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As it rises, it displaces air which descends outside the core of the vortex. The secondary flow in the dust devil causes other hot air to speed horizontally inward to the bottom of the newly forming vortex. Dust devils form as a swirling updraft under sunny conditions during fair weather, rarely coming close to the intensity of a tornado. If conditions are just right, the updraft may begin to rotate. Certain conditions increase the likelihood of dust devil formation. Dust devils form when a pocket of hot air near the surface rises quickly through cooler air above it, forming an updraft. Usually it occurs when the dust devil is moving slowly (depletion) or begins to enter a terrain where the surface temperatures are cooler. The dust devil may be sustained if it moves over nearby sources of hot surface air. A dust devil, fully formed, is a funnel-like chimney through which hot air moves, both upwards and in a circle. As the hot air rises, it cools, loses its buoyancy and eventually ceases to rise. If you love to mix the funky, sentimental, pretty, and whimsical, come home to vintage charm.
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- 1, Aug, 2025
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