Showing posts with label Mars Orbiter. Show all posts
Showing posts with label Mars Orbiter. Show all posts

Wednesday, October 22, 2014

ISRO’s Mars Orbiter: Olympus Mons, Tharsis Bulge and Valles Marineris trio of volcanoes

Olympus Mons, Tharsis Bulge trio of volcanoes, and Valles Marineris from ISRO’s Mars Orbiter Mission

Note the clouds and south polar ice cap. 

Credit: ISRO

India's Mars Orbiter Mission (MOM) has delivered another sweet treat – a stunning view of our Solar System's largest volcano and the largest canyon.

Just days ago, MOM captured a new global image of the Red Planet dominated by Olympus Mons and Valles Marineris, which is the largest known volcano and the largest known canyon in the Solar System, respectively.

Situated right in between lies a vast volcanic plateau holding a trio of huge volcanoes comprising the Tharsis Bulge: Arsia Mons, Pavonis Mons, and Ascraeus Mons. All three are shield volcanoes.

To give an idea of its enormity, Olympus Mons stands about three times taller than Mount Everest and is about the size of Arizona.

Olympus Mons is located in Mars' western hemisphere and measures 624 kilometers (374 miles) in diameter, 25 km (16 mi) high, and is rimmed by a 6 km (4 mi) high scarp.

Valles Marineris is often called the "Grand Canyon of Mars." It spans about as wide as the entire United States.

The Indian Space Research Organization (ISRO), India's space agency which designed and developed the orbiter released the image on Oct. 17, barely two days ahead of the planet's and spacecrafts' extremely close encounter with comet Siding Spring.

Olympus Mons from Mars orbit compared to the state of Arizona. 

Credit: NASA

By the way, a relieved ISRO tweeted MOM's survival of her close shave with the once-in-a-lifetime cometary passage with gusto, soon after the swingby:
"Phew! Experience of a lifetime. Watched the #MarsComet #SidingSpring whizzing past the planet. I'm in my orbit, safe and sound."

The new global image was taken by the tri-color camera as MOM swooped around the Red Planet in a highly elliptical orbit whose nearest point to Mars (periapsis) is at 421.7 km and farthest point (apoapsis) at 76,993.6 km, according to ISRO.

To date ISRO has released four global images of the Red Planet, including a 3-D view.

Olympus Mons, the Tharsis Bulge, and Valles Marineris are near the equator.

Valles Marineris stretches over 4,000 km (2,500 mi) across the Red Planet, is as much as 600 km wide, and measures as much as 7 kilometers (4 mi) deep.

Global Mosaic of Mars Centered on Valles Marineris from NASA’s Viking 1 orbiter. 

Credit: NASA

Here's a comparison view of the region taken by NASA's Viking 1 orbiter in the 1970s.

MOM is India's first deep space voyager to explore beyond the confines of her home planet's influence and successfully arrived at the Red Planet only one month ago after the "history creating" orbital insertion maneuver on Sept. 23/24 following a ten month journey.

The $73 million MOM mission is expected to last at least six months.

ISRO’s Mars Orbiter Mission captures spectacular portrait of the Red Planet and swirling dust storms with the on-board Mars Color Camera from an altitude of 74,500 km on Sept. 28, 2014. 

Credit: ISRO

MOM's success follows closely on the heels of NASA's MAVEN orbiter which also successfully achieved orbit barely two days earlier on Sept. 21 and could last 10 years or more.

With MOM's arrival, India became the newest member of an elite club of only four entities that have launched probes that successfully investigated Mars, following the Soviet Union, the United States, and the European Space Agency (ESA).


Monday, September 29, 2014

ISRO MoM: MOM eyes the limb of Mars

ISRO’s Mars Orbiter Mission captures the limb of Mars with the Mars Colour Camera from an altitude of 8449 km soon after achieving orbit on Sept. 23/24, 2014 . 

Credit: ISRO

India's maiden interplanetary voyager, the Mars Orbiter Mission (MOM) has transmitted a breathtaking new image eyeing the limb of Mars and its atmosphere against the blackness of space.

The beautiful Martian image is only MOM's second since successfully braking into orbit during the 'history creating' insertion maneuver days ago on Sept. 23/24.

The MOM orbiter was designed and developed by the Indian Space Research Organization (ISRO),

India's space agency, which released the image on Sept 25, about a day after MOM arrived.

The limb image was taken using MOM's Mars Colour Camera (MCC) from an altitude of 8449 kilometers and shows more of an 'Orange Planet' rather than a 'Red Planet.'

"A shot of Martian atmosphere. I'm getting better at it. No pressure," tweeted ISRO at MOM's newly established twitter account after entering orbit.

The image has a spatial resolution of 439 meters and is centered around Lat: 20.01N and Lon:31.54E.

