ADO Datasets from deliverable D.T2.1.1 are downscaled from ERA5 surface datasets (Hersbach et al. 2018) using quantile mapping. As ERA5 snow data cannot be downscaled in a similar manner (no snow data
Long wave incoming radiation (wavelengths of 5 to 50 µm) measured on two proximal climate stations at 200 cm above ground as a 5min average (W/m2). The double masted climate station is located betwee
