The two-layer model of Shuttlerworth and Wallace (SW) was evaluated to estimate actual evapotranspiration (ETa) above a drip-irrigated Merlot vineyard, located in the Talca Valley, Region del Maule, Chile (35o 25' LS; 71o 32' LW; 136m above the sea level). An automatic weather system was installed in the center of the vineyard to measure climatic variables (air temperature, relative humidity, and wind speed) and energy balance components (solar radiation, net radiation, latent heat flux, sensible heat flux, and soil heat flux) during November and December 2006. Values of Eta estimated by the SW model were tested with latent heat flux measurements obtained from an eddy-covariance system on a 30 minute time interval. Results indicated that SW model was able to predict Eta with a root mean square error (RMSE) of 0.44 mm d~(-1) and mean absolute error (MAE) of 0.36 mm d~(-1). Furthermore, SW model predicted latent heat flux with RMSE and MAE of 32 W m~(-2) and 19W m~(-1), respectively.
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