Deep Impact observations by OSIRIS onboard the Rosetta spacecraft.

نویسندگان

  • Horst Uwe Keller
  • Laurent Jorda
  • Michael Küppers
  • Pedro J Gutierrez
  • Stubbe F Hviid
  • Jörg Knollenberg
  • Luisa-Maria Lara
  • Holger Sierks
  • Cesare Barbieri
  • Philippe Lamy
  • Hans Rickman
  • Rafael Rodrigo
چکیده

The OSIRIS cameras (optical, spectroscopic, and infrared remote imaging system) onboard the European Space Agency's Rosetta spacecraft observed comet 9P/Tempel 1 for 17 days continuously around the time of NASA's Deep Impact mission. The cyanide-to-water production ratio was slightly enhanced in the impact cloud, compared with that of normal comet activity. Dust particles were flowing outward in the coma at >160 meters per second, accelerated by the gas. The slope of the brightness increase showed a dip about 200 seconds after the impact. Dust Afrho values before and long after the impact confirm the slight decrease of cometary activity. The dust-to-water mass ratio was much larger than 1.

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عنوان ژورنال:
  • Science

دوره 310 5746  شماره 

صفحات  -

تاریخ انتشار 2005