Evaporation Hysteresis over Vegetation: The Impact of Surface Processes and Boundary Layer Dynamics

The non-linear relation between Evapotranspiration (ET) and the atmospheric moisture demand in terms of vapor pressure deficit (VPD) has been widely reported. Observations point towards a diverse range of potential drivers; however, without uncovering why the identified factors are found to control diurnal ET-VPD hysteresis. Modelling efforts...

Sensitivity of snow models in the semi-arid Andes of Chile: A comparison between SNOWPACK and SnowModel