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Weather officials reported that the system strengthened faster than computer models initially predicted. The primary driver behind the storm’s development was the convergence of two contrasting air masses: a warm, moisture-rich flow from the south and a fast-advancing cold front dropping in from the northwest. This clash created an unstable atmosphere, allowing towering thunderstorm clouds to form over a relatively short period. Specialists note that the energy in the atmosphere is more than sufficient to produce widespread thunderstorms, some of which could briefly reach severe criteria.