New Earth Measurement Data Released

Image credit: NASA

NASA has released detailed topographical data of Europe and Asia that was gathered by the space shuttle as part of the 10-day Shuttle Radar Topography Mission (SRTM) in February 2000 that mapped 80% of the Earth’s surface. This data represents 40-percent of the data collected during the mission. North and South American data has already been made available, and the remainder should be completed by 2004. This precise 3-D mapping information is being used in many applications, including studying natural disasters, planning development, and aircraft navigation.

Marco Polo. Alexander the Great. They were some of history’s most prolific explorers, each trekking across sweeping stretches of Europe and Asia in their lifetimes. But these greats of world history had nothing on you, thanks to a new topographic data set from NASA and the National Geospatial-Intelligence Agency (NGA). You now can explore the vast reaches of most of Europe, Asia and numerous islands in the Indian and Pacific Oceans, from the comfort of home, without breaking a sweat.

Gathered in just 10 days by NASA’s Shuttle Radar Topography Mission (SRTM) in February 2000, the new digital elevation data set showcases some of Earth’s most diverse, mysterious and extreme topography. Much of it previously had been very poorly mapped due to persistent cloud cover or inaccessible terrain. The new data being released comprise more than one-third of the entire SRTM data set.

The new images are available on the JPL Planetary Photojournal at:

http://photojournal.jpl.nasa.gov/catalog/PIA03398
http://photojournal.jpl.nasa.gov/catalog/PIA03399
http://photojournal.jpl.nasa.gov/catalog/PIA04950
http://photojournal.jpl.nasa.gov/catalog/PIA04951

“People around the world will benefit from the release of the SRTM Europe and Asia topographic data sets because they greatly extend our knowledge of this immense region that also is home to most of Earth’s citizens,” said Dr. John LaBrecque, manager, Solid Earth and Natural Hazards Program, NASA Headquarters, Washington.

“The shape of Earth’s surface affects nearly every natural process and human endeavor. Precise, uniform, 3-D elevation data are needed for a wide range of applications from studying earthquakes, volcanism, floods and other natural hazards, to planning development, managing precious water resources, and insuring the safety of aircraft navigation,” LaBrecque noted.

“Releasing the Eurasia SRTM data provides geospatial data users with a remarkably consistent Earth-elevation surface. This enhances our global knowledge, provides a baseline for any future comparisons, and delivers accuracy and integrity unparalleled in any other global-elevation model of the Earth,” said NGA’s Technical Executive Roberta Lenczowski. “This SRTM data represents 40 percent of the data collected during the mission that covered roughly 80 percent of the landmass of the Earth. The cooperative effort between NASA and NGA, fusing science objectives with national security requirements, benefits all,” Lenczowski added.

The area covered in the current data-release stretches eastward from the British Isles and the Iberian Peninsula in the west, across the Alps and Carpathian Mountains, as well as the Northern European Plain, to the Ural and Caucasus Mountains bordering Asia. The Asian coverage includes a great variety of landforms, including the Tibetan Plateau, Tarim Basin, Mongolian Plateau and the mountains surrounding Lake Baikal, the world’s deepest lake. Mt. Everest in the Himalayas, at 8,848 meters (29,029 feet) is the world’s highest mountain. From India’s Deccan Plateau, to Southeast Asia, coastal China, and Korea, various landforms place constraints on land-use planning during periods of population growth. Volcanoes in the East Indies, the Philippines, Japan and the Kamchatka Peninsula form the western part of the “Ring of Fire” around the Pacific Ocean.

Previous releases from the mission covered North and South America. Forthcoming releases in 2004 will include Africa-Arabia and Australia, as well as an “islands” release for those islands not included in the continental data-releases. Together, these data-releases constitute the world’s first high-resolution, near-global elevation model. The resolution of these data for Europe and Asia is three arc seconds (1/1,200 of a degree of latitude and longitude), which is about 90 meters (295 feet).

The SRTM mission is a cooperative project of NASA, NGA and the German and Italian space agencies. NASA’s Jet Propulsion Laboratory, Pasadena, Calif., processed the data into research-quality digital elevation data. The National Geospatial-Intelligence Agency is providing additional processing to develop mapping products. The U.S. Geological Survey Earth Resources Observation Systems Data Center in Sioux Falls, S.D., provides final archiving and distribution of the SRTM data products.

Information about SRTM is available at:

http://www.jpl.nasa.gov/srtm

More information about NASA is at:

http://www.jpl.nasa.gov/srtm

Original Source: NASA News Release

Distance to Pleiades Calculated

Image credit: NOAO

Astronomers from NASA’s Jet Propulsion Laboratory have measured the distance to the Pleiades star cluster to greatest precision ever. After a decade’s worth of interferometric measurements, the team found that the star cluster is between 434 and 446 light years from Earth. This is important because the European Hipparcos satellite previously measured a distance to the cluster that would have contradicted theoretical models of the life cycles of stars. This new measurement shows that Hipparcos was incorrect, and the established theory still holds.

