Lightning produces nitrogen oxides (NO_x) as the extreme temperatures within lightning channels break apart molecular nitrogen (N₂) and oxygen (O₂) . NO_x produced by lightning (LNO_x) plays an important role in determining mid- and upper-tropospheric amounts of the hydroxyl radical (OH), the atmosphere’s cleanser; methane (CH₄), an especially potent greenhouse gas; and ozone (O₃), a greenhouse gas and pollutant. On the afternoons of June 19, 20, and 24th of 2025, high temporal resolution (10-minutes) observations of NO₂ were obtained over the eastern United States by TEMPO, an instrument aboard a geostationary satellite. The days were chosen several days in advance based on forecast thunderstorm activity and outflow regions. In this study, the amount of NO_x produced per lightning flash will be estimated using these NO₂ columns over thunderstorms and ten-minute flash counts from a Geostationary Lightning Mapper (GLM) aboard a weather satellite and the ground-based Earth Networks Total Lightning Network (ENTLN). The high temporal resolution was critical for good results because the lifetime of individual thunderstorms is short (~20-30 minutes), their direction erratic, and their flash rate variable. The flash rate is important because the amount of NO_x produced per flash is believed to vary with flash rate.