The DLR institute established at Berlin-Adlershof was founded in 1992 and is involved in all major European missions of planetary research venturing out into our Solar System.
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The European Space Agency's (ESA) Venus Express mission has provided a great amount of data from the surface and atmosphere of Earth's inner twin planet. Among these observations was the mapping of the southern hemisphere of Venus in the near infrared spectral range using the VIRTIS (Visible and InfraRed Thermal Imaging Spectrometer) instrument.
Since 14 March 2016, the Trace Gas Orbiter (TGO) and the Schiaparelli lander have been flying together towards Mars for the ESA ExoMars mission. On 16 October 2016, the journey to the Martian surface begins for the lander, while the TGO will enter orbit around Mars.
These images, acquired by the High Resolution Stereo Camera (HRSC) operated by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) on board the European Mars Express spacecraft, show structures that formed as a result of glacial activity in the Colles Nili region.
On 30 September 2016 at 13:19 CEST, the final signal from the Rosetta orbiter was received back on Earth. The ESA mission ended when the spacecraft touched down on Comet 67P/Churyumov-Gerasimenko. The international team of scientists had already said their farewells to the Philae lander back in February 2016, when its prolonged radio silence indicated that it would no longer report back to the team in the control centre at the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR).