Posted on by Fraser Cain

Spacedev Puts a Satellite Up for Sale on eBay

Image credit: SpaceDev

Satellite manufacturer SpaceDev announced today that it has put a satellite up for sale on the Internet auction site eBay. The high bidder will win a spacecraft built by SpaceDev, or an interested party can just “Buy it Now” for $9.5 million USD. The auction begins on Monday, November 10 and ends 10 days later. The default satellite will come with an Earth observation camera, but the winning bidder can supply additional payloads, name the satellite, and attend the launch.

SpaceDev (OTCBB: SPDV) is auctioning a world exclusive private space mission on eBay. This first of its kind eBay auction is being listed for the ten-day period of 8:00 PM (PST) Monday, November 10, through 8:00 PM (PST) Thursday, November 20th.

The SpaceDev space mission auction is at:

http://cgi.ebay.com/ws/eBayISAPI.dll?ViewItem&item=2572382454&category=45046&rd=1

Most earth orbiting small satellite missions can cost $25 million or more, not including the launch. To demonstrate the affordability of private space missions, SpaceDev has posted a ?Buy it Now? price of $9.5 million. The high bidder will win a spacecraft based on SpaceDev?s Maneuvering and orbit Transfer Vehicle (MTV?).

?I founded SpaceDev to accelerate the development of space, to get the public involved in space and to have fun,? said Jim Benson, SpaceDev founder and CEO. ?With our successful launch and operation of CHIPSat earlier this year, and after being competitively selected to provide safe hybrid rocket propulsion for manned space flight, we are offering this unique space mission to the public.?

The high bidder has the right to supply his or her own payload, to name the SpaceDev MTV? satellite and to name the mission. The winning bidder, which could be an individual, company or government agency, can also be involved in the mission design, satellite assembly and testing (including putting small personal items on the spacecraft), can attend the launch, and can participate in on-orbit operations.

The nominal payload is a camera that provides a view of the launch separation on-orbit, a buyer-controlled camera on the spacecraft looking back down on earth and into space 24 hours a day, or the buyer can supply a SpaceDev-approved payload. The microsatellite camera can be operated over the Internet by the winning bidder, similar to SpaceDev?s CHIPSat microsat, which is the world?s first orbiting node on the Internet. Specific terms are included in the eBay auction listing. Search eBay for ?SpaceDev.?

Original Source: SpaceDev News Release

Posted on by Fraser Cain

Gamma Ray Map of the Milky Way

Image credit: ESA

The European Space Agency’s Integral gamma-ray observatory has produced a new map of the Milky Way in the gamma-ray spectrum. Integral is looking for traces of radioactive aluminum, which gives off gamma rays with a specific wavelength. But the question is, what’s producing all this aluminum? Some astronomers believe these could be created by specific objects in the Milky Way, like Red Giant stars or hot blue stars. Another possibility is that it’s produced as part of supernova explosions. Integral will help get to the bottom of this mystery.

ESA’s gamma-ray observatory Integral is making excellent progress, mapping the Galaxy at key gamma-ray wavelengths.

It is now poised to give astronomers their truest picture yet of recent changes in the Milky Way’s chemical composition. At the same time, it has confirmed an ‘antimatter’ mystery at the centre of the Galaxy.

Since its formation from a cloud of hydrogen and helium gas, around 12 000 million years ago, the Milky Way has gradually been enriched with heavier chemical elements. This has allowed planets and, indeed, life on Earth to form.

Today, one of those heavier elements – radioactive aluminium – is spread throughout the Galaxy and, as it decays into magnesium, gives out gamma rays with a wavelength known as the ‘1809 keV line.’ Integral has been mapping this emission with the aim of understanding exactly what is producing all this aluminium.

In particular, Integral is looking at the aluminium ‘hot spots’ that dot the Galaxy to determine whether these are caused by individual celestial objects or the chance alignment of many objects.

Astronomers believe that the most likely sources of the aluminium are supernovae (exploding high-mass stars) and, since the decay time of the aluminium is around one million years, Integral’s map shows how many stars have died in recent celestial history. Other possible sources of the aluminium include ‘red giant’ stars or hot blue stars that give out the element naturally.

