Spitzer Finds Starburst Galaxies

A major breakthrough in pinpointing some of the most primordial and violently star forming galaxies in the Universe has been made by a joint collaboration of UK and US astronomers using the Spitzer Space Telescope to resolve primordial galaxies initially detected by the James Clerk Maxwell telescope [JCMT]. UK astronomers from the University of Kent, The Royal Observatory Edinburgh and the University of Oxford teamed up with American cosmologists to finally identify these elusive galaxies. The work will be published in the Astrophysical Journal Supplement Spitzer Special Issue in September 2004.

Back in 1995, the UK’s SCUBA camera (Sub-millimetre Common User Bolometer Array) on the James Clerk Maxwell Telescope in Hawaii, which detects light with wavelengths just under a millimetre, began finding fuzzy traces of very distant, primordial galaxies. Some of these are either too distant or too dusty to be seen even by the Hubble Space Telescope. But SCUBA’s images on their own, and those of other similar cameras, are not fine enough: within the fuzzy SCUBA detections are sometimes many galaxies. So astronomers have spent enormous effort following up these SCUBA galaxies on other telescopes, particularly radio telescopes, to answer the question: which one is the primordial galaxy, and which ones are in the foreground? But even with the most sensitive radio telescope images ever made, only around half the SCUBA galaxies can be pinpointed unambiguously. Even worse, the radio telescopes miss all of the most distant and most primordial of SCUBA’s galaxies.

UK and US astronomers teamed up to combine Spitzer’s sharp images with SCUBA’s ability to find primordial galaxies. The team were stunned to find all the SCUBA galaxies in Spitzers field of view detected in only ten minutes with Spitzer. These breakthrough observations, described as a watershed by the team, finally give astronomers a way of unambiguously pinpointing even the most distant of SCUBA’s galaxies. This could only be done by combining SCUBA with the Spitzer Space Telescope: SCUBA shows there is a primordial, violent starburst somewhere in the vicinity, which is then pinpointed by Spitzer.

At the same time, Spitzer solved another mystery about SCUBA galaxies. When Galileo first trained a telescope at the Milky Way, he was astonished to find the fuzzy light resolved into many individual stars. This is, in essence, what the team of astronomers have done with the diffuse extragalactic background light seen from all directions at a wavelength of about half a millimetre. By comparing the distinct Spitzer galaxies with the SCUBA data, the team discovered that they had identified the sources of this cosmic background for the first time. This background is caused by an important population of galaxies: most of the stars in the early Universe are created in these galaxies, and star formation is where everything comes from – including the material that makes planets like our own. Finding where this star formation happens tells us, in a sense, where we came from. Identifying most of these galaxies is a second coup for the joint UK/US team.

Dr. Stephen Serjeant (University of Kent, UK) said, Our Spitzer Space Telescope images picked our galaxies out astonishingly quickly, in only ten minutes, when the community has been pouring effort into detecting them. This really is pioneering work and a great triumph for the Spitzer Space Telescope and the UKs SCUBA camera. To cap it all, at the same time weve found the galaxies that dominate the star formation in the early Universe. The Earth and everything on it is made from the dust created in stars like those people, trees, beef burgers, the lot.

Dr. Rob Ivison (Royal Observatory Edinburgh, UK) said, In 10 minutes, the Spitzer Space Telescope has managed to pinpoint the galaxies we have been chasing for 7 years. We can finally begin to sort the babies and teenagers of the galaxy world from the adults and senior citizens.

Dr. Herv Dole (University of Arizona USA and IAS, Orsay, France) said, These Spitzer observations were designed as the first joint survey using the MIPS and IRAC instruments on Spitzer, to assess the instrument sensitivities. As a matter of fact, it’s a great technological, operational and scientific success, overwhelming our wildest expectations. This demonstrates the amazing capabilities of Spitzer for studying galaxy evolution at high redshifts; no doubt that deeper and larger ongoing surveys will give even more exciting results!

