Mars Express is a Mars exploration mission of the European Space Agency and the first planetary mission attempted by the agency. "Express" originally referred to the spacecraft's relatively short interplanetary voyage, a result of being launched when the orbits of Earth and Mars brought them closer than ever before in recorded history (about 60,000 years). However "express" also describes the speed and efficiency with which the spacecraft was designed and built.
Mars Express consists of two parts, the Mars Express Orbiter and the Beagle 2, a lander designed to perform exobiology and geochemistry research. It was hoped the lander would shed light on whether Mars had once supported or possibly currently supports living organisms. Many of the instruments on the orbiter, including the camera systems and some spectrometers, are duplicates of those lost in the failed launch of the Russian Mars 96 mission in 1996 (European countries had provided much of the instrumentation and financing for that unsuccessful mission). The basic design of Mars Express is based on ESA's Rosetta mission, on which considerable money was spent developing the spacecraft. The same design will also be used for the Venus Express mission in order to increase reliability and reduce development cost and time.
In the meantime, the Mars Express Orbiter has started its science phase and is performing excellently at the start of a two year survey of Mars.
In 2005, ESA scientists reported that the OMEGA (Visible and Infrared Mineralogical Mapping Spectrometer) instrument data indicates the presence of hydrated sulphates, silicates and various rock-forming minerals.
The Fourier spectrometer has detected methane in the atmosphere coming from areas near the equator with subsurface ice, a very important discovery indicating either some form of active vulcanism or subsurface microorganisms.
On May 4 2005, Mars Express deployed the first of its two 20-metre-long radar booms for its MARSIS (Mars Advanced Radar for Subsurface and Ionosphere Sounding) experiment. At first the boom didn't lock fully into place; however, exposing it to sunlight for a few minutes on May 10 fixed the glitch. The second 20 m boom was successfully deployed on June 14. Both 20 m booms were needed to create a 40 m dipole antenna for MARSIS to work; a less crucial 7-meter-long monopole antenna was deployed on June 17. The radar booms were originally scheduled to be deployed in April 2004, but this was delayed out of fear that the deployment could damage the spacecraft through a whiplash effect. Due to the delay it was decided to split the four week commissioning phase in two parts, with two weeks running up to July 4 and another two weeks in December 2005. Nominal science observations began during July 2005. (For more info, see *, and [http://www.esa.int/esaCP/SEMEV82DU8E_index_0.html ESA press release.)
In November 2005, with just a few weeks of measurements having been taken thus far, ESA released data from MARSIS which included buried impact craters, and hints of the presence of underground water-ice.
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