Abstract

A study was carried out to parameterize the METRIC (Mapping EvapoTranspiration at high Resolution with Internalized Calibration) model for estimating instantaneous values of albedo (shortwave albedo) (alpha(i)), net radiation (R-ni) and soil heat flux (G(i)), sensible (H-i) and latent heat (LEi) over a drip-irrigated Merlot vineyard (location: 35 degrees 25' LS; 71 degrees 32' LW; 125 m.a.s. (l). The experiment was carried out in a plot of 4.25 ha, processing 15 Landsat images, which were acquired from 2006 to 2009. An automatic weather station was placed inside the experimental plot to measure alpha(i), R-ni and G(i). In the same tower an Eddy Covariance (EC) system was mounted to measure H-i and LEi. Specific sub-models to estimate G(i), leaf area index (LAI) and aerodynamic roughness length for momentum transfer (zom) were calibrated for the Merlot vineyard as an improvement to the original METRIC model. Results indicated that LAI, zom and G(i) were estimated using the calibrated functions with errors of 4%, 2% and 17%, while those were computed using the original functions with errors of 58%, 81%, and 5%, respectively. At the time of satellite overpass, comparisons between measured and estimated values indicated that METRIC overestimated alpha(i) in 21% and R-ni in 11%. Also, METRIC using the calibrated functions overestimated H-i and LEi with errors of 16% and 17%, respectively while it using the original functions overestimated H-i and LEi with errors of 13% and 15%, respectively. Finally, LEi was estimated with root mean square error (RMSE) between 43 and 60 W.m(-2) and mean absolute error (MAE) between 35 and 48 W.m(-2) for both calibrated and original functions, respectively. These results suggested that biases observed for instantaneous pixel-by-pixel values of R-ni, G(i) and other intermediate components of the algorithm were presumably absorbed into the computation of sensible heat flux as a result of the internal self-calibration of METRIC.