The cluster of stars known as the Pleiades is one of the most recognizable objects in the night sky, and for millennia has been celebrated in literature and legend. Now, a group of astronomers has obtained a highly accurate distance to one of the stars of the Pleiades known since antiquity as Atlas. The new results will be useful in the longstanding effort to improve the cosmic distance scale, and to conduct research on the stellar life-cycle.

In the January 22 issue of the journal Nature, astronomers from the California Institute of Technology and NASA?s Jet Propulsion Laboratory, both in Pasadena, Calif., report the best-ever distance to the double-star Atlas. The star, along with “wife” Pleione and their daughters, the “seven sisters,” are the principal stars of the Pleiades that are visible to the unaided eye, although there are actually thousands of stars in the cluster. Atlas, according to the team’s decade of careful interferometric measurements, is somewhere between 434 and 446 light-years from Earth.

The range of distance to the Pleiades cluster may seem somewhat imprecise, but in fact is accurate by astronomical standards. The traditional method of measuring distance is by noting the precise position of a star and then measuring its slight change in position when Earth itself has moved to the other side of the sun. This approach can also be used to find distance on Earth: If you carefully record the position of a tree an unknown distance away, move a specific distance to your side, and measure how far the tree has apparently “moved,” then it’s possible to calculate the actual distance to the tree by using trigonometry.

However, this procedure gives only a rough distance estimate to even the nearest stars, due to the gigantic distances involved and the subtle changes in stellar position that must be measured.

The team’s new measurement settles a controversy that arose when the European satellite Hipparcos provided a much shorter distance measurement to the Pleiades than expected and contradicted theoretical models of the life cycles of stars.

This contradiction was due to the physical laws of luminosity and its relationship to distance. A 100-watt light bulb one mile away looks exactly as bright as a 25- watt light bulb half a mile away. So to figure out the wattage of a distant light bulb, we have to know how far away it is. Similarly, to figure out the “wattage” (luminosity) of observed stars, we have to measure how far away they are. Theoretical models of the internal structure and nuclear reactions of stars of known mass also predict their luminosities. So the theory and measurements can be compared.

However, the Hipparcos data provided a distance lower than that assumed from the theoretical models, thereby suggesting either that the Hipparcos distance measurements themselves were off, or else that there was something wrong with the models of the life cycles of stars. The new results show that the Hipparcos data was in error, and that the models of stellar evolution are indeed sound.

The new results come from careful observation of the orbit of Atlas and its companion — a binary relationship that wasn’t conclusively demonstrated until 1974 and certainly was unknown to ancient watchers of the sky. Using data from the Mount Wilson stellar interferometer, next to the historic Mount Wilson Observatory, and the Palomar Testbed Interferometer at Caltech’s Palomar Observatory near San Diego, the team determined a precise orbit of the binary.

Interferometry is an advanced technique that allows, among other things, for the “splitting” of two bodies so far away that they normally appear as a single blur, even in the biggest telescopes. Knowing the orbital period and combining it with orbital mechanics allowed the team to infer the distance between the two bodies, and with this information, to calculate the distance of the binary to Earth.

“For many months I had a hard time believing our distance estimate was 10 percent larger than that published by the Hipparcos team,” said the lead author, Xiao Pei Pan of JPL. “Finally, after intensive rechecking, I became confident of our result.”

Coauthor Shrinivas Kulkarni, a Caltech astronomy and planetary science professor, said, “Our distance estimate shows that all is well in the heavens. Stellar models used by astronomers are vindicated by our value.”

“Interferometry is a young technique in astronomy and our result paves the way for wonderful returns from the Keck interferometer and the anticipated Space Interferometry Mission that is expected to be launched in 2009,” said coauthor Michael Shao of JPL, prinicipal investigator for that planned mission, and for the Keck Interferometer, which links the two 10-meter telescopes at the Keck Observatory in Hawaii. The Palomar Testbed Interferometer was designed and built by a team of researchers from JPL led by Mark Colavita and Shao. It served as an engineering testbed for the Keck Interferometer.

Original Source: NASA/JPL News Release

Weather on Earth is a Problem for Spirit

Image credit: NASA/JPL

A thunderstorm in Australia has hampered communications between NASA and the Spirit rover on Mars. The rover was supposed to use its Rock Abrasion Tool (RAT) to grind into the rock 5 mm, but the weather interfered with the commands sent from Earth. When it doesn’t receive orders from Earth, Spirit goes into a stasis mode where it runs checks on its systems, and takes photographs of its surroundings. Engineers are hoping to try again tonight.

Ground controllers were able to send commands to the Mars Exploration Rover Spirit early Wednesday and received a simple signal acknowledging that the rover heard them, but they did not receive expected scientific and engineering data during scheduled communication passes during the rest of that martian day.

Project managers have not yet determined the cause, but similar events occurred several times during the Mars Pathfinder mission. The team is examining a number of different scenarios, some of which would be resolved when the rover wakes up after powering down at the end of the martian day (around midday Pacific time Wednesday).

The next opportunity to hear from the vehicle is when the rover may attempt to communicate with the Mars Global Surveyor orbiter at about 8:30 p.m. Pacific time tonight. A second communication opportunity may occur about two hours later during a relay pass via the Mars Odyssey orbiter. If necessary, the flight team will take additional recovery steps early Thursday morning (the morning of sol 19 on Mars) when the rover wakes up and can communicate directly with Earth.

