in situ dataset was also used as a reference to compare our models with four other models used for the Caatinga, as well as the MODIS-derived LAI products (MCD15A3H/A2H). Our main findings were as follows: (i) Six models use NDVI (Normalized Difference Vegetation Index), SAVI (Soil-Adjusted Vegetation Index) and EVI (Enhanced Vegetation Index) as input, and performed well, with r2 ranging from 0.77 to 0.79 (PAI) and 0.76 to 0.81 (LAI), and RMSE with a minimum of 0.41m2m?2 (PAI) and 0.40m2m?2 (LAI). The SAVI models showed values 20% and 32% (PAI), and 21% and 15% (LAI) smaller than those found for the models that use EVI and NDVI, respectively; (ii) the other models (ten) use only two bands, and in contrast to the first six models, these new models may abstract other physical processes and components, such as leaves etiolation and increasing protochlorophyll. The developed models used the near-infrared band, and they varied only in relation to the inclusion of the red, green, and blue bands. (iii) All previously published models and MODIS-LAI underperformed against our calibrated models. Our study was able to provide several PAI and LAI models that realistically represent the phenology of the Caatinga.
650 $aLandsat
650 $aPhenology
650 $aTropical forests
650 $aCaatinga
650 $aFenologia
650 $aFloresta Tropical
653 $aÍndice de área arborizada
653 $aÍndice de área foliar
653 $aPlant Area Index
653 $aSemiárido
700 1 $aNÓBREGA, R. L. B.
700 1 $aMOURA, M. S. B. de
700 1 $aRAGHAVANE, S.
700 1 $aGALVÍNCIO, J. D.
773 $tInternational Journal of Applied Earth Observation and Geoinformation$gv. 85, 2020.
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Embrapa Semiárido (CPATSA) |
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