Spatial uncertainty assessment in modelling reference evapotranspiration at regional scale

G. Buttafuoco,T. Caloiero,R. Coscarelli

doi:10.5194/hess-14-2319-2010

Abstract

Abstract. Evapotranspiration is one of the major components of the water balance and has been identified as a key factor in hydrological modelling. For this reason, several methods have been developed to calculate the reference evapotranspiration (ET0). In modelling reference evapotranspiration it is inevitable that both model and data input will present some uncertainty. Whatever model is used, the errors in the input will propagate towards the output of the calculated ET0. Neglecting the information about estimation uncertainty, however, may lead to improper decision-making and water resources management. One geostatistical approach to spatial analysis is stochastic simulation, which draws alternative and equally probable, realizations of a regionalized variable. Differences between the realizations provide a measure of spatial uncertainty and allows to carry out an error propagation analysis. The aim of this paper is to assess spatial uncertainty of a monthly reference evapotranspiration model resulting from the uncertainties in the input attributes (mainly temperature) at a regional scale. A case study was presented for the Calabria region (southern Italy). Temperature data were jointly simulated by a conditional turning bands simulation with elevation as external drift and 500 realizations were generated. Among the evapotranspiration models, the Hargreaves-Samani model was used. The ET0 was then estimated for each set of the 500 realizations of the input variables, and the ensemble of the model outputs was used to infer the reference evapotranspiration probability distribution function. This approach allowed for the delineation of the areas characterised by greater uncertainty, to improve supplementary sampling strategies and ET0 value predictions.

Highlights

The assumption of normal distribution was not accepted for both mean maximum (Tmax) and mean minimum temperature (Tmin) data at a probability level p > 0.10, and the data distributions showed long negative tails
The results of a spatial uncertainty analysis have shown that the prediction quality depends on the uncertainties of the data used in the analysis; map makers should convey the accuracy of the maps they produce (Heuvelink, 1998)
A complete characterisation of the accuracy of spatial data should include the spatial correlation of the attributes used for estimation and stored in a Geographical Information Systems (GIS)

Summary

Introduction

The concept of reference evapotranspiration was introduced to study the evaporative demand of the atmosphere independently of crop type, crop development and management practices. As water is abundantly available at the reference evapotranspiring surface, soil factors do not affect ET0. The only factors affecting ET0 are climatic attributes. ET0 is a climatic attribute and can be computed from weather data. ET0 expresses the evaporating power of the atmosphere at a specific location and time of the year and does not consider the crop characteristics and soil factors (Allen et al, 1998)

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Conclusion