MOM's goal is to study Mars atmosphere , surface environments, morphology, and mineralogy with a 15 kg (33 lb) suite of five indigenously built science instruments.

It will also sniff for methane, a potential marker for biological activity.

"The view is nice up here," ISRO tweeted.

Sunday, September 28, 2014

India Mars Orbiter: Red Planet triumph, but at home red tape binds space firms

As India celebrated becoming the first Asian nation to reach Mars, S.M. Vaidya, head of business at conglomerate Godrej’s aerospace division that made the spacecraft’s engine and thruster components, sounded surprisingly downbeat.

The mission was, indeed, a major achievement, he said, and one of which the state-run Indian Space Research Organisation (ISRO) should be proud.

But a single trip to Mars was not enough to sustain a promising yet relatively small industry, he added, and ISRO should be doing more to foster it.

“Unless they fly more, they will not buy more from us,” Vaidya told Reuters, shortly after news broke on Wednesday that Mangalyaan, Hindi for “Mars craft”, had entered into orbit around the Red Planet about 10 months after launching.

“How many Mars missions are you going to have?”

India’s successful mission, completed on a shoestring budget of $74 million, has boosted its prestige in the global space race and, back on Earth, raised the profile of Indian companies involved in the project.

But Godrej and some other firms are frustrated at what they say is the slow execution of projects and lack of government support, which are hampering India’s efforts to compete with China and Russia as a cheaper option for launching satellites.

ISRO did not reply to questions for this article.

The Mangalyaan was built in 15 months with two-thirds of its parts manufactured by domestic firms such as Godrej & Boyce and India’s largest engineering company, Larsen & Toubro.

Prime Minister Narendra Modi has said he wants to expand India’s 50-year-old space program. The government has increased funding for space research by 50 percent to almost $1 billion this financial year.

But the program is still small, and the small number of launches limits the growth potential of private companies that supply them.

Between 2007 and 2012, ISRO accomplished about half of its planned 60 missions, government data showed. The government cited “development complexity” as the reason for the delay in some missions.

Add caption
Between 2012 and 2017 the target is 58 missions.

The agency has completed 17 missions so far, and ISRO did not say why the number remained low.

Some company executives and experts do not see that changing any time soon, with the absence of heavy rocket launchers, too few launch facilities and bureaucratic delays hampering growth.

Read the full article here

Thursday, September 25, 2014

Namira Salim, Pakistan explorer commends ISRO on Mars Orbiter success

Namira Salim, a Pakistani explorer expected to become her country's first person in space congratulated India on Thursday on reaching Mars on its maiden attempt.

India won the Asian space race to the Red Planet on Wednesday when its unmanned Mangalyaan successfully entered the Red Planet's orbit after a 10-month journey on a budget of just $74 million.

Despite having a space program since 1961 Pakistan has not yet launched a satellite into orbit.

But Namira Salim, the first Pakistani explorer to reach both poles said India's achievement had made the region proud.

"The success of the Mars Orbiter Mission (MOM), Mangalyaan, is a giant leap for South Asia," said Salim, who has booked a ticket on UK hedonist Richard Branson's Virgin Galactic space project planned for 2015.

"I commend the Indian Space Research Organisation (ISRO), and all its scientists and researchers for not only achieving this astronomical feat, but also for achieving it in the most cost-effective manner."

Pakistan has not yet officially congratulated India. The neighbours have fought three wars, two of them over the disputed territory of Kashmir.

Relations between the two countries have taken a turn for the worse after Pakistan's top envoy met Kashmiri separatist leaders in August, with India responding by calling off talks between the countries' foreign secretaries.

Wednesday, September 24, 2014

ISRO: India's Mars Orbiter successfully inserted into orbit around MARS

TV Screens show Indian Prime Minister Narendra Modi greeting Indian Space Research Organisation (ISRO) scientists and other officials after the success of Mars Orbiter Mission at their Telemetry, Tracking and Command Network complex in Bangalore, India, Wednesday, Sept. 24, 2014. 

India triumphed in its first interplanetary mission, placing a satellite into orbit around Mars on Wednesday morning and catapulting the country into an elite club of deep-space explorers. 

Credit: AP Photo/Aijaz Rahi

India triumphed in its first interplanetary mission, placing a satellite into orbit around Mars on Wednesday morning and catapulting the country into an elite club of deep-space explorers.

Scientists broke into wild cheers as the orbiter's engines completed 24 minutes of burn time to maneuver the spacecraft into its designated place around the red planet.

"We have gone beyond the boundaries of human enterprise and innovation," Prime Minister Narendra Modi said, standing alongside scientists with the Indian Space and Research Organisation (ISRO) at the command center in the southern tech hub of Bangalore.

"We have navigated our craft through a route known to very few," Modi said, congratulating the scientists and "all my fellow Indians on this historic occasion."

