The University of Utah two-dimensional variation analysis (UU2DVAR) system was used to create the gridded analyses from all of the available observations. Hourly background grids were determined from averages of the available observations over land distinct from those over the lake as well as assumptions regarding the variation of ozone with elevation. Sensitivity of the analyses to the assumed background fields as well as observational error have been assessed. The high spatial and temporal resolution gridded analyses help to delineate the spatial heterogeneity and temporal evolution of the distribution of ozone during poor air quality episodes arising from the influence of the Great Salt Lake, including thermally-driven circulations such as lake and land breezes.
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