Full details on the rover’s status will be described in the next daily news conference Thursday at 9 a.m. Pacific time at the Jet Propulsion Laboratory, which will be broadcast live on NASA Television.

Original Source: NASA/JPL News Release

Next Steps for Beagle 2

Image credit: Beagle2

Controllers initiated a state of radio silence with the Beagle 2 lander after it failed to report in, or communicate through Mars Express. In theory this radio silence should force Beagle 2 to enter into “Communication Mode 2”, where it attempts to call out constantly throughout the Martian day. The best opportunities to make contact with the lander will happen on the nights of January 24/25 when Mars Express passes over a significant portion of the landing area.

On 12 January a period of radio silence was initiated when no attempts were made to contact Beagle 2. Maintaining radio silence for a period of ten days is intended to force Beagle 2 into a communication mode that should ensure that the transmitter is switched on for the majority of the daytime on Mars and thus will improve the chance of the Mars Express orbiter making contact.

During this ten-day period Mars Express has listened for Beagle 2 but only for very short periods when Beagle 2 may not have been switched on.

The ten-day radio silence period ends today [22 January], just before a fly-over by Mars Express. However, it is not intended to hail the Lander immediately. This cautious approach is based on the fact that the end of the ten-day period of radio silence cannot be predicted with total confidence. This is because the absolute accuracy of the timer on Beagle 2 could have been affected by the temperature on Mars, making the clock run slightly faster or slower than predicted.

It has therefore been decided to choose a pair of opportunities when Mars Express flies over the Beagle 2 landing site, namely the nights of 24 and 25 January. These two flights cover the widest possible area where Beagle 2 should be, giving the best chance of calling the Lander and getting a response from the continuous transmission.

The results from these latest attempts to communicate with Beagle 2 will be announced by Prof. Colin Pillinger, Beagle 2 Lead Scientist and Dr. Mark Sims, Beagle 2 Mission Manager, on 26 January, at a media briefing to be held at The Science Media Centre, The Royal Institution of Great Britain, 21 Albemarle Street, London W1S 4BS, at 1400 GMT.

Original Source: PPARC News Release

Selecting Stars Very Similar to Our Own

Image credit: John Rowe

The search for Earthlike planets begins with the search for Sunlike stars. At the top of the list is a reasonably nearby star called 37 Gem; located in the Gemini constellation. Astronomer Maggie Turnbull was asked to make a short list of thirty candidate stars that closely matched our own Sun out of a total list 2,350 stars which are within one hundred light years from us. This short list, including 37 Gem will be used by the Terrestrial Planet Finder mission, which will search for habitable planets by looking for the visible light of oxygen or water in an Earthlike planet – a sure sign of life.

The thirty-seventh most westerly star in the constellation, Gemini, is a yellow-orange star like our own sun. The star is called 37 Geminorum, but for astrophysicist Margaret Turnbull, the star is special because it offers a case study for considering what might qualify as a good candidate for harboring habitable planets.

In building her list of stars that might support planets with liquid water and oxygen, she has to exclude suns that are extreme: either too young or too old, that rotate too fast, or that are variable enough in brightness to cause climatic chaos on any nearby world.

At a distance of 56.3 light-years away, the star 37 Gem has yet to show tell-tale signs of having such planets, or any planets–but future NASA and European telescopes are looking to target stars just like 37 Gem since they might share some of the same properties that made our own solar system habitable. More than 100 extrasolar planets have been found so far using ground-based telescopes, and estimates for the total such planets in our galaxy may total in the billions of candidate worlds.

Working from the University of Arizona in Tucson, Maggie Turnbull was asked to make a short list of thirty star candidates that most closely resembled other suns capable of supporting the conditions for life to flourish. Starting her search among stars less than one hundred light-years away yielded about 2,350 stars to consider further.

Turnbull recently presented her results to a group of scientists from NASA’s space-telescope project, the Terrestrial Planet Finder (TPF), which will search for habitable planets by using visible light with the “signature” of water and/or oxygen from an Earth-type planet. After TPF’s scheduled launch around 2013, will follow the European Darwin project involving six space telescopes.

The stellar list was pared down from an even larger list (17,129 stars within 450 light-years, or 140 parsecs), which Turnbull and adviser Jill Tarter of the SETI Institute first published in Astrophysical Journal. The list became known as the Catalog of Nearby Habitable Stellar Systems (or HabCat ). Their article published in August, entitled “Target Selection for SETI: I. A Catalog of Nearby Habitable Stellar Systems,” expanded previous candidate lists by nearly ten-fold, or an order-of-magnitude.

To support complex life, a candidate star must be the right color, brightness, and age. If it is a middle-aged star like our own, it will have burned through enough fusionable light elements to produce heavier metals like iron, but not so old that it is collapsing or so young that life is only a distant future prospect. Based on what fragments we know about how complex life appeared on Earth, Turnbull’s search aims to find the ‘Goldilocks’ of stars that seems ‘just right’.