Dr. Steve Willner (Harvard-Smithsonian Center for Astrophysics, USA) said, We expected to detect one or a few of these galaxies, but I was stunned that we detected all of the ones we looked at. The new data finally tell us what these galaxies are all about. We’ve known all along that they had to be far away and rapidly turning all their gas into stars, but now we know their true distances and ages.

Original Source: PPARC News Release

New Frontiers Missions Shortlisted

NASA today announced the selection of two proposals for detailed study as candidates for the next mission in the agency’s New Frontiers Program.

The proposals are missions that would drop robotic landers into a crater at the south pole of the moon and return samples to Earth, and a mission that would orbit Jupiter from pole to pole for the first time to conduct an in-depth study of the giant planet.

“These two outstanding proposals were judged to be the best science value among the seven submitted to NASA in 2004,” said Dr. Ed Weiler, associate administrator for space science at NASA Headquarters, Washington. “It was a very tough decision, but we’re excited at the prospect of the discoveries either of them could make in continuing our mission of exploration of the solar system, and what they could tell us about our place in the universe,” he added.

Each proposal will now receive up to $1.2 million to conduct a seven-month implementation feasibility study focused on cost, management and technical plans, including educational outreach and small business involvement.

Following detailed mission concept studies, due for submission by March 2005, NASA intends to select one of the mission proposals for full development as the second New Frontiers mission by May 2005. The selected New Frontiers science mission must be ready for launch no later than June 30, 2010, within a mission cost cap of $700 million.

The selected full mission investigations, and the Principal Investigators, are:

– “Moonrise: Lunar South Pole-Aitken Basin Sample Return Mission,” Dr. Michael Duke Principal Investigator, Colorado School of Mines, Boulder. This investigation proposes to land two identical landers on the surface near the moon’s south pole and to return over two kilograms (about five pounds) of lunar materials from a region of the moon’s surface believed to harbor materials from the moon’s mantle.

– “Juno,” Dr Scott Bolton, Principal Investigator, NASA’s Jet Propulsion Laboratory, Pasadena, Calif. This investigation proposes to use a highly instrumented spacecraft placed in a polar orbit about the planet Jupiter to investigate the existence of an ice-rock core, determine the global water and ammonia abundances in Jupiter’s atmosphere, study convection and deep wind profiles in the atmosphere, investigate the origin of the jovian magnetic field, and explore the polar magnetosphere.

The two selected proposals were submitted to NASA in February 2004, in response to the New Frontiers Program 2003 and Missions of Opportunity Announcement of Opportunity.

The New Frontiers Program is designed to provide opportunities to conduct several of the medium-class missions identified as the top priority objectives in the Decadal Solar System Exploration Survey, conducted by the Space Studies Board of the National Research Council.

NASA’s New Horizons mission, which will fly by the Pluto-Charon system in 2014 and then target another Kuiper belt object, was designated the first New Frontiers mission.

Original Source: NASA News Release

Hotspot Found on Geminga

Astronomers using ESA?s X-ray observatory XMM-Newton have detected a small, bright ?hot spot? on the surface of the neutron star called Geminga, 500 light-years away. The hot spot is the size of a football field and is caused by the same mechanism producing Geminga?s X-ray tails. This discovery identifies the missing link between the X-ray and gamma-ray emission from Geminga.

Neutron stars are the smallest kind of stars known. They are the super-dense remnants of massive stars that died in cataclysmic explosions called supernovae. They have been thrown through space like cannonballs and set spinning at a furious rate, with magnetic fields hundreds of billions of times stronger than Earth?s.

In the case of Geminga, this cannonball contains one and a half times the mass of the Sun, squeezed into a sphere just 20 kilometres across and spinning four times every second.

A cloud bustling with electrically charged particles surrounds Geminga. These particles are shepherded by its magnetic and electric fields. ESA?s XMM-Newton observatory had already discovered that some of these particles are ejected into space, forming tails that stream behind the neutron star as it hurtles along.

