A team led by Professor Kenneth Mease will develop an algorithm to control a Mars lander's flight during the hypersonic entry phase and deliver the vehicle with pinpoint accuracy. The first demonstration of pinpoint landing is under consideration for a Mars mission in 2011.
Researchers at the University of Washington are developing a new propulsion concept that could dramatically cut the time needed for astronauts to travel to and from Mars. The mag-beam concept uses a space-based station to generate a stream of magnetized ions that propel a spacecraft through the solar system, potentially reducing round ...
Scientists found evidence of jarosite and gypsum on Mars' surface, indicating that liquid water likely existed in the past. The discovery suggests a brief geological window where conditions may have been hospitable for life.
Researchers found that different magnesium sulfate salts contain varying amounts of water, which could provide insight into Mars' history. The proportion and distribution of these salts may hold clues about past climate changes and water presence on the planet.
An international team of scientists has successfully tested an integrated Mars life-detection strategy, finding evidence of even a single-cell organism. The experiment used specially adapted instruments to identify organic and mineralogical markers in Arctic hot springs, which resemble Martian environments.
Researchers found a large body of water, comparable to the Baltic Sea or all Great Lakes combined, near the NASA Opportunity rover's landing site on Mars. The study suggests that the ancient sea was present for an extended period and must have been deep enough to build up sediments roughly one-third of a mile deep.
Despite searching for large lakes and seas, no conclusive evidence of water has been found. However, the Spirit rover did uncover small amounts of water in rock samples. The team also took spectacular photographs of Martian landscapes, including 3-D images that provided valuable insights.
Researchers confirm albedo changes in Martian soil, correlating with changes seen from Mars orbiters, providing ground-truth information. The findings indicate important variations in mineral and dust composition.
Researchers suggest Martian and Utah rocks formed underground when minerals precipitated from flowing groundwater, providing clues to the origin of 'blueberries' discovered on Mars. The study also sheds light on the search for evidence of past life on Mars.
Researchers will examine submicroscopic bubbles in Martian meteorites to search for evidence of water on Mars. They will also use a new instrument to predict future volcanic eruptions by analyzing fluid inclusions in rocks.
Three undergraduate students at the University of Alberta designed a space suit for Mars that balances radiation protection, mobility, and cost efficiency. The suit incorporates new polymeric materials, such as Demron, and innovative designs like ball bearings and compression rings to address the unique challenges of Martian exploration.
A team of scientists led by UC Berkeley's Richard Mathies is developing the Mars Organic Analyzer to test for amino acid handedness, a crucial characteristic of life-based amino acids. The instrument aims to provide absolute proof of life on Mars, as detecting left-handed or right-handed amino acids could indicate biological activity.
Researchers found that heating and cooling alone can create spiral patterns on Mars, contrary to previous theories. The model suggests that differential melting and refreezing cause the spirals' unique shape and spacing.
A joint research effort discovered Mars-like soils in Chile's Atacama Desert, which are depleted in organic materials and would have been missed by NASA's Viking missions. The team found that the conditions in this environment represent a limit for microbial life on Earth.
Dr. Squyres and over 40 team members will undergo a sleep study to adapt to Mars' 24-hour day/night cycle during the two-rover mission. The team will work six-sol weeks with varying weekend lengths, aiming to mitigate 'Martian jet lag'.
The PERs will allow museum visitors to search for organo-fluorescent evidence of life in a Martian terrain, mimicking the role of NASA's Mars Exploration Rovers. The robots are powered by Intel technology and can move at 1.6 inches per second, providing an interactive experience for visitors.
The Mars landers will display images of EarthDials from around the world, showcasing differences in shadows between hemispheres and equator. The project aims to educate about timekeeping and our planet's unique features.
Ripple features on Mars have been found to be almost 20 feet high, much taller than those on Earth, with the exact heights and grain sizes still unknown. The dimensions of these Martian ripples are likely influenced by lower gravity and may reveal insights into local and regional weather patterns.
The USGS has discovered a vast area of green mineral olivine on Mars, suggesting that the planet's surface has been dry and free from recent water activity. This finding is significant as it implies that the Martian surface has not experienced significant chemical weathering due to liquid water.
Researchers at Lawrence Berkeley National Laboratory and NASA have developed a process to convert inedible wheat grass into activated carbon, absorbing nitrogen oxides and producing fertilizer. This technology could support a crew of six astronauts on a three-year Mars mission by recycling waste and conserving materials.
