Comet dust and nuclei:Clues from meteor studies - PowerPoint PPT Presentation

1 / 22
About This Presentation
Title:

Comet dust and nuclei:Clues from meteor studies

Description:

Showers appear at the same SIDERIAL time each year (indicating an extra-terrestrial origin) ... Shoemaker-Levy 9. SW3 in 2006 ... – PowerPoint PPT presentation

Number of Views:78
Avg rating:3.0/5.0
Slides: 23
Provided by: iwanwi
Category:

less

Transcript and Presenter's Notes

Title: Comet dust and nuclei:Clues from meteor studies


1
Comet dust and nuclei-Clues from meteor studies
  • Iwan Williams
  • Rosetta Meeting Budapest
  • 17-19 December 07

2
Meteor showers
  • Meteor Showers represent an increased flux of
    meteors above the normal background (about 6
    meteors per hour)
  • Showers appear at the same SIDERIAL time each
    year (indicating an extra-terrestrial origin)
  • In showers, all meteors appear to radiate from
    same point on the sky, called the radiant.
  • CONCLUSION. They are caused when the Earth
    intersects a stream of small dust grains or
    meteoroids.
  • Showers are named after the constellation in
    which the radiant lies.

3
  • Some showers can be spectacular, for example the
    Leonids every 30 years or so with rates in excess
    of 1 per second.
  • The majority are not, they just produce 10-20
    meteors per hour on an annual basis

4
What do we get directly from showers, that is
simply from looking at individual meteors and
measuring deceleration and magnitude?
  • Brightness is proportional to rate of change of
    kinetic energy ( mass, velocity, deceleration,
    mass loss rate)
  • Deceleration depends cross-section, mass and speed

5
  • In principle, we know velocity, deceleration and
    brightness.
  • This leaves two equations and three variables,
  • mass, cross section and mass loss rate.
  • So need an other equation. This is usually done
    by relating mass loss rate to surface temperature
    or by approximating( eg ,mass loss small, ok for
    big things but not for all then the first
    equation gives mass)

6
Mass range
  • Interest is in the large end. There are quite
    large bodies associated with well-known showers.
  • Five Perseids with masses of 3,10,16,16 and 600g
    have been measured.The largest of these could be
    as much as 4cm in radius.

7
Mass distribution function
  • dn CM-s dM, ie dn is the number with mass
    between m and mdm.
  • Note if slt2 mass is dominated by large meteoroids
  • And if sgt2 by the small end
  • There is some indication that s is larger for
    meteors with mass above .08g, say s 1.7 below
    this and 2.3 above. If true total mass is finite
    even for 0 to infinity range. (cumulative 3)
  • There is some variation from shower to shower eq
    Lyrids about 1.7 and Orionids at 2.1
  • This number is same ball-park as is obtained by
    theoretical collisional fragmentation models

8
Density (value depends on whether fragmentation
in the atmosphere is assumed- sudden
fragmentation increase the surface area to mass
ratio, slow continuous sputtering affects mass
loss rate)
9
Meteor Streams
  • For a given meteor it position is known- that of
    the Earth.
  • Its Geocentric speed is determined, hence its
    energy, semi-major axis and period are easily
    obtained.
  • Its path (giving the radiant)
  • This is sufficient to determine its orbital
    elements.
  • It has been recognized for a long time that
    stream orbital elements are very similar to those
    of specific comets, eg Orionids and Halley,
    Perseids and Swift-Tuttle or the Leonids and
    Tempel-Tuttle.

10
Stream Formation
  • Meteoroid are carried away from the nucleus by
    the normal gas production process. (Called large
    cometary dust grains)
  • They thus have a slightly different heliocentric
    velocity to that of the comet.
  • This implies a different orbital energy and thus
    a different semi-major axis (and Period)

11
  • Hence, the difference in semi-major axis gives us
    the ejection velocity?
  • Unfortunately planetary perturbations change
    orbits, so its not quite that simple.
  • This process is repeated at every perihelion
    passage, giving rise to a broad stream with many
    strands in it since the orbit of the comet will
    have changed, mainly due to planetary
    perturbations.

12
  • As the stream ages, these strands may merge
    together, giving a broad stream with the shower
    having a broad activity curve
  • The most recent activity may still show up (eg
    Perseids) or there may be resonance effects
    maintaining the strands (eg Leonids)

13
  • Detailed modeling of the Perseids or Quadrantids
  • can however give a strong indication of the value
    of the ejection velocity
  • This usually turns out at 10s m/sec (Not 100s)

14
Is there an other way of forming meteor showers?
  • Some asteroids have orbits that are very similar
    to stream orbits and of course, collisions can
    cause dust to be ejected from the asteroid.

15
  • Such a process can not really insert enough dust
    in orbit to form a strong meteor shower, it is a
    one-off event.
  • A collision between two big bodies, forming an
    asteroid family might, but all know events
    happened a long time ago, so the dust will have
    dispersed

16
Some comets break up, for example Comet Biela
  • Pre 1833 a normal comet.
  • 1839 Not observe.
  • 1846 Two comets present
  • 1852 Both comets still present but fainter.
  • 1872 a strong meteor shower seen at the time the
    Earth passed close to where comet Biela would
    have been.

17
Shoemaker-Levy 9
18
SW3 in 2006
  • Such a break-up releases vast amounts of dust and
    this is taking place now.
  • SW3s orbit does not intersect the Earths orbit
    so we are unlikely to observe a meteor shower
    from it.

19
The Quadrantids may have a complex history with
all activities possible
  • The Quadrantid parent had been around for several
    thousand years ejecting meteoroids in the normal
    way
  • Comet Maccholtz may well represent a fragment of
    this.

20
  • Comet of 1491 may also be a sighting of some
    fragment.
  • Sometime later (about 1800) a major fragmentation
    took place, leaving a dormant fragment 2003EH1and
    a large new shower ( the narrow strong Quadrantid
    peak)

21
Is this distinction in stream formation processes
important?
  • Yes. Normal stream formation essentially produces
    data only on near surface grains.
  • Comet break-up produces data on interior grains
  • Quadrantids are essentially no different to
    others shower grains so perhaps the surface
    grains are good representatives of all. BUT 2003
    EH1 is a big bit (several kilometers) so there
    may be big bits inside

22
Conclusions
  • Fragility from Deep Impact (No large grains
    observed)
  • However large grains (over cm size) are initially
    there.
  • Density is the real problem. Is the high or the
    low values the correct ones?
  • For the cm sized, the high is more likely
    correct??
Write a Comment
User Comments (0)
About PowerShow.com