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HRSC: High/Super Resolution Stereo Imager
/ en / projekte / mars-express / hrsc /

HRSC: High/Super Resolution Stereo Imager

for the Mars Express Mission

HRSC-Instrument


Mars Express is the name of the 2003 ESA mission to Mars. It consists of an orbiter and a small lander, Beagle-2. One of the primary instruments on the orbiter will be the High/Super Resolution Stereo Imager (HRSC).

> Science objectives of HRSC
> HRSC instrument description
> MPS involvement
contact: Markiewicz
> Related links
> Mars-Express publications by MPS members
> HRSC publications by MPS members
> Group Homepage

Science objectives of HRSC

The scientific objectives of the HRSC as formulated by 36 scientists from 7 different countries are:

  • characterization of the surface structure and morphology at high resolution
  • characterization of the surface topography at high spatial and vertical resolution
  • investigation of the geologic evolution of the Martian surface and determination of the sequence of events
  • terrain classification at high spatial resolution by means of colour imaging
  • acquisition of data of the structure of the Martian crust and the elastic response of the lithosphere
  • refinement of the geodetic control network and the Martian cartographic basis
  • characterization of the evolution of volcanism and its influence on the Martian environment
  • information on the past climate, its variability and the role of water through Martian history
  • analysis of surface-atmosphere interactions (variable features, frosts) and eolian processes and phenomena
  • analysis of atmospheric phenomena (dust devils, cloud topography, aerosol content)
  • characterization of past, present, and future landing sites and support for lander experiments
  • support for exobiological studies
  • observation of Phobos and Deimos
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HRSC instrument description

The HRSC will take images of the surface and atmosphere of Mars in full colour, 3D and at high resolution. Its greatest strength, however, is its unprecedented pointing accuracy, which it achieves by combining images at two different resolutions. This makes it particularly useful for, among other things, assessing potential landing sites for future missions to Mars. The camera, which weighs 21.2 kg will take 3D colour pictures of the Martian surface and of atmospheric phenomena, such as cloud cover and dust storms, at a resolution of 10-30 m. At the same time, a super resolution channel will allow it to home in on selected sites of particular interest for imaging down to 2 m/pixel resolution. Although cameras on other spacecraft have imaged small areas at high resolution, or large areas at low resolution, they have never before combined the two and hence have been unable to determine the location of high resolution images to better than a few kilometres. The HRSC's images will be in 3D and full colour. The 3D imaging will provide a measurement of the height of features within an image relative to each other. The vertical resolution will be similar to the horizontal resolution.

The camera has ten channels, each consisting of a CCD (charge coupled device). One will be the super resolution channel and the other nine will record the same image almost simultaneously at the lower resolution. Four of these channels will record the image at different wavelengths (colours), and five will view it from different angles to provide the 3D effect. 

When the camera is 300 km above the surface, its footprint will be 62 km by 206 km. The diagram to the right shows the CCD lines except for the super resolution channel. The five white lines are used to provide the stereo effect.

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MPS involvement

MPS has no hardware participation in HRSC. We have have however, the leading role within the HRSC team, in the Martian atmospheric science to be done with this instrument. Some of the topics which interest us are:

  • synaptic observations of the Martian atmosphere and its diurnal and seasonal variations
  • dust devils and storms
  • atmospheric aerosols including dust and ice particles
  • clouds and fogs
  • seasonal variations of the polar cap region
  • so-called surface variable features
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Related links

> Institute of Space Sensor Technology and Planetary Exploration at the DLR, in Berlin


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