So why 37 Gem?
37 Geminorum lies in the northwest part of constellation Gemini , named after the Twins. For amateur astronomers with a good backyard telescope, 37 Gem is visible. In Greek mythology, the Gemini twins sailed with Jason in the quest for the Golden Fleece; during a storm, the twins helped save their ship ARGO from sinking, and so the constellation became much valued by sailors.

Most stars like Gem 37 are grouped into a small number of spectral classes, based roughly on the color of light they emit. Called the Henry Draper Catalog, the star compendium lists spectral classes in seven broad categories, from the hottest to the coolest stars. These types are designated, in order of decreasing temperature, by the letters O, B, A, F, G, K, and M. The nomenclature is rooted in long-obsolete ideas about stellar evolution, but the terminology remains. Our sun, classified on a finer scale as a typical ‘G2V’ dwarf, is approximately 4.5 billion years old. The candidate star, 37 Gem, is similarly middle-aged, but somewhat older by a billion years, at 5.5 billion years.

The spectra of G-type stars like our own (and 37 Gem) are dominated by certain chemical elements, as signaled by their characteristic spectral lines (or emissions). The elements of most current interest are metals, particularly for those star-signatures rich in iron, calcium, sodium, magnesium, and titanium. In astronomical terms, compared to our sun’s classification as a typical G2V dwarf, 37 Gem has a slightly hotter surface temperature. Thus Turnbull’s prime pick–37 Gem– is catalogued as a G0V dwarf–meaning it is also a yellow-orange main sequence dwarf star. Because G stars are characterized by the presence of these metallic lines and a weak hydrogen spectra, they share a common age, mass, and luminosity.

Otherwise, 37 Gem is close to our own solar twin, or a Gemini-like counterpart to the Sun: 1.1 times our sun’s mass, 1.03 times its diameter, and 1.25 times its luminosity.

Luminosities are “perhaps the most important information”, Turnbull told Astrobiology Magazine, “we use in determining the habitability of nearby stars” for complex life, because luminosity indicates which phase of life the star is in, and that in turn dictates how long the star will remain stable.

Astrobiology Magazine had the opportunity to talk with Maggie Turnbull at the Steward Observatory in Tucson about how to select stellar candidates for habitability.

Astrobiology Magazine (AM): Your recent survey began looking at around 100-light years distant from our Sun, and all stars inwards from that radius, correct? That was the visual sphere for starting the search?

Margaret Turnbull (MT): There are about 2,350 Hipparcos stars within 30 parsecs (90 light
years), the maximum distance for the Terrestrial Planet Finder (TPF) mission. There are about 5,000 total stars within that distance, but we are only looking at Hipparcos stars so my starting list is 2,350 stars long.

AM: Have you ever gotten hold of a backyard telescope to see 37 Gem?

MT: It should certainly be visible with a backyard telescope, but no, I haven’t looked at it with my own eyes! Because of the photometry (measuring its brightness) and spectroscopy (measuring its composition) I have looked at, I feel like I “know” it without ever having seen it.

However, there is more observing to be done for 37 Gem. For example, we do need to carry out high resolution infrared imaging of this star before we can say it should be a target–if we discover that there is a lot of debris floating around, we’ll have to take it off the list.

AM: Was the star, 37 Gem, much different from number two on the list of the thirty best candidates?

MT: Actually, the “best” stars are all very similar to one another, and in reality it doesn’t make much sense to try to rank them. 37 Gem happens to be one of the very nearest stars that also satisfies the engineering criteria, so at this time it looks like a very good candidate for the TPF search.

AM: Just out of curiousity, what star was officially number two on the list?

MT: When you are only going to look at thirty stars, they all better be “number one.” That is, every star we observe has to be of primary interest to the mission, because we have no time to waste. We are still in the process of precisely defining the primary mission goal.

If the goal is to look at range of spectral types, then the top stars may include very nearby K or M stars, but if the goal is to look at 30 of the most Sun-like stars, then stars like 18 Sco (a solar twin at 14 parsecs in the Constellation Scorpius), beta CVn (the “hound”), or 51 Peg (“Pegasus”, the flying horse) may end up being our best bets.

AM: Are there one or two pieces of missing data that would help the classification hone in better on star candidates?

MT: At this time, high-resolution infrared imaging is the missing piece of data that we definitely need. We need to know if these stars have dusty debris disks that would make it hard to detect planets orbiting there.

The Sun has a substantial amount of zodiacal dust because Jupiter is constantly stirring up the asteroid belt and as the asteroids collide they add dust to the Solar System.

A similar level of dust around other stars might not ruin our chances of seeing planets, but we’d certainly like to keep that to a minimum.

AM: What are your future plans for the stellar list in support of the Terrestrial Planet Finder and Darwin missions?

MT: I haven’t yet presented my ‘final’ list to the TPF science working group on Nov 18th and 19th at the US Naval Observatory, during a meeting with others who are creating their own lists.

I have already presented my methodology to the group, but now we will be meeting with engineers who will explain to us the constraints of the instrument and we will have to refine further the list to accommodate their criteria.