Scientists did not know whether Geminga?s tails are formed by electrons or by their twin particles with an opposite electrical charge, called positrons. Nevertheless, they expected that, if for instance electrons are kicked into space, then the positrons should be funnelled down towards the neutron star itself, like in an ?own goal?. Where these particles strike the surface of the star, they ought to create a hot spot, a region considerably hotter than the surroundings.

An international team of astronomers, lead by Patrizia Caraveo, IASF-CNR, Italy, has now reported the detection of such a hot spot on Geminga using ESA?s XMM-Newton observatory.

With a temperature of about two million degrees, this hot spot is considerably hotter than the one half million degrees of the surrounding surface. According to this new work, Geminga?s hot spot is just 60 metres in radius.

“This hot spot is the size of a football field,” said Caraveo, “and is the smallest object ever detected outside of our Solar System.” Details of this size can presently be measured only on the Moon and Mars and, even then, only from a spacecraft in orbit around them.

The presence of a hot spot was suspected in the late 1990s but only now can we see it ?live?, emitting X-rays as Geminga rotates, thanks to the superior sensitivity of ESA?s X-ray observatory, XMM-Newton.

The team used the European Photon Imaging Cameras (EPIC) to conduct a study of Geminga, lasting about 28 consecutive hours and recording the arrival time and energy of every X-ray photon that Geminga emitted within XMM-Newton?s grasp.

“In total, this amounted to 76 850 X-ray counts ? twice as many as have been collected by all previous observations of Geminga, since the time of the Roman Empire,” said Caraveo.

Knowing the rotation rate of Geminga and the time of each photon?s arrival meant that astronomers could identify which photons were coming from each region of the neutron star as it rotates.

When they compared photons coming from different regions of the star, they found that the ?colour? of the X-rays, which corresponds to their energy, changed as Geminga rotated. In particular, they could clearly see a distinct colour change when the hot spot came into view and then disappeared behind the star.

This research closes the gap between the X-ray and gamma-ray emission from neutron stars. XMM-Newton has shown that they both can originate through the same physical mechanism, namely the acceleration of charged particles in the magnetosphere of these degenerate stars.

“XMM-Newton?s Geminga observation has been particularly fruitful,” said Norbert Schartel, ESA?s Project Scientist for XMM-Newton. “Last year, it yielded the discovery of the source tails and now it has found its rotating hot spot.”

Caraveo is already applying this new technique to other pulsating neutron stars observed by XMM-Newton looking for hot spots. This research represents an important new tool for understanding the physics of neutron stars.

Original Source: ESA News Release

Aura Finally Launches

Aura, a mission dedicated to the health of the Earth’s atmosphere, successfully launched today at 6:01:59 a.m. EDT (3:01:59 a.m. PDT) from Vandenberg Air Force Base, Calif., aboard a Boeing Delta II rocket. Spacecraft separation occurred at 7:06 a.m. EDT (4:06 a.m. PDT), inserting Aura into a 438-mile (705-kilometer) orbit.

NASA’s latest Earth-observing satellite, Aura will help us understand and protect the air we breathe.

“This moment marks a tremendous achievement for the NASA family and our international partners. We look forward to the Aura satellite offering us historic insight into the tough issues of global air quality, ozone recovery and climate change,” said NASA Associate Administrator for Earth Science Dr. Ghassem Asrar. “This mission advances NASA’s exploration of Earth and will also better our understanding of our neighbors in the planetary system. Aura joins its siblings, Terra, Aqua and 10 more research satellites developed and launched by NASA during the past decade, to study our home planet,” he added.

Aura will help answer three key scientific questions: Is the Earth’s protective ozone layer recovering? What are the processes controlling air quality? How is the Earth’s climate changing? NASA expects early scientific data from Aura within 30-90 days.

Aura also will help scientists understand how the composition of the atmosphere affects and responds to Earth’s changing climate. The results from this mission will help scientists better understand the processes that connect local and global air quality.

