Resumo -O objetivo deste trabalho foi mapear a evapotranspiração real (ETr) e determinar o volume de água utilizado no projeto de irrigação de São Gonçalo, PB, no Semiárido brasileiro, com auxílio do sensoriamento remoto. Foram adquiridas imagens TM/Landsat 5 da área em estudo, em 2008, que foram utilizadas na obtenção dos mapas temáticos da ETr diária. Selecionaram-se dois pomares de coqueiro-anão para validação dos resultados da evapotranspiração obtida com o "surface energy balance algorithm for land" (ET Sebal ) e com o método FAO-56 (ET FAO ). Para determinação da ET FAO , utilizou-se o produto entre o coeficiente de cultura, o coeficiente de ajuste e a evapotranspiração de referência. As diferenças obtidas, com uso das duas técnicas, resultaram em raiz do erro quadrado médio, erro relativo médio e erro absoluto médio iguais a 0,53 mm, 9,46% e 0,43 mm, respectivamente. Nas áreas irrigadas, a ETr representou 85% do saldo de radiação e, nas de sequeiro, apenas 12,5%. O mapeamento da ETr delimitou claramente as áreas irrigadas das de sequeiro, bem como as diferenças existentes no interior do perímetro irrigado do projeto em investigação. O volume de água empregado no projeto de irrigação representa, somente no período de julho a dezembro, mais de 60% da capacidade do açude de São Gonçalo.Termos para indexação: albedo, Landsat 5, saldo de radiação, temperatura da superfície. Evapotranspiration and assessment of water consumed in irrigated area of the Brazilian Semiarid Region by remote sensingAbstract -The objective of this work was to map the actual evapotranspiration (ETr) and to determine the volume of water used in the irrigation project of São Gonçalo, PB, in the Brazilian Semiarid Region, using remote sensing. TM/Landsat 5 images were acquired from the study area, in 2008, and were used to obtain thematic maps of daily ETr. Two dwarf coconut crops were selected for validation of the results of evapotranspiration obtained by the surface energy balance algorithm for land (ET Sebal ) and the FAO-56 method (ET FAO ). In order to determine ET FAO , the product between the culture coefficient, the adjustment coefficient, and the reference evapotranspiration was used. The differences obtained by the two techniques resulted in root mean square error, mean relative error, and mean absolute error equal to 0.53 mm, 9.46%, and 0.43 mm, respectively. In the irrigated areas, ETr represented about 85% of net radiation and, in rainfed plots, only 12.5%. The mapping of ETr clearly delimitated the irrigated and nonirrigated plots, as well as the differences within the irrigated perimeter of the project under investigation. The volume of water applied in the irrigation project, only in the period from July to December, represents more than 60% of the capacity of the São Gonçalo reservoir.
Resumo -O objetivo deste trabalho foi avaliar quantitativamente os parâmetros biofísicos obtidos por sensoriamento remoto, para a área de abrangência da Bacia Hidrográfica do Rio Tapacurá Quantitative analysis of biophysical parameters of watershed by remote sensingAbstract -The objective of this work was to quantitatively evaluate the biophysical parameters, obtained by remote sensing, for the range area of the Tapacurá River Basin, in Pernambuco state, Brazil. Landsat 5-TM images of 7/10/1989, 7/6/2005, and 8/29/2007 were used. The images were registered with a polynomial geometric correction of first order. Radiometric calibration, reflectance, transmittance and planetary albedo were calculated and, subsequently, thematic maps of surface albedo, surface temperature and enhanced vegetation index (EVI) were generated. The surface albedo showed increasing average values between the 1989 and 2005 images, which indicates the urban territorial expansion. The image of 8/29/2007 showed the highest land surface temperature, followed by the temperatures showed in the images of 7/10/1989 and 7/6/2005, and the highest values were those of the urban networks. The 1989 image showed the highest average value for EVI, which indicates that there was a higher vegetation presence in that date.
