MarsNews.com
March 28th, 2013

Why a Mars Comet Impact Would be Awesome Discovery News

When Jupiter’s tides ripped Comet Shoemaker–Levy 9 to shreds, only for the icy chunks to succumb to the intense Jovian gravity, ultimately slamming into the gas giant’s atmosphere, mankind was treated to a rare cosmic spectacle (in human timescales at least). That was the first time in modern history that we saw a comet do battle with a planet… and lose.
But next year, astronomers think there’s a chance — albeit a small one — of a neighboring planet getting punched by an icy interplanetary interloper. However, this planet doesn’t have a generously thick atmosphere to soften the blow. Rather than causing bruises in a dense, molecular hydrogen atmosphere, this comet will pass through the atmosphere like it wasn’t even there and hit the planetary surface like a cosmic pile-driver, ripping into the crust.
What’s more, we’d have robotic eyes on the ground and in orbit should the worst happen.

August 15th, 2012

ESA spacecraft records crucial NASA signals from Mars ESA

ESA’s Mars Express acquired signals from NASA’s Mars Science Laboratory as it delivered the car-sized Curiosity rover onto the Red planet’s surface. ESA’s New Norcia tracking station also picked up signals directly from the NASA mission, 248 million km away at Mars.
A key step was completed today in ESA’s ongoing support to NASA’s Mars Science Laboratory (MSL) mission. Signals recorded by Mars Express during MSL’s entry and descent were successfully received at ESOC, ESA’s European Space Operations Centre, Darmstadt, Germany.
The open-loop recording of radio Doppler and signal spectrum transmitted by the NASA mission were stored on Mars Express and then downloaded to Earth.

August 15th, 2012

Mars Rover’s ‘Voice’ Captured During Nail-Biting Landing Space.com

NASA’s Mars rover Curiosity may seem like the strong, silent type, but the 1-ton robot was making a lot of noise during its harrowing Red Planet touchdown on Aug. 5.
Curiosity phoned home throughout its daring and unprecedented landing sequence that night, giving its nervous handlers step-by-step status and health updates. The European Space Agency’s Mars Express orbiter recorded some of this chatter, and now we can hear what Curiosity had to say.
Sort of. ESA scientists have processed Curiosity’s radio signals, shifting them to frequencies the human ear can hear.

February 6th, 2012

ESA’s Mars Express radar gives strong evidence for former Mars ocean ESA

ESA’s Mars Express has returned strong evidence for an ocean once covering part of Mars. Using radar, it has detected sediments reminiscent of an ocean floor within the boundaries of previously identified, ancient shorelines on Mars.
The MARSIS radar was deployed in 2005 and has been collecting data ever since. Jérémie Mouginot, Institut de Planétologie et d’Astrophysique de Grenoble (IPAG) and the University of California, Irvine, and colleagues have analysed more than two years of data and found that the northern plains are covered in low-density material.
“We interpret these as sedimentary deposits, maybe ice-rich,” says Dr Mouginot. “It is a strong new indication that there was once an ocean here.”

November 1st, 2011

Mars Express observations temporarily suspended ESA

Anomalies in the operation of the solid-state mass memory system on board Mars Express have caused science observations to be temporarily halted. A technical work-around is being investigated that will enable the resumption of a number of observations and should evolve into a long-term solution.
In mid-August, Mars Express autonomously entered safe mode, an operational mode designed to safeguard both the spacecraft itself and its instrument payload in the event of faults or errors.
The cause of entering the safe mode was a complex combination of events relating to reading from and writing to memory modules in the Solid-State Mass Memory (SSMM) system. This is used to store data acquired by the instruments and housekeeping data from the spacecraft’s subsystems, prior to its transmission to Earth, and is also used to store commands for the spacecraft that have been received from the ground stations, while awaiting execution.

September 3rd, 2011

Rare martian lake delta spotted by Mars Express ESA

ESA’s Mars Express has spotted a rare case of a crater once filled by a lake, revealed by the presence of a delta. The delta is an ancient fan-shaped deposit of dark sediments, laid down in water. It is a reminder of Mars’ past, wetter climate. The delta is in the Eberswalde crater, in the southern highlands of Mars. The 65 km-diameter crater is visible as a semi-circle on the right of the image and was formed more than 3.7 billion years ago when an asteroid hit the planet.

February 6th, 2011

Mars Express puts craters on a pedestal ESA

ESA’s Mars Express has returned new views of pedestal craters in the Red Planet’s eastern Arabia Terra.
Craters are perhaps the quintessential planetary geological feature. So much so that early planetary geologists expended a lot of effort to understand them. You could say they put craters on a pedestal. This latest image of Mars shows how the Red Planet does it in reality. Craters are the result of impacts by asteroids, comets and meteorites. In a pedestal crater, the surrounding terrain is covered by pulverised rock thrown out of the crater. This material creates a platform or pedestal around the crater often with steep cliffs, and is usually rich in volatile materials such as water and ice.

March 21st, 2010

The groovy moon ESA

Without doubt, Phobos is the grooviest moon of the Solar System. By that I mean, that it is covered with a multitude of parallel grooves.
Initially, it was thought that these markings radiated away from the largest crater on Phobos. Called Stickney, the crater has a diameter of 9 km and is the most obvious feature of the moon’s pockmarked surface. Some thought that the grooves were debris ejected across Phobos during Stickney’s creation. In other words, they were similar to the bright rays of material seen emanating from some craters on the Moon. Most thought that they were fractures in the moon, opened up by the mighty impact. But these hypotheses were based upon an incomplete picture of Phobos – literally and metaphorically.

March 17th, 2010

Bad News for Terraformers: Periodic Bursts Of Solar Radiation Destroy The Martian Atmosphere Popular Science

Unfortunately for anyone looking to terraform Mars, a new study shows that powerful waves of solar wind periodically strip the Red Planet of its atmosphere. Scientists had known for years that Mars has atmosphere troubles, but only by analyzing new data from he Mars Express spacecraft were they able to identify the special double solar waves as the specific cause.
Double solar waves are a rare phenomenon that result when the Sun emits waves of differing speeds. If a fast wave follows a slow wave, the fast wave crashes into the back of the slow one, rolling them both up into a super-charged double wave. Scientists were able to correlate Martian atmosphere loss, as measured by the the Mars Express spacecraft, with records of double radiation waves in 2007 and 2008 taken by the Advanced Composition Explorer spacecraft. According to the study, one third of Martian atmosphere loss occurs during these waves, which are only present 15 percent of the time.

March 17th, 2010

Martian Moon in Spotlight MSNBC

Fresh imagery from Europe’s Mars Express orbiter shows the Martian moon Phobos in sharp, 3-D detail. This isn’t the first time Phobos has gotten its close-up, but interest in the irregular moon is rising – in part because it’s increasingly seen as a steppingstone for Mars-bound astronauts.
Last month, NASA shifted its focus from sending humans back to the moon to a “flexible path” that includes the moons of Mars as potential destinations. The idea is that low-gravity locales such as Phobos (and Mars’ other moon, Deimos) should be easier to get to because they’re more accommodating for landing and ascent.

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