The outflow from the main line of storms was moving west and combined with a strong cell which was spawned off the dryline, resulting in a strong line of storms forming where the two converged. Something that was noted was the delay in GLM FED with the developing convection, where flashes could be seen quickly from the ENTLN. Chalked this up to the optical depth of the storm at the time covering the flashed from the GLM given the extent of cloud-to-ground strikes. Later on, a line of increased GLM FED could be seen.

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