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dc.contributor.authorRodrigues, Italo Sampaio-
dc.contributor.authorCosta, Carlos Alexandre Gomes-
dc.contributor.authorLima Neto, Iran Eduardo-
dc.contributor.authorHopkinson, Christopher-
dc.date.accessioned2023-06-23T12:51:51Z-
dc.date.available2023-06-23T12:51:51Z-
dc.date.issued2021-
dc.identifier.citationRODRIGUES, Italo Sampaio; COSTA, Carlos Alexandre Gomes; LIMA NETO, Iran Eduardo; HOPKINSON, Christopher. Trends of evaporation in Brazilian tropical reservoirs using remote sensing. Journal of Hydrology, [S. l.], v. 598, n. 126473, p. 1-13, 2021.pt_BR
dc.identifier.issn0022-1694-
dc.identifier.urihttp://www.repositorio.ufc.br/handle/riufc/73027-
dc.description.abstractThis paper aims to analyze the trends (Mann-Kendall test) of evaporation and climatological variables, including air temperature, relative humidity and wind speed in four reservoirs located in the Brazilian Northeast. The evaporation was estimated through remote sensing using the Surface Energy Balance System for Water (AquaSEBS) model from 1985 to 2018. In addition, it was verified which meteorological parameter has the highest correlation (R2) with the evaporation in order to assess why this process is changing throughout the years in each reservoir. The model performed well, with root mean square error (RMSE) ≤ 1.25 mm/day, percent bias (PBIAS) ≤ 13.70% and coefficient of determination (R2) ≥ 0.51. One reservoir located closer to a coastal zone presented a positive trend (+0.24 mm/34 years), corroborating the measurements of a reference class A pan, and Penman-Monteith equation, while the others, located closer to industrial areas, displayed negative trends (−0.26 to −0.080 mm/34 years). This reduced evaporation was attributed to the impact of industrial pollutant release to the atmosphere, while the increasing effect in the other reservoir was due to its proximity to the coast, which implies an air renewal as the sea breeze contributes for an improvement in the air quality. The meteorological data also presented positive and negative correlations: Temperature exhibited a positive trend (+0.57 °C/34 years), whereas humidity (−4.83%) and wind speed (−0.29 m/s), a negative trend. Evaporation displayed moderate coefficient of determination (R2 > 0.31) with wind speed and humidity. Yet, the reduction of evaporation may be associated with a possible counterbalancing effect of wind speed over humidity. Overall, the results contribute to a better understanding of evaporation trends in a water-scarce region and can be used in a water resources management context as the increasing/reduction of evaporation might significantly impact water availability in this area.pt_BR
dc.language.isoenpt_BR
dc.publisherJournal of Hydrologypt_BR
dc.rightsAcesso Abertopt_BR
dc.subjectClimate changept_BR
dc.subjectEvaporationpt_BR
dc.subjectHydroclimatic datapt_BR
dc.subjectReservoirspt_BR
dc.subjectTrendspt_BR
dc.titleTrends of evaporation in Brazilian tropical reservoirs using remote sensingpt_BR
dc.typeArtigo de Periódicopt_BR
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