Each of Aura’s four instruments is designed to survey different aspects of Earth’s atmosphere. Aura will survey the atmosphere from the troposphere, where mankind lives, through the stratosphere, where the ozone layer resides and protects life on Earth.

With the launch of Aura, the first series of NASA’s Earth Observing System satellites is complete. The other satellites are Terra, which monitors land, and Aqua, which observes Earth’s water cycle.

Aura’s four instruments are: the High Resolution Dynamics Limb Sounder (HIRDLS); the Microwave Limb Sounder (MLS); the Ozone Monitoring Instrument (OMI); and the Tropospheric Emission Spectrometer (TES). HIRDLS was built by the United Kingdom and the United States. OMI was built by the Netherlands and Finland in collaboration with NASA. NASA’s Jet Propulsion Laboratory in Pasadena, Calif., constructed TES and MLS. NASA’s Goddard Space Flight Center, Greenbelt, Md., manages the Aura mission.

“Many people have worked very hard to reach this point and the entire team is very excited,” said Aura Project Manager Rick Pickering of Goddard.

NASA’s Earth Science Enterprise is dedicated to understanding the Earth as an integrated system and applying Earth System Science to improve prediction of climate, weather and natural hazards using the unique vantage point of space.

For Aura information and images on the Internet, visit:

http://www.gsfc.nasa.gov/topstory/2004/0517aura.html

and

http://www.nasa.gov/aura

Original Source: NASA News Release

Spirit’s Got a Bad Wheel

As winter approaches on Mars, NASA’s Opportunity rover continues to inch deeper into the stadium-sized crater dubbed “Endurance.” On the other side of the planet, the Spirit rover found an intriguing patch of rock outcrop while preparing to climb up the “Columbia Hills” backward. This unusual approach to driving is part of a creative plan to accommodate Spirit’s aging front wheel.

Spirit, with an odometer reading of over 3.5 kilometers (2.2 miles), has already traveled six times its designed capacity. Its right front wheel has been experiencing increased internal resistance, and recent efforts to mitigate the problem by redistributing the wheel’s lubricant through rest and heating have been only partially successful.

To cope with the condition, rover planners have devised a roundabout strategy. They will drive the rover backward on five wheels, rotating the sixth wheel only sparingly to ensure its availability for demanding terrain. “Driving may take us a little bit longer because it is like dragging an anchor,” said Joe Melko, a rover engineer at NASA’s Jet Propulsion Laboratory, Pasadena, Calif. “However, this approach will allow us to continue doing science much longer than we ever thought possible.”

On Thursday, July 15, Spirit successfully drove 8 meters (26 feet) north along the base of the Columbia Hills backward, dragging its faulty wheel. The wheel was activated about 10 percent of the time to surmount obstacles and to pull the rover out of trenches dug by the immobile wheel.

Along the way, Spirit drove over what scientists had been hoping to find in the hills — a slab of rock outcrop that may represent some of the oldest rocks observed in the mission so far. Spirit will continue to drive north, where it likely will encounter more outcrop. Ultimately, the rover will drive east and hike up the hills backward using all six wheels.

“A few months ago, we weren’t sure if we’d make it to the hills, and now here we are preparing to drive up into them,” said Dr. Matt Golombek, a rover science-team member from JPL. “It’s very exciting.”

For the past month, the Spirit rover has been parked near several hematite-containing rocks, including “Pot of Gold,” conducting science studies and undergoing a long-distance “tuneup” for its right front wheel.

Driving with the wheel disabled means that corrections might have to be made to the rover’s steering if it veers off its planned path. This limits Spirit’s accuracy, but rover planners working at JPL’s rover test facility have come up with some creative commands that allow the rover to auto-correct itself to a limited degree.