To decide between these options, Integral is also mapping radioactive iron, which is only produced in supernovae. Theories suggest that, during a supernova blast, aluminium and iron should be produced together in the same region of the exploding star. Thus, if the iron’s distribution coincides with that of the aluminium, it will prove that the overwhelming majority of aluminium comes indeed from supernovae.

These measurements are difficult and have not been possible so far, since the gamma-ray signature of radioactive iron is about six times fainter than that of the aluminium. However, as ESA’s powerful Integral observatory accumulates more data in the course of the next year, it will finally be possible to reveal the signature of radioactive iron. This test will tell astronomers whether their theories of how elements form are correct.

In addition to these maps, Integral is also looking deeply into the centre of the Galaxy, to make the most detailed map ever of ‘antimatter’ there.

Antimatter is like a mirror image to normal matter and is produced during extremely energetic atomic processes: for example, the radioactive decay of aluminium. Its signature is known as the ‘511 keV line.’ Even though Integral’s observations are not yet complete, they show that there is too much antimatter in the centre of the Galaxy to be coming from aluminium decay alone. They also show clearly that there must be many sources of antimatter because it is not concentrated around a single point.

There are many possible sources for this antimatter. As well as supernovae, old red stars and hot blue stars, there are jets from neutron stars and black holes, stellar flares, gamma-ray bursts and interaction between cosmic rays and the dusty gas clouds of interstellar space.

Chris Winkler, Integral’s Project Scientist, says: “We have collected excellent data in the first few months of activity but we can and will do much more in the next year. Integral’s accuracy and sensitivity have already exceeded our expectations and, in the months to come, we could get the answers to some of astronomy’s most intriguing questions.”

Original Source: ESA News Release

Posted on by Fraser Cain

No Newsletter for a Couple of Days

I just wanted to warn you that I’m probably not going to be able to email out the newsletter for the next couple of days. My high-speed Internet connection is down until Wednesday at the earliest, so all I’ve got is dial-up. I can update the website, but I can’t send out the newsletter without a high-speed connection.

I’ll keep updating the site, and then send out a monster edition in a couple of days.

Sorry for the inconvenience.

Fraser Cain
Publisher
Universe Today

Posted on by Fraser Cain

Big Dunes on Mars

Image credit: NASA/JPL

Mars has the largest volcano, the deepest canyon, and it’s got the biggest sand dunes. Several conditions on the Red Planet, including its low gravity, air pressure and sand probably contribute to the gigantic sand dunes that can form there. Dunes have been seen by the Mars Global Surveyor which reach twice as tall as they get on Earth. The Mars Exploration Rovers, currently on track to reach Mars in early 2004 will have cameras on board that may help scientists take a closer look at the sand that makes up these gigantic dunes.

Mars is kind of like Texas: things are just bigger there. In addition to the biggest canyon and biggest volcano in the solar system, Mars has now been found to have sand ripples twice as tall as they would be on Earth.

Initial measurements of some of the Red Planet’s dunes and ripples using stereo-images from the Mars Orbiter Camera onboard the Mars Global Surveyor have revealed ripple features reaching almost 20 feet high and dunes towering at 300 feet.

One way to imagine the taller dimension of ripples on Mars is to visualize sand ripples on Earth, then stretch out the vertical dimension to double height, without changing the horizontal dimension.

“They do seem higher in relation to ripples on Earth,” said Kevin Williams of the Smithsonian National Air and Space Museum. Williams will be presenting this latest insight into the otherworldly scale of Marscapes on Monday, Nov. 3 at the annual meeting of the Geological Society of America in Seattle, WA.

Ripples are common on Mars and usually found in low-lying areas and inside craters, says Williams. On Earth they tend to form in long parallel lines from sand grains being pushed by water or air at right angles to the ripple lines. Dunes, on the other hand, are formed when grains of sand actually get airborne and “saltate” (a word based on the Latin verb “to jump”). That leads to cusp-shaped, star-shaped, and other dune arrangements that allow materials to pile sand much higher.

