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News • Mission Update Space Shorts India’s off to the Moon Chandrayaan-1, India’s first Moon mission, was launched successfully from the Satish Dhawan Space Centre (SHAR) in Sriharikota, off India’s Andhra Pradesh coast, on the morning of 22 October. It since moved into increasingly elliptical orbits around Earth, while its performance is monitored, and then set off on its way to the Moon. Once there, it will take up a polar lunar orbit at 100 km altitude, before releasing the Moon Impact Probe. http://www.chandrayaan-i.com/ Hang on Hubble The Hubble servicing mission will be delayed again because a replacement data handling unit will not be ready in time for the proposed February launch date. The unit, known as the Science Instrument Command and Data Handling system, failed in September. Its replacement has been stored at the Goddard Space Flight Center since 1991, as a back-up, but needs more testing than is possible to be ready for February. The other equipment to be sent to the HST on this servicing mission, such as the Wide Field Camera 3, and the Cosmic Origins Spectrograph, will remain packaged ready to go, with some attention to batteries and lubrication. http://hubble.nasa.gov Delay for GOCE ESA’s GOCE satellite (Gravity field and steady-state Ocean Circulation Explorer) has had its launch delayed until at least February 2009 because of a fault in the Russian Rockot launcher. An anomaly in the guidance system requires hardware changes that will take at least two months to implement. When in orbit, GOCE will map Earth’s gravity field in detail for around 20 months, producing a much improved model of the geoid, useful for solid Earth and ocean science, as well as for mapping sea-level change and for precision surveying. It is an innovative mission in many ways, not least in that it employs gradiometry – measurements from ultrasensitive accelerometers – to measure the variations in the gravitational field as the spacecraft orbits the Earth at just 250 km altitude. http://www.esa.int/esaLP/LPgoce.html 6.8 Mission update 1: Mercury has given up more of its secrets to Messenger in the recent flyby, but there remains 5% of the surface that hasn’t been observed by either Messenger or Mariner 10. So far, Mercury is proving remarkably different from the other terrestrial planets (NASA/Johns Hopkins University Applied Physics Laboratory/ Carnegie Institution of Washington) Messenger revisits Mercury The NASA spacecraft Messenger has taken the opportunity of a second swing past Mercury in preparation for going into orbit around the planet to explore more of the previously unseen surface in its western hemisphere (figure 1). Messenger’s camera, laser altimeter, magnetometer and spectrometer were collecting data during the flyby, adding to the haul from the previous fly-past and from Mariner 10. The images and topography from both of Messenger’s close encounters overlapped so that mission scientists now have a much better correlation between surface appearance and shape, which will aid future geological interpretation of surface data. And the magnetometry showed that Mercury’s magnetic field so far measured is symmetrical in eastern and western hemispheres. The Mercury Atmospheric and Surface Composition Spectrometer observed Mercury’s exosphere – its thin atmosphere – looking for sodium, calcium, magnesium and hydrogen atoms. First results suggest that sodium, calcium and magnesium – an element detected around Mercury for the first time by Messenger – have different spatial distributions around the planet, hinting at varied processes perhaps in the interaction between surface and exosphere. Now that researchers have seen 95% of Mercury’s surface (combining Messenger’s data on 80% of the surface with that of Mariner 10) it is clear that the planet is very different from the Moon and Mars. Mercury’s surface is typically homogeneously ancient and heavily cratered. charging within a few hours, without any loss of capability. The problem may have arisen because it was colder than usual at the landing site, meaning that the battery heaters were used, drawing more power at a time when dust storms and ice on the atmosphere were decreasing the solar power available. Phoenix was to sit tight and build up power supplies before attempting any more science tasks. http://www.nasa.gov/phoenix Magnetic traces Phoenix lander in meteorites plays it safe Traces of magnetic fields in some http:// www.nasa.gov/messenger NASA’s Mars lander Phoenix went into safe mode for a short time at the end of October, thought to be a response to low power resulting from low surface temperatures and decreased sunlight around the north pole. In this state, the lander stops any activities not considered critical; in this case Phoenix also switched off one of its batteries and changed to a redundant set of electronics. Mission engineers were able to contact the lander and restart battery ancient meteorites suggest that planetesimals formed in the early stages of the life of the solar system may have been big enough to have melted, differentiated and formed magnetic dynamos. Some of the angrites, a class of iron meteorites formed early in the evolution of the solar system, show signs that their parent bodies had magnetic fields around 20–40% as strong as Earth’s field today. These samples formed in the first 3 million years of the solar system’s lifetime, suggesting not only that the A&G • December 2008 • Vol. 49 News • Mission Update Hubble gets back to business Space Shorts Armstrong archived The astronaut Neil Armstrong has