The gridded hourly solar irradiance derived from satellite imagery by the Australian Bureau of Meteorology represents the current state of the art in quantification of the long-term solar resource for locations where no ground measurements are available. Using nonparametric regression, we test the potential for the satellite-derived global horizontal irradiance and direct normal irradiance to be improved by combining with irradiance that has been dynamically downscaled using a numerical weather prediction (NWP) model. NWP irradiance, together with the satellite irradiance, solar zenith angle and their interaction terms are used as inputs to generalised additive models (GAM) using smoothing splines. The spatial weighting of these empirical models according to distance is also tested. Cross validation with ground measurements indicates that RMSE can be improved by a few percent over the satellite-derived irradiance. The addition of dynamically downscaled irradiance as a GAM predictor further improves RMSE by a few percent, depending on location. When these empirical models are weighted spatially over large distances (hundreds of kilometres), the results are more equivocal. However, spatial weighting of the regression functions should be possible over smaller regions where the atmospheric turbidity properties are similar. (C) 2016 Elsevier Ltd. All rights reserved.