As Spirit prepares to climb upward, Opportunity is rolling downward. Probing increasingly deep layers of bedrock lining the walls of Endurance Crater at Meridiani Planum, the rover has observed a puzzling increase in the amount of chlorine. Data from Opportunity’s alpha particle X-ray spectrometer show that chlorine is the only element that dramatically rises with deepening layers, leaving scientists to wonder how it got there. “We do not know yet which element is bound to the chlorine,” said Dr. Jutta Zipfel, a rover science-team member from the Max Planck Institute for Chemistry, Mainz, Germany.

Opportunity will roll down even farther into the crater in the next few days to see if this trend continues. It also will investigate a row of sharp, teeth-like features dubbed “Razorback,” which may have formed when fluid flowed through cracks, depositing hard minerals. Scientists hope the new data will help put together the pieces of Meridiani’s mysterious and watery past. “Razorback may tell us more about the history of water at Endurance Crater,” said Dr. Jack Farmer, a rover science-team member from Arizona State University, Tempe.

Rover planners are also preparing for the coming Martian winter, which peaks in mid-September. Dwindling daily sunshine means the rovers will have less solar power and take longer to recharge. Periods of rest and “deep sleep” will allow the rovers to keep working through the winter at lower activity levels. Orienting the rovers’ solar panels toward the north will also elevate power supplies. “The rovers might work a little bit more every day, or a little bit more every other day. We will see how things go and remain flexible,” said Jim Erickson, project manager for the Mars Exploration Rover mission at JPL.

JPL, a division of the California Institute of Technology in Pasadena, manages the Mars Exploration Rover project for NASA’s Office of Space Science, Washington.

Images and additional information about the project are available on the Internet at http://marsrovers.jpl.nasa.gov and http://athena.cornell.edu

Original Source: NASA/JPL News Release

Saturn’s Two-Faced Moon

The moon with the split personality, Iapetus, presents a puzzling appearance. One hemisphere of the moon is very dark, while the other is very bright. Whether the moon is being coated by foreign material, or being resurfaced by material from within is not yet known.

At 1436 kilometers (892 miles across), Iapetus is about 2.5 times smaller than our own Moon.

The brightness variations in this image are real. The face of Iapetus visible here was observed at a Sun-Iapetus-spacecraft, or phase, angle of about 10 degrees.

The image was taken in visible light with the narrow angle camera on July 3, 2004, from a distance of 3 million kilometers (1.8 million miles) from Iapetus. The image scale is 18 kilometers (11 miles) per pixel. The image was magnified by a factor of two to aid visibility.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA’s Office of Space Science, Washington, D.C. The imaging team is based at the Space Science Institute, Boulder, Colorado.

For more information about the Cassini-Huygens mission, visit http://saturn.jpl.nasa.gov and the Cassini imaging team home page, http://ciclops.org.

Original Source: CICLOPS News Release

Anik F2 Launched on Ariane 5

Telesat, one of the world?s leading satellite operators, announced today the successful launch of the Anik F2 – the world?s largest commercial communications satellite. Telesat?s Anik F2 also makes history as the first satellite to fully commercialize the Ka frequency band ? a breakthrough satellite communications technology for delivering cost-effective, two-way broadband services.

Telesat?s Anik F2 will enable dramatic improvements in access to two-way, high-speed Internet services for consumers and businesses. The satellite will also provide new capacity for a wide range of broadcasting and telecommunications services across North America.

?With Anik F2 we enter a new frontier in satellite communications ? not just for Telesat, but also for the global communications industry,? said Larry Boisvert, Telesat?s president and CEO. ?Once again, Telesat is making advanced communications more accessible for everyone. With Telesat?s Anik F2, North American consumers and businesses will have access to the most advanced broadband services ? anywhere and anytime.?

Anik F2 will be used in innovative ways for both commercial and public services. For example, the Canadian government can use Anik F2 to improve services to remote communities through tele-health, tele-learning and other applications.

Manufactured by Boeing Satellite Systems, Telesat?s Anik F2 was launched on an Ariane 5G rocket from Europe?s Spaceport in Kourou at 9:44 p.m. local time. Arianespace provided mission management. Anik F2 represents Telesat?s fifteenth successful satellite launch.