How exactly Martian dunes and ripples form is still unknown, says Williams, since the images from space give us no clues to the grain sizes or whether they are migrating or moving in any way. Though there are Viking spacecraft images from almost 30 years ago to compare with, the images do not have the resolution to confirm whether ripples have moved much in that time. For now, the dimensions of ripple-forms on Mars are the only indications of whether they are large ripples or small dunes. Williams’ results came about from the advantageous combination of image parameters to get the first height measurements of these ripple-like features at the limit of image resolution.

According to Williams, it’s likely the doubled heights of Mars ripples relative to their spacing is made possible by the same thing that makes Mars’ volcanoes so tall: lower gravity. With about one-third the gravity of Earth, sand, silt, and dust can theoretically stack up higher before gravity causes a slope failure.

However, other differences could play roles in making these large piles of sand as well. “It could also be from different wind speeds, air densities or other factors,” said Williams. Mars has a perennially subfreezing, very thin atmosphere in which global dust storms have been known to obscure the surface from view.

The study of Mars dunes and ripples has been underway since Viking spacecraft images of Mars first revealed such features in the late 1970s and early 1980s, says Williams. The primary difficulty of the work continues to be in discerning the close-up details, like the exact heights of features and grain sizes. As with dunes and ripples on Earth, these wind-blown features could reveal a lot about local and regional weather and wind currents ? if more was known about ripple and dune building under the very un-Earthlike conditions of Mars.

So far the only close-encounters humans have ever had with Martian dunes were with the Viking Landers and the Pathfinder mission, which sent the Sojourner rover trundling among Martian boulders. “There were some small dunes in the area of Pathfinder,” Williams said.

There are also likely to be ripples or small dunes within range of the far more mobile Mars Exploration Rovers now enroute to the Red Planet, Williams said. The Mars Exploration Rovers, Spirit and Opportunity, are larger and will be able to travel much further than Sojourner, making it more likely they will be taking a closer look at ripples as well as other geological features of Mars.

Original Source: Geological Society of America News Release

Posted on by Fraser Cain

Envisat Watches an Iceberg Break Up

Image credit: ESA

The European Space Agency’s Envisat Earth observation satellite captured images of a gigantic iceberg as it broke up during an Antarctic storm. The iceberg, called B-15A, was created in March 2000 when a Jamaican-sized chunk of ice broke away from the Ross Ice Shelf. It broke into smaller pieces shortly after that, but the largest chunk, B-15A grounded itself off the coast and stuck around for a few years. Finally in October, 2003, a giant storm helped split the iceberg up.

ESA’s Envisat satellite was witness to the dramatic last days of what was once the world’s largest iceberg, as a violent Antarctic storm cracked a 160-km-long floe in two.

A series of Envisat Advanced Synthetic Aperture Radar (ASAR) instrument images acquired between mid-September and October record how the bottle-shaped iceberg B-15A was split by the onslaught of powerful storms, waves and ocean currents as its own weight kept it fixed on the floor of Antarctica’s Ross Sea.

ASAR is especially useful for polar operations because its radar signal can pierce thick clouds and works through both day and night. Radar imagery charts surface roughness, so can easily differentiate between different ice types. Old ice ? as on the surface of B-15A ? is rougher than newly formed ice.

B-15A began its existence as B-15 in March 2000 – with an area of 11,655 sq km it was the world’s largest known iceberg. This Jamaica-sized floe was created when it broke away from the Ross Ice Shelf. The initial monster berg split into numerous pieces shortly afterwards, with the largest piece designated B-15A.

Like a wall of ice, B-15A remained a stubborn presence for the next two and a half years, diverting ocean currents. This caused increased ice around Ross Island that disrupted breeding patterns for the local penguin colony and required extra icebreaker activity to maintain shipping access to the US base at McMurdo Sound.

B-15A’s end came in sight on 7 October this year, as 120 kph winds buffeted the grounded iceberg during a storm. Two cracks ran into the heart of the iceberg from opposite ends until finally the entire berg gave way.

The larger of the two new pieces has inherited the name B-15A, and the smaller berg named B-15J. They remain largely locked in place, some 3,800 kilometres south of New Zealand. The bergs could persist there for many years ? a GPS station has been placed on the 3,496 sq km B-15A to enable study of its future progress.

