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Evapotranspiration in the Brazilian municipalities surrounding the Itaipu Binacional reservoir: characterization process and estimation methods
Evapotranspiración en los municipios brasileños que rodea el reservatorio de Itaipu Binacional: proceso de caracterización y métodos de estimación
DOI:
https://doi.org/10.15446/dyna.v88n219.97015Palabras clave:
hydrological cycle, temperature data, water resources (en)ciclo hidrológico, datos de temperatura, recursos hídricos (es)
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Seeking to contribute with the management of water resources in the Itaipu Binacional reservoir region, this research aimed to characterize the dynamics of evapotranspiration and evaluate the performance of different mathematical methods, which determine reference evapotranspiration (ETo) from air temperature values. Fifteen municipalities were analyzed. After obtaining the data series, ETo was estimated using six methods: Camargo (C), Hargreaves-Samani (HG-S), Jensen-Haise (JH), Penman-Monteith with missing data (PMm), Thornthwaite-Camargo (TW-C) and Penman-Monteith (PM) – the latter was the reference method. The performance of the methods was analyzed by several statistical indexes. Daily ETo values ranged from 2 to 10 mm d-1, with an annual mean of 5.78 mm d-1. We also observed that it is determined predominantly by radioactive parameters, which annually represent 76% of the evapotranspiration process, while aerodynamic parameters represent 24%. Among the ETo estimation methods, HG-S and PMm were the most suitable for estimating.
Buscando contribuir con la gestión de los recursos hídricos en la región del reservorio de Itaipu Binacional, esta investigación tuvo como objetivo caracterizar la dinámica del proceso de evapotranspiración y evaluar el desempeño de diferentes métodos matemáticos, que determinan la evapotranspiración de referencia (ETo) a partir de los valores de temperatura del aire. Se analizaron quince ciudades. Después de obtener la serie de datos, la ETo se estimó utilizando seis métodos: Camargo (C), Hargreaves-Samani (HG-S), Jensen-Haise (JH), Penman-Monteith con datos faltantes (PMm), Thornthwaite-Camargo (TW- C) y Penman-Monteith (PM), siendo este último el método de referencia. El desempeño de los métodos ocurrió mediante varios índices estadísticos. Los valores diarios de ETo variaron de 2 a 10 mm d-1, con una media anual de 5,78 mm d-1. También observamos que ETo es determinada predominantemente por parámetros radiactivos, que anualmente representan el 76% del proceso de evapotranspiración, mientras que los parámetros aerodinámicos representan el 24%. Entre los métodos de estimación de ETo, los métodos HG-S y PMm fueron los más adecuados para estimar.
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