Satelliteâbased measurements of the column CH2O/NO2 ratio have previously been used to estimate nearâsurface ozone (O3) sensitivity (i.e., NOx or VOC limited), and the forthcoming launch of air qualityâfocused geostationary satellites provides a catalyst for reevaluating the ability of satelliteâmeasured CH2O/NO2 to be used in this manner. In this study, we use a 0âD photochemical box model to evaluate O3 sensitivity and find that the relative rate of radical termination from radicalâradical interactions to radicalâNOx interactions (referred to as LROx/LNOx) provides a good indicator of maximum O3 production along NOx ridgelines. Using airborne measurements from NASA's Deriving Information on Surface Conditions from Column and Vertically Resolved Observations Relative to Air Quality (DISCOVERâAQ) deployments in Colorado, Maryland, and Houston, we show that in situ measurements of CH2O/NO2 can be used to indicate O3 sensitivity, but there is an important âtransition/ambiguousâ range whereby CH2O/NO2 fails to categorize O3 sensitivity, and the range and span of this transition/ambiguous range varies regionally. Then, we apply these findings to aircraftâderived column density measurements from DISCOVERâAQ and find that inhomogeneities in vertical mixing in the lower troposphere further degrades the ability of column CH2O/NO2 to indicate nearâsurface O3 sensitivity (i.e., the transition/ambiguous range is much larger than indicated by in situ data alone), and we hypothesize that the global transition/ambiguous range is sufficiently large to make the column CH2O/NO2 ratio unuseful for classifying nearâsurface O3 sensitivity. Lastly, we present a case study from DISCOVERâAQâHouston that suggests that O3 sensitivity on exceedance days may be substantially different than on nonexceedance days (which may be observable from space) and explore the diurnal evolution of O3 sensitivity, O3 production, and the column CH2O/NO2 ratio. The results of these studies suggest that although satellite measurements of CH2O/NO2 alone may not be sufficient for accurately classifying nearâsurface O3 sensitivity, new techniques offered by geostationary platforms may nonetheless provide methods for using spaceâbased measurements to develop O3 mitigation strategies.