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role in the computation of the principal mass and energy fluxes. In the literature these parameters are usually defined using soil texture maps ( Rawls and Brakensiek 1985 ), but problems of representativeness arise owing to pixel heterogeneity. Satellite images of land surface temperature can help in the calibration of these parameters in each pixel of the analyzed domain, overcoming the traditional calibration based on a single multiplicative value retrieved from the comparison between observed
role in the computation of the principal mass and energy fluxes. In the literature these parameters are usually defined using soil texture maps ( Rawls and Brakensiek 1985 ), but problems of representativeness arise owing to pixel heterogeneity. Satellite images of land surface temperature can help in the calibration of these parameters in each pixel of the analyzed domain, overcoming the traditional calibration based on a single multiplicative value retrieved from the comparison between observed