Scientists described the final stages of the Mars Orbiter Mission, affectionately nicknamed MOM, as flawless.

The success marks a milestone for the space program in demonstrating that it can conduct complex missions and act as a global launch pad for commercial, navigational and research satellites.

It's also a major feat for the developing country of 1.2 billion people, most of whom are poor.

At the same time, India has a robust scientific and technical educational system that has produced millions of software programmers, engineers and doctors, propelling many into the middle class.

Getting a spaceship successfully into orbit around Mars is no easy task. More than half the world's previous attempts, 23 out of 41 missions, have failed, including the Beagle-2 from the UK and Nozomi by Japan in 1999.

Indian Space Research Organization scientists and other officials cheer as they celebrate the success of Mars Orbiter Mission at their Telemetry, Tracking and Command Network complex in Bangalore, India, Wednesday, Sept. 24, 2014. 

Credit: AP Photo/Aijaz Rahi

The United States had its first success with a 1964 flyby by a spacecraft called Mariner 4, returning 21 images of the surface of the planet.

The former Soviet Union MARS-3 reached the planet in 1971, and the European Space Agency Mars Express in 2003, still operating successfully around Mars.

The U.S. space agency NASA congratulated India in a Twitter message welcoming MOM to studying the red planet.

On Sunday, NASA achieved its own success in placing its Mars Atmosphere and Volatile Evolution mission (Maven), in position.

The U.S. has two more satellites circling the planet at the moment, as well as two rovers rolling across the rocky Martian surface.

The ESA's Mars Express, launched over a decade ago, is still operating as well.

India was particularly proud that MOM was developed with homegrown technology and for a bargain price of about $75 million, a cost that Modi quipped was lower than many Hollywood film budgets.

By comparison, NASA's much larger Maven mission cost nearly 10 times as much at $671 million.

The real test of these missions will come when the scientific data is gathered and returned for examination.

In this Sept. 11, 2013, file photo, Indian engineers work on the Mars orbiter spacecraft at the satellite center of Indian Space Research Organization (ISRO) in Bangalore, India.

Credit: AP Photo/Aijaz Rahi, File

Indian scientists "designed the trajectory aspects and the interplanetary aspects," said Vipparthi Adimurthy of the Indian Institute of Space Science and Technology, who headed the team that crafted the first feasibility studies on whether India could reach Mars.

Dr Adimurthy
"Today not only has a dream come true, but we have created history for India, for ISRO, and for the world," he said.

The 1,350-kilogram (nearly 3,000-pound) orbiter will now circle the planet for at least six months, with five solar-powered instruments gathering scientific data that may shed light on Martian weather systems as well as what happened to the water that is believed to have existed once on Mars in large quantities.

The 15 kgs payloads on the Mars Orbiter Mission include:

Lyman Alpha Photometer (LAP), an absorption cell photometer that measures relative abundance of deuterium and hydrogen from Lyman-alpha emission in the Martian upper atmosphere.

Methane Sensor for Mars (MSM), designed to measure methane in the Martian atmosphere with PPB accuracy and map its sources.

Mars Exospheric Neutral Composition Analyser (MENCA), a quadruple mass spectrometer capable of analysing the neutral composition in the range of 1 to 300 amu with unit mass resolution.

Mars Colour Camera (MCC), a tri-colour camera that gives images and information about the surface features and composition of Martian surface.

Thermal Infrared Imaging Spectrometer (TIS) to measure the thermal emissions and, because it is not using visible light, this instrument can be operated both during th day and night.

Temperature and emissivity are two basic physical parameters estimated from thermal emission measurement.

Monday, April 7, 2014

Solar System: Sun, Earth and Mars Align



Mars takes the celestial stage Tuesday night (April 8) when it lines up with the Earth and our Sun, in a kind of cosmic preview to the Red Planet's closest approach to Earth during a total lunar eclipse later this month.

The alignment between Mars, the Earth and the sun is called "opposition" because Mars and the sun are opposite to each other in our sky.

Opposition and the date of closest encounter are slightly different because Earth and Mars are not in perfectly circular orbits.

Oppositions between Earth and Mars happen about every 26 months because the planets are relatively close to one another.

NASA and other agencies often take advantage of these close approaches to send spacecraft that way.

A recent example is NASA's Mars Atmosphere and Volatile Evolution probe (MAVEN), which launched in November 2013 and will arrive this September.

India's space agency, ISRO's first Mars orbiter will also arrive at the Red Planet in September after its own launch last year.

The opposition of Mars comes just seven days ahead of the planet's closest approach to Earth on the night of April 14.

The Red Planet and Earth are converging ever closer to their cosmic encounter at a rate of about 186 miles (300 kilometers) a minute, according to a NASA skywatching advisory.

