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poster - International Conference of Agricultural Engineering

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4. Conclusions<br />

When comparing the evapotranspiration values estimated by means <strong>of</strong> the Bowen<br />

Ratio-Energy Balance method (BREB) with the values measured in the lysimeter, in any <strong>of</strong><br />

the modalities studied in this paper, it was followed that Bowen method underestimated the<br />

evapotranspiration flux, allowing to detect a process <strong>of</strong> sensible heat advection, which can be<br />

considered as an important energy source that increases the crop evapotranspiration.<br />

Nevertheless, no greater attention to this phenomenon was paid, since it was out <strong>of</strong> the<br />

scope <strong>of</strong> this study. The heat flux advection and its influence when measuring and estimating<br />

evapotranspiration was analysed by Gavilán (2002), who considers that it can contribute up<br />

to 40% <strong>of</strong> the total energy used in the evapotranspiration process.<br />

A comparison <strong>of</strong> the hourly values <strong>of</strong> ET calculated by applying the FAO-56 Penman-<br />

Monteith equation (Allen et al. 1998) with the ones estimated by the BREB method, using<br />

both thermocouples and RTDs for measuring the temperature gradients, proved that both<br />

systems underestimated the evapotranspiration, existing significant differences between both<br />

systems. Even though, the ET values estimated with the BREB method by using RTDs<br />

showed a better adjustment, precision and stability, highlighting a better suitability for<br />

calculating the Bowen ratio.<br />

Acknowledgements<br />

This work has been partially supported by the PPII10-0319-8732 (Ministry <strong>of</strong> Education<br />

and Science from the Government <strong>of</strong> Castilla la Mancha) and 08729/PI/08 (Seneca<br />

Foundation) projects.<br />

References<br />

Allen, R.G., Pereira, L.S., Raes, D., & Smith, M. (1998). Crop evapotranspiration: guidelines<br />

for computing crop water requirements. Paper number 56. Rome: FAO Irrigation and<br />

drainage.<br />

Bowen, J.S. (1926). The ratio <strong>of</strong> heat losses by conduction and by evaporation from any<br />

water surface. Physical Review, 27, 779-787.<br />

Casa, R., Russell, G., & Lo Casciom, B. (2000). Estimation <strong>of</strong> evapotranspiration from a field<br />

<strong>of</strong> linseed in central Italy. <strong>Agricultural</strong> and Forest Meteorology, 104(4), 289-301.<br />

Dunin, F.X., Barrs, H.D., Meyer, W.S., & Trevitt, A.C.F. (1991). Foliage temperature and<br />

latent flux <strong>of</strong> irrigated wheat. <strong>Agricultural</strong> and Forest Meteorology, 55, 133-147.<br />

Farahani, H.J., & Bausch, W.C. (1995). Performance <strong>of</strong> Evapotranspiration models for maize<br />

–bare soil to closed canopy. Transactions <strong>of</strong> the ASAE, 38(4), 1049-1059.<br />

Gavilán, P.D. (2002). La advección de calor sensible en el Valle Medio del Guadalquivir y su<br />

influencia en la medida y estimación de la evapotranspiración. Doctoral Thesis. Córdoba:<br />

Universidad de Córdoba.<br />

Ibañez, M., & Castellví, F. (2000). Simplifying daily evapotranspiration estimates over short<br />

full-canopy crops. Agronomy Journal, 92, 628-632.<br />

Kjelgaard, J.F., Stockle, C.O., Villar Mir, J.M., Evans, R.G., & Campbell, G.S. (1994).<br />

Evaluating methods to estimated corn evapotranspiration from short-time interval weather<br />

data. Transactions <strong>of</strong> the ASAE, 37(6), 1825-1833.

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