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Deformation of a Meteor Stream Caused by an Approach to Jupiter

Published online by Cambridge University Press:  14 August 2015

B. Yu. Levin
Affiliation:
O. Schmidt Institute of Physics of the Earth, U.S.S.R. Academy of Sciences, Moscow, U.S.S.R.
A. N. Simonenko
Affiliation:
Committee on Meteorites, U.S.S.R. Academy of Sciences, Moscow, U.S.S.R.
L. M. Sherbaum
Affiliation:
Astronomical Observatory, Kiev University, Kiev, U.S.S.R.

Abstract

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The increase in the width of a meteor stream with time is usually regarded as due to differences in the secular variations of the slightly different orbits of individual meteoroids. However, the ordinary differential planetary perturbations acting on different parts of an elliptical ring of meteoroids have a more important effect. Model calculations are presented for a filament-like stream that makes close approaches to Jupiter. They confirm the major importance of deformations of the stream by direct planetary perturbations that act even on a filament-like stream of zero thickness. The disturbed part of the stream takes the form of a bend, dispersing along the initial orbit and producing a significant decrease in the spatial density of the meteoric particles.

Type
Part VI/Relationship With Meteors and Minor Planets
Copyright
Copyright © Reidel 1972 

References

Ahnert-Rohlfs, E.: 1952, Veroeffentl. Sternw. Sonneberg 2, 38.Google Scholar
Levin, B. Yu.: 1956, Fizicheskaya Teoriya Meteorov i Meteor noe Veshchestvo v Solnechnoj Sisteme , Akad. Nauk SSSR, Moscow. (See also Levin, B. Yu.: 1961, Physikalische Theorie der Meteore und die meteoritische Substanz im Sonnensystem, Akademie-Verlag, Berlin.) Google Scholar
Sherbaum, L. M.: 1970, Vestn. Kiev. Gos. Univ. Ser. Astron. No. 12.Google Scholar