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The high frequency of thunderstorms in central Colorado and northeastern New Mexico can be attributed to the presence of the Rocky Mountains. The orographic lift caused by the mountains forces moist air to rise, cool, and condense, leading to the development of thunderstorms. Additionally, the region's elevation and climate conditions, including warm temperatures and moisture from the surrounding areas, further enhance thunderstorm activity. Together, these factors create an environment conducive to frequent thunderstorms.

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