Despite events such as these there is so far no conclusive evidence as to whether polar ice is actually thinning. Next year will see the launch of ESA?s CryoSat mission, a dedicated ice-watching satellite designed to map precise changes in the thickness of polar ice-sheets and floating sea-ice.

CryoSat will be the first satellite to be launched as part of the Agency?s Living Planet Programme. This small research mission will carry a radar altimeter that is based on a heritage from existing instruments, but with several major enhancements to improve the measurement of icy surfaces.

By determining rates of ice-thickness change CryoSat will contribute to our understanding of the relationship between the Earth?s ice cover and global climate.

Original Source: ESA News Release

Posted on by Fraser Cain

Desert in Chile Could Help Explain Mars Environment

Image credit: NASA

A team of scientists have traveled to one of the driest places on Earth to help understand why past missions to Mars have failed to detect any life in the soil. The Atacama Desert is located in a region of Chile which is blocked on both sides by high mountain ranges, so it’s incredibly dry. The scientists have studied the soil and realized that organic material is there, it’s just so minimal that the instruments on board the Viking lander, which visited Mars in the 1970s, wouldn’t have been able to sense them. More sophisticated instruments should be installed on future missions to find evidence of life.

A team of scientists from NASA, the Universidad Nacional Autonoma de Mexico, Louisiana State University and several other research organizations has discovered clues from one of Earth’s driest deserts about the limits of life on Earth, and why past missions to Mars may have failed to detect life.

The results were published this week in Science magazine in an article entitled “Mars-like Soils in the Atacama Desert, Chile, and the Dry Limit of Microbial Life.”

NASA’s Viking missions to Mars in the 1970s showed the martian soil to be disappointingly lifeless and depleted in organic materials, the chemical precursors necessary for life. Last year, in the driest part of Chile’s Atacama Desert, the research team conducted microbe-hunting experiments similar to Viking’s, and no evidence of life was found. The scientists called the finding “highly unusual” in an environment exposed to the atmosphere.

“In the driest part of the Atacama, we found that, if Viking had landed there instead of on Mars and done exactly the same experiments, we would also have been shut out,” said Dr. Chris McKay, the expedition’s principal investigator, who is based at NASA Ames Research Center, Moffett Field, Calif. “The Atacama appears to be the only place on Earth Viking would have found nothing.”

During field studies, the team analyzed Atacama’s depleted Mars-like soils and found organic materials at such low levels and released at such high temperatures that Viking would not have been able to detect them, said McKay, who noted that the team did discover a non-biological oxidative substance that appears to have reacted with the organics — results that mimicked Viking’s results.

“The Atacama is the only place on Earth that I’ve taken soil samples to grow microorganisms back at the lab and nothing whatsoever grew,” said Dr. Fred A. Rainey, a co-author from Louisiana State University, who studies microorganisms in extreme environments.

According to the researchers, the Atacama site they studied could serve as a valuable testbed for developing instruments and experiments that are better tailored to finding microbial life on Mars than the current generation. “We think Atacama’s lifeless zone is a great resource to develop portable and self-contained instruments that are especially designed for taking and analyzing samples of the martian soil,” McKay said.

More sophisticated instruments on future sample-return Mars missions are a necessity if scientists are to avoid contaminating future martian samples, McKay noted. “We’re still doing the first steps of instrument development for Mars.” Recently, researchers have developed a method to extract DNA from soil without humans getting involved in processing the data, which is “a step in the right direction,” according to McKay.

The reason Chile’s Atacama Desert is so dry and virtually sterile, researchers say, is because it is blocked from moisture on both sides by the Andes mountains and by coastal mountains. At 3,000 feet, the Atacama is 15 million years old and 50 times more arid than California’s Death Valley. The scientists studied the driest part of the Atacama, an area called the ‘double rain shadow.’ During the past four years, the team’s sensor station has recorded only one rainfall, which shed a paltry 1/10 of an inch of moisture. McKay hypothesizes that it rains in the arid core of the Atacama on average of only once every 10 years.

The Atacama research was funded by NASA’s Astrobiology Science and Technology for Exploring Planets program, by Louisiana State University, the National Science Foundation and by several other organizations.

