Ian S. Murray,
University of Regina, Canada.
Last updated: October 2002
E-mail: murray1 [at] uregina.ca
Brief Biographical Information:
Graduate student at the University of Regina (Department of Physics), in
the heart of the Canadian prairies. My work (a study of the physical structure of meteoroids)
is being completed under the watchful eye of my supervisor Prof. Dr. Martin
Beech also in collaborations with Dr. Robert Hawkes at Mount Allison
University.Born and raised in Moncton, New Brunswick on the East coast of
Canada. Looking forward to participating in my third MAC, it was a
wonderful and enriching experience in previous years.
Research on Leonid MAC:
- Physical Structure of Meteoroids
- Lunar Impacts
- VLF Detection of Fireballs
- Flickering Events in the Peekskill Fireball
- Unusual Phenomena
Related studies of the leonids in November 1998
We have used dual coaxial microchannel plate image intensified monochrome CCD detectors run at standard
NTSC frame rates (30 fps) to study the Leonid meteor shower on Nov. 17, 1998 from an airborne platform at
an altitude of about 13 km. The observing systems had fields of view (width) of 16.3ÿý and 9.5ÿý, and limiting stellar
sensitivities of +8.3m and +8.9 m. Over 12 hours of recording 230 meteors were detected, of which 65 were
Light curves are presented for 53 of these meteors. The magnitudes at peak brightness of the meteors investigated
were generally in the range from +4.0m to + 6.0m. The mass distribution indicies for the two samples are 1.67 and
1.44, with the former being based on the wider field of view dataset. The light curves were skewed with the brightest
point towards the beginning of the meteor trail. The F parameter for points one magnitude below maximum
luminosity had a mean value of 0.47 for the wider field system and 0.37 for the more sensitive narrower field system.
We provide leading and trailing edge light curve slopes for each meteor as another indication of light curve shape.
There were few flares obvious on the light curves, indicating that in-flight fragmentation into large number of grains
is not common.
There is variability in light curve shape from meteor to meteor. The light curves are inconsistent
with single, compact body meteor theory, and we interpret the data as indicative of a two component dustball model
with metal or silicate grains bonded by a lower boiling point, possibly organic, substance. The variation in light
curve shape is due to differences in mass distribution of the constituent grains. We provide trail length versus
magnitude data. There is only a slight hint of a bend in the data representing the difference between meteors which
have broken into a cluster of grains prior to grain ablation, and those which continue to fragment during the grain
ablation phase. Several specific meteors show interesting light curve features. One meteor is nebulous in appearance,
with significant transverse width. The apparent light production region extends for 450 m from the centre of the meteor
path. Another meteor has several main fragments, and evidence of significant separated fragments.
In the 1999 Leonid MAC, we discovered that the lightcurves tended to differ from those in the 1998 campaign,
suggesting that meteoroids fragmented differently. More about this published work can be found
In future missions, we will continue to study the morphological
changes as a function of different positions in the comet dust trails and as a function of age since ejection.