Global NEST Journal, Vol 14, No 3, pp 335-343, 2012 Copyright© 2012 Global NEST Printed in Greece. All rights reserved SENSITIVITY ANALYSIS OF DIFFERENT EVAPOTRANSPIRATION METHODS USING A NEW SENSITIVITY COEFFICIENT V.Th. AMBAS 1,* 1 Region of Western Macedonia E. BALTAS 2 Department of soil-water resources conservation Ptolemeon 1, 53100, Florina, Greece 2 Aristotle University of Thessaloniki, Department of Hydraulics Soil Science and Agriculture Engineering Thessaloniki, Greece Received: 20/05/12 *to whom all correspondence should be addressed: Accepted: 27/07/12 e-mail: ambasv@gmail.com ABSTRACT The estimation of evapotranspiration is essential in water resources management. Among a group of methods, the Penman–Monteith has been commonly applied to calculate reference evapotranspiration as this method has been also recommended by the Food and Agriculture Organization of the U.N. (FAO). Other methods widely used are: the FAO 24 Penman, the modified Blaney and Criddle, the FAO 24 Makkink, and the Hargreaves. Sensitivity analysis is required to gain a better understanding of the meteorological systems; particularly to indicate the physical meaning of each meteorological parameter used in the estimation of the reference evapotranspiration. Several dimensionless sensitivity coefficients have been proposed, based on the partial derivative of the dependent variable (reference evapotranspiration) to the independent variables (meteorological variables). In this paper, a new sensitivity coefficient is proposed to drive sensitivity analysis of the evapotranspiration methods. The new sensitivity coefficient uses the partial derivative and the standard deviation of each independent variable. The meteorological variables, whose influence has been examined, are all the necessary meteorological parameters for the calculation of reference evapotranspiration, such as temperature, solar radiation, wind speed and relative humidity for each method. Data from the automatic meteorological station of Aminteo in the Prefecture of Florina, Western Macedonia, were used. The sensitivity coefficients were calculated for each month, year and irrigation period. The comparison of the sensitivity coefficients is performed for the month of water peak demand (July), the irrigation period and the year for each evapotranspiration method. Results show that the influence of the variables to evapotranspiration is not the same for each period, and also the order that the variables influence evapotranspiration is changing. A comparison between the five evapotranspiration methods shows that solar radiation and temperature are the main parameters that affect evapotranspiration, while relative humidity and wind speed are not so important for the calculation of evapotranspiration. KEYWORDS: sensitivity coefficient, reference evapotranspiration, evapotranspiration method, meteorological parameters. 1. INTRODUCTION Evapotranspiration is an important component of the hydrologic cycle as it can significantly affect the water budget of the natural (i.e. approximately 62% of all precipitation falling on land is evapotranspirated. Consequently, its accurate estimation is essential for, among others, water availability, plant growth, irrigations efficiency, reservoir operation,,and water resources management. Several empirical methods have been developed to derive evapotranspiration estimates. Among others, the Penman–Monteith method is recommended by the Food and