After a ten year journey, Rosetta and Philae will attempt the first soft landing upon a comet’s surface. (Credits: ESA, Composite, T.Reyes)
In contrast to NASA’s Deep Impact mission which directed a high speed impactor onto the surface of comet Tempel 1, ESA’s Philae lander is designed to execute the first soft landing. The landing must be as gentle as any landing that a respectable bird might accomplish. Philae’s nominal landing speed is about 1.0 meter/sec, that is, 2.2 mph. But like the Deep Impact impactor, Philae is flying solo. Software onboard will function alone without assistance from ground control.
The circumstances surrounding this momentous event – the first landing on a comet – has quite an amazing history and geography. Philae is truly a European Union mission with the design distributed across Europe, spanning from Hungary to Finland to Spain, Ireland to Italy and including UK and Germany.
As is common, the project development spanned several years. A sample return mission was considered the next step after ESA’s Giotto mission that studied Halley’s Comet, but Rosetta evolved out of the cancelled NASA mission Comet Rendezvous Asteroid Flyby (CRAF). ESA could not afford a sample return mission on its own, so Rosetta used the CRAF design but without sample return. Instead it would rendezvous and orbit a comet and include a lander.
Rosetta’s mission began on March 2, 2004 from the Guiana Space Centre in French Guiana and it now flies quietly alongside a comet 400 million kilometers from Earth. 67p is falling towards the Sun and perihelion will be on August 13, 2015.
Escape from Devil’s Island, 14 Km off the coast from the Guiana Space Centre is no longer through the jungles of South America. For Rosetta, it was straight up, then eastward and then finally into a Solar orbit to catch 67P/Churyumov-Gerasimenko. (Photo Credit: ESA)
Illustration of Philae on a cometary surface. The actual surface of 67P/Churyumov-Gerasimenko is actually as dark as a barbecue briquette. (Credit: ESA)
An illustration of the elements of the Philae landing dynamics. (Credit: “Simulation of the Landing of Rosetta Philae on Comet 67P”, M. Hilchenbach, et al., Max Planck Institute)
Illustration and Photo of Philae Pendulum Tests. The force of impact on the wall simulates the force due to descent velocity, comet’s gravity and cold thrusters upon touchdown. (Credit: Simulation of the Landing of Rosetta Philae on Comet 67P, M. Hilchenbach, et al., Max Planck Institute)
The landing mechanisms are: landing legs with ice screws, propulsion system and harpoons. The legs were designed with the intent of landing softly. The harpoons are designed to secure Philae to the surface. The gravity of the comet is so weak, Philae could bounce off the surface or roll over. The purpose of the harpoons – to be fired at the moment of contact — is to prevent bouncing off the surface or tipping over. The direction and strength of gravity at the landing site will not be absolutely known so there is the risk of roll over after landing, albeit very slowly. Tipping over is mitigated by screws under the footpads to penetrate the surface immediately after landing.
The Philae Lander anchoring harpoon with the integrated MUPUS-accelerometer and temperature sensor. (Credit: “Philae Lander Fact Sheet”, ESA)
Clean Room photo of Philae with Principal Investigator Dr. Helmut Rosenbauer, Director at the Max-Planck-Institute for Aeronomy. Philae’s mass is 100 kg including 21 kg of instrument payload It’s dimensions are 1 × 1 × 0.8 meters (3.3 × 3.3 × 2.6 ft) Photo Credit: Max Planck Institute, Filser)
Philae illustration showing the landing feet ice screws and the two harpoons (blue), below the center pedestal (dampener) (Credit: ESA)
Philae has a simple cold gas propulsion system and its purpose is not to slow down the descent, as we often imagine for landers, but rather to push the lander onto the surface. Rosetta will accurately push off Philae at the right time, speed and direction to reach the landing spot.
So imagine if you will that it is the mid-1990s and you are designing a lander. It must accomplish the landing on its own, without help from Earth — except for what is built into the mechanisms and software. Philae’s software operates on a simple computer chip in the Command, Data and Management System (CDMS) jointly developed and tested in Hungary – Institute for Particle and Nuclear Physics, Wigner Research Centre for Physics, Hungarian Academy of Sciences and Germany – the Max Planck Institute. The Hungarian Institute also constructed the Power Subsystem (PSS) which is critical to Philae’s success. The PSS must produce and store power while enduring extremes in temperature and periods of no sunlight.
The computer processing power is about the same as that of a 1990s hand calculator, however, the chips used were radiation hardened to survive space conditions. Philae’s systems will be watching and making navigation corrections throughout the descent. Nothing fancy, this is a simple and straightforward execution with a modest control system on board. Nevertheless, it has everything necessary to accomplish the soft landing on a comet.
When studying the design, I first imagined that Philae would make a long descent and the comet would make a full rotation. But rather, Rosetta will be navigated to somewhere between 2 to 10 km above the comet surface then release Philae. Because of the comet’s odd shape, the probes could be 4 km above the surface at one time and then just 2 km at another, due to the rotation of the comet. The odd rotating shape means that the gravity field effecting the descent will be constantly changing. One might compare the effects of 67P’s gravity on Philae as similar to the motion of a well thrown knuckleball (e.g., Wakefield, Wilhelm). Catchers resort to using a larger catchers mitt and likewise, the landing zone (or ellipse) is 1 square kilometer, sizable considering 67P’s dimensions are 3.5 × 4 km (2.2 × 2.5 miles).
Five candidate landing sites on 67P as viewed from three perspectives. Down selection from 10 to 5 was announced August 25. The final selection is to be announced by September 14th for the landing scheduled on November 11th. (Photo Credit: ESA)
If anyone recalls the lander simulations that one could play on a computer or even a hand calculator, the simulations for Philae are a bit more challenging. Mission planners must have a good estimate of the comet’s gravity field, as strange as it is. They must know the rotation axis and rate of the comet accurately, and also know the relative position of Rosetta and Philae at the beginning of the descent.
The steps for the landing are: 1) release Philae towards the comet, 2) Descent: the comet is rotating and its gravity is weirdly pulling on the little probe during descent. Sounds like fun and one can be certain that mission planners are loving it. The descent that is undertaken is likely to be about 2 hours long. With a rotation period of 12.7 hours, the comet will rotate about 20%. But wait, there’s more. Rosetta is moving too and its orbital motion will be carried by Philae. This motion will offset the comet’s rotation to some degree.
Artist’s illustration of Philae upon touchdown. The lander is capable of landing on up to 30% slopes. (Credits: ESA)
So one can imagine that all the variables and possibilities have been considered by the mission planners. But not so fast. This is Humanity’s first visit to the surface of a comet. The name Rosetta and Philae were chosen because comets are like a Rosetta Stone that is revealing the secrets of our origins – the early formation of the planets. Carl Sagan explained that we are all made of star stuff but more recently, about 4.3 billion years ago, it was comet stuff that may have delivered the building blocks of life and possibly even the water that fills our oceans. We do not know for certain but studying, landing upon, touching and analyzing 67P/Churyumov–Gerasimenko will increase our understanding of the link between comets and the Earth.
The Journey of the Rosetta probe to the comet 67P/Churyumov-Gerasimenko. Image, linked to the ESA animation of the 10 year journey. (Credit: ESA)
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