Mars Express

Data and scientific objectives

Crater with water ice
Water ice at the bottom of a crater near the Martian North Pole. The white water ice stands out clearly in the centre of the crater, which measures approximately 35 kilometres across. The impact crater is located in the northern lowlands of Vastitas Borealis. Water ice can persist year-round in the centre of the crater, as the temperature and atmospheric pressure are too low to cause sublimation – the direct transition from a solid to a gaseous state. When this image was taken (during late northern summer on Mars), carbon dioxide ice had already disappeared from the entire polar cap, leaving only water ice. Earlier measurements suggest that the ice layer has an estimated thickness of only a few decimetres.
 
Copyright note: In December 2014, DLR, ESA and FU Berlin agreed to publish the HRSC images from the Mars Express mission under a Creative Commons license: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO. This licence applies to all HRSC images released to date.
Credit:

ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO.

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Data

Mission

 

Launch

2 June 2003, 19:45 CEST

Arrival in Mars orbit (lander)

25 December 2003, 04:00 CET

Launch site

Baikonur, Kazakhstan

Launch vehicle

Soyuz/Fregat

Ground stations

Perth (Australia), Kourou (French Guiana)

Ground reception time

6.5–7 hours per day

Mission control centre

European Space Operations Centre (ESOC), Darmstadt, Germany

Nominal mission duration

One Martian year (approx. two Earth years or 687 days); due to its significant scientific achievements, ESA has extended the Mars Express mission several times, most recently until the end of 2026

Orbit

Elliptical final orbit: 250 kilometres (pericentre) x 11,583 km (apocentre) from Mars; inclination: 87 degrees; orbital period: 7.5 hours

Spacecraft

 

Launch mass

1042 kilogrammes, including 427 kilogrammes of fuel

Scientific payload

Orbiter 116 kilogrammes; lander 60 kilogrammes

Dimensions

Orbiter: 1.5 x 1.8 x 1.4 metres; solar panel wingspan: 12 metres; surface area: 11.42 square metres

Power supply

Solar arrays with silicon cells: 660 watts at 1.5 astronomical units; energy storage: three lithium-ion batteries with a total capacity of 64.8 ampere-hours; power supply: 28 volts; peak power output: 450 watts

Data transfer

X-band: 7.1 gigahertz; S-band: 2.1 gigahertz; communication: omnidirectional low-gain antenna (LGA), four metres; directional high-gain antenna (HGA), 1.8 metres; two di-pole antennas: both 20 metres

Propulsion

Eight engines for orbital corrections, each delivering 10 newtons of thrust; one main engine with 400 newtons of thrust, for braking manoeuvres in Mars orbit; three-axis stabilisation

Orbiter instruments

 

HRSC (High Resolution Stereo Camera)

German-led project; high-resolution colour stereo camera; developed for the Mars 96 mission

MaRS (Mars Radio Science Experiment)

German-led project; investigates Mars' atmosphere, surface and gravity

PFS (Planetary Fourier Spectrometer)

Italian-led project with German participation; infrared spectrometer for atmospheric research

ASPERA (Analyser of Space Plasmas and Energetic Atoms)

Swedish-led project; analyses the interaction between Mars' atmosphere and the interplanetary medium

MARSIS (Mars Advanced Radar for Subsurface and Ionospheric Sounding)

Italian-led project; studying the deep layers of the Martian soil and upper atmosphere

OMEGA (Observatoire pour la Minéralogie, l’Eau, les Glaces et l'Activité)

French-led project; infrared spectrometer investigates Mars' surface composition; developed for the Mars 96 mission

SPICAM (Spectroscopic Investigation of the Atmosphere of Mars)

Ultraviolet spectrometer for investigating the atmosphere; developed for the Rosetta mission

Mars Express orbiter mission objectives:

Findings from previous Mars missions suggest that Mars was once a warm, wet planet before undergoing a climate shift around 3.5 billion years ago. Mars Express is investigating the climate history of the Red Planet through global orbital surveys and aims to clarify the role and fate of water. As part of comparative planetology, scientists hope to establish parallels between Mars and Earth that would enable more accurate predictions about the long-term development of our planet.

Key scientific goals:

  • Generate geological and mineralogical maps using multispectral imaging
  • Analyse atmospheric processes and composition
  • Investigate the subsurface structure (especially regarding permafrost)
  • Study interactions between the Mars' surface and atmosphere
  • Study interactions between the atmosphere and the interplanetary medium

The Beagle 