Philae landing preview: What to expect on landing day
The timeline is up-to-date as of November 12 at 07:30 UTC.
Ten years. That's how long it took Rosetta to get from Earth to comet 67P/Churyumov-Gerasimenko from its launch on March 2, 2004, to the beginning of its first orbit on August 6, 2014. For the Philae lander, bolted to the side of Rosetta, the journey has been slightly longer, and it's not quite over yet.
Philae has warmed up its science instruments and has even taken a couple of amazing photos of the comet with Rosetta's solar panel in the foreground, but the lander doesn't really begin to get to work until November 12 at 8:35 UT, when it will finally separate from the orbiter. Seven hours later, it will arrive at the surface of the comet. Hopefully, Philae will survive the landing, and begin to return data.
All next week, I'll be in Darmstadt, Germany, at the European Space Operations Centre (ESOC), to witness the historic attempt at landing on a comet. I'm not going to lie to you: I'm going to be terrified about Philae's survival until I see ESA engineers leaping from their seats and cheering. To be clear, I have no specific doubts about the spacecraft or its designers. It's just that we have never landed on anything like a comet before. We don't really know what the surface of a comet is like -- is it a hard, crusty shell of rocky material? A diaphanously fluffy, almost cloud-like layer of highly porous dust? Gravelly? Crunchy? Crystalline? Powdery? Sandpapery? Slippery? Who knows? The last time we landed on a surface that we knew so little about was when ESA landed Huygens on Titan in 2004. But Huygens did almost all of its science on the way down, returning all its data to the Cassini orbiter in real time, so it didn't matter whether Huygens survived its arrival on Titan's surface. In contrast, almost all of Philae's science will not come until after a successful landing. It's going to be terrifying. But I wouldn't miss it for the world.
What will we know, when? Below is a timeline of Philae events, and a brief summary of what Philae intends to do. Media-related events are highlighted yellow; mission control events in orange; and the major separation and landing events in red, most of it taken from this timeline released November 7 by ESA (PDF).
A note on timing. Events are shown in both spacecraft event time (SCET) -- the time on the spacecraft's clock, which will correspond to timestamps on images and data -- and in Earth time (Universal, Central European, and Pacific time zones). On the day of landing, the comet will be about 510 million kilometers from Earth, so one-way light time between the spacecraft and Earth is just shy of half an hour (28 minutes 20 seconds, to be exact). For events that will take place aboard spacecraft, like rocket maneuvers, I take spacecraft time from the ESA published timeline and add one-way light time to get Earth time, because that is the time on Earth that we should hear that those events happen. The first version of this timeline is almost certain to contain some errors; I will update this post to correct those and add more information as I find it. The graphical timeline below, which came from ESA, is actually a mix of spacecraft and Earth event times, confusingly. Other sources of timeline information include the ESA TV website and the ESA invitation to media.
Graphical timeline of the Philae landing
Rosetta moves from lower right to upper left in this diagram. T0 -- the time of separation -- is November 12 at 08:35 UT, according to the spacecraft's clock. "GONOGO" points along the timeline indicate places where the spacecraft waits for permission to proceed from Earth before performing irreversible actions like separating the lander. With a half-hour one-way light time between Rosetta and Earth, it takes at least an hour for Rosetta to send telemetry to Earth and then receive an instruction in response to that telemetry.
Philae's instruments: A brief guide
Science instruments come in two types: remote sensing (which detect things from a distance) and in-situ (which must be in contact with what they measure). Philae can use its remote sensing instruments during descent, but the in-situ instruments don't get to operate until after landing.
Remote sensing instruments include the CIVA and ROLIS imagers and CONSERT radar sounder. CIVA's 6 cameras can produce panoramic images of the comet's surface; the side-looking ones have produced Rosetta's iconic self-portraits. ROLIS is intended to provide context images for in-situ measurements; it will take photos during descent. CONSERT has components on both orbiter and lander; it transmits radio waves from orbiter to the lander, sometimes through the comet itself.
Because magnetic fields and plasma exist in the space around a comet, not just on the surface, one in-situ instrument will be able to operate during descent: the Rosetta Lander Magnetometer and Plasma Monitor (ROMAP). ROMAP studies the magnetic field and interaction between comet and solar wind.
In-situ instruments include the Alpha Particle X-Ray Spectrometer (APXS), the Cometary Sampling and Composition Experiment (COSAC), Multi-Purpose Sensors for Surface and Subsurface Science (MUPUS), Ptolemy, and the Surface Electrical Sounding and Acoustic Monitoring Experiments (SESAME), which will only be used after landing. APXS measures elemental composition. COSAC and Ptolemy are evolved-gas analyzers, which can determine molecular and isotopic composition from samples delivered to it by Philae's drill and sampling mechanism (SD2). MUPUS and SESAME are suites of sensors that will measure the physical properties of the comet's surface.