given his personal papers to the university where he gained his degree in aeronautical engineering, where they will be kept as a record of his career. Purdue University, West Lafayette, Indiana, USA, will keep the archive, together with 55 hours of interviews prepared for a biography of Armstrong, as a resource for scholars. It is seeking comparable information from other people involved in the spaceflight programme, in order to build a comprehensive collection. Purdue also holds the George Palmer Putnam Collection of Amelia Earhart Papers, and the papers of Ralph Johnson, who was the first person to document aircraft landing procedures that are still used today. School payload This image of the interacting galaxy pair Arp 147 was taken by the Wide Field Planetary Camera 2 after the Hubble Space Telescope came back online after an equipment failure in September this year. The fault was managed by transferring processing tasks to a part of the HST unused and untested since its launch in 1990. This image is testament to the success of the process, taken a couple of days after the reboot. It is a composite of three colour images – blue, green and red indicating blue, visible light and infrared radiation respectively – and demonstrates that the camera is working as it was before the fault became apparent. This pair of galaxies were listed by Halton Arp in his Catalogue of Peculiar Galaxies, published in 1966. The galaxy on the left, aligned roughly edge-on, has passed through the galaxy on the right, leaving behind a blue ring of intense star formation, triggered by the galaxy “impact”. The dusty reddish knot at the lower left of the blue ring probably marks the location of the original nucleus of the galaxy that was hit. (NASA, ESA, M Livio [STScI]) A satellite currently being built by Surrey Satellite Technology Ltd has gained an extra experiment, thanks to a school competition sponsored by the British National Space Centre. The challenge was to design an instrument to fit in a lunchbox-sized space, weighing no more than a kilogram and using less than 1 W of power. Shrewsbury School won with an ionospheric experiment called POISE, which should fly in 2010. http://www.bnsc.gov.uk relatively small bodies existing then had melted and differentiated enough to produce a dynamo effect, but that they did so very quickly. It may be that these short-lived planetary dynamos were widespread among the planetesimals of the early solar system, which has implications for the processes of collision and assimilation considered important in the development of the planetary system we know today. The results were published in Science, 31 October. COROT catches shaking stars COROT, a joint mission of the French Space Agency (CNS) and the European Space Agency, has directly observed “stellar seismology” data from three stars similar to the Sun, for the first time. Detecting fluctuations in brightness that arise from these internal oscillations is tricky, made easier by space-based observation, which is A&G • December 2008 • Vol. 49 not interrupted by the rotation of the Earth nor by weather. The patterns of oscillation of the sound waves within a star reveals information about its internal structure and the transfer of energy from the interior to the surface. And information from several stars like the Sun will also aid understanding of the Sun itself. The three stars probed by COROT – HD49933, HD181420 and HD181906 – are similar to the Sun, but far enough away for their light not to blind COROT’s instruments. The research was published in Nature by lead author E Michel. http://www.esa.int SST spies twin solar system The Spitzer Space Telescope has found a pair of rocky asteroid belts in a nearby planetary system, with the inner one almost the same as the asteroid belt in our solar system, plus an outer icy belt. The implication is that planets between these belts are confining and shaping them, as happens around the Sun. e Eridani is a slightly smaller and cooler star than the Sun, just 10.5 light-years away. It is considered a close analogue of our solar system when young, at the time when life was beginning on Earth. Our asteroid belt has around 5% of the mass of Earth’s Moon in it, and orbits at 3 AU; e Eridani has an identical belt at the same distance, plus one at around 20 AU, roughly where Uranus is in our system. And the icy outer belt corresponds to the Edgeworth–Kuiper belt, but in a state before much of the material was swept further into the solar system in the Late Heavy Bombardment. The gaps between the rings strongly suggest that there are planets there – and three planets with masses between those of Neptune and Jupiter would fit the observations nicely. This work will be published in the 10 January issue of the Astrophysical Journal. CESAR rules rovers An ESA contest to find the best rover to venture into a lunar crater has been won by a Bremen University team with their rover CESAR. ESA set the first Lunar Robotics Challenge within Tenerife’s Teide National Park, a bleak pumice landscape comparable to the Moon. Rovers had to descend into and escape from a 15 m crater with 40% slopes, and pick out soil from a specific location, in the dark. The challenge also covered control of the rovers and tested other potential technology for ESA’s space programme. Heavy rain and clouds provided a distinctly terrestrial tinge to the challenge, and all the competing teams learnt from the experience, which ESA hopes to repeat. The University of Surrey’s SELENE was unable to join in because of mechanical failure. http://www.esa.int http://www.cfa.harvard.edu 6.9