The article was also authored by Dr. Rafael Navarro-Gonzalez, Dr. Paola Molina and Dr .Jose de la Rosa from the Universidad Nacional Autonoma de Mexico, Mexico City, MX; Danielle Bagaley, Becky Hollen and Alanna Small, Louisiana State University, Baton Rouge, LA.; Dr. Richard Quinn, the SETI Institute, Mountain View, Calif.; Dr. Frank Grunthaner, NASA Jet Propulsion Laboratory, Pasadena, Calif.; Dr. Luis Caceres, Instituto del Desierto y Departameno de Ingenieria, Quimica; and Dr. Benito Gomez-Silva, Instituto del Desierto y unidad de Bioquimica, Universidad de Antofagasta, Antofagasta, Chile.

For images of the field experiments, please go to: http://www.sciencemag.org

Original Source: NASA News Release

Posted on by Fraser Cain

Three New Astronauts Added For Next Shuttle Mission

Image credit: NASA

NASA announced that three additional astronauts will fly into space aboard the space shuttle when it returns to flight some time after September 2004. STS-114 will consist of Mission Commander Eileen Collins, Pilot James Kelly, and Mission Specialists Stephen Robinson, Soichi Noguchi, Andrew Thomas, Wendy Lawrence and Charles Camarda. The mission objectives for the flight will be to test the new safety procedures developed as part of the Columbia accident investigation including shuttle inspection and repair techniques.

The STS-114 crew, augmented by three new members, is in place for the Space Shuttle’s Return to Flight mission. Three Mission Specialists have been added to the four astronauts already in training for the STS-114 mission planned for launch no earlier than September 2004.

The new crewmembers, Andrew Thomas (Ph.D.), Wendy Lawrence (Capt., USN) and Charles Camarda (Ph.D.) join mission commander Eileen Collins (Col., USAF), Pilot James Kelly (Lt. Col., USAF), Mission Specialists Stephen Robinson (Ph.D) and Soichi Noguchi, of the Japan Aerospace Exploration Agency, who were named to this flight in 2001.

“STS-114 is going to be a complex developmental test flight, and this crew has the right set of skills and experience to help get the Space Shuttles safely flying again,” said NASA’s Associate Administrator for Space Flight William Readdy. “STS-114 was always slated to have a crew of seven. But now, instead of three crew rotating on-and-off the International Space Station, all crew members will be dedicated to the STS-114 mission objectives,” Readdy said.

The major mission objectives of the STS-114 flight have shifted from International Space Station logistics and crew rotation to testing and evaluating new procedures for flight safety. This includes Shuttle inspection and repair techniques. It also includes a smaller set of Space Station tasks from what was scheduled before the Shuttle Columbia accident in February.

“This is a demanding mission and the addition of Andy, Wendy and Charlie, to this already well-qualified crew, ensures they have all the skills necessary to meet the challenge of Return to Flight and the resumption of Space Shuttle support of the International Space Station,” said Bob Cabana, Director of Flight Crew Operations at NASA’s Johnson Space Center.

“Andy brings a wealth of experience in all areas of operations from his previous Shuttle flights and Mir space station mission. Wendy is a superb robotics operator with detailed knowledge of all the Shuttle systems. Charlie has been actively involved with the thermal protection system repair activities and has trained as a backup Space Station crewmember. He is thoroughly familiar with the systems on board the International Space Station,” Cabana said.

“When coupled with Eileen, Jim, Steve and Soichi, who were already trained to perform the assembly tasks on this mission, the full crew will have the expertise and crew time to accomplish all mission objectives,” Cabana said.

Collins served as pilot on STS-63 in 1995 and STS-84 in 1997. She flew as commander in 1999 on STS-93. Kelly piloted his first mission aboard STS-102 in 2001. Robinson was on STS-85 in 1997 and STS-95 in 1998. He served as a backup crewmember for Expedition 4. Thomas, a long-duration Russian Space Station Mir veteran, also served aboard STS-77 in 1996, STS-89 and 91 to and from the Mir in 1998, and STS-102 in 2001. Lawrence, another space veteran, brings experience from STS-67 in 1995, STS-86 in 1997, and STS-91 in 1998. Noguchi and Camarda, both selected as astronauts in 1996, will make their first flight to space on STS-114.