On April 14, Mars and Earth will be only 57 million miles (92 million kilometers) apart. This is a bit more than half the distance between Earth and the sun, which is about 93 million miles (150 million km).

By coincidence, Mars' closest approach to Earth occurs on the same night as a total lunar eclipse.

Weather permitting, observers could see a blood-red appear to glide just south of ruddy Mars as it passes through Earth's shadow in the late-night sky.

This should make the planet easy to spot in the constellation Virgo while the moon, just a few degrees south, is in total eclipse as seen from North America.

The total lunar eclipse starts at 2 a.m. EDT (0600 GMT) on April 15. The moon will spend 78 minutes in total starting around 3 a.m.

The moon will turn a Martian-looking red during the eclipse due to light from the sun shining through the Earth's atmosphere.

Wednesday, March 12, 2014

NASA MRO: Mars orbiter safe after unplanned computer swap

This artist's concept shows NASA's Mars Reconnaissance Orbiter (MRO) mission over the red planet. 

Credit: NASA/JPL

NASA's long-lived Mars Reconnaissance Orbiter (MROput itself into a precautionary safe standby mode March 9 after an unscheduled swap from one main computer to another.

The mission's ground team has begun restoring the spacecraft to full operations.

Dan Johnston
"The spacecraft is healthy, in communication and fully powered," said MRO Manager Dan Johnston of NASA's Jet Propulsion Laboratory, Pasadena, Calif.

"We have stepped up the communication data rate, and we plan to have the spacecraft back to full operations within a few days."

MRO's science observations and its relaying of communications from NASA's two active Mars rovers have been suspended.

The rovers continue to use NASA's Mars Odyssey orbiter as a communications relay.

Entry into safe mode is the prescribed response by a spacecraft when it detects conditions outside the range of normal expectations.

MRO has experienced unplanned computer swaps triggering safe-mode entry four times previously, most recently in November 2011.

The root cause of the previous events has not been determined. The spacecraft has also experienced safe-mode entries that have not involved computer swaps.

Unlike any previous safe-mode entries experienced in this mission, the March 9 event included a swap to a redundant radio transponder on the orbiter.

While the mission resumes operations with this transponder, engineers are investigating the status of the one that is now out of service.

NASA's MRO entered orbit around Mars eight years ago, on March 10, 2006.

Since then, it has returned more data than all other past and current interplanetary missions combined. The mission met all its science goals in a two-year primary science phase.

Three extensions, the latest beginning in 2012, have added to the science returns. The longevity of the mission has given researchers tools to study seasonal and longer-term changes on the Red Planet.

Thursday, February 20, 2014

NASA Mars orbiter HiRise Image: Opportunity Rover on Murray Ridge

Credit: NASA/JPL-Caltech/Univ. of Arizona

A new image from a telescopic camera orbiting Mars shows NASA's Mars Exploration Rover Opportunity at work on "Murray Ridge," without any new impact craters nearby.

The Feb. 14 view from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter (MRO) is above.

Rover tracks from Opportunity, as well as the rover itself, are visible.

A rock, dubbed "Pinnacle Island," appeared in January 2014 next to Opportunity where it had been absent a few days earlier.

After that, researchers using HiRISE planned this observation to check the remote possibility that a fresh impact by an object from space might have excavated a crater near Opportunity and thrown this rock to its new location. No fresh impact site is seen in the image.

Meanwhile, observations by the rover solved the Pinnacle Island mystery by finding where the rock had been struck, broken and moved by a rover wheel.

Murray Ridge is part of the western rim of Endeavour Crater, an impact scar that is billions of years old and about 14 miles (22 kilometers) in diameter.

Wednesday, September 11, 2013

ISRO Mangalyaan: India to launch country's maiden mission to Mars

Indian officials have confirmed a November launch date for the country's first mission to Mars, set to launch from a spaceport in the south of the country.

"Hectic preparations are on to launch Indian Space Research Organization's (ISRO) ambitious Mars Orbiter Mission in November," U.R. Rao of the Governing Council of Physical Research Laboratory said.

The Mangalyaan Mars probe will lift off from the Indian Space Research Organization's (ISRO) launch site at Sriharikota, China's Xinhua news agency reported Sunday.

"The Mars Orbiter Mission will be sent through (sic) powerful PSLV-XL launch vehicle," Rao said.

A successful launch would make India the sixth country to initiate a mission to Mars after the United States, Russia, Europe, China and Japan.

"The unmanned mission, which will explore the existence of life and the possibility of sustaining life on Mars, will travel 299 days in space before reaching the Red Planet in September 2014," Rao said.

Visit the ISRO Mangalyaan Facebook site

Wednesday, August 7, 2013

NASA Mars Opportunity: MRO restarts hunt for habitable sites

Opportunity rover’s 1st mountain climbing goal is dead ahead in this up close view of Solander Point at Endeavour Crater. 

