Cometary Dust Trail Associated with Rosetta Mission Target: 67P/Churyumov-Gerasimenko
Masateru Ishiguro

TL;DR
This study definitively identifies and characterizes the dust trail and neckline structure of comet 67P/Churyumov-Gerasimenko, estimating dust grain sizes and assessing the comet's activity over multiple apparitions.
Contribution
It provides the first definitive identification of the dust trail and neckline structure of 67P and estimates dust grain sizes and mass-loss rates over time.
Findings
Dust trail observed consistently from 2002 to 2003
Maximum dust grain size approximately 1 cm
Comet's activity remained stable over a dozen years
Abstract
A thin, bright dust cloud, which is associated with the Rosetta mission target object (67P/Churyumov-Gerasimenko), was observed after the 2002 perihelion passage. The neckline structure or dust trail nature of this cloud is controversial. In this paper, we definitively identify the dust trail and the neckline structure using a wide-field CCD camera attached to the Kiso 1.05-m Schmidt telescope. The dust trail of 67P/Churyumov-Gerasimenko was evident as scattered sunlight in all images taken between September 9, 2002 and February 1, 2003, whereas the neckline structure became obvious only after late 2002. We compared our images with a semi-analytical dynamic model of dust grains emitted from the nucleus. A fading of the surface brightness of the dust trail near the nucleus enabled us to determine the typical maximum size of the grains. Assuming spherical compact particles with a mass…
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