The location of the video camera and the apparent trail given by
Eq. (1) defines
a plane, in which the atmospheric
trajectory had to be located.
Visual sightings of
casual observers were necessary to derive the atmospheric
trajectory in this plane. We
have used a method and computer code by
Borovicka (1990)
to do this. Each visual observation
can be checked not only against the others, but against the video recorded
apparent trail, which makes the decision on what visual observations
are realistic more objective. In the final reduction we have used
the following visual observations of Table 1 combined
with the video recorded
trail from station 2: stations 1,3,4,5,6,7,8,9,10,
12,14,15,16,18,19,21,24,26,31,32,and 33.
The first observed point from station 12 was located at
E,
N,
km.
Video recorded frame 2 was located at
E,
N,
km.
The last point observed (video recorded frame 191) was located at
E,
N,
km.
Azimuth and zenith distance of the radiant for this terminal point
(frame 191) were
,
,
and the right ascension and declination of the apparent radiant were
,
.
The trajectory was very shallow, almost tangential to the Earth's
surface. The Earth-grazing character of the trajectory is also the main
reason that there was enough time to take the video record of the bolide.
On the other hand, the standard deviation of distances along the
trajectory are rather high, i.e. km for one point. Thus also the
velocities derived directly from the end part of the trajectory
using distances of only about 20 km are inaccurate.
This will be dealt with in the next section. Because the final
data on velocity and thus also for location of individual video frames
can be improved by using combination of the geometrical solution of this section.
with modeling the motion, ablation (including discrete fragmentation), and
luminosity of the bolide, we present also the final data on locations
together with velocities in Table 4 of the next section.
Copyright The European Southern Observatory (ESO)