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Rosetta: Days from the toughest space landing ever

Ten years after leaving Earth, one of humanity's most ambitious space missions is ready for its climax – a nail-biting drop onto the surface of a comet

Video: Homemade Rosetta comet recreates duck shape

Ten years after leaving Earth, one of humanity’s most ambitious space missions is ready for its climax – a nail-biting drop onto the surface of a comet

MATT TAYLOR will soon experience the most agonising 28 minutes and 20 seconds of his life. That’s how long it takes a signal to travel the 500 million kilometres from the surface of comet 67P Churyumov-Gerasimenko to the European Space Agency’s mission control in Darmstadt, Germany. So that’s how long Taylor must wait to find out if his team has made history by landing a spacecraft on a comet for the very first time.

The European Space Agency (ESA) craft, Rosetta, has been orbiting comet 67P since August. But the most daring part of the mission begins on 12 November. At 0835 GMT, Rosetta will cast adrift a washing-machine-sized lander called Philae. For the next 7 hours or so, Philae will be pulled down by the comet’s puny gravity, dropping 23 kilometres. Touchdown is scheduled for around 1530 GMT, when the nail-biting wait to hear a signal from Philae will begin.

Rosetta: Days from the toughest space landing ever

Can mission controllers pull off the toughest landing ever? (Image: ESA/Rosetta/Philae/CIVA)

Plenty could go wrong. Philae could overshoot its target. It could bounce off the comet. Or crash land. It could even be blasted to pieces by jets of gas erupting from the comet. “This is the most challenging mission ESA has ever attempted,” says Taylor. By 1600 GMT, we will know if Philae has earned a place in the space hall of fame and started its pioneering scientific investigations, or become an extremely expensive piece of space junk.

There is a great deal we want to find out about 67P. “Many of us are now convinced that life was possible on Earth only because water and certain organics were brought by the comets,” says Philae’s lead scientist Jean-Pierre Bibring of the Space Astrophysics Institute in Orsay, France.

Comets are often called dirty snowballs. They appeared early in the solar system’s history and formed anywhere water can freeze. Back then, dust and rocks merged into ever larger proto-worlds that went on to merge and make planets. Comets were also part of this process and brought their supply of water to the forming planets.

The comets that remain today are the astronomical leftovers – the getaways. They were slingshotted to the farthest reaches of the solar system by the gravity of Jupiter and Saturn. Now they wander in darkness, bound to the sun by only the weakest of gravitational threads. Occasionally, one falls back towards the sun and we catch a window back in time to when they filled the solar system.

Ground-based observations of about 150 comets have revealed that most have an abundance of organic compounds. There is little doubt that they helped to supply our planet with the molecular building blocks of life. “A fundamental question to answer is what are all the complex molecules that are on the comet?” says Mike A’Hearn at the University of Maryland in College Park.

Identifying these molecules from Earth is difficult because it relies on the comet throwing them into space to form its tail. The molecules seldom survive intact and so astronomers see only fragments, usually just pairs and triplets of carbon atoms. The unbroken molecules on a comet’s surface can sometimes be seen using infrared equipment, but rarely do comets become bright enough at these wavelengths to produce adequate signals.

A better way is to visit a comet. In 2005, A’Hearn headed a NASA mission called Deep Impact that fired a copper cannonball into comet Tempel 1 and observed the cloud of dust and gas the collision threw up. The trouble was that the impact also broke up many of the organic molecules in which they were interested.

From a distance, Rosetta has already caught a passing whiff of rotten eggs, cat urine and bitter almonds.

Philae's first science

Having tried a slap, it’s time for a tickle. Philae will put its mechanical hands into the undamaged carbon compounds and analyse them with its many instruments. “Philae should sort this all out,” says A’Hearn.

But first it has to get there. Usually, space flight is a comparative piece of cake. With no air pressure or friction to disturb spacecraft, they follow precise orbits that can be predicted using Newton’s law of gravity. Around a comet, things are different. First, comets boast hardly any gravity. Rosetta had to get within 30 kilometres to experience 67P’s gravitational pull. Before then thrusters had to be fired now and again to manoeuvre the spacecraft around its target.

But that’s not the worst of it. Heat from the sun boils away the ice on the comet to create an atmosphere, known as the coma, that streams away to become the characteristic tails. This is not a gradual or a uniform process. The activity comes from specific sites on the comet, and is highly variable in the amount of gas that is driven away.

Peril at every turn

Rosetta’s giant solar panels, which measure 70 square metres, act like sails and mean the spacecraft is constantly buffeted, unpredictably changing its course and its orientation. The ground crew have had to become used to the navigation-camera images showing empty space when they should be showing the comet. “With Rosetta, you’re never where you think you are,” says ESA’s Nicolas Altobelli, who works on the mission.

Although mission controllers are now adept at correcting these meanderings, there is no way to predict them in advance. And as the comet warms up as it gets closer to the sun, the activity increases and the problem gets worse.

The upshot is that the team cannot know exactly where Rosetta will be when the lander is released. Neither can they know exactly how Philae will drop to the surface. Taking all the uncertainty into account, the lander could touchdown anywhere within half a kilometre of its designated target spot – and that’s a big problem.

At the beginning of the mission, the design team had assumed that the comet was a potato-shaped object with large, smooth areas on its surface. They pegged their chances of a successful landing at 70 to 75 per cent. Now, all bets are off.

“At the beginning, mission planners assumed the comet was potato shaped”

The reason is the comet’s dramatic and unexpected shape. When new images from Rosetta arrived at Bibring’s laboratory on 14 July, they showed that 67P looks more like a rubber duck than a potato. Even now, the smaller lobe is still referred to as the head and the larger lobe as the body.

