Author/Authors :
Furusho، نويسنده , , Reiko and Ikeda، نويسنده , , Yuji and Kinoshita، نويسنده , , Daisuke and Ip، نويسنده , , Wing-Huen and Kawakita، نويسنده , , Hideyo and Kasuga، نويسنده , , Toshihiro and Sato، نويسنده , , Yusuke and Lin، نويسنده , , Hung-Chin and Chang، نويسنده , , Ming-Shin and Lin، نويسنده , , Zhong-Yi and Watanabe، نويسنده , , Jun-ichi، نويسنده ,
Abstract :
The NASAʹs Deep Impact mission was the first impact experiment to a cometary nucleus. The target of the mission was Comet 9P/Tempel, one of the Jupiter family comets. The impact was performed on July 4th, 2005. Imaging polarimetric observations were carried out by Polarimetric Imager for COmets (PICO) mounted on the Lulin One-meter Telescope (LOT) at Lulin Observatory, Taiwan. Intensity and linear polarization degree maps were obtained on July 3–5, 2005. Impact ejecta plume was clearly recognized in the enhanced intensity map. Furthermore, arc-shaped region of high polarization was recognized in the polarization map. Dust grains in this region had larger expansion velocity than the grains which provided the brightest area in the intensity map. comparing our results with the MIR spectroscopy obtained by Subaru Telescope we conclude that very small carbonaceous grains might be responsible for the region of high polarization.
Keywords :
Comet Tempel-1 , The Deep Impact , Polarimetry , Cometsdust