For biographical information about the STS-114 crew and other astronauts on the Internet, visit the NASA astronaut biography page at:

http://www.jsc.nasa.gov/Bios/
For more information about NASA’s Return to Flight efforts on the Internet, visit:

http://www.nasa.gov/news/highlights/returntoflight.html

Original Source: NASA News Release

Posted on by Fraser Cain

Total Lunar Eclipse Was a Treat on Saturday Night

Skywatchers from Alaska to Eastern Europe were treated to a total lunar eclipse on Saturday night, when the Moon dipped behind the Earth’s shadow. Chunks of the Moon began to disappear at 2332 Universal Time (6:32 pm EST), and then it turned a coppery red about two hours later. And then four hours after it started, the eclipse was over. Many observers said it was one of the brightest eclipses they’d seen in recent years. If you missed this show, don’t worry, there are two more lunar eclipses coming in 2004. Then a break; there won’t be another total lunar eclipse visible until 2007.

Posted on by Fraser Cain

ESA Cancels Eddington

Image credit: ESA

The European Space Agency announced this week that it has canceled Eddington, a space-based observatory designed to search for extrasolar planets. They’re also going to be scaling back the BepiColombo mission to Mercury by removing the lander that was supposed to accompany the spacecraft. The agency blamed the cuts on budget overruns with other missions, such as Rosetta. One new mission was announced, however. The LISA Pathfinder will serve as a prototype to help search for gravity waves.

Today, at its 105th meeting, ESA’s Science Programme Committee (SPC) has made important decisions concerning the Cosmic Vision programme. Due to the current financial exigencies and an outlook with no budget increase or other relief, the SPC was forced to cancel the Eddington mission and rescope the BepiColombo mission.

Eddington had two aims, both remarkable and very pertinent to front-line astronomical interests. The first aim was to look for Earth-like planets outside our solar system – one of the key goals in the search to understand how life came to be, how we came to live where we do in the universe and whether there are other potential life supporting environments ‘out there’. At the same time it was going to follow on the path blazed by the ESA-NASA mission SOHO had taken with the Sun of using astroseismology to look ‘inside’ stars. In the longer term, the loss of this one mission will not stop us pursuing the grand quests for which it is a step.

The loss of the BepiColombo lander is also scientifically hard to take. ESA, in conjunction with the Japanese space agency, JAXA, will still put two orbiters around Mercury but the ?ground truth? provided by the lander is a big loss. However, to land on a planet so near the Sun is no small matter and was a bridge too far in present circumstances, and this chance for Europe to be first has probably been lost.

The origins of the problems were recognized at the ESA Council, held in June 2003. Several sudden demands on finance occurred in the spring, the most obvious and public being the unforeseen Ariane 5 grounding in January. A loan of 100 million Euro was temporarily granted, that must be paid back out of present resources by the end of 2006.

ESA’s SPC were therefore caught in a vice. Immediate mission starts had to be severely limited and the overall envelope of the programme kept down.

By making today’s decision, the SPC has brought down the scope of the Cosmic Vision programme to a level that necessarily reflects the financial conditions rather than the ambitions of the scientific community.

A long and painful discussion during the SPC meeting resulted in the conclusion that only one new mission can be started at this time, namely LISA Pathfinder. The mission is the technical precursor to the world?s first gravitational wave astronomical observatory, LISA. The LISA mission itself (to be made in cooperation with the United States) is scheduled for launch in 2012.

ESA’s Cosmic Vision, set to last until 2012, is a living programme. It has to be able to constantly adapt to to the available funding as well as respond to the expectations of the scientific community, to technological developments. Within these boundaries, the decisions made by the SPC try to maximize the outcome of Cosmic Vision across disciplines, keeping it at the same time challenging and affordable. Nonetheless, there are many European scientists with ambitions that exceed the programme?s ability to respond.

