Dust Streams from Comet 67P/Churyumov-Gerasimenko

Rosetta’s comet 67P/Churyumov-Gerasimenko is beginning to show a clearly visible increase in activity.
While in the past months most of the dust emitted from the body’s surface seemed to originate from the neck region which connects the two lobes, images obtained by Rosetta’s scientific imaging system OSIRIS now show jets of dust along almost the whole extent of the comet.

“At this point, we believe that a large fraction of the illuminated comet’s surface is displaying some level of activity,” says OSIRIS scientist Jean-Baptiste Vincent from the Max Planck Institute for Solar System Research (MPS) in Germany. During the past few weeks, the OSIRIS team has witnessed a gradual but qualitative change. “In the first images from this summer that showed distinct jets of dust leaving the comet, these jets were limited to the neck region,” says OSIRIS Principal Investigator Holger Sierks from the MPS. Now, jets appear also on the “body” and “head” of the comet.

Currently, still more than 450 million kilometers are separating 67P from the Sun. Based on a rich history of ground-based observations scientists expect a comet’s activity to pick-up noticeably once it comes within 300 million kilometers of the Sun. “Being able to monitor these emissions from up close for the first time gives us much more detailed insights,” says Sierks. From the OSIRIS images, the team now wants to derive a better understanding of the evolution of cometary activity and the physical processes driving it.

Since under normal circumstances the comet’s nucleus would outshine the jets, the necessary images must be drastically overexposed. “In addition, one image alone cannot tell us the whole story,” says Sierks. “From one image we cannot discern exactly where on the surface a jet arises.” Instead, the researchers compare images of the same region taken from different angles in order to reconstruct the three-dimensional structure of the jets.

While 67P’s overall activity is clearly increasing, the mission’s designated landing site on the “head” of the comet still seems to be rather quiet. However, there is some indication that new active areas are waking up about one kilometer from landing area J. These would allow the lander’s instruments to study the comet’s activity from an even closer distance.

Rosetta is an ESA mission with contributions from its member states and NASA. Rosetta’s Philae lander is provided by a consortium led by DLR, MPS, CNES and ASI. Rosetta will be the first mission in history to rendezvous with a comet, escort it as it orbits the Sun, and deploy a lander to its surface.

The scientific imaging system OSIRIS was built by a consortium led by the Max Planck Institute for Solar System Research (Germany) in collaboration with CISAS, University of Padova (Italy), the Laboratoire d’Astrophysique de Marseille (France), the Instituto de Astrofísica de Andalucia, CSIC (Spain), the Scientific Support Office of the European Space Agency (The Netherlands), the Instituto Nacional de Técnica Aeroespacial (Spain), the Universidad Politéchnica de Madrid (Spain), the Department of Physics and Astronomy of Uppsala University (Sweden), and the Institute of Computer and Network Engineering of the TU Braunschweig (Germany). OSIRIS was financially supported by the national funding agencies of Germany (DLR), France (CNES), Italy (ASI), Spain (MEC), and Sweden (SNSB) and the ESA Technical Directorate.