Their criteria will include things like: can’t have a companion star within several arcseconds even if the companion is not a concern for planet stability, because the extra light will contaminate the field of view; can’t look at stars fainter than about 6th magnitude; can only look at stars at least ~60 degrees away from the Sun during the whole year, etc.

AM: You published your first catalog of habitable stars in August of this year, and there is a part two to that classification. What are the main plans for Part II of the HabCat?

MT: Jill Tarter and I have recently submitted a second paper on the SETI target list which will appear in the Astrophysical Journal Supplements in December. This paper gives a list of old, high metallicity open clusters, the nearest 100 stars regardless of stellar type, and about 250,000 main sequence stars from the Tycho Catalogue, all of which will be observed by the Allen Telescope Array (ATA) whenever a HabCat star isn’t available for us to observe.

The primary ATA beam will be pointed by radio astronomers, and they will be making very high resolution maps of their own targets, while at the same time we will be observing HabCat stars (or stars from our lists in Paper 2) for SETI.

AM: Finally, are the missions, Kepler and TPF, planning the kinds of enhancements that would yield a detection of more Earth-sized planets, not just gas giants, for a given star in their surveys?

MT: Yes. Kepler will give us an indication of how common terrestrial planets are by watching thousands of sun-like stars for “transits”–events where the planet actually passes in front of the star it is orbiting and temporarily blocks a little of the star’s light.

Terrestrial Planet Finder will follow up on this by actually imaging planets orbiting the nearest stars, and telling us whether these planets have atmopheres by taking spectra.

We can look for water, oxygen, and carbon dioxide, and if we’re lucky we may even see some direct indications of life in the form of a vegetation signature or strong atmospheric disequilibrium, such as the simultaneous presence of oxygen and methane (due to the simultaneous presence of plants and methanogen bacteria on Earth).

What’s Next
Any mission to detect and spectroscopically characterize terrestrial planets around other stars must be designed so that it can detect diverse types of terrestrial planets with a useful outcome. Such missions are now under study–the Terrestrial Planet Finder (TPF), by NASA, and Darwin by ESA, the European Space Agency. The principal goal of TPF/Darwin is to provide data to the biologists and atmospheric chemists.

The TPF/Darwin concept hinges on the assumption that one can screen extrasolar planets for habitability spectroscopically. For such an assumption to be valid, we must answer the following questions. What makes a planet habitable and how can they be studied remotely? What are the diverse effects that biota might exert on the spectra of planetary atmospheres? What false positives might we expect? What are the evolutionary histories of atmospheres likely to be? And, especially, what are robust indicators of life?

TPF/Darwin must survey nearby stars for planetary systems that include terrestrial sized planets in their habitable zones (“Earth-like” planets). Through spectroscopy, TPF/Darwin must determine whether these planets have atmospheres and establish whether they are habitable.

The Kepler mission is also scheduled for launch into solar orbit in October 2006. Kepler is intended as a mission to determine the frequency of inner planets near the habitable zone of a wide range of stars. Kepler will simultaneously observe 100,000 stars in our galactic “neighborhood,” looking for Earth-sized or larger planets within the “habitable zone” around each star – the not-too-hot, not-too-cold zone where liquid water might exist on a planet.

To highlight the difficulty of detecting an Earth-sized planet orbiting a distant star, Kepler’s principal investigator, William Borucki of NASA Ames points out it would take 10,000 Earths to cover the Sun’s disk. One NASA estimate says Kepler should discover 50 terrestrial planets if most of those found are about Earth’s size, 185 planets if most are 30 percent larger than Earth and 640 if most are 2.2 times Earth’s size. In addition, Kepler is expected to find almost 900 giant planets close to their stars and about 30 giants orbiting at Jupiter-like distances from their parent stars.

Because most of the gas giant planets found so far orbit much closer to their stars than Jupiter does to the Sun, Borucki believes that during the four- to six-year mission, Kepler will find a large proportion of planets quite close to stars. If that proves true, he says, “We expect to find thousands of planets.”

Using present methods, astronomers today would find it very difficult to detect an Earth-sized planet around the star 37 Gem. Past analyses have however ruled out some choices. For instance, a giant planet like our own Jupiter or Saturn does not orbit around 37 Gem. These studies have suggested that giant planets of one-tenth to 10 times the mass of Jupiter do not exist close to 37 Gem (within 0.1 to four astronomical units, or one earth-sun distance, AUs, see also Cummings et al, 1999 ). Because of the challenges of finding dim planets near to much brighter stars, almost all of the extrasolar planets found so far are like our own Jupiter–massive, probably gaseous, and unlikely to harbor conditions for life owing to their close proximity to a parent star.

But conditions around 37 Gem might support smaller, inner planets like Venus or Earth. No one knows. Only future surveys will have the instrumentation capable of finding such Earth-like planets.

Models of stars like 37 Gem, do however, support the possible existence of at least one stable orbit for an Earth-like planet (with liquid water) centered around one earth-sun distance (1.12 AU). Such a presumed planet would orbit between the distances of Earth and Mars in our Solar System. This undiscovered planet, if it can be detected in future studies, would have a year that lasts more than 450 days, or an orbital period of around 1.3 Earth-years.

