Latest images show spectacular streams of dust from Rosetta’s comet

Max Planck Institute for Solar System Research Press Release

Credits: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/ INTA/UPM/DASP/IDA.
Credits: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/ INTA/UPM/DASP/IDA.

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.

ESA_ROSETTA_OSIRIS_WAC_141020b
This image was taken with an exposure time of less than a second and shows details on the comet’s surface. Image: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA.
ESA_ROSETTA_OSIRIS_WAC_141020a
This image was overexposed (exposure time of 18.45 seconds) to bring out the details of the jets arising from the comet’s surface. The images were obtained by the OSIRIS wide-angle camera on 20 October 2014 from a distance of 7.2 kilometres from the surface. Image: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA.

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.