Telesat?s Anik F2 is equipped with 38 Ka-band transponders, 32 Ku-band transponders and 24 C-band transponders. The spacecraft has a launch mass of 5,950 kg (13,118 lb), a solar array span of 48 metres once deployed in orbit, and spacecraft power of 15 kw at end of life. The satellite, operating in geostationary orbit, will provide commercial services for an estimated 15 years.

Following in-orbit tests this summer and fall, Telesat will take possession of Anik F2 and begin commercial service in the fall.

Original Source: Telsat News Release

Saturn and Jupiter Formed Differently

Nearly five billion years ago, the giant gaseous planets Jupiter and Saturn formed, apparently in radically different ways.

So says a scientist at the University of California’s Los Alamos National Laboratory who created exhaustive computer models based on experiments in which the element hydrogen was shocked to pressures nearly as great as those found inside the two planets.

Working with a French colleague, Didier Saumon of Los Alamos’ Applied Physics Division created models establishing that heavy elements are concentrated in Saturn’s massive core, while those same elements are mixed throughout Jupiter, with very little or no central core at all. The study, published in this week’s Astrophysical Journal, showed that refractory elements such as iron, silicon, carbon, nitrogen and oxygen are concentrated in Saturn’s core, but are diffused in Jupiter, leading to a hypothesis that they were formed through different processes.

Saumon collected data from several recent shock compression experiments that have showed how hydrogen behaves at pressures a million times greater than atmospheric pressure, approaching those present in the gas giants. These experiments – performed over the past several years at U.S. national labs and in Russia – have for the first time permitted accurate measurements of the so-called equation of state of simple fluids, such as hydrogen, within the high-pressure and high-density realm where ionization occurs for deuterium, the isotope made of a hydrogen atom with an additional neutron.

Working with T. Guillot of the Observatoire de la Cote d’Azur, France, Saumon developed about 50,000 different models of the internal structures of the two giant gaseous planets that included every possible variation permitted by astrophysical observations and laboratory experiments.

“Some data from earlier planetary probes gave us indirect information about what takes place inside Saturn and Jupiter, and now we’re hoping to learn more from the Cassini mission that just arrived in Saturn’s orbit,” Saumon said. “We selected only the computer models that fit the planetary observations.”

Jupiter, Saturn and the other giant planets are made up of gases, like the sun: They are about 70 percent hydrogen by mass, with the rest mostly helium and small amounts of heavier elements. Therefore, their interior structures were hard to calculate because hydrogen’s equation of state at high pressures wasn’t well understood.

Saumon and Guillot constrained their computer models with data from the deuterium experiments, thereby reducing previous uncertainties for the equation of state of hydrogen, which is the central ingredient needed to improve models of the structures of the planets and how they formed.

“We tried to include every possible variation that might be allowed by the experimental data on shock compression of deuterium,” Saumon explained.

By estimating the total amount of the heavy elements and their distribution inside Jupiter and Saturn, the models provide a better picture of how the planets formed through the accretion of hydrogen, helium and solid elements from the nebula that swirled around the sun billions of years ago.

“There’s been general agreement that the cores of Saturn and Jupiter are different,” Saumon said. “What’s new here is how exhaustive these models are. We’ve managed to eliminate or quantify many of the uncertainties, so we have much better confidence in the range within which the actual data will fall for hydrogen, and therefore for the refractory metals and other elements.

“Although we can’t say our models are precise, we know quite well how imprecise they are,” he added.

These results from the models will help guide measurements to be taken by Cassini and future proposed interplanetary space probes to Jupiter.

Los Alamos National Laboratory is operated by the University of California for the National Nuclear Security Administration (NNSA) of the U.S. Department of Energy and works in partnership with NNSA’s Sandia and Lawrence Livermore national laboratories to support NNSA in its mission.

