Regional calibration of Hargreaves equation for estimating reference ET in a semiarid environment

By P. Gavilán, Ignacio J. Lorite, S. Tornero, J. Berengena. 2006

345 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Plant Science, Soil Science

View Paper: https://www.semanticscholar.org/paper/4d3d372b00f45c85d92a168c77cd244ea997cb40

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Citations in the corpus

Spatially distributed monthly reference evapotranspiration derived from the calibration of Thornthwaite equation: a case study, South of Iran (2008, methodology): “Irmak et al. (2003), Pereira and Pruitt (2004), Gavilan et al. (2006) , Dinpashoh (2006), and Fooladmand and Haghighat (2007) considered the Penman-Monteith method as the basis for the evapotranspiration studies, as”
Aerodynamic Parameterization of the Satellite-Based Energy Balance (METRIC) Model for ET Estimation in Rainfed Olive Orchards of Andalusia, Spain (2012, methodology): “For both methodologies, weather data including rainfall, air temperature, relative humidity, wind speed and solar radiation from five weather stations within or near the study area were obtained from the Agroclimatic Information Network of Andalusia (Gavilán et al. 2006).”
Parametric expressions for the adjusted Hargreaves coefficient in Eastern Spain (2015, background): “, 2006) or, more commonly, 110 Penman Monteith calculated benchmarks (e.g. Itenfisu et al., 2003; Vanderlinden et al., 111 2004; Trajkovic, 2005, 2007; Gavilán et al., 2006; Fooladmand and Haghighat, 2007; 112 Ravazzani et al., 2012; Bachour et al., 2013; Mendicino and Senatore, 2013; Berti et al., ”
Calibration and validation of four common ET0 estimation equations by lysimeter data in a semi-arid environment (2012, methodology): “( 2005 ) compared daily ET 0 estimated using the Hargreaves–Samani equation with values obtained with the Penman–Monteith equation under semi-arid conditions in southern Spain.”
Evaluation of FAO-56 Penman-Monteith and Temperature Based Models in Estimating Reference Evapotranspiration Using Complete and Limited Data, Application to Nigeria (2009, methodology): “Generally these classifications include the temperature-based models such as Thornthwaite (1948); Blaney-Criddle (1950); Hargreaves and Samani (1982). The mass-transfer models which is based on vapour pressure or relative humidity include: Rohwer (1931) and Harbeck (1962)); the radiation models whic”