Abstract. Reported sulfur dioxide (SO 2 ) emissions from US and Canadian sources have declined dramatically since the 1990s as a result of emission control measures. Observations from the Ozone Monitoring Instrument (OMI) on NASA's Aura satellite and ground-based in situ measurements are examined to verify whether the observed changes from SO 2 abundance measurements are quantitatively consistent with the reported changes in emissions. To make this connection, a new method to link SO 2 emissions and satellite SO 2 measurements was developed. The method is based on fitting satellite SO 2 vertical column densities (VCDs) to a set of functions of OMI pixel coordinates and wind speeds, where each function represents a statistical model of a plume from a single point source. The concept is first demonstrated using sources in North America and then applied to Europe. The correlation coefficient between OMI-measured VCDs (with a local bias removed) and SO 2 VCDs derived here using reported emissions for 1 • by 1 • gridded data is 0.91 and the best-fit line has a slope near unity, confirming a very good agreement between observed SO 2 VCDs and reported emissions. Having demonstrated their consistency, seasonal and annual mean SO 2 VCD distributions are calculated, based on reported point-source emissions for the period 1980-2015, as would have been seen by OMI. This consistency is further substantiated as the emission-derived VCDs also show a high correlation with annual mean SO 2 surface concentrations at 50 regional monitoring stations.