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Potential evaporation estimation through an unstressed surface energy balance and its sensitivity to climate change

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Figure

Table 2. Description of ETon and the assumptions made for their calculation. The computation has been carried out at a daily time step, except for the following cases:abP USEB, ETP BULK, ETP Milly and the cases defined to compute ETP FAO, according to the v
Table 3. Mean ETP for the reference period regarding the USEB and Milly methods, as well as the FAO’s six cases.
Fig. 1. The USEB method’s ETprovide higher values dealing the USEB method, blue ones imply that FAO’s reference equation or Milly’s method provide higher ETP mean annual values (mm d−1) for the reference period (a)
Fig. 2. Significant trends showing the increasing or decreasing % per decade for the aerodynamic resistance (gradient, and the net radiation (ra), the VPD, the humidityRn), regarding the IPSL A2 scenario and the different formulations
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