Category Archives: rosetta spacecraft

The Rosetta Mission at Comet 67P Will Soon End

Studying a Comet Long Term

This four-image montage shows the spectacular region of activity at the 'neck' of 67P/C-G. This is the product of ices sublimating and gases escaping from inside the comet, carrying streams of dust out into space. ESA/Rosetta/NAVCAM
This four-image montage shows the spectacular region of activity at the ‘neck’ of 67P/C-G. This is the product of ices sublimating and gases escaping from inside the comet, carrying streams of dust out into space. ESA/Rosetta/NAVCAM

I’ve been a comet fan since my grad school days. That was when I got pointed at Comet Halley and told, “study these images, and let’s figure out what’s happening with the plasma tail”. So, I pored over images of the comet taken from 1985-1986. I made lots of measurements and worked on papers with my team members. Eventually, we figured out what was happening with the plasma tail (hint: it’s affected by the solar wind). It was a pretty exciting time in my life, standing at the “frontier” of comet science (at that time) and opening my mind to the idea that what happens in the solar wind can make intricate “designs” in the shape and behavior of a plasma tail.

During that whole time, I was also intrigued by what a comet REALLY looks like. We didn’t have any close-up pictures of a comet nucleus. Sure, we had the Fred Whipple model of a chunky block of dusty ice (or icy dust, if you prefer) to study. And, there WERE some Giotto spacecraft images of the Halley nucleus. But they had to suffice until we could get REAL close-ups. What was needed was a long-term study of a nucleus. That’s what the Rosetta mission has done at the nucleus of Comet 67P/Churyumov-Gerasimenko.

Rosetta Orbits a Piece of Solar System History

For the better part of two years, the Rosetta spacecraft has visited the comet. It studied the chemical composition, sent back images, and gave astronomers the longest “timelapse” look at a comet ever. Along with its Philae lander, which functioned for only a short time, Rosetta is a great achievement. It’s something the European Space Agency and scientists around the world can be very proud to have sent. They’ve orbited a major piece of solar system history. They opened a window into the distant past when comets formed from materials that existed before the Sun and planets did. Studying a comet is like opening a treasure box.

In a few weeks, the mission will send its final images and data, and on September 30, 2016, the orbiter will do a slow crash landing on the surface of the comet. Its last messages should contain some very high-resolution images and data. You can follow the Rosetta mission at the ESA Website for the mission and track the spacecraft’s final days and weeks.

Rosetta: the Executive Summary

It’s been an amazing couple of years. Sure, we see what the comet’s surface looks like with its icy plains, boulders, and rocky inclusions. However, Rosetta’s chemical analysis on the comet’s ices and dust reveal information about the comet’s origins in the early epochs of the solar system’s formation. It also shows that the comet contains ingredients crucial to the formation of life. Mind you, Rosetta didn’t find life. However, uncovering the ingredients of life tells an important story. What did it find? Rosetta detected the amino acid glycine as well as the element phosphorus in the comet’s ices. These are key elements in our DNA and cell structures.

Comets as a Source of Water?

Another question astronomers wanted to answer was “Did Earth’s water come from comets?” Rosetta showed that the comet’s water chemistry is slightly different from Earth’s water. That means that ocean water on our planet didn’t all come from comets like 67P. Understanding where Earth’s water came from is still a big question in planetary science, and now astronomers are looking at other comets and asteroids for keys to the mystery.

I’m looking forward to the last images and data from Rosetta. I’m sure many comet fans, scientists, and graduate students are, too. There’s enough work in the treasury of information the spacecraft sent back to keep whole teams busy for years. In the end, even though Rosetta will no longer be working, its work WILL live on. That’s a major legacy for any mission!

It’s the Pits On Comet 67P

From Sinkholes to Jets

Active areas with sinkholes and pits on the Seth Region of Comet 67P/Churyumov-Gerasimenko. The central pit is about 220 meters across and 185 meters deep. Courtesy ESA/Rosetta/MPS for OSIRIS team/MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

It’s quite a week for solar system exploration news. Pluto (which is way more than a planet!) continues to be on everybody’s mind with the upcoming close flyby of the New Horizons mission.  Dwarf planet Ceres is still getting the once-over from Dawn. And, today we’re starting to get more high-resolution images from the Rosetta mission’s OSIRIS camera as it scans Comet 67P/Churyumov-Gerasimenko.  Check out this latest image, showing sinkholes and pits on the surface. It’s more than likely they play an important role in creating the jets of dust we see flowing away from the nucleus. A number of the dust jets trace back to these pits, and that’s giving mission scientists a peek into the interior processes that drive those outbursts.

Active Pits and Sinkholes

Scientists have found at least 18 pits, sort of circular in shape, across various parts of the cometary nucleus. They range in size from a few tens of meters across to a few hundred meters. The deepest ones are around 210 meters, and their floors seem to be covered in dust. Other images of the comet show dust jets rising up from fractures in the walls of the pits. The fractures mean that there are volatiles (gases and ices) just below the surface. AS those materials get warmed by the Sun, they expand, and that forces cracks into the sinkhole walls. The trapped materials, plus dust, come rushing out of the cracks and out to space, creating the jets we’ve all been seeing emanating from the comet.

The pits likely form as the materials rush out, leaving behind a cavity under the surface. The cavities could also have existed since the comet was formed, or some other heating caused ices to vent out after the upper layers warmed up. However the cavities formed, eventually their ceilings can’t hold up any more, and they collapse, creating the pit.

Comet 67P is due to make its closest approach to the Sun on August 13, 2015. The Rosetta spacecraft is orbiting the comet’s nucleus and will be charting how the comet changes up to, during, and after perihelion. The newly awakened Philae lander may also contribute observations, depending on how well it can communicate with the orbiter. This mission is giving us all a new look at some very old ice as it makes its passage through our part of the solar system.

Want to follow the mission? Check out the Rosetta mission pages for more images and announcements.