Rosetta data give closest-ever look at a comet

January 22, 2015, University of Maryland
The wide-angle camera of Rosetta's OSIRIS instrument took this image on Nov. 22, 2014, at a distance of 30 kilometers from Comet 67P/Churyumov-Gerasimenko. The image resolution is 2.8 meters per pixel. The nucleus is deliberately overexposed in order to reveal the faint jets of activity. Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

On Nov. 12, 2014, the European Space Agency's Rosetta mission made history when its Philae lander touched down on the surface of comet 67P/Churyumov-Gerasimenko. While this exciting technical achievement gained lots of headlines, it was only the beginning for researchers back on Earth who are receiving and analyzing comet data. The latest chapter in the story provides the closest and most detailed look at a comet that scientists have ever seen. The results—including four papers co-authored by University of Maryland scientists—appear in a special issue of the journal Science, published on Jan. 23, 2015.

UMD astronomers Michael A'Hearn and Dennis Bodewits co-authored three of the papers, as members of the team for Rosetta's Optical, Spectroscopic and Infrared Remote Imaging System (OSIRIS). This trio of papers helps us to better understand how comets form in the first place, how their surfaces evolve over time and how to (potentially) predict their lifespans.

"We are trying to see how a comet evolves over time, and also through the course of its orbit. Gaining this detailed time series is what distinguishes Rosetta from other missions, such as Deep Impact," said A'Hearn, a Distinguished University Professor Emeritus of astronomy at UMD. A'Hearn served as principal investigator on the Deep Impact mission, which sent an impactor module to the surface of comet Tempel I in 2005. This mission was the first to remove material from the interior of a comet's nucleus—the solid central lump of ice, dust and debris—and compare it to the material at the surface.

The versatile OSIRIS imager consists of two cameras, each with its own set of specialized filters. The narrow angle camera is designed to image the surface of the comet's nucleus, while the wide angle camera focuses on the cloud of gas and dust around it.

One of the Rosetta papers uses OSIRIS images to analyze the structure of 67P/Churyumov-Gerasimenko, known to the mission team simply as C-G. Described as roughly the shape of a rubber duck, it consists of two lobes connected by a thin "neck." The team found that the majority of outgassing activity from the comet is occurring at the neck, where the OSIRIS cameras have consistently seen jets of gas and debris. The finding raises questions as to whether C-G formed from the combination of two smaller bodies, or began as one large body that shrank around the middle, like an apple that has been eaten around its core.

A second paper describes, in detail, the surface of the portion of C-G that is currently visible to Rosetta. (The "southern" face of C-G has not been seen yet, because it is facing away from the sun.) This "northern" region makes up more than half of the comet's total surface area. It is divided into 19 distinct regions, all named for ancient Egyptian deities in keeping with the nomenclature of the mission. Details about the textures and geomorphology of C-G's nucleus will help the team determine how the comet's shape has evolved over time, and where it might contain larger deposits of water and ice. This search should become easier as C-G gets closer to the sun.

This color image of Comet 67P/Churyumov-Gerasimenko is composed of three images taken by Rosetta's OSIRIS cameras using red, green and blue filters. The images were taken on Aug. 6, 2014 at a distance of 120 kilometers from the comet. Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
"Comets are effectively twice as black as coal, with a thick dust layer shrouding the surface," said Bodewits, an assistant research scientist at UMD. "It's important to look for sublimating gas. This is where there are cracks in the dust layer, which can help us find water ice and track small changes in the comet's surface."

A third paper combines data from OSIRIS and another instrument, the Grain Impact Analyzer and Dust Accumulator (GIADA). This study looks at C-G's coma—the thick cloud of dust and gas that envelops the nucleus. As the comet gets closer to the sun, the coma grows more massive as the nucleus heats up and loses more material. By measuring the activity in the coma, including changes in the ratio of dust to gas, the team should be able to estimate how quickly C-G is outgassing and losing mass. In so doing, the team hopes to learn more about how comets evolve.

"Because comets have very little gravity, dust and gas flow freely into space. But we were surprised to find a cloud of particles orbiting the comet that are large and heavy enough to defy the sun's radiation pressure," Bodewits said. The team was able to make this discovery thanks to OSIRIS' very sensitive cameras. "Each pixel is about 30 centimeters. You couldn't see a coffee cup, but you could see a large lunchbox. The resolution is about 10 times higher than Google Earth."

A'Hearn and Bodewits are particularly excited for further developments, as C-G and Rosetta hurtle ever closer to the sun. The comet will be most active when it reaches perihelion, or the single point in C-G's orbit that is the closest and most intensely affected by solar radiation. It will reach this point on Aug. 13, 2015, after which it will head away from the sun once again.

"We are already seeing more activity. Jets are sprouting up everywhere," Bodewits said. "We've been surprised to see how active it is. It already has more jets than many other comets do at perihelion."

