During the entry of a meteoroid or asteroid into the upper atmosphere, an ionization trail is created, where the molecules in the upper atmosphere are ionized by the passage of the meteor. Such ionization trails can last up to 45 minutes at a time. Small, sand-grain sized meteoroids are entering the atmosphere constantly, essentially every few seconds in any given region of the atmosphere, and thus ionization trails can be found in the upper atmosphere more or less continuously. When radio waves are bounced off these trails, it is called meteor burst communications.
Meteor radars can measure atmospheric density and winds by measuring the decay rate and Doppler shift of a meteor trail.
Source : http://en.wikipedia.org/wiki/Meteoroid
Source : http://en.wikipedia.org/wiki/Meteoroid
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