Researchers analyzed TES observations and found trace amounts of carbonate minerals in Martian dust, indicating a thin atmosphere interacting with dust. The discovery contradicts the idea of past oceans on Mars and suggests a climate history dominated by ice and frozen water.
New research suggests that hot spots on Mars could be the key to finding signs of water and life on the planet. The study, led by Dr Hoffman, compares similarities between Antarctica's Mt Erebus ice towers and potential Martian structures, proposing a new focus for the search.
A NASA scientist has discovered a new species of organism that thrives in a salty, alkaline environment without oxygen. The Spirochaeta americana microorganism can survive in conditions inhospitable to humans and is of great interest to astrobiologists studying the possibility of life on Mars.
Researchers have discovered kilometer-wide stretches of bare bedrock, exposing strong environmental forces that scour the surface. The data also reveals common accumulations of loose rock on martian hillsides, indicating recent weathering processes. These findings suggest a dynamic Mars with active geological features.
The MARSIS project aims to probe several miles beneath Mars' surface and study the ionosphere. Researchers hope to detect signs of liquid water, which may have shaped the planet's deep canyons.
Scientists have found that bacterial endospores can survive in a simulated Martian environment, raising concerns about future space missions. The discovery highlights the potential for Earth-borne endospores to hitch a ride to Mars and compromise efforts to detect life on the planet.
A team from Los Alamos National Laboratory has mapped the hydrogen distribution on Mars, indicating significant water reserves near the surface and subsurface. The findings suggest that Mars could support future human exploration with its extensive water resources.
Researchers discover new life forms living in extreme environments, such as gold mines and volcanic rocks, providing clues to the origins of life on Earth and potentially on Mars. These microorganisms may be using nuclear energy or toxic waste as fuel, shedding light on the diversity of possible fuel sources for life.
Early Mars research suggests that the planet may have been too cold to melt water, contradicting Dr. James F. Kasting's theory of a greenhouse effect. However, Kasting proposes that methane-producing bacteria could have warmed the planet, allowing for the formation of features like Nanedi Vallis.
Geologist Dr Nick Hoffman claims that recent gully development on Mars was caused by frozen carbon dioxide, contradicting the majority scientific opinion that it was carved by liquid water. This raises concerns about the possibility of life existing on Mars.
Researchers challenge the long-held idea of a warm, wet Mars with evidence from large asteroid and comet impacts. These events created short-lived but intense periods of rain and flooding on the planet's surface, leading to the formation of rivers and valleys.
Case Western Reserve University's ANSMET team will conduct six-week Antarctic expedition to recover rare Martian meteorites, expanding planetary science research capabilities.
Herb Frey and his daughter Erin have discovered subtle quasi-circular depressions, or QCDs, that suggest a Pre-Noachian period on Mars. These findings indicate that the oldest visible Martian crust is not the oldest, but rather part of an even earlier geological time period.
The University of Houston is developing blueprints for Texas spaceports and a Mars colony, aiming to provide a less expensive alternative to government-run facilities. The program will consider factors such as propulsion systems, habitat design, and radiation protection, with the goal of creating a sustainable human presence on Mars.
Researchers used a climate change model on Earth to analyze Mars' polar regions, finding a correlation between the layers of ice and dust and changes in climate. The study suggests that Mars' climate changes can be explained by orbital theory, similar to Earth.
A new undersea data network, MARS, will be deployed in Monterey Bay to provide real-time monitoring of ocean conditions. The network will support a variety of research devices and supply power to instruments, enabling continuous and long-term data collection.
Researchers conducted a high-tech simulation to test the Mars Exploration Rover mission, which will arrive on Mars in early 2004. The test aimed to understand the nature and accumulation patterns of Mars' signature red dust, crucial for ensuring astronaut safety.
The proposed system uses autonomous spaceships to transport crews between Earth and Mars, enabling frequent 5-month trips. The design architecture includes Astrotels and Taxis, which will facilitate sustainable Mars habitation and exploration.
MERBoards will provide a new tool to support collaborative processes in Mars Surface Operations, enhancing mission operations with interactive displays and annotation capabilities.
The Marsquake sensors will detect weight shuddering caused by liquid water beneath the Martian equator, pinpointing each quake's location. This new method will help scientists find life on Mars and shed light on the planet's internal structure.
A recent study by Dr. Lidija Siller from Newcastle University suggests that water might be trapped beneath the surface of Mars' south polar ice cap, a key factor in the formation of life on the planet. The research involves studying photochemical reactions in ice and has potential implications for the detection of life on Mars.