RESUMOAs trocas de energia na interface solo-planta-atmosfera, por meio das componentes do balanço de radiação (Rn) e dos fluxos de calor no solo (G), sensível (H) e latente (LE), são essenciais para a modelagem climática e hidrológica que, por sua vez, afetam toda a biosfera. Dessa forma, esta pesquisa teve por objetivos: (1) estimar e comparar o comportamento dos componentes do balanço de energia, usando o algoritmo SEBAL -Surface Energy Balance Algorithm for Land, em diferentes tipos de uso e cobertura do solo e (2) validar o algoritmo. Para isso, foram usadas três imagens TM -Landsat 5 de órbita e ponto 214/066, com datas de passagem em 26 de agosto de 2006, 6 de setembro de 2010 e 28 de janeiro de 2011, todas recortadas para enquadrar o litoral sul de Pernambuco. Os resultados mostraram a capacidade do SEBAL de estimar a variabilidade espacial dos diferentes componentes do balanço de energia, com capacidade de distinguir diferentes ocupações do solo. O cômputo do balanço de energia possibilita observar as formas diferenciadas do uso da energia pelos diferentes tipos de cobertura do solo e verificar aqueles que propiciam melhor conforto térmico. As estimativas da evapotranspiração obtidas pelo algoritmo SEBAL apresentaram uma boa concordância com os resultados obtidos pelo método da FAO-Penman-Monteith demonstrando, dessa forma, a potencialidade da abordagem metodológica escolhida. Palavras-chave: SEBAL, balanço de energia, evapotranspiração. ABSTRACT: ASSESSMENT OF ENERGY BALANCE USING TM -LANDSAT 5 DIGITAL IMAGES AND SEBAL ALGORITHM OVER THE SOUTHERN PERNAMBUCO SEACOASTThe energy exchange across soil vegetation-atmosphere interface through the net radiation components (Rn) the soil heat flux (G), sensible heat flux (H) and latent heat flux (LE) are of vital importance for the climatic and hydrologic modeling, which affects all biosphere. The main objectives of this research are: (1) to estimate and compare the several energy balance components behavior, using SEBAL algorithm, under different soil usages; and (2) to validate SEBAL algorithm. In order to make the analysis, three TM -Landsat 5 images, from orbit and point 214/066, the South Coast of Pernambuco State (Brazil) were used. The results showed the ability of SEBAL to estimate the spatial variability of the different components of energy balance, with the ability to distinguish different soil occupations. The calculation of the energy balance components allows to figure the different forms of energy usages by different soil coverage and to find those that provide better thermal comfort. Estimates of evapotranspiration obtained by the algorithm SEBAL showed a good agreement with the results obtained by the FAO-Penman-Monteith, thus demonstrating the potential of this methodological approach.
O sensoriamento remoto possibilita identificar alterações que ocorrem na superfície terrestre, resultantes de fenômenos naturais e/ou antrópicos, muitas das quais podem ser diagnosticadas a partir do monitoramento das trocas radiativas à superfície. Neste sentido, o presente estudo objetiva determinar o saldo da radiação à superfície apenas com o emprego de imagens TM-Landsat 5, na Ilha do Bananal, TO. Foram selecionadas imagens de 2005 sem presença de nuvens e gerados mapas do saldo de radiação instantâneo e diário utilizando-se o algoritmo SEBAL. Os dados obtidos foram validados com medições realizadas no interior da área estudada. O saldo de radiação instantâneo médio situou-se entre 488 e 535 W m-2; enquanto a variação espacial do saldo de radiação diário - Rn24h médio, foi de 132,7 a 145,3 W m-2. As áreas antropizadas apresentaram redução no saldo radiativo. O Erro Médio Relativo, Médio Absoluto e a Raiz do Erro Quadrático Médio, associados ao Rn24h apresentaram valores de 1,95%, 2,78 W m-2 e 3,36 W m-2; respectivamente, evidenciando a importância da técnica empregada.
Evapotranspiration (ET) is normally considered as the sum of all water that evaporates from the soil and transpires from plants. However, accurately estimating ET from complex landscapes can be difficult because of its high spatial heterogeneity and diversity of driver factors, which make extrapolation of data from a point to a larger area quite inaccurate. In this paper, we hypothesize that MODIS products can be of use to estimate ET in areas of Caatinga vegetation, the hydrology of which has not been adequately studied. The experiment was conducted in a preserved level area of Caatinga in which meteorological and water flux measures were taken throughout 2012 by eddy covariance. Evapotranspiration estimates from eddy covariance were compared with remotely sensed evapotranspiration estimates from MOD16A2 and SAFER products. Correlations were performed at monthly, 8-day, and daily scales; and producedr2values of monthly scale = 0.92, 8-day scale = 0.88, and daily scale = 0.85 for the SAFER algorithm. Monthly MOD16A2 data produced a value ofr2=0.82, and they may be useful because they are free, downloadable, and easy to use by researchers and governments.
Reliable information on vegetation cover and its dynamics over time is essential for managing life, resources, and supporting policies. Although many related initiatives have been undertaken in Brazil since the 1980s, knowledge about its dry forests is still limited. In this study, we address the drivers of deforestation and their threat to the Brazilian dry forest called Caatinga. We evaluated the land cover dynamics and landscape metrics in the watershed of the Pontal River, as it has become one of the most socially and environmentally important areas in Brazil. The overall process consists of a systematic sampling grid of hydrological samples, where Landsat images (1975 to 2013) combined with the FRAGSTATS package were used to evaluate landscape metrics indices for the Caatinga. Data showed that the relative area (RA) decreased from 90.25% to 60.98% over the 38-year period, while fragmentation (PD) presented an increasing bias. In addition, the spatial distribution of both indices became more heterogeneous and clustered in the north. We suggest that appropriateness of land for farming was the leading cause of deforestation; rainfall is 112% more intense in the north of the watershed than in the south. Therefore, the northern fauna and flora have been significantly altered and reduced. The relationship between deforestation and time shows an increasing threat. Further studies evaluating these causes are needed to improve our understanding of the vegetation dynamics in this region.
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