News on Mars
- Discovery of significant changes in Martian sand-dunes
- Signs of ancient flowing water on Mars
- ESAs Mars Express gravity results plot volcanic history
- Impact sites hint at life on Mars
- Pit chains may hold caverns ideal for life
- New explanation for layered deposits in Mars Grand-Canyon
- A mounting - INSIDE a crater on Mars
- Wake-up on to a dusty season on Mars
- Discovery of new kind of surface on mars
- Lakes and shorelines on mars
- Tornado on Mars
- Recent geological activity on Mars
- ESA's Mars-express find evidence of past ocean
- Surface on Mars unlikely place for life
- Mars: A thin but windy atmosphere
- Observing campain of Mars's north pole
- Landslides on Mars occur spontaniously
- Martian avalanches caused by meteor impacts
- Water on Mars: maybe martian microbes
- Mars rover finds mineral vein deposited by water
- Martian polar gullies created by CO2 fluidation
- Sand-dunes move on Mars
- Most Martian-clay is subsurface originated
- Direct measurement of Mars's past temperature
- Clusters of newly formed craters on Mars
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Mars facts

Mars: 4th planet from the Sun
Distance from Sun: 228mio km.
Diameter: 6.794km.
Surface-pressure: 0,001atm.
Atm composition: 99% CO
Temp: -100ºC to +20ºC
Moons: Phobos & Deimos
Newsletter
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Mega poster of the Mars moon Phobos
Friday, 11 February 2011 14:18
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| Solar system - Mars |
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During the last of a series of eight encounters with the martian moon Phobos, the High-Resolution Stereo Camera (HRSC) on ESA's Mars Express spacecraft acquired a detailed view of the martian satellite. German DLR has compiled an enormous 40mp image of the small moon The orbiter flew past Phobos at a distance of only 100km on 9 January 2011 and imaged the southern hemisphere of the irregularly-shaped moon. Researchers at the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) planned the image acquisitions, during which the orbiter was moving past Phobos at 2.3 kilometres per second, and processed the resulting data.
KLICK IMAGE to see full resolution Since Mars express flies in an elliptical orbit around the Red Planet, it regularly moves away from Mars and approaches Phobos, which orbits the planet at an altitude of roughly 6000km, about every five months. With data obtained during this flyby, the researchers were able to image large parts of the southern hemisphere of the moon for the first time at a resolution of 3,8m/pixel. HRSC scanned the martian moon, which is just over 20km across, with five of its nine sensors that are located sequentially in the camera. The sensors were active for a total of about a minute per sensor; Phobos was in the field of view for only 9 seconds. Klaus Dieter Matz, a researcher at the DLR Institute of Planetary Research (Institut für Planetenforschung), planned the image acquisition. To obtain the sharpest possible images given the high speed of the spacecraft during the flyby, Mars Express had to slew during the rendezvous. For the computation of this complicated manoeuvre, the researchers considered the orbit of the moon and the exact path of the Mars Express orbiter, which ESA determines from a variety of parameters. Corrections during image acquisition were not possible as control signals transmitted from ground stations on Earth would have taken 19 minutes and 47,4 seconds to reach the spacecraft, but he manoeuvre was accomplished without any problems. However, "The maximum speed at which ESA could turn Mars Express during the flyby was 0,15 degrees/second. For ideal images, the spacecraft must be rotated at 0,26 degrees per second during the high-speed flyby," explained Matz. The effects caused by the limited slew rate were corrected later during processing Source: DLR |