Original Source: ESA News Release

Posted on by Fraser Cain

NASA Selects Five Potential New Missions

Image credit: NASA

NASA has selected five proposals as part of its Small Explorer (SMEX) missions – these are low-cost, highly specialized missions to help advance science in a specific area. The candidates are: the Normal-incidence Extreme Ultraviolet Spectrometer, the Dark Universe Observatory, the Interstellar Boundary Explorer, the Nuclear Spectroscopic Telescope Array, and the Jupiter Magnetospheric Explorer. Two finalists will eventually be chosen for launch by 2007-2008.

NASA recently selected candidate mission proposals that would study the universe, from Jupiter and the sun to black holes and dark matter. The proposals are candidates for missions in NASA’s Explorer Program of lower cost, highly focused, rapid-development scientific spacecraft.

Following detailed mission concept studies, NASA intends to select two of the mission proposals by fall 2004 for full development as Small Explorer (SMEX) missions. The two missions developed for flight will be launched in 2007 and 2008.

NASA has also decided to fund as a “Mission of Opportunity” a balloon-borne experiment to detect high-energy neutrinos, ghostly particles that fill the universe.

“The Small Explorer mission proposals we received show that the scientific community has a lot of innovative ideas on ways to study some of the most vexing questions in science, and to do it on a relatively small budget,” said Dr. Ed Weiler, associate administrator for space science at NASA Headquarters, Washington. “It was difficult to select only a few from among the many great proposals we received, but I think the selected proposals have a great chance to really push back the frontiers of knowledge,” he said.

The selected proposals were judged to have the best science value among 36 submitted to NASA in February 2003. Each will receive $450,000 ($250,000 for the Mission of Opportunity) to conduct a five-month implementation feasibility study. The selected SMEX proposals are:

  • The Normal-incidence Extreme Ultraviolet Spectrometer (NEXUS): a solar spectrometer with major advances in sensitivity and resolution to reveal the cause of coronal heating and solar wind acceleration. Joseph M. Davila of NASA’s Goddard Space Flight Center (GSFC), Greenbelt, Md., would lead NEXUS at a total mission cost to NASA of $131 million.
  • The Dark Universe Observatory (DUO): seven X-ray telescopes to measure the dark matter and dark energy that dominate the content of the universe with 100 times the sensitivity of previous X-ray studies. Richard E. Griffiths of Carnegie Mellon University, Pittsburgh, would lead DUO at a total mission cost to NASA of $132 million.
  • The Interstellar Boundary Explorer (IBEX): a pair of cameras to image the boundary between the solar system and interstellar space with 100 times the sensitivity of previous experiments. David J. McComas of the Southwest Research Institute, San Antonio, would lead IBEX at a total mission cost to NASA of $132 million.
  • The Nuclear Spectroscopic Telescope Array (NuSTAR): a telescope to carry out a census of black holes with 1000 times more sensitivity than previous experiments. NuSTAR would be lead by Fiona Anne Harrison of the California Institute of Technology, Pasadena, at a total mission cost to NASA of $132 million.
  • The Jupiter Magnetospheric Explorer (JMEX): a telescope to study Jupiter’s aurora and magnetosphere from Earth orbit. Nicholas M. Schneider of the University of Colorado at Boulder would lead JMEX, at a total mission cost to NASA of $133 million.

NASA selected a long-duration balloon payload as the mission of opportunity. The Antarctic Impulsive Transient Antenna (ANITA) would detect radio waves emitted when high-energy neutrinos interact in the Antarctic ice shelf. ANITA would be led by Peter W. Gorham of the University of Hawaii at Manoa in Honolulu, at a total mission cost to NASA of $35 million.

In addition, NASA selected a proposed mission for technology-development funding of the proposed instrument. Jean Swank of GSFC will develop a polarization sensitive X-ray detector. Swank will receive up to $300,000 over the next two years for her study.

The five selected SMEX proposals are vying to be the tenth and eleventh SMEX missions selected for full development. Recent selections include the Reuven Ramaty High Energy Solar Spectroscopic Imager (RHESSI), launched in February 2002; the Galaxy Evolution Explorer (GALEX), launched in April 2003; and the Aeronomy of Ice in the Mesosphere mission (AIM), to be launched in 2006. The Explorer Program, managed by GSFC for NASA’s Office of Space Science, is designed to provide frequent, low-cost access to space for physics and astronomy missions with small to mid-sized spacecraft.

Original Source: NASA News Release