Polynomial regression techniques were used to derive a baseline climatology for Ireland at a scale of l km2 for the p eriod 1961-90. Monthly climate variables were related to position and elevation on a digital elevation model and these were found to provide good predictors for precipitation and m aximum/minimum temperature. Baseline maps for mean monthly radiation receipt and potential evapotranspiration were a lso derived at 1 km2 scales. The National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) Reanalysis D ata were then related to this b aseline climatology and relationships be n veen upper air variables and surface climate established as a basis for statistical downscaling of global climate models. Monthly output for the spatial domain over Ireland were extrac ted from th e latest Hadley Centre Clobal Climate Model (HadCM3). Using the upper air/surface relationships the climate differences be t\'Veen a modelled run for the 1961-90 period and the period 204 1-70 was establish ed. These differences were th en applied to the baseline climate d ata to provide future climatic scenarios for Ireland for these period s. Mean temperature increases of 2-3°C we re projected for mid century for both summer and winter. Precipitation changes showed w inter increases of the order of 10% in western Ireland and similar summer decreases especially in eastern Ireland. Observation al data trends appear to match these projections.