Mc. Kelley et al., First observations of long-lived meteor trains with resonance lidar and other optical instruments, GEOPHYS R L, 27(13), 2000, pp. 1811-1814
In November 1998 the earth passed through a maximum in the cometary materia
l responsible for the yearly Leonids meteor shower. The meteor storm event
produced numerous examples of long-lived chemiluminescent trails-visible to
the naked eye-over New Mexico, where a major observation campaign was cent
ered. One trail was detected for over an hour with a CCD camera employing a
narrow sodium filter, and many others were observed for over ten minutes e
ach. For the first time, sodium densities in such trails were measured whil
e also being imaged in sodium light. We have verified one source of long-li
ved light emissions-a sodium-catalyzed reaction involving ozone-but it is f
ar too weak to explain the visibility of such trails. In addition, we prese
nt a new explanation for the cylindrical shell appearance long reported for
chemiluminescent trails and show that ozone depletion by chemical processe
s is a possible explanation for this phenomenon.