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Upscaling of evapotranspiration fluxes from instantaneous to daytime scales for thermal remote sensing applications

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Figure

Table 1. Study site information. The ID represents the standard AmeriFlux identification code, and the column Years reports the 2 observationyears analyzed for each site.
Figure 1. Statistical metrics computed using observed daytime-integrated “daily” ET (obtained using different closure constraints) and modeled values upscaled from half-hourly observations collected midday (from 0900 to 1500 solar time) time-of-day
Figure 4.       Monthly variability of the accuracy of upscaling meth-ods. The black central bar represents the frequency of data betweenETmax and ETmin, the light-gray bars represent the “moderate” er-rors, while dark gray bars represent “major” errors
Figure 6.  Monthly variability of the accuracy of EF upscaling meth-ods using different components of available energy

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