Los Alamos develops and applies science and technology to ensure the safety and reliability of the U.S. nuclear deterrent; reduce the threat of weapons of mass destruction, proliferation and terrorism; and solve national problems in defense, energy, environment and infrastructure.

Original Source: Los Alamos News Release

New Plan to Move an Asteroid

On 9 July 2004, the Near-Earth Object Mission Advisory Panel recommended that ESA place a high priority on developing a mission to actually move an asteroid. The conclusion was based on the panel?s consideration of six near-Earth object mission studies submitted to the Agency in February 2003.

Of the six studies, three were space-based observatories for detecting NEOs and three were rendezvous missions. All addressed the growing realisation of the threat posed by Near-Earth Objects (NEOs) and proposed ways of detecting NEOs or discovering more about them from a close distance.

A panel of six experts, known as the Near-Earth Object Mission Advisory Panel (NEOMAP) assessed the proposals. Alan Harris, German Aerospace Centre (DLR), Berlin, and Chairman of NEOMAP, says, ?The task has been very difficult because the goalposts have changed. When the studies were commissioned, the discovery business was in no way as advanced as it is now. Today, a number of organisations are building large telescopes on Earth that promise to find a very large percentage of the NEO population at even smaller sizes than visible today.?

As a result, the panel decided that ESA should leave detection to ground-based telescopes for the time being, until the share of the remaining population not visible from the ground becomes better known. The need for a space-based observatory will then be re-assessed. The panel placed its highest priority on rendezvous missions, and in particular, the Don Quijote mission concept. ?If you think about the chain of events between detecting a hazardous object and doing something about it, there is one area in which we have no experience at all and that is in directly interacting with an asteroid, trying to alter its orbit,? explains Harris.

The Don Quijote mission concept will do this by using two spacecraft, Sancho and Hidalgo. Both are launched at the same time but Sancho takes a faster route. When it arrives at the target asteroid it will begin a seven-month campaign of observation and physical characterisation during which it will land penetrators and seismometers on the asteroid?s surface to understand its internal structure.

Sancho will then watch as Hidalgo arrives and smashes into the asteroid at very high speed. This will provide information about the behaviour of the internal structure of the asteroid during an impact event as well as excavating some of the interior for Sancho to observe. After the impact, Sancho and telescopes from Earth will monitor the asteroid to see how its orbit and rotation have been affected.

Harris says, ?When we do actually find a hazardous asteroid, you could imagine a Don Quijote-type mission as a precursor to a mitigation mission. It will tell us how the target responds to an impact and will help us to develop a much more effective mitigation mission.?

On 9 July, the findings were presented to the scientific and industrial community. Representatives of other national space agencies were also invited in the hope that they will be interested in developing a joint mission, based around this concept.

Andr?s Galvez, ESA?s Advanced Concepts Team and technical officer for the NEOMAP report says, ?This report gives us a solid foundation to define programmatic priorities and an implementation strategy, in which I also hope we are joined by international partners?.

With international cooperation, a mission could be launched as early as 2010-2015.

The six mission concepts studied were:

* Earthguard-1 ? a small space telescope for NEO discovery, especially the Atens and ?inner-Earth objects? (IEOs) that are difficult to detect from the ground.
* European Near-Earth Object Survey (EUNEOS) ? a space telescope for NEO discovery
* NEO Remote Observations (NERO) ? an optical/infrared space telescope for NEO discovery and physical characterisation.
* Smallsat Intercept Missions to Objects Near Earth (SIMONE) ? a flotilla of low-cost microsatellites for near-Earth asteroid rendezvous and in-situ remote sensing
* Internal Structure High-resolution Tomography by Asteroid Rendezvous (ISHTAR) ? uses radar tomography for an in-situ study of internal structure
* Don Quijote ? uses explosive charges, an impactor, seismic detectors and accelerometers for an in-situ study of internal structure and momentum transfer

Original Source: ESA News Release

Two Ecosystems in Antarctica’s Vostok?