ESA / ATG medialab
Philae has 10 instruments: APXS: Alpha Particle X-ray Spectrometer, for studying elemental composition CIVA: Comet Nucleus Infrared and Visible Analyser, six black-and-white cameras for panoramic imaging CONSERT: COmet Nucleus Sounding Experiment by Radiowave Transmission, for studying comet interior COSAC: The COmetary SAmpling and Composition, an evolved gas analyzer for identifying organic molecules Ptolemy: an evolved gas analyzer for measuring isotopes of light elements MUPUS: MUlti-PUrpose Sensors for Surface and Sub-Surface Science, for studying comet physical properties ROLIS: Rosetta Lander Imaging System, will provide context images of landing site ROMAP: Rosetta Lander Magnetometer and Plasma Monitor, for studying the magnetic field and plasma environment of the comet SD2: Sampling, drilling and distribution subsystem, can drill to 23 centimeters depth SESAME: Surface Electric Sounding and Acoustic Monitoring Experiment, for studying comet physical properties
Setting Up for Landing
Philae will land at a site named "Agilkia" for an island in the Nile river in a public contest. Agilkia is on the smaller of the comet's two lobes, though not on the end; hopefully CONSERT will be able to see completely through the small lobe when Rosetta is in the right position.
ESA / Rosetta / NavCam / MPS for OSIRIS Team MPS / UPD / LAM / IAA / SSO / INTA / UPM / DASP / IDA
Philae's selected landing site: "Agilkia"
Rosetta NavCam and OSIRIS views of the selected primary landing site for Philae. The Navcam image of the whole comet was taken on August 16, 2014 from a distance of 100 kilometers; the comet is about 4 kilometers across. The OSIRIS image was taken on August 20, 2014 from a distance of 67 kilometers. The "+" marks the center of the landing site; the square is about 1 kilometer on a side. The site was named "Agilkia" in a public contest.
To deliver Philae to Agilkia, Rosetta fires rockets to put it on a collision course with the comet. Back on Earth, mission controllers will check that the maneuver was successful and on target before delivering the "go for separation" command. With a half-hour one-way light time between Rosetta and Earth, this cycle will take an hour to complete. Two hours after the pre-delivery maneuver, Rosetta will release Philae. Forty minutes after that, Rosetta will perform a divert maneuver, allowing it to continue onward to a relay orbit around the comet, from which Rosetta can receive Philae transmissions and perform the CONSERT experiment.
On November 12 at about 6:35 UT, Rosetta will place itself on a collision course with comet Churyumov-Gerasimenko. Two hours later, the Philae lander will separate. Another 40 minutes after that, the orbiter will perform a divert maneuver to put it into a relay orbit. Landing is expected to happen at about 15:35 UT, with confirmation received on Earth about 30 minutes later. (Clip from this longer YouTube video)
Separation, Descent, and Landing
Separation, Descent, and Landing (SDL) events are described in detail on the Rosetta blog.
The lander will be pushed from the orbiter at a commanded, precise speed. If the commanded deploy does not succeed, a backup spring can push the lander off at a speed of 18 centimeters per second. CIVA will take a "farewell" image of the orbiter, which should be returned during the descent. Hopefully Rosetta's NavCam will capture the return image, of Philae departing.
It will take Philae 7 hours to free-fall the 22.5 kilometers to Churyumov-Gerasimenko's surface. Within an hour of separation, Philae will establish radio contact with Rosetta, unfold its three-legged landing gear, deploy the CONSERT radio antenna, deploy the boom holding the ROLIS camera, and begin taking photos with ROLIS.
Forty minutes after separation, Rosetta will perform a divert maneuver. Two hours after separation, Rosetta will turn to watch Philae drift toward the comet.
Throughout its descent, Philae will be actively gathering data. ROLIS will shoot descent images. COSAC, Ptolemy, and SESAME will attempt to sample gas and dust around the comet. ROMAP and SESAME will measure magnetic fields and plasma. CONSERT will measure the separation between lander and orbiter, and also try to actively sense the surface of the comet.
A little of the descent data will be transmitted to Rosetta during the descent, so regardless of what happens to Philae when it contacts the comet, there will be some science returned. Descent data may include the CIVA farewell image and CONSERT data on the range from orbiter to lander with respect to time, among other information. (Ref)
Philae's legs are designed to damp out the forces of a hard landing to reduce the lander's chance of bouncing. When Philae touches down, it will fire two harpoons to attach it firmly to the comet's surface. A thruster on top of the lander fires at the same time as the harpoons, keeping the lander on the ground. Ice screws also deploy from the three lander feet.
Upon landing, the first science activities will be CIVA panoramic imaging, MUPUS acceleration measurements, and SESAME elastic properties measurements. The descent data and these first images will be returned as soon as possible so that mission engineers can determine the orientation of the lander, and then command it to rotate it to best illuminate its solar panels and optimize the positions of the lander instruments. Mission engineers will also use these early data to calculate tables describing when the orbiter will be visible from the lander (for communication) and when the ground will be illuminated. (Ref)
If the comet turns out to be very soft (with a compressive strength less than 2 kPa, similar to lightly compacted snow), the lander could sink in up to its baseplate, which would prevent it from rotating. The lander would only sink farther if the compressive strength were less than 100 Pa (similar to powder snow). (Ref 1, ref 2)
The first science sequence lasts five days and can be performed entirely under battery power; with solar power, the lander could survive and continue doing science for much longer. For more post-landing plans, read the Rosetta blog.
Visualisation of the deployment of the Philae lander from Rosetta at comet 67P/Churyumov-Gerasimenko in November 2014. Rosetta will come to within 2.5 km of the comet’s surface to deploy Philae, which will then take around 2 hours to reach the surface.
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