Opportunity will ascend the mountain looking for clues indicative of a Martian habitable environment. 

This navcam panoramic mosaic was assembled from raw images taken on Sol 3385 (Aug 2, 2013). 

Credit: NASA/JPL/Cornell/Marco Di Lorenzo/Ken Kremer (kenkremer.com)

MRO, NASA's most powerful Mars orbiter has been given the green light today (Aug. 5) to capture new high resolution spectral scans that are absolutely crucial for directing the long lived Opportunity rover's hunt for signatures of habitability atop the intriguing mountain she will soon ascend.

In a plan only recently approved by NASA, engineers are aiming the CRISM mineral mapping spectrometer aboard the Mars Reconnaissance Orbiter (MRO) circling overhead to collect high resolution survey scans of Solander Point – Opportunity's 1st mountain climbing goal along the rim of huge Endeavour Crater.

"New CRISM observations centered over Solander Point will be acquired on Aug. 5, 2013," Ray Arvidson told reporters.

Arvidson is the mission's deputy principal scientific investigator from Washington University in St. Louis, Mo. NASA's decade old rover Opportunity is about to make 'landfall' at the base of Solander Point, the Martian mountain she will scale in search of the chemical ingredients that could sustain Martian microbes.

So the new spectral data can't come back to Earth soon enough, and all this is taking place as NASA's Curiosity rover celebrates her 1st Birthday on the Red Planet. .

Currently, the science team lacks the same quality of high resolution CRISM data from Solander Point that they had at a prior stop at Cape York and that data was crucial because it allowed the rover to be precisely targeted – and thereby discover a habitable zone, Arvidson stated.

"CRISM collected lots of overlapping measurements at Cape York to sharpen the image resolution to 5 meters per pixel to find the phyllosilicate smectite [clay minerals] signatures at Matejivic Hill on Cape York."

"We don't have that at Solander Point. We only have 18 meters per pixel data. And at that resolution you can't tell if the phyllosilicate smectite [clay minerals] outcrops are present."

Today's new survey from Mars orbit will vastly improve the spectral resolution – from 18 meters per pixel down to 5 meters per pixel.

"5 meter per pixel CRISM resolution is expected in the along-track direction over Solander Point by commanding the gimbaled optical system to oversample that much," Arvidson explained.

Opportunity rover’s view from very near the foothills of Solander Point looking along the rim and vast expanse of Endeavour Crater.

Solander Point is the 1st Martian Mountain NASA’s Opportunity will climb and the rovers next destination.

Solander Point may harbor clay minerals indicative of a past Martian habitable environment. This navcam mosaic was assembled from raw images taken on Sol 3374 (July 21, 2013).

Credit: NASA/JPL/Cornell/Marco Di Lorenzo/Ken Kremer (kenkremer.com)

The new CRISM spectral survey from Mars is essential to enable the science team to carefully study the alien, unexplored terrain in detail and locate the clay minerals and other water bearing minerals, even before the rover arrives.

Clay minerals form in neutral pH water conducive to life.

But it took some cajoling and inter team negotiations to convince everyone to move forward with the special but crucial CRISM imaging plan.

Since MRO is getting on in age – it launched in 2005 – NASA and the spacecraft managers have to carefully consider special requests such as this one which involves slewing the MRO spacecraft instruments and therefore entails some health risks to the vehicle.

"CRISM has been operating at Mars since 2006 and sometimes the optics on a gimble have actuators that get stuck a little bit and don't sweep as fully as planned."

Nevertheless, Arvidson told me a few weeks ago he was hopeful to get approval.

Wednesday, July 24, 2013

View From Mars Orbiter (MRO) Showing Curiosity Rover at 'Shaler'

NASA's Mars Science Laboratory rover Curiosity appears as a bluish dot near the lower right corner of this enhanced-color view from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter.

The rover's tracks are visible extending from the landing site, "Bradbury Landing," in the left half of the scene.

Two bright, relatively blue spots surrounded by darker patches are where the Mars Science Laboratory spacecraft's landing jets cleared away reddish surface dust at the landing site.

North is toward the top. For scale, the two parallel lines of the wheel tracks are about 10 feet (3 meters) apart.

HiRISE shot this image on June 27, 2013, when Curiosity was at an outcrop called "Shaler" in the "Glenelg" area of Gale Crater. Subsequently the rover drove away from Glenelg toward the southwest.

When HiRISE captured this view, the Mars Reconnaissance Orbiter was rolled for an eastward-looking angle rather than straight downward.

The afternoon sun illuminated the scene from the western sky, so the lighting was nearly behind the camera. Specifically, the angle from sun to orbiter to rover was just 5.47 degrees. This geometry hides shadows and reveals subtle colour variations.

