Curved, Kinked, Spiral and Wavy Meteors

Meteor theory dictates that when an object enters the atmosphere at hypervelocity (11 - 72 km/s or 24,750 - 162,000 mph) it will travel in a straight line. Yet a number of conflicting reports exist in which the meteor's path has been described as being curved, kinked, spiral or wavy.

Curved Meteor Curved meteors are by far the most common. In some cases the cause is quite simple: a meteoroid entering the atmosphere at an oblique angle will bounce out again in much the same way as a pebble can be bounced across the surface of a pond. There is actually photographic evidence of this happening. In 1972 James M. Baker captured a bright daylight fireball on film as it skipped across the skies over Great Jackson Lake in Wyoming. However, there are a number of observations that cannot be explained so easily.

One of the earliest reports came from B.J.Hopkins who recorded in the Monthly Notices of the Royal Astronomical Society (1885) that on 20th October 1879 at 18h 48m GMT he...

Wavy Meteor Observed a bright yellow meteor, which described a zigzag path with two bends.....Appeared between Alpha and Beta Cameli, disappeared near Theta Persei.

It is difficult to explain how meteors can deviate in this way but one possible explanation may be that the meteoroid has an aerodynamic shape which produces "lift". Opponents of this view argue that most meteoroids are fragile dustballs rather than solid rocks - but that could be the very reason why such occurrences are rare.

Wavy and spiral meteors may be one and the same thing: it depends on how the observer perceives the object. But kinked meteors are almost certainly an optical illusion.

Kinked Meteor
 
 

Like curved meteors, kinked meteors begin normally but then suddenly develop a kink in their paths before returning to their original trajectory. This may be due to a temporary or permanent defect in the observer's eye (e.g. water on the eyeball) or, as has been suggested, to water vapor in the atmosphere having a slightly different refractive index to the surrounding air.
 
 

Copyright 1996 Philip M. Bagnall

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