2.4
Forming of meteor currents
By fragmentation of comet nucleus it
is possible to explain the shaping not only of the cometary’s
tails but also of the meteor currents.
As before mentioned, in 1866 the
comet Biela completely disintegrated and arouse a
cloud of meteorites that seemed originating from the constellation Andromeda.
E. Weis calculated that the Earth will pass in close proximity to the orbit of
the late comet on November 1872. Indeed on November 27, 1872, fragments of the
comet Biela appeared like a swarm of falling stars of
an extension and intensity rarely seen from the Earth. At Moncaliery
(
Later on, other relations were
established among nuclei of certain comets and meteor currents. Lyrids (from the constellation Lyra)
were associated to the comet 1861 I. Leonids (from
the constellation Leo) were associated to the comet 1866 I.
The comet Halley has already
produced two swarms: Eta Aquarids, between April 30
and May 11, appearing in May, and Orionids, in
October 15-26.
D.
The distribution of the particles of
a meteor current along the mother orbit is not uniform; here and there appear
some accumulation of particles. This explains "the rains of falling
stars", more or less intense, when the Earth crosses the orbit of a
current. The distribution of the particles on the initial orbit gets so much
more uniform as the current seems older, and on this basis it is possible to
calculate the "age" of the current. The lack of uniformity of the
meteor’s current it explained in vortex theory by two mechanisms:
As to the breadth of the meteor currents,
it is proportional to the duration of activity of the respective radiant. Thus
the radiant activity of the Perseids (current
proceeding from the comet 1892 II) was observed by Hoffmeister
from July 20 to August 19, 1948. Thereby was obtained the conclusion that the
breadth of this current was of 0,5a.u., approximately
75,000,000 km. The distribution of the particles along the current was almost
uniform. According to E. Ahmert-Rohlfs, the age of
this current may be of 80,000 years.
By the hourly frequency of the
meteors it is also possible to evaluate the spatial density of the current,
precisely the mean distance among its particles. There are very dense currents
(Leonid, observed in 1833), where the measured mean distances among particles
are of 15-30 km, and there are currents where distances are of 1,000 to 2,000
km, and more. Of course, in the evolution of the meteor fragments, under the
action of the differentiated motion, there is a moment when the width of the
meteor current is so large that the current itself loses its individuality and
diffuses throughout the fluid environment.