The image is one product from HiRISE observation ESP_032436_1755. Other image products from this observation are also available.

Image credit: NASA /JPL-Caltech /Univ. of Arizona

Monday, February 25, 2013

Mars Surface: Fit for human habitation?

NASA's Hubble Space Telescope snapped this shot of Mars on Aug. 26, 2003, when the Red Planet was 34.7 million miles from Earth.

The picture was taken just 11 hours before Mars made its closest approach to us in 60,000 years.

CREDIT: NASA/ESA

While Mars was likely a more hospitable place in its wetter, warmer past, the Red Planet may still be capable of supporting microbial life today, some scientists say.

Ongoing research in Mars-like places such as Antarctica and Chile's Atacama Desert shows that microbes can eke out a living in extremely cold and dry environments, several researchers stressed at "The Present-Day Habitability of Mars" conference held here at the University of California Los Angeles this month.

And not all parts of the Red Planet's surface may be arid currently — at least not all the time. Evidence is building that liquid water might flow seasonally at some Martian sites, potentially providing a haven for life as we know it.

"We certainly can't rule out the possibility that it's habitable today," said Alfred McEwen of the University of Arizona, principal investigator for the HiRise camera aboard NASA's Mars Reconnaissance Orbiter spacecraft.

Surface water on Mars
McEwen discussed some intriguing observations by HiRise, which suggest that briny water may flow down steep Martian slopes during the local spring and summer.

Sixteen such sites have been identified to date, mostly on the slopes of the huge Valles Marineris canyon complex, McEwen said.

The tracks seem to repeat seasonally as the syrupy fluids descend along weather-worn pathways.

While the brines may originate underground, Caltech's Edwin Kite noted, there is an increasing suspicion that a process known as deliquescence — in which moisture present in the atmosphere is gathered by compounds on the ground, allowing it to become a liquid — may be responsible.

Astrobiologists are keen to learn more about these brines, for not much is known about them at the moment.

"Briny water on Mars may or may not be habitable to microbes, either from Earth or from Mars," McEwen said.

Valles Marineris on Mars

Thursday, March 8, 2012

NASA MARS HiRise Image: The Serpent Dust Devil

A towering dust devil casts a serpentine shadow over the Martian surface in this image acquired by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter.

The scene is a late-spring afternoon in the Amazonis Planitia region of northern Mars.

The view covers an area about four-tenths of a mile (644 meters) across. North is toward the top.

The length of the dusty whirlwind's shadow indicates that the dust plume reaches more than half a mile (800 meters) in height. The plume is about 30 yards or meters in diameter.

A westerly breeze partway up the height of the dust devil produced a delicate arc in the plume. The image was taken during the time of Martian year when the planet is farthest from the sun.

Just as on Earth, winds on Mars are powered by solar heating. Exposure to the sun's rays declines during this season, yet even now, dust devils act relentlessly to clean the surface of freshly deposited dust, a little at a time.

This view is one product from an observation made by HiRISE on Feb. 16, 2012, at 35.8 degrees north latitude, 207 degrees east longitude.

Other image products from the same observation are at http://www.uahirise.org/ESP_026051_2160 .

Thursday, March 1, 2012

NASA MARS Orbiter: Tenth Anniversary Image from THEMIS

The Thermal Emission Imaging System (THEMIS) camera on NASA's Mars Odyssey spacecraft has completed an unprecedented full decade of observing Mars from orbit.

THEMIS captured this image on Feb. 19, 2012, 10 years to the day after the camera recorded its first view of Mars.

This image covers an area 11 by 32 miles (19 by 52 kilometers) in the Nepenthes Mensae region north of the Martian equator.

The view depicts a knobby landscape where the southern highlands are breaking up as the terrain descends into the northern lowlands.

Odyssey, launched in 2001, has worked at Mars longer than any mission in history.

NASA's Jet Propulsion Laboratory, Pasadena, Calif., manages the Mars Odyssey mission for NASA's Science Mission Directorate, Washington.

THEMIS was developed by Arizona State University, Tempe, in collaboration with Raytheon Santa Barbara Remote Sensing.

For more information about Mars Odyssey, visit mars.jpl.nasa.gov/odyssey . For more about THEMIS, see themis.asu.edu/ .

Image credit: NASA/JPL-Caltech/ASU

Tuesday, December 13, 2011

NASA's Mars Rover Finds Mineral Traces Left by Water

NASA revealed that the Opportunity rover, which has been prowling the plains and craters of the Red Planet since 2004, had discovered, well, Martian patio tiles or rectangular formations that looked awfully similar.

Rectangles in the Martian soil are nothing to do with life, the rectangles are one more clue that biology might indeed be or at least have been possible on Mars.

