Spatial distribution of reference crop evapotranspiration and effective rainfall in the central-northeastern provinces of Argentina

Authors

  • José Morábito Centro Regional Andino. Instituto Nacional del Agua. Belgrano 2010 Oeste (M55500FIF). Mendoza. Argentina
  • Santa Salatino Centro Regional Andino. Instituto Nacional del Agua. Belgrano 2010 Oeste (M55500FIF). Mendoza. Argentina
  • Rocío Hernández Centro Regional Andino. Instituto Nacional del Agua. Belgrano 2010 Oeste (M55500FIF). Mendoza. Argentina
  • Carlos Schilardi Facultad de Ciencias Agrarias- Universidad Nacional de Cuyo. Almirante Brown 500- Luján. C. P. M5528AHB. Mendoza. Argentina
  • Alisa Álvarez Centro Regional Andino. Instituto Nacional del Agua. Belgrano 2010 Oeste (M55500FIF). Mendoza. Argentina
  • Paula Rodríguez Palmieri Centro Regional Andino. Instituto Nacional del Agua. Belgrano 2010 Oeste (M55500FIF). Mendoza. Argentina

Keywords:

irrigation requirements, crop water demand, water use planning, complementary/supplementary irrigation, productivity

Abstract

This paper falls within the framework of the FAO-INA Agreement that was entered into to "identify new potential irrigated and supplementary-irrigated areas in the basins of northeastern Argentina". The agreement seeks to collect information on monthly reference crop evapotranspiration (ETo), analyze its variability, and show it on isoline maps. The study comprised the central northeastern part of Argentina; the program used was CROPWAT 8.0 – FAO; and climate data were obtained from CLIMWAT 2.0. The information was plotted with ArcView 3.2ª and the variables of interest were
interpolated with the Kriging method. Results show that: a) Santiago del Estero is the station with the highest annual ETo: 1767 mm.year-1, while the lowest ETo value is found in Loreto (Misiones) with 1150 mm.year-1; b) the average ETo in January ranges between 160 to 200 mm.month-1, while in July it is between 35 - 90 mm.month-1; c) the average ETo in January in the northeastern part of Cordoba ranges between 165 - 185 mm. month-1 while in July the variability is less pronounced; and d) rainfall in an average hydrological year ranges between 605 and 1825 mm.year-1 with an effective rainfall of 500 and 1400 mm.year-1 that tends to increase towards the northeast.

Published

01-06-2015

Issue

Section

Natural resources and environment