Researchers found that volcanic regions on Mars' Hellas basin were eroded by liquid carbon dioxide due to explosive eruptions. The 'magmatic erosion model' suggests catastrophic erosion occurred when molten rock rose to the surface, causing debris flow and shaping features.
Scientists found a unique microbial community in Idaho's Beverhead Mountains that thrives without sunlight, using hydrogen gas from deep Earth as an energy source. This discovery mirrors Martian subsurface chemistry and has implications for searching for life on Mars.
Recent Martian gullies and debris flows likely resulted from the melting of near-surface ground ice due to warming temperatures. The orientation of these features closely matches the predicted latitudinal distribution of warmest near-surface temperatures at high obliquity.
Researchers found dramatic erosion of frosty layers on Mars' south pole, suggesting global climate change. The Martian snow is dense and ice-like, and its seasonal cycle affects the planet's long-term climate and atmosphere.
Researchers analyzed topographic maps and meteorites to determine that water circulated in the upper part of Mars' crust within the last billion years. This finding suggests that water may still be present near the surface, with evidence of recent gullies forming in high-latitude regions.
A recent discovery of buried impact craters on Mars indicates that the planet's northern lowlands formed very early in its history, possibly as a result of a shallow ocean. This finding provides crucial insights into the origin of Mars' crustal dichotomy and challenges traditional theories about the planet's geological evolution.
Recent studies on Mars' Elysium and Amazonis Planitia regions reveal regionally extensive lava eruptions from the same vent system as water. The findings suggest that these volcanic and hydrologic events are both young and related in origins, potentially indicating ongoing volcanic activity.
The Mars Odyssey spacecraft has entered into orbit around Mars, providing a key communications link for the Mars Exploration Rover (MER) mission. The two Rovers will be able to upload data on mineral and element composition of rocks and soils to a state-of-the-art communications package.
NASA's Mars Global Surveyor and Hubble Space Telescope provide a unique view of the largest global dust storm on Mars in several decades. The storm, which has engulfed the entire planet for three months, raises questions about Mars' thin atmosphere and climate change.
A USC neuroscientist re-analyzed data from the Viking landers, finding a distinct biological rhythm in the soil that suggests the presence of life. The signal has a precise circadian rhythm of 24.66 hours, entrained to temperature fluctuations on Mars.
Researchers at Brown University have discovered direct evidence of climate change on Mars, finding that water ice was once present closer to the equator. The findings suggest that the icy region has moved from the planet's poles to nearer its equator due to climate change.
Scientists have observed a sudden shift in Mars' atmosphere, with temperatures increasing by about 30 degrees Centigrade, due to a massive dust storm. This phenomenon is similar to Earth's global warming, but much more extreme and potentially leading to a significant cooling of the planet.
Dr. Baerbel K. Lucchitta's research finds that some Martian outflow channels display similar characteristics to those on the Antarctic sea floor, carved by ice streams. The study suggests an ancient ocean may have existed in Mars' northern plains.
A new map of Mars' ionosphere reveals strong localized magnetic fields as a significant barrier to atmospheric erosion by the solar wind. The findings suggest that these crustal fields played an important role in the past evolution of Mars' atmosphere and could have protected it from being stripped away.
Researchers believe that parts of ancient Mars may have resembled a land of lakes, with layered geologic outcrops suggesting sedimentary rock deposited in horizontal layers. The discovery suggests an extremely dynamic environment on early Mars, with water likely playing a key role in shaping the planet's geology.
Researchers like Dr. Melanie Mormile are exploring the possibility of finding ancient bacteria on Mars, which could provide evidence for life on the planet. By dating salt-loving bacteria on Earth, scientists aim to confirm whether similar organisms can survive for hundreds of millions of years.
Scientists have discovered a wealth of green minerals, including olivine, on the Martian surface, indicating low levels of chemical weathering by water. This suggests that Mars has remained cold and dry for most of its geologic history, contradicting previous theories about a warm, wet past.
Scientists analyzed the magnetic field of the ALH84001 Martian meteorite using a new microscope, revealing that its interior remained cool enough to support life. The findings suggest that microbial life may have traveled from Mars to Earth via the meteorite, but do not prove it.
A team of scientists suggests that meteorites like ALH84001 could have transferred life between Mars and Earth. The analysis of the meteorite's magnetic field supports the hypothesis that meteorites can be an interplanetary delivery system capable of transferring life.