Since oxygen-generating life on Earth took about two billion years to take hold, stars much younger than this would likely not have had sufficient time for life to evolve towards any complex forms. Given the billions of years required for evolution of life on earth, scientists could question whether life would stand a chance in a shorter-lived solar system. Hotter, more massive stars have always been considered less likely to harbor life but not because they would be too hot. Planets could still enjoy temperate climates, just further out than Earth is from the Sun, and at orbits farther away from the its own parent star. The first problem of habitability is one of time, not temperature. Hotter stars tend to burn out faster — perhaps too fast for life to develop there.

Original Source: Astrobiology Magazine

Spirit Reaches Out to Adirondack

Image credit: NASA/JPL

Spirit is reaching out to test the nearby rock, “Adirondack”, which controllers targeted to get a better understanding of its composition and origin; it will be performing a series of tests today and tonight. The rover already used its instruments to examine a patch of soil near the lander and found some surprising results: the soil in Gusev Crater seems volcanic in origin, not sedimentary. Its instruments have also found the presence of a mineral called olivine, which doesn’t resist weathering very well and is normally evidence of volcanic deposits.

The first use of the tools on the arm of NASA’s Mars Exploration Rover Spirit reveals puzzles about the soil it examined and raises anticipation about what the tool will find during its studies of a martian rock.

Today and overnight tonight, Spirit is using its microscope and two up-close spectrometers on a football-sized rock called Adirondack, said Jennifer Trosper, mission manager at NASA’s Jet Propulsion Laboratory, Pasadena, Calif.

“We’re really happy with the way the spacecraft continues to work for us,” Trosper said. The large amount of data — nearly 100 megabits — transmitted from Spirit in a single relay session through NASA’s Mars Odyssey spacecraft today “is like getting an upgrade to our Internet connection.”

Scientists today reported initial impressions from using Spirit’s alpha particle X-ray spectrometer, Moessbauer spectrometer and microscopic imager on a patch of soil that was directly in front of the rover after Spirit drove off its lander Jan. 15.

“We’re starting to put together a picture of what the soil at this particular place in Gusev Crater is like. There are some puzzles and there are surprises,” said Dr. Steve Squyres of Cornell University, Ithaca, N.Y., principal investigator for the suite of instruments on Spirit and on Spirit’s twin, Opportunity.

One unexpected finding was the Moessbauer spectrometer’s detection of a mineral called olivine, which does not survive weathering well. This spectrometer identifies different types of iron-containing minerals; scientists believe many of the minerals on Mars contain iron. “This soil contains a mixture of minerals, and each mineral has its own distinctive Moessbauer pattern, like a fingerprint,” said Dr. Goestar Klingelhoefer of Johannes Gutenberg University, Mainz, Germany, lead scientist for this instrument.

The lack of weathering suggested by the presence of olivine might be evidence that the soil particles are finely ground volcanic material, Squyres said. Another possible explanation is that the soil layer where the measurements were taken is extremely thin, and the olivine is actually in a rock under the soil.

Scientists were also surprised by how little the soil was disturbed when Spirit’s robotic arm pressed the Moessbauer spectrometer’s contact plate directly onto the patch being examined. Microscopic images from before and after that pressing showed almost no change. “I thought it would scrunch down the soil particles,” Squyres said. “Nothing collapsed. What is holding these grains together?”

Information from another instrument on the arm, an alpha particle X- ray spectrometer, may point to an answer. This instrument “measures X-ray radiation emitted by Mars samples, and from this data we can derive the elemental composition of martian soils and rocks,” said Dr. Johannes Brueckner, rover science team member from the Max Planck Institute for Chemistry, Mainz, Germany. The instrument found the most prevalent elements in the soil patch were silicon and iron. It also found significant levels of chlorine and sulfur, characteristic of soils at previous martian landing sites but unlike soil composition on Earth.

Squyres said, “There may be sulfates and chlorides binding the little particles together.” Those types of salts could be left behind by evaporating water, or could come from volcanic eruptions, he said. The soil may not have even originated anywhere near Spirit’s landing site, because Mars has dust storms that redistribute fine particles around the planet. The next target for use of the rover’s full set of instruments is a rock, which is more likely to have originated nearby.

Spirit landed in the Connecticut-sized Gusev Crater on Jan. 3 (EST and PST; Jan. 4 Universal Time). In coming weeks and months, according to plans, it will examine rocks and soil for clues about whether the past environment there was ever watery and possibly suitable to sustaining life. Spirit’s twin Mars Exploration Rover, Opportunity, will reach Mars on Jan. 25 (EST and Universal Time; 9:05 p.m., Jan. 24, PST) to begin a similar examination of a site on the opposite side of the planet.

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, D.C. Images and additional information about the project are available from JPL at http://marsrovers.jpl.nasa.gov and from Cornell University, Ithaca, N.Y., at http://athena.cornell.edu .

