The debris trail and near-nucleus dust environment of the ROSETTA mission target 67P/Churyumov-Gerasimenko.

Details The debris trail and near-nucleus dust environment of the ROSETTA mission target 67P/Churyumov-Gerasimenko. The debris trail and near-nucleus dust environment of the ROSETTA mission target 67P/Churyumov-Gerasimenko.

May 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003dps....35.3007r&link_type=abstract

American Astronomical Society, DPS meeting #35, #30.07; Bulletin of the American Astronomical Society, Vol. 35, p.970

Astronomy and Astrophysics

Astronomy

2

Scientific paper

It is thought that most short-period comets are trailed by large (>mm sized) particles ejected from the nucleus and in the process of dynamical evolution along the comet's orbit through the influence of solar gravity and radiation pressure. The intersection of cometary debris trails with the orbit of Earth gives rise to meteor streams. Cometary debris trails where first discovered by the Infrared Astronomical Satellite[1] in thermal emission at mid-IR wavelengths and have only recently have been detected in reflected visible light [2,3].
The primary target of the ESA ROSETTA mission is the periodic comet 67P/Churyumov-Gerasimenko (CG), which is known to have an IRAS dust trail. We have obtained several nights of deep imaging at the Palomar Mountain 60 and 200-inch telescopes in May/June 2003. Figure 1 clearly shows the dust trail of CG, which extends behind the comet several tens of arcminutes. We use the surface brightness profiles to characterize the particle size and mass fraction of dust in the trail as well as quantify the dust production in the near-nuclear environment. A more complete understanding of CG will be afforded by the planned 5-40 micron observations of the Space Infrared Telescope Facility (SIRTF), scheduled soon after launch in August 2003.
References: [1] Sykes & Walker (1992) Icarus, 95, 180. [2] Ishiguro et al. (2003) ApJ, 589 L101. [3] Weissman et al. (2003) LPS 34, 2056.

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