This study aims to quantify hail fall characteristics during a 22-year period, a markedly longer timeframe than previous studies, using both radar observations and reanalyses. Environments likely to produce hail can be identified by leveraging reanalyses to better inform radar-derived hail proxies. First, the improved MESH configuration is applied to the full archive of gridded hourly radar observations known as GridRad (1995-2016). Next, environmental constraints obtained from the Modern-Era Retrospective analysis for Research and Applications, Version 2 (MERRA-2) are applied to the MESH distributions to produce a modified hail fall climatology that accounts for the likelihood of hail reaching the ground based on melting characteristics. Spatial, diurnal, and seasonal patterns are investigated for each of these climatologies and evaluated against hail report distributions. Results show that in contrast to the report climatology indicating only one major hail frequency maximum centered on the Great Plains, the MESH-only method characterizes two regions, the Great Plains and the Gulf Coast. The inclusion of environmental information is found to correct some of these differences between MESH and observations, suggesting that MESH-only estimates of hail climatology need be treated carefully.