Scientists from the Lamont-Doherty Earth Observatory (LDEO) at Columbia University and Rensselaer Polytechnic Institute in New York State have developed the first-ever map of water depth in Lake Vostok, which lies between 3,700 and 4,300 meters (more than 2 miles) below the continental Antarctic ice sheet. The new comprehensive measurements of the lake?roughly the size of North America’s Lake Ontario?indicate it is divided into two distinct basins that may have different water chemistry and other characteristics. The findings have important implications for the diversity of microbial life in Lake Vostok and provide a strategy for how scientists study the lake?s different ecosystems should international scientific consensus approve exploration of the pristine and ancient environment.

Michael Studinger, of the Lamont-Doherty Earth Observatory (LDEO) at Columbia University, said that the existence of two distinct regions with the lake would have significant implications for what sorts of ecosystems scientists should expect to find in the lake and how they should go about exploring them.

“The ridge between the two basins will limit water exchange between the two systems,” he said. “Consequently, the chemical and biological composition of these two ecosystems is likely to be different.”

The National Science Foundation (NSF), an independent federal agency that supports fundamental research and education across all fields of science and engineering, supported the work. NSF manages the U.S. Antarctic Program, which coordinates almost all U.S. science on the southernmost continent.

The new measurements are significant because they provide a comprehensive picture of the entire lakebed and indicate that the bottom of the lake contains a previously unknown, northern sub-basin separated from the southern lakebed by a prominent ridge.

Using laser altimeter, ice-penetrating radar and gravity measurements collected by aircraft, Studinger and Robin Bell, of LDEO, and Anahita Tikku, formerly of the University of Tokyo and now at Rensselaer Polytechnic Institute, estimate that Lake Vostok contains roughly 5400 cubic kilometers (1300 cubic miles) of water. Their measurements also indicate that the top of the ridge dividing the two basins is only 200 meters (650 feet) below the bottom of the icesheet. Elsewhere, the water ranges from roughly 400 meters (1,300 feet) deep in the northern basin to 800 meters (2,600 feet) deep in its southern counterpart.

Water that passes through the lake starts on one end as melted ice from the very bottom of the ice sheet, which refreezes at the other end. According to the new measurements, the base of the ice sheet melts predominantly over the smaller northern basin, while the water in the lake refreezes over the larger southern basin. The researchers assert that water takes between 55,000 and 110,000 years to cycle through the lake.

The arrangement of the two basins, their separation and the characteristics of the meltwater may, the scientists conclude, all have implications for the circulation of water within the lake. It is possible, for example, that if the water in the lake were fresh, meltwater in the northern basin would sink to the bottom of that basin, limiting the exchange of waters between the two basins. The meltwater in the adjacent basin likely would be different.

The two lake basins, they argue, could therefore have very different bottoms.

The scientists also point out that the waters of the two basins may, as a result of the separation, have a very different chemical and even biological composition. Indeed, Lake Vostok, is also of interest to those who search for microbial life elsewhere in the solar system. The lake is thought to be a very good terrestrial analog of the conditions on Europa, a frozen moon of Jupiter. If life can exist in Vostok, scientists have argued, then microbes also might thrive on Europa.

The new measurements also indicate that different strategies may be needed to target sampling of specific types of lake sediments. Those released from the ice sheet represent the rocks over which the ice traveled, for example, and would be more prominent in the northern basin. Material in the southern basin would be more likely to represent the environmental conditions before the ice sheet sealed off the lake.

Scientists deciding whether and how to proceed with an exploration of Lake Vostok say a great deal of technological development would likely be needed before a device could be deployed to conduct contamination-free sampling. Currently, no scientific sampling of the lake is being carried out.

The ultimate goal of any sampling would be to obtain water and sediment samples from the lake bottom.

The team published the new maps in the June 19 edition of Geophysical Research Letters, a publication of the American Geophysical Union.

Original Source: NSF News Release