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Combining remote sensing and GIS climate modelling to estimate daily forest evapotranspiration in a Mediterranean mountain area

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Figure

Fig. 1. Location of SMC meteorological stations and Vallcebre research catchments in Universal Transversal Mercator (UTM) projection(UTM coordinates are expressed in km)
Figure 2. Monthly temporal distribution of satellite data (clear sky and without bow tie effect: an artefact of the arrangement of sensors on the MODIS instrument, in which the main factors on whichaerodynamic resistance; therefore, B depends, such as wind velocity and B can also be defined as:
Table 1. (a): Descriptive statistics of daily net radiation (Rnd) and daily evapotranspiration (ETd) measured over the Scots pine stand, andLandsat Rn and ETd modelled using 3 methods: B-Rn ratio regional, B-Rn ratio local and B-NDVI (see text)
Figure 3. Mean monthly local and regional RFig. 3. Mean monthly local and regional Rn at the Landsat/TERRAand AQUA satellite pass on clear sky days from 2003 to 2005.n at the Landsat/TERRA and AQUA 2 3
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