Original Source: NASA/JPL News Release

Latest Status on the Shuttle’s Return to Flight

Image credit: NASA

It looks like NASA is still a long way from getting the space shuttles ready to fly again, according to the interim report released today by the Return to Flight task group. Although NASA is addressing all 29 issues suggested by the recommendations of the Columbia Accident Investigation Board, the progress is reported as “uneven”. So far, none of the tasks have been completed. NASA is currently targeting September 12 for the date of the first shuttle launch after the Columbia disaster, but many experts think that date could be pushed back even further.

The Stafford-Covey Return to Flight Task Group will issue an interim report Tuesday, Jan. 20. The group is making an independent assessment of NASA’s implementation of the Columbia Accident Investigation Board Space Shuttle return to flight recommendations.

http://returntoflight.org

Co-Chairman Richard Covey will be available to answer questions from the news media at 2:30 p.m. EST, Wednesday, Jan. 21 at the Task Group office at 1740 NASA Parkway, Suite 101, Houston. A telephone bridge will be provided for media unable to attend in person. Interested media should call Shannon Bach at: 281/792-7523 no later than 11 a.m. EST. Jan. 21.

The 28-member task group is co-chaired by Covey, a former Space Shuttle Commander and retired Air Force Lieutenant General and former Apollo Mission Commander Thomas Stafford. The Task Group will continue to report results to NASA at appropriate intervals and will provide a final report to the agency approximately one month before the Space Shuttle’s return to flight.

Original Source: RTF TG News Release

Humans Will Need Robots to Go to Mars

Image credit: NASA

Before humans can take the first tentative steps onto the Martian surface, our robots will have spent many years examining the planet to let us know exactly what to expect. Spirit and Opportunity will examine the dirt to see if there’s water that can be extracted. They’ll also examine the dust to see if it contains chemicals that could be detrimental to humans if it was inhaled. Robots will also help us figure out the best location humans should go to maybe mine for subsurface reserves of water or stay protected from the solar radiation.

Around the same time when Spirit?s older sister, Sojourner, was testing rover technologies on Mars during the Pathfinder mission in 1997, Mars Exploration Rover soil scientist, Doug Ming, was ?living off the martian land,? locked away in a biosphere for 30 days, sacrificing his normal life on Earth to experience ?living? on Mars. ?We simulated how astronauts would work, eat, and conduct experiments on Mars, and we even had to recycle our own urine – create purified water from it – to survive the sparse water resources on Mars,? laughed Ming.

After 15 years of researching plant growth systems and irrigation techniques for humans to use both on the Moon and Mars, Doug Ming is currently utilizing the Spirit rover to further understand the nitty-gritty composition of the dirt on Mars. His analysis will help meet the mission goal of understanding whether Gusev Crater was ever a lake. In the long term, however, studies of soil characteristics will help future scientists develop ways to extract useful materials for their colonies and safely arrive and survive on the red planet.

Humans Need Oxygen, Water, and Shelter on Mars
?In NASA?s Advanced Life Support Program, we regenerate the air by using plants to convert carbon dioxide into oxygen in closed chambers. To live safely on Mars, which has 95% carbon dioxide in its atmosphere, we?ll have to create a lot of technology tricks like that to survive,? explained Ming. Explorers visiting Mars will have to live in habitats where the oxygen is regenerated, wear spacesuits with oxygen masks, drive radiation-proof vehicles, and grow food by adding nutrients to the ?topsoil? that currently seems unable to nourish plants. But before astronauts can do all of these activities on Mars, robots need to teach humans where and how to land, where to build, and how to survive in the harsh martian environment. ?The Mini-TES instrument on Spirit is searching for water bound in soils and rocks on Mars. Water bound up in the soil and rocks could be extracted by astronauts to use as nourishment for themselves or fuel for their machines,? said Ming.

Science instruments on Spirit’s robotic arm will provide information on the martian environment that may be helpful for future human explorers.

Dirt That Hurts
?We?re also studying the chemical composition of the soil on Mars with our M?ssbauer Spectrometer and APXS instruments, which will tell us what chemicals might be detrimental to humans if they inhale the dust. For example, trace metals could be toxic to lungs, and dust could also affect electronic devices like computers and vehicles that humans will need on Mars. We?re also concerned that dust and soil could have the potential to develop electric charges. We?re taking pictures and making ?mini-movies? of dust devils that will better help us understand dust and soil movement on Mars? said Ming.

Location, Location, Location
Where should humans land on Mars? Where does enough subsurface water ice exist that humans could drill and extract? Where does the radiation penetrate the surface the least to prevent sickness and cancer-causing exposure to humans? Where is the ground strong enough to withstand a heavy human-filled mini-apartment building with parking spots for martian cars and spaceships? How do you enter the martian atmosphere with a spaceship at least thirty times larger and heavier than any spaceship humans have ever sent to Mars?

Scientists and engineers must figure out the answers to these complicated questions through the knowledge they gain from the robots sent before humans. ?Engineers and navigators will study how hot the spacecraft heat shield got as it entered the martian atmosphere, which will help future engineers model, design, and build heat shields that will ultimately protect humans as they land on Mars,? explained Ming. The The Martian Radiation Environment Experiment on NASA?s Mars Odyssey orbiter already successfully calculated that the radiation exposure on the way to Mars is twice the amount of radiation exposure that humans encounter in low-Earth orbit. Scientists are currently taking that data to model what the radiation levels would be on the surface of Mars to help build protective materials for humans during the flight to Mars and living on Mars.

