Turbulence is nothing more than equalization of diurnal (during the day) temperature variations in the atmosphere in which rising warm air meets descending cooler air, triggering uneven motion across layers of different densities. This constant push and pull, most especially near the Earth's surface, results in eddies, swirls, and abrupt changes in wind direction and speed. As the sun heats the ground during the day, localized pockets of thermal instability form, creating invisible rivers of shi...
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