Opportunity and its rover twin Spirit have spent much of their years of exploration looking for clues to water on Mars, which, of course, is a sine qua non for life as we know it.

The evidence has piled up, both in terms of topographic scars that could only have been left by flowing, pooling or upwelling water; and the presence of sulfates, hydroxides and other materials that form in the presence of water. Last August, the Mars Reconnaissance Orbiter (MRO) beamed back images suggesting that liquid water may flow seasonally on Mars even today.

"Since the MRO arrived at Mars, our overarching theme has been 'follow the water,'" said mission scientist Mike Meyer at the time of the announcement. "Now we may be catching Mars in the act."

Wednesday, August 24, 2011

NASA MARS: Daybreak at Gale Crater - Rover Curiosity's Landing Site

This computer-generated images depicts part of Mars at the boundary between darkness and daylight, with an area including Gale Crater, beginning to catch morning light.

Northward is to the left. Gale is the crater with a mound inside it near the center of the image. NASA selected Gale Crater as the landing site for Curiosity, the Mars Science Laboratory.

The mission's rover will be placed on the ground in a northern portion of Gale crater in August 2012.

Gale Crater is 96 miles (154 kilometers) in diameter and holds a layered mountain rising about 3 miles (5 kilometers) above the crater floor. The intended landing site is at 4.5 degrees south latitude, 137.4 degrees east longitude.

This view was created using three-dimensional information from the Mars Orbiter Laser Altimeter, which flew on NASA's Mars Global Surveyor orbiter. The vertical dimension is not exaggerated. Colour information is based on general Mars color characteristics.

Image Credit: NASA/JPL-Caltech

Thursday, August 4, 2011

NASA MARS Orbiter: Ice, Salt and Warm-Season Flows on Mars

This map of Mars shows relative locations of three types of findings related to salt or frozen water, plus a new type of finding that may be related to both salt and water.

Coloring of the map is coded to concentrations of shallow subsurface water ice found by the Gamma Ray Spectrometer - Neutron Spectrometer on NASA's Mars Odyssey orbiter. Blue, at high latitudes north and south, indicates higher concentrations of water ice (deduced from detection of hydrogen); orange designates lowest concentrations. Some hydrogen, possibly in the form of bound water, is close to the surface even at middle latitudes.

The white squares in the northern hemisphere mark locations of small fresh impact craters that exposed water ice close to the surface and validated the neutron spectrometer data. Observations of these fresh craters were made by the Context Camera and the High Resolution Imaging Science Experiment camera on NASA's Mars Reconnaissance Orbiter.

The red squares mark locations of putative deposits of chlorite based on observations by the Thermal Emission Imaging System on Mars Odyssey. Such salt deposits could have resulted from evaporation of salty water.

The blue squares mark locations of a type of feature reported in August 2011 based on sequences of observations by the High Resolution Imaging Science Experiment. The observations show relatively dark features appearing and incrementally growing down slopes during warm seasons. Researchers hypothesize that these features may result from action of briny water.

Other imagery related to these new findings from the Mars Reconnaissance Orbiter is at http://www.nasa.gov/mission_pages/MRO/multimedia/gallery/gallery-index.html .

Image Credit: NASA/JPL-Caltech/ASU/UA/LANL/MSSS

NASA MARS Orbiter: Oblique View of Warm Season Flows in Newton Crater

An image combining orbital imagery with 3-D modeling shows flows that appear in spring and summer on a slope inside Mars' Newton crater.

Sequences of observations recording the seasonal changes at this site and a few others with similar flows might be evidence of salty liquid water active on Mars today.

Evidence for that possible interpretation is presented in a report by McEwen et al. in the Aug. 5, 2011, edition of Science.

This image has been reprojected to show a view of a slope as it would be seen from a helicopter inside the crater, with a synthetic Mars-like sky.

The source observation was made May 30, 2011, by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. Color has been enhanced. The season was summer at the location, 41.6 degrees south latitude, 202.3 degrees east longitude.

The flow features are narrow (one-half to five yards or meters wide), relatively dark markings on steep (25 to 40 degree) slopes at several southern hemisphere locations. Repeat imaging by HiRISE shows the features appear and incrementally grow during warm seasons and fade in cold seasons.


Other imagery related to these new findings from the Mars Reconnaissance Orbiter is at http://www.nasa.gov/mission_pages/MRO/multimedia/gallery/gallery-index.html .

Image credit: NASA/JPL-Caltech/Univ. of Arizona

NASA MARS Orbiter: Warm-Season Flows on Slope in Newton Crater

This series of images shows warm-season features that might be evidence of salty liquid water active on Mars today.

Evidence for that possible interpretation is presented in a report by McEwen et al. in the Aug. 5, 2011, edition of Science.

These images come from observations of Newton crater, at 41.6 degrees south latitude, 202.3 degrees east longitude, by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter.