Worse, they showed that 67P was rotating every 12 hours around an axis that passed at an angle through the duck’s neck rather than from head to toe. “It was juggling around in all different directions,” says Bibring, “When we saw that, we feared this is just not going to happen. There will be nowhere that we can land safely. We were excited, but desperate.”

But you only live once, so the flight-dynamics team began to look for ways to make it happen. To everyone’s surprise, landings were possible in a number of locations, albeit at the highest touchdown speed that the lander was designed to survive. Spirits lifted.

Then more detailed pictures arrived. “Our fears returned when we saw a large variety of surface features we hadn’t envisioned. Instead of being flat, the surface looks terribly odd,” says Bibring.

Of five candidate sites, the most promising was labelled B. It was the only one that looked more or less flat across the whole landing area. But there was more bad news just around the corner. Higher-resolution images showed that the landing field was strewn with boulders 2 to 10 metres in size. Tens of thousands of smaller boulders might be there too. Each rock could upturn or wreck Philae if the lander happened to come down on top of one.

So mission controllers finally plumped for landing site J on their shortlist. J is located on the top of the duck’s head. It’s not the flattest area but there are fewer slopes steeper than 30 degrees, the maximum Philae is designed to cope with. “It is not necessarily the best site for science, but it offers the best chance of success,” says Bibring.

If Philae makes it, its science investigations will start as soon as possible (see diagram). These will answer one of the most obvious questions about 67P: is it two objects stuck together or one gradually eroding into two?

Bibring is keeping an open mind but points out that a comet’s activity is driven by its shape. Sunlight entering a crack in the surface, for example, drives off volatile ice underneath and widens the crack. This enhances the activity and sets up a feedback loop. Where you once had a crack, now you have a crevasse. This chimes with what might have happened at 67P. Most of the activity observed so far is coming from the neck, meaning that it is inexorably becoming narrower and weaker. “If we are lucky, it will fall to pieces the day after we land,” he says, only half-jokingly.FIG-mg29940601.jpg

Rosetta’s instruments have already started sizing up 67P. They show that the comet is 4 kilometres across at its widest point and isn’t very dense at all – in fact, its density is much lower than water ice. This means that 67P must be more than 60 per cent empty space. Perhaps that means there are large caverns inside – cathedral-sized spaces that could burst open as the comet becomes more active. “We just don’t know yet,” says Martin Pätzold at the University of Cologne in Germany. It could be that the dust and gas is instead in a fluffy, loosely bound aggregate. “Whatever it is, it will help tell us how comets are formed. We really don’t know that yet either,” he says.

If Philae lands successfully, its instruments will give us answers. While the first science sequence is taking place, the confirmation signal of landing will arrive at Earth. This will contain information on Philae’s position, orientation and condition. As the lander team analyse this, Philae will begin drilling into the comet to begin its chemistry experiments.

These will continue for as long as Philae’s initial battery power lasts. Once that runs out – anytime between 40 and 50 hours after landing – it will switch to rechargeable batteries powered from solar panels. All being well, Philae will then enter the long-term science phase in which the experiments on the surface will continue with increasing refinement.

So long as the rechargeable batteries hold out, and there is no untoward comet activity that damages the lander, the mission’s natural end will come in March 2015. By then, the comet will be closer to the sun, and the temperature will begin to affect the lander’s electronics.

If Philae survives that far, it will be a major triumph. Its measurements will keep cometary scientists busy for years. For Bibring, it is the organic chemistry and its role in the origin of life on Earth – and potentially elsewhere too – that holds the greatest promise. “The question ‘are we alone in the universe?’ is directly connected to what we are investigating with this mission,” he says.

“The question ‘are we alone in the universe’ is directly connected to this mission”

After all, exoplanet hunters have catalogued orbiting more than 1100 stars. They may not look much like our solar system, but does that mean they are all barren? Not necessarily. Excitingly, researchers have spotted comets in 11 other solar systems. So understanding the complex organic chemistry that takes place in comets and young solar systems may be the clue we need to unlock how life gains its foothold and turns a young planet into a potential habitat.

So perhaps it is no wonder that when Taylor stood in front of hundreds of planetary scientists to give a status report in September, he elicited a round of spontaneous applause with his first sentence: “This is the sexiest mission that’s ever been flown in space.”

But make no mistake; sexy comes with risks. The chances of failure are high. While the main orbiter mission will continue regardless of whether or not Philae makes it, the world will be watching on 12 November.

“If we fail because of something that we could not predict, then ok,” says Bibring. “Worse would be if we have underestimated something we should not have underestimated.” That’s why he and every other Rosetta team member is working overtime to think through every eventuality and prepare as best as possible. “I look this old because it’s such hard work,” quips 41-year-old Taylor.

Rosetta itself was first discussed 25 years ago, and Bibring was there. “You put a lot of yourself into a mission over that length of time,” he says. “As someone once said: failure is not an option. So we won’t fail. This is it. What else can I say?”

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Close encounters

We have seen six comets up close and they all look very different. Among the geographical features are craters, boulders, landslips, cliffs, crevasses and smooth plains. Comet 67P Churyumov-Gerasimenko (left) has them all. When did all these features appear and how have they developed over the eons? Rosetta’s mission is to find out.

For the next year, it will circle the comet, watching how the sun boils away its icy surface, sculpting the landform. Comet 67P completes one of its elliptical orbits of the sun every 6.5 years, so it has been around the block several times. “Rosetta will allow us to separate features that are to do with evolution from features that are primordial,” says Mike A’Hearn at the University of Maryland in College Park.

Topics: Asteroids / Comets / Solar system / Space flight