Robots Pave the Way for Humans
?First and foremost, the Mars Exploration Rover mission and every mission to Mars are scientifically exciting in the present because we instantly learn about our neighboring planet. By comparing Earth to Mars, we learn more about how to protect our home planet,? said Ming. But, everything we learn now will also help us grow and evolve as explorers at exponential levels for the future. ?Space navigators still incorporate sky charts drawn by Babylonian star gazers to send spacecraft on a perfect trajectory to Mars today. Humans going to Mars – soon or even thousands of years from now – will depend on what we learn from our current robotic missions to create the right spacesuits, habitats, and roving vehicles humans will someday drive on Mars,? said Ming. ?Robots will probably even deliver our first building materials to Mars, so when humans first land, robots will have paved the way for us in more ways than one,? said Ming.

Original Source: NASA News Release

Photo Gallery: Mars Express First Image

Here’s a 1024×768 resolution wallpaper of the amazing first photograph of Mars taken by the European Space Agency’s Mars Express spacecraft. The stereoscopic image was taken on January 14, 2004 by Mars Express when it was 275 kilometres above the Valles Marineris – a 1700 km long by 65 km wide canyon that runs across the surface of Mars.

Spirit Investigates a Nearby Rock

Image credit: NASA/JPL

NASA’s Mars Exploration Rover Spirit drove a few metres yesterday to get nice and close to a large rock nearby the landing site which scientists have dubbed “Adirondack”. Spirit will examine the rock with its microscope and two instruments that will reveal its composition. To make the drive to this rock, Spirit turned 40-degrees and then rolled 1.9 metres. Engineers are still taking “baby steps” with Spirit, since this first target took the rover 30 minutes to travel.

NASA’s Spirit rover has successfully driven to its first target on Mars, a football-sized rock that scientists have dubbed Adirondack.

The Mars Exploration Rover flight team at NASA’s Jet Propulsion Laboratory, Pasadena, Calif., plans to send commands to Spirit early Tuesday to examine Adirondack with a microscope and two instruments that reveal the composition of rocks, said JPL’s Dr. Mark Adler, Spirit mission manager. The instruments are the M?ssbauer spectrometer and the alpha particle X-ray spectrometer.

Spirit successfully rolled off the lander and onto the martian surface last Thursday. To make the drive to Adirondack, the rover turned 40 degrees in short arcs totaling 95 centimeters (3.1 feet). It then turned in place to face the target rock and drove four short moves straightforward totaling 1.9 meters (6.2 feet). The moves covered a span of 30 minutes on Sunday, though most of that was sitting still and taking pictures between moves. The total amount of time when Spirit was actually moving was about two minutes.

“These are the sorts of baby steps we’re taking,” said JPL’s Dr. Eddie Tunstel, rover mobility engineer.

“The drive was designed for two purposes, one of which was to get to the rock,” Tunstel said. “From the mobility engineers’ standpoint, this drive was geared to testing out how we do drives on this new surface.” Gathering new information such as how much the wheels slip in the martian soil will give the team confidence for more ambitious drives in future weeks and months.

“Adirondack is now about one foot (30 centimeters) in front of the front wheels,” he said.

Scientists chose Adirondack to be Spirit’s first target rock rather than another rock, called Sashimi, that would have been a shorter, straight-ahead drive. Rocks are time capsules containing evidence of the environmental conditions of the past, said Dr. Dave Des Marais, a rover science-team member from NASA Ames Research Center, Moffett Field, Calif. “We needed to decide which of these time capsules to open.”

Sashimi appears dustier than Adirondack. The dust layer could obscure good observations of the rock’s surface, which may give information about chemical changes and other weathering from environmental conditions affecting the rock since its surface was fresh. Also, Sashimi is more pitted than Adirondack. That makes it a poorer candidate for the rover’s rock abrasion tool, which scrapes away a rock’s surface for a view of the interior evidence about environmental conditions when the rock first formed. Adirondack has a “nice, flat surface” well suited to trying out the rover’s tools on their first martian rock, Des Marais said.

“The hypothesis is that this is a volcanic rock, but we’ll test that hypothesis,” he said. Spirit arrived at Mars Jan. 3 (EST and PST; Jan. 4 Universal Time) after a seven-month journey. In coming weeks and months, according to plans, it will be exploring for clues in rocks and soil to decipher whether the past environment in Gusev Crater was ever watery and possibly suitable to sustain life.

Spirit’s twin Mars Exploration Rover, Opportunity, will reach Mars on Jan. 25 (EST and Universal Time; 9:05 p.m., Jan. 24, PST) to begin a similar examination of a site on the opposite side of the planet from Gusev Crater.

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, D.C. Images and additional information about the project are available from JPL at http://marsrovers.jpl.nasa.gov and from Cornell University, Ithaca, N.Y., at http://athena.cornell.edu.

Original Source: NASA/JPL News Release