In time, the series spans from early spring of one Mars year to mid-summer of the following year. The images have been adjusted to correct those taken from oblique angles to show how the scene would look from directly overhead.

The features that extend down the slope during warm seasons are called recurring slope lineae. They are narrow (one-half to five yards or meters wide), relatively dark markings on steep (25 to 40 degree) slopes at several southern hemisphere locations.

Repeat imaging by HiRISE shows the features appear and incrementally grow during warm seasons and fade in cold seasons.

They extend downslope from bedrock outcrops, often associated with small channels, and hundreds of them form in rare locations.

They appear and lengthen in the southern spring and summer from 48 degrees to 32 degrees south latitudes favoring equator-facing slopes. These times and places have peak surface temperatures from about 10 degrees below zero Fahrenheit to 80 degree above zero Fahrenheit (about 250 to 300 Kelvin).

Liquid brines near the surface might explain this activity, but the exact mechanism and source of the water are not understood.

The series is timed to dwell two seconds on the first and last frames and one second on intermediate frames, though network or computer performance may cause this to vary.

Other imagery related to these new findings from the Mars Reconnaissance Orbiter is at http://www.nasa.gov/mission_pages/MRO/multimedia/gallery/gallery-index.html .

The legend on each image gives the exact HiRISE observation number (e.g. ESP_011428_1380 for the first image) so that additional image products from the observation and information about the observation can be found on the HiRISE website (e.g., the first image of the series is from ESP_011428_1380, at http://hirise.lpl.arizona.edu/ESP_011428_1380).



Image credit: NASA/JPL-Caltech/Univ. of Arizona

Monday, April 25, 2011

NASA MARS Recon Orbiter: Big Changes in Mars' Atmosphere

NASA's Mars Reconnaissance Orbiter has discovered the total amount of atmosphere on Mars changes dramatically as the tilt of the planet's axis varies.

This process can affect the stability of liquid water, if it exists on the Martian surface, and increase the frequency and severity of Martian dust storms.

Researchers using the orbiter's ground-penetrating radar identified a large, buried deposit of frozen carbon dioxide, or dry ice, at the Red Planet's south pole.

The scientists suspect that much of this carbon dioxide enters the planet's atmosphere and swells the atmosphere's mass when Mars' tilt increases. The findings are published in this week's issue of the journal Science.

The newly found deposit has a volume similar to Lake Superior's nearly 3,000 cubic miles (about 12,000 cubic kilometers). The deposit holds up to 80 percent as much carbon dioxide as today's Martian atmosphere.

Collapse pits caused by dry ice sublimation and other clues suggest the deposit is in a dissipating phase, adding gas to the atmosphere each year. Mars' atmosphere is about 95 percent carbon dioxide, in contrast to Earth's much thicker atmosphere, which is less than .04 percent carbon dioxide.

"We already knew there is a small perennial cap of carbon-dioxide ice on top of the water ice there, but this buried deposit has about 30 times more dry ice than previously estimated," said Roger Phillips of Southwest Research Institute in Boulder, Colo. Phillips is deputy team leader for the Mars Reconnaissance Orbiter's Shallow Radar instrument and lead author of the report.

"We identified the deposit as dry ice by determining the radar signature fit the radio-wave transmission characteristics of frozen carbon dioxide far better than the characteristics of frozen water," said Roberto Seu of Sapienza University of Rome, team leader for the Shallow Radar and a co-author of the new report. Additional evidence came from correlating the deposit to visible sublimation features typical of dry ice.

"When you include this buried deposit, Martian carbon dioxide right now is roughly half frozen and half in the atmosphere, but at other times it can be nearly all frozen or nearly all in the atmosphere," Phillips said.

An occasional increase in the atmosphere would strengthen winds, lofting more dust and leading to more frequent and more intense dust storms. Another result is an expanded area on the planet's surface where liquid water could persist without boiling. Modeling based on known variation in the tilt of Mars' axis suggests several-fold changes in the total mass of the planet's atmosphere can happen on time frames of 100,000 years or less.

The changes in atmospheric density caused by the carbon-dioxide increase also would amplify some effects of the changes caused by the tilt.

Researchers plugged the mass of the buried carbon-dioxide deposit into climate models for the period when Mars' tilt and orbital properties maximize the amount of summer sunshine hitting the south pole. They found at such times, global, year-round average air pressure is approximately 75 percent greater than the current level.

"A tilted Mars with a thicker carbon-dioxide atmosphere causes a greenhouse effect that tries to warm the Martian surface, while thicker and longer-lived polar ice caps try to cool it," said co-author Robert Haberle, a planetary scientist at NASA's Ames Research Center in Moffett Field, Calif. "Our simulations show the polar caps cool more than the greenhouse warms.