The Canadian Meteor Orbit Radar Meteor Stream Catalogue

Author(s):  
Peter Brown ◽  
Robert J. Weryk ◽  
Daniel K. Wong ◽  
James Jones
Keyword(s):  
2007 ◽  
Vol 102 (1-4) ◽  
pp. 209-219 ◽  
Author(s):  
Peter Brown ◽  
Robert J. Weryk ◽  
Daniel K. Wong ◽  
James Jones
Keyword(s):  

2004 ◽  
Vol 33 (9) ◽  
pp. 1486-1490 ◽  
Author(s):  
A.B. Beletsky ◽  
O.G. Gress ◽  
A.V. Mikhalev ◽  
A.Yu. Shalin ◽  
A.S. Potapov
Keyword(s):  

1980 ◽  
Vol 90 ◽  
pp. 153-156
Author(s):  
David W. Hughes ◽  
Iwan P. Williams ◽  
Carl D. Murray

At the present time the orbit of the Quadrantid meteor stream not only intersects the orbit of Earth but also passes very close to the orbit of the planet Jupiter. This causes considerable perturbations. In a series of three papers (1,2,3) the authors replaced the myriad of meteoroids in the stream by ten test particles set at equal intervals of eccentric anomaly around the orbit. The equations of motion of these particles in the solar system were solved using a standard fourth order Runge–Kutta technique with self–adjusting step lengths. The orbits of the test particles were output at ten year intervals going back from the present to the year 300 B.C. and forward into the future to the year A.D. 3780.


1980 ◽  
Vol 90 ◽  
pp. 101-104
Author(s):  
W.G. Elford.

The majority of radio studies of meteors have been carried out at frequencies higher than 17MHz and most of the rate observation at frequencies above 30MHz. At these frequencies a severe height selection of meteors occurs. In Figure 1(a) are shown the normalized height distributions of sporadic meteors observed at Adelaide on frequencies of 27MHz and 2MHz (Brown, 1976). The sharp cutoff of the latter distribution below 87 km is instrumental. The difference in the height distributions is due to the effect of the finite diameter of a meteor trail on its radar detectability. If the trail diameter is ≪ λ signals from the near and far edges reinforce but as the trail expands due to diffusion and the diameter becomes ≃ λ/4, interference reduces the amplitude. A meteor trail, produced by a particle with a velocity of 30 km s−1, has an initial diameter of 0.4m at 80 km, 2.0m at 104 km and 4.0m at 116 km.


Author(s):  
Vladimir Porubčan ◽  
Leonard Kornoš
Keyword(s):  

1996 ◽  
Vol 150 ◽  
pp. 137-140
Author(s):  
J. Jones ◽  
P. Brown

AbstractWe have reworked Whipple's (1951) theory of the ejection of meteoroids from comets to include the effects of cooling by the sublimation of the cometary ice and the adiabatic expansion of the escaping gases. We consider only those particles moving significantly slower than the gas speed and find that the inclusion of these effects does not yield results much different from Whipple's theory. We have extended the theory to include the case of an active area in the form of a spherical cap and have shown how the characteristics of the ejection process change when the cap is in the form of a pit or a depression. We present a empirical formulae which should be useful to modellers of meteor stream evolution.


1992 ◽  
Vol 254 (4) ◽  
pp. 627-634 ◽  
Author(s):  
R. Gonczi ◽  
H. Rickman ◽  
C. Froeschle
Keyword(s):  

1985 ◽  
Vol 83 ◽  
pp. 179-180
Author(s):  
Cl. Froeschlé

We investigated the orbital evolution of Quadrantid-like meteor streams situated in the vicinity of the 2/1 resonance with Jupiter. For the starting orbital elements we took the values of the orbital elements of the Quadrantid meteor stream except for the semi-major axis which was varied between a = 3.22 and a = 3.34 AU. We considered these meteor streams as a ring and we investigated the resonant effect on the dispersion of this ring over a period of 13 000 years. Only gravitational forces due to the Sun and due to Jupiter were taken into account.


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