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A Change of Seasons

The most immediate change that meteorologists and pilots see in the weather pattern is an increase in the tropospheric flow across the United States and southern Canada at all levels. This starts in earnest in September and continues through October. Temperatures decrease rapidly in the polar regions as fall progresses, dramatically strengthening temperature contrasts between high latitudes and the tropics. This enhances the jet stream pattern and surface patterns alike. So across the board we see an increase in clear air and mechanical turbulence everywhere.

Gemini Sparkle

Key Takeaways:

  • Autumn is a transitional season marked by strengthening atmospheric flow, increased turbulence, and heightened temperature contrasts, leading to dynamic weather patterns.
  • Weather varies significantly across U.S. regions in autumn, bringing diverse hazards such as lake effect precipitation, coastal and interior fog, strong winds (e.g., Santa Ana), active frontal systems, cold air outbreaks, and the potential for severe thunderstorms or tropical storm remnants.
  • Pilots must understand these distinct regional weather patterns and anticipate specific hazards, including the increasing possibility of ice, for safe and effective flight planning throughout the season.
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We often think of autumn as the end of summer, but it’s much more than that. Autumn starts on the equinox and ends at the winter solstice, so meteorologically the northern hemisphere is already hurtling headlong into the cool season, with fall ending at the time of minimum insolation. Fall would be a bitterly cold season if not for so much summer heat that was stored in the surrounding ocean waters.

The most immediate change that meteorologists and pilots see in the weather pattern is an increase in the tropospheric flow across the United States and southern Canada at all levels. This starts in earnest in September and continues through October. Temperatures decrease rapidly in the polar regions as fall progresses, dramatically strengthening temperature contrasts between high latitudes and the tropics. This enhances the jet stream pattern and surface patterns alike. So across the board we see an increase in clear air and mechanical turbulence everywhere.

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