Sensitivity of the RDI and SPEI Drought Indices to Different Models for Estimating Evapotranspiration Potential in Semiarid Regions

Author:

Ortiz-Gómez RupertoORCID,Flowers-Cano Roberto S.,Medina-García Guillermo

Publisher

Springer Science and Business Media LLC

Subject

Water Science and Technology,Civil and Structural Engineering

Reference53 articles.

1. Allen RG (1993) Evaluation of a temperature difference method for computing grass reference evapotranspiration. Report to Water Resources Development and Management Service Land and Water Development Division. FAO. Rome, Italy

2. Allen RG, Pereira LS, Raes D, Smith M (1998) Crop evapotranspiration: Guidelines for computing crop water requirements. FAO Irrigation and Drainage Paper 56. Rome, Italy

3. Azhar AH, Perera B (2010) Evaluation of reference evapotranspiration estimation methods under southeast Australian conditions. J Irrig Drain Eng ASCE 137:268–279. https://doi.org/10.1061/(ASCE)IR.1943-4774.0000297

4. Bayissa Y, Maskey S, Tadesse T, van Andel SJ, Moges S, van Griensven A, Solomatine D (2018) Comparison of the performance of six drought indices in characterizing historical drought for the Upper Blue Nile Basin. Ethiopia Geosci 8:81. https://doi.org/10.3390/geosciences8030081

5. Blaney HF, Criddle WD (1950) Determining water requirements in irrigated areas from climatological and irrigation data. Soil Conservation Service Technical Paper 96. Soil Conservation Service. Washington, US Department of Agriculture

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