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Figure 1: Mars-orbit-plane view of the positions of particles ejected from 79P/du Toit-Hartley in 1814 and propagated forward in time to 26 April, 2003. The asterisks mark the position of Mars and Jupiter along their orbits in 2003. The observed strands and kinks were created as a result of close approaches to Jupiter. X and Y are cartesian coordinates in the Martian orbit plane. |
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Figure 2:
Passages of 79P particles through the vicinity of Mars in
1999 ( left panel) and 2000 ( right panel). In the first instance we
observe at least three distinct strands crossing the Martian orbit when the
stream is on the outbound leg of its orbit with a daytime radiant. The first
two contain the bulk of the meteoroid flux in this instance and
occur within ![]() |
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Figure 3: As Fig. 2 for the years 2003 and 2005, At both of these epochs, MGS was monitoring the Martian ionosphere. The structure on the left panel was relatively short in duration and coincided with a close approach of the comet to Mars in late April 2003. The 2005 passage on the right panel shows a structure that is broader and more compact, with a division in intensity at the orbit of Mars. This should result in a longer, potentially stronger outburst. See Table 3 for details. |
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Figure 4:
Twelve ionospheric profiles collected during 21 MGS orbits
between
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Figure 5:
Distribution of structures identified by the CVW criterion
within the period between
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Figure 6:
As Fig. 5 but for the outburst
predicted in 2005. The period covered here is between
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Figure 7:
Two ionospheric electron density profiles collected during
consecutive MGS orbits at 10:58 UT and 12:56 UT on 26 Apr., 2003.
The continuous, dashed and dotted vertical lines indicate electron density values
of 0, 5.0 ![]() ![]() |
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