A fourth paper is co-authored by Murthy Gudipati, a part-time senior research scientist at the UMD Institute for Physical Science and Technology. This study describes evidence for carbon-based molecules on C-G's surface, gathered by Rosetta's Visible and Infrared Thermal Imaging Spectrometer (VIRTIS) instrument.

Based on past comet studies, the team expected to see signatures of slightly more complex molecules such as alcohols, carboxylic acids and nitrogen-containing amines. However, the evidence from VIRTIS suggests that C-G's surface is instead dominated by simpler hydrocarbons. The discovery could have implications for our understanding of how carbon-based molecules first developed and spread through our solar system.

"Comets have always surprised humanity," Gudipati said. "C-G seems to be no exception."

The Rosetta mission is operated by the European Space Agency with national agencies funding the instrumentation and scientific activities. University of Maryland participation in the OSIRIS camera team is funded by NASA's Jet Propulsion Laboratory (Contract # 1267923) and a Gauss Professorship from the Göttingen Academy of Sciences (to Michael A'Hearn). The content of this article does not necessarily reflect the views of these organizations.

Four research papers described in this release were published Jan. 23, 2015, in the journal Science:

  • "On the nucleus structure and activity of comet 67P/Churyumov-Gerasimenko," Sierks et al.
  • "The morphological diversity of comet 67P/Churyumov-Gerasimenko," Thomas et al.
  • "Dust measurements in the coma of comet 67P/Churyumov-Gerasimenko inbound to the Sun," Rotundi et al.
  • "The organic-rich surface of 67P/Churyumov-Gerasimenko as seen by VIRTIS/Rosetta," Capaccioni et al.

Explore further: OSIRIS images of Rosetta's comet show spectacular streams of dust emitted into space

More information: www.sciencemag.org/lookup/doi/ … 1126/science.aaa1044
www.sciencemag.org/lookup/doi/ … 1126/science.aaa0440
www.sciencemag.org/lookup/doi/ … 1126/science.aaa3905
www.sciencemag.org/lookup/doi/ … 1126/science.aaa0628

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6 comments

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Solon
2.3 / 5 (6) Jan 22, 2015
We need data from the Langmuir probe experiment, but none is forthcoming.
Vietvet
3.3 / 5 (7) Jan 22, 2015
It makes sense that an EU advocate would be unaware of how common Langmuir probes are flown on spacecraft.

http://www.terrap..._063.pdf
Vietvet
3 / 5 (6) Jan 22, 2015
67P could float on water.

http://www.wsj.co...21953201
mreda14
1 / 5 (1) Jan 29, 2015
This article claims that they have discovered the relationship between the compositions of the interior of this comet to the composition of the surface layer. This article said the following: " This mission was the first to remove material from the interior of a comet's nucleus—the solid central lump of ice, dust and debris—and compare it to the material at the surface" , I believe that such a statement actually means that they going to send someone ( Bruce Willis) to the comet to dig deep and get samples and compare the chemical composition to the surface materials. The movie Armageddon (1998) Directed by Michael Bay. With Bruce Willis, Billy Bob Thornton, Ben Affleck, Liv Tyler. After discovering that an asteroid the size of Texas is going to impact Earth.
mreda14
1 / 5 (1) Jan 29, 2015

I do not think that such a statement is correct:
"The team found that the majority of out-gassing activity from the comet is occurring at the neck, where the OSIRIS cameras have consistently seen jets of gas and debris. The finding raises questions as to whether C-G formed from the combination of two smaller bodies, or began as one large body that shrank around the middle, like an apple that has been eaten around its core".
The reason that most out-gassing occurs at the neck is got to do with diffusion and mass transfer from a rotating object ( one large sphere connected to a smaller sphere or rubber duck rotating in vacuum) in which the surface is subliming into zero pressure (vacuum). The velocity profile and thus the concentration profile are very intense at the neck.
mreda14
1 / 5 (1) Jan 29, 2015
I have heard jokes before but this is new to me. Listen to this.
Because comets have very little gravity, dust and gas flow freely into space. But we were surprised to find a cloud of particles orbiting the comet that are large and heavy enough to defy the sun's radiation pressure," Bodewits said. The team was able to make this discovery thanks to OSIRIS' very sensitive cameras.
The surface of this comet is covered with materials that are easily sublimed (convert from solid state to the gas state) because it sublime into zero pressure or vacuum. It like a steam pipe at 2000 psi suddenly opens to the atmospheric pressure. It will burst. I do not think the weak gravity of this comet has anything to do with this.
Rate of material subliming from the surface of the comet = Mass transfer coefficient [Pressure at the surface - Vacuum pressure). Vacuum pressure = 0.0. So the Rate of material subliming from the surface of the comet is proportional to the surface pressure or the volatility

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