Abstract

Determination of surface energy balance depends on the energy exchange between land and atmosphere. Thus, crop, soil and meteorological factors are crucial, particularly in agricultural fields. Evapotranspiration is derived from latent heat component of surface energy balance and is a key factor to clarify the energy transfer mechanism. Development of the methods and technologies for the aim of determining and measuring of evapotranspiration have been one of the main focus points for researchers. However, the direct measurement systems are not common because of economic reasons. This situation causes that different methods are used to estimate evapotranspiration, particularly in locations where no measurements are made. Thus, in this study, non-linear techniques were applied to make accurate estimations of evapotranspiration over the winter wheat canopy located in the field of Atatürk Soil Water and Agricultural Meteorology Research Institute Directorate, Kırklareli, Turkey. This is the first attempt in the literature which consist of the comparison of different machine learning methods in the evapotranspiration values obtained by the Bowen Ratio Energy Balance system. In order to accomplish this aim, support-vector machine, Adaptive neuro fuzzy inference system and Artificial neural network models have been evaluated for different input combinations. The results revealed that even with only global solar radiation data taken as an input, a high prediction accuracy can be achieved. These results are particularly advantageous in cases where the measurement of meteorological variables is limited. With the results of this study, progress can be made in the efficient use and management of water resources based on the input parameters of evapotranspiration especially for regions with limited data.

Highlights

  • Investigation of the relocation of water with events such as precipitation, surface flow, evapotranspiration and infiltration are of great importance for the management of water resources

  • The field measurement of various climatic variables that are used in the calculation of evapotranspiration has been carried out, and estimationss have been made depending on these parameters

  • Global solar radiation, relative humidity, mean temperature and vapor pressure deficit were used as input variables to the proposed models, while actual ET as the output

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Summary

Introduction

Investigation of the relocation of water with events such as precipitation, surface flow, evapotranspiration and infiltration are of great importance for the management of water resources. Sustainable use of water resources is only possible through accurate monitoring of all hydrological cycle elements and utilizing this information for decision support in water resources management. Evapotranspiration (ET) is one of the most important components in hydrological cycle among the others which are precipitation, infiltration, surface and groundwater flow. Evapotranspiration can be described as the change of phase of water in the soil, plants, rivers, lakes and seas with the effect of atmospheric conditions and movement towards the atmosphere. It consists of two factors: evaporation and transpiration. The Bowen Ratio Energy Balance (BREB) method was used to measure actual ET and mathematical models have been proposed using the data obtained from the measurements

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