A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas

Detalhes bibliográficos
Autor(a) principal: Ruhoff, Anderson Luis
Data de Publicação: 2012
Outros Autores: Paz, Adriano Rolim da, Collischonn, Walter, Aragao, Luiz E.O.C., Rocha, Humberto Ribeiro da, Malhi, Yadvinder S.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UFRGS
Texto Completo: http://hdl.handle.net/10183/246904
Resumo: Evapotranspiration (ET) plays an important role in global climate dynamics and in primary production of terrestrial ecosystems; it represents the mass and energy transfer from the land to atmosphere. Limitations to measuring ET at large scales using ground-based methods have motivated the development of satellite remote sensing techniques. The purpose of this work is to evaluate the accuracy of the SEBAL algorithm for estimating surface turbulent heat fluxes at regional scale, using 28 images from MODIS. SEBAL estimates are compared with eddy-covariance (EC) measurements and results from the hydrological model MGB-IPH. SEBAL instantaneous estimates of latent heat flux (LE) yielded r 2= 0.64 and r2 = 0.62 over sugarcane croplands and savannas when compared against in situ EC estimates. At the same sites, daily aggregated estimates of LE were r 2 = 0.76 and r2 = 0.66, respectively. Energy balance closure showed that turbulent fluxes over sugarcane croplands were underestimated by 7% and 9% over savannas. Average daily ET from SEBAL is in close agreement with estimates from the hydrological model for an overlay of 38,100 km2 (r2 = 0.88). Inputs to which the algorithm is most sensitive are vegetation index (NDVI), gradient of temperature (dT) to compute sensible heat flux (H) and net radiation (Rn). It was verified that SEBAL has a tendency to overestimate results both at local and regional scales probably because of low sensitivity to soil moisture and water stress. Nevertheless the results confirm the potential of the SEBAL algorithm, when used with MODIS images for estimating instantaneous LE and daily ET from large areas.
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spelling Ruhoff, Anderson LuisPaz, Adriano Rolim daCollischonn, WalterAragao, Luiz E.O.C.Rocha, Humberto Ribeiro daMalhi, Yadvinder S.2022-08-16T04:46:08Z20122072-4292http://hdl.handle.net/10183/246904000824109Evapotranspiration (ET) plays an important role in global climate dynamics and in primary production of terrestrial ecosystems; it represents the mass and energy transfer from the land to atmosphere. Limitations to measuring ET at large scales using ground-based methods have motivated the development of satellite remote sensing techniques. The purpose of this work is to evaluate the accuracy of the SEBAL algorithm for estimating surface turbulent heat fluxes at regional scale, using 28 images from MODIS. SEBAL estimates are compared with eddy-covariance (EC) measurements and results from the hydrological model MGB-IPH. SEBAL instantaneous estimates of latent heat flux (LE) yielded r 2= 0.64 and r2 = 0.62 over sugarcane croplands and savannas when compared against in situ EC estimates. At the same sites, daily aggregated estimates of LE were r 2 = 0.76 and r2 = 0.66, respectively. Energy balance closure showed that turbulent fluxes over sugarcane croplands were underestimated by 7% and 9% over savannas. Average daily ET from SEBAL is in close agreement with estimates from the hydrological model for an overlay of 38,100 km2 (r2 = 0.88). Inputs to which the algorithm is most sensitive are vegetation index (NDVI), gradient of temperature (dT) to compute sensible heat flux (H) and net radiation (Rn). It was verified that SEBAL has a tendency to overestimate results both at local and regional scales probably because of low sensitivity to soil moisture and water stress. Nevertheless the results confirm the potential of the SEBAL algorithm, when used with MODIS images for estimating instantaneous LE and daily ET from large areas.application/pdfengRemote Sensing. Basel : MDPI AG, 2012. Vol. 4, n. 3 (Mar. 2012), p. 703-725EvapotranspiraçãoModelos hidrológicosSensoriamento remotoBiomasEvapotranspirationHydrological modellingMODISSEBALTropical biomesA MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannasEstrangeiroinfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da UFRGSinstname:Universidade Federal do Rio Grande do Sul (UFRGS)instacron:UFRGSTEXT000824109.pdf.txt000824109.pdf.txtExtracted Texttext/plain59904http://www.lume.ufrgs.br/bitstream/10183/246904/2/000824109.pdf.txtb7d2f0ac8151f60fa05dd42f931ee3a7MD52ORIGINAL000824109.pdfTexto completo (inglês)application/pdf1412453http://www.lume.ufrgs.br/bitstream/10183/246904/1/000824109.pdf2749bcde46ad5e5d8bd3c4fb5ba759baMD5110183/2469042022-08-17 04:47:23.20421oai:www.lume.ufrgs.br:10183/246904Repositório de PublicaçõesPUBhttps://lume.ufrgs.br/oai/requestopendoar:2022-08-17T07:47:23Repositório Institucional da UFRGS - Universidade Federal do Rio Grande do Sul (UFRGS)false
dc.title.pt_BR.fl_str_mv A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
title A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
spellingShingle A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
Ruhoff, Anderson Luis
Evapotranspiração
Modelos hidrológicos
Sensoriamento remoto
Biomas
Evapotranspiration
Hydrological modelling
MODIS
SEBAL
Tropical biomes
title_short A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
title_full A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
title_fullStr A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
title_full_unstemmed A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
title_sort A MODIS-based energy balance to estimate evapotranspiration for clear-sky days in Brazilian tropical savannas
author Ruhoff, Anderson Luis
author_facet Ruhoff, Anderson Luis
Paz, Adriano Rolim da
Collischonn, Walter
Aragao, Luiz E.O.C.
Rocha, Humberto Ribeiro da
Malhi, Yadvinder S.
author_role author
author2 Paz, Adriano Rolim da
Collischonn, Walter
Aragao, Luiz E.O.C.
Rocha, Humberto Ribeiro da
Malhi, Yadvinder S.
author2_role author
author
author
author
author
dc.contributor.author.fl_str_mv Ruhoff, Anderson Luis
Paz, Adriano Rolim da
Collischonn, Walter
Aragao, Luiz E.O.C.
Rocha, Humberto Ribeiro da
Malhi, Yadvinder S.
dc.subject.por.fl_str_mv Evapotranspiração
Modelos hidrológicos
Sensoriamento remoto
Biomas
topic Evapotranspiração
Modelos hidrológicos
Sensoriamento remoto
Biomas
Evapotranspiration
Hydrological modelling
MODIS
SEBAL
Tropical biomes
dc.subject.eng.fl_str_mv Evapotranspiration
Hydrological modelling
MODIS
SEBAL
Tropical biomes
description Evapotranspiration (ET) plays an important role in global climate dynamics and in primary production of terrestrial ecosystems; it represents the mass and energy transfer from the land to atmosphere. Limitations to measuring ET at large scales using ground-based methods have motivated the development of satellite remote sensing techniques. The purpose of this work is to evaluate the accuracy of the SEBAL algorithm for estimating surface turbulent heat fluxes at regional scale, using 28 images from MODIS. SEBAL estimates are compared with eddy-covariance (EC) measurements and results from the hydrological model MGB-IPH. SEBAL instantaneous estimates of latent heat flux (LE) yielded r 2= 0.64 and r2 = 0.62 over sugarcane croplands and savannas when compared against in situ EC estimates. At the same sites, daily aggregated estimates of LE were r 2 = 0.76 and r2 = 0.66, respectively. Energy balance closure showed that turbulent fluxes over sugarcane croplands were underestimated by 7% and 9% over savannas. Average daily ET from SEBAL is in close agreement with estimates from the hydrological model for an overlay of 38,100 km2 (r2 = 0.88). Inputs to which the algorithm is most sensitive are vegetation index (NDVI), gradient of temperature (dT) to compute sensible heat flux (H) and net radiation (Rn). It was verified that SEBAL has a tendency to overestimate results both at local and regional scales probably because of low sensitivity to soil moisture and water stress. Nevertheless the results confirm the potential of the SEBAL algorithm, when used with MODIS images for estimating instantaneous LE and daily ET from large areas.
publishDate 2012
dc.date.issued.fl_str_mv 2012
dc.date.accessioned.fl_str_mv 2022-08-16T04:46:08Z
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dc.relation.ispartof.pt_BR.fl_str_mv Remote Sensing. Basel : MDPI AG, 2012. Vol. 4, n. 3 (Mar. 2012), p. 703-725
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