<Tr> <Th> Effect </Th> <Td> Dust spread in surrounding area, possibly coughing . </Td> </Tr> <P> A dust devil is a strong, well - formed, and relatively long - lived whirlwind, ranging from small (half a metre wide and a few metres tall) to large (more than 10 metres wide and more than 1000 metres tall). The primary vertical motion is upward . Dust devils are usually harmless, but can on rare occasions grow large enough to pose a threat to both people and property . </P> <P> They are comparable to tornadoes in that both are a weather phenomenon involving a vertically oriented rotating column of wind . Most tornadoes are associated with a larger parent circulation, the mesocyclone on the back of a supercell thunderstorm . Dust devils form as a swirling updraft under sunny conditions during fair weather, rarely coming close to the intensity of a tornado . </P> <P> Dust devils form when a pocket of hot air near the surface rises quickly through cooler air above it, forming an updraft . If conditions are just right, the updraft may begin to rotate . As the air rapidly rises, the column of hot air is stretched vertically, thereby moving mass closer to the axis of rotation, which causes intensification of the spinning effect by conservation of angular momentum . The secondary flow in the dust devil causes other hot air to speed horizontally inward to the bottom of the newly forming vortex . As more hot air rushes in toward the developing vortex to replace the air that is rising, the spinning effect becomes further intensified and self - sustaining . 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 . As it rises, it displaces air which descends outside the core of the vortex . This cool air returning acts as a balance against the spinning hot - air outer wall and keeps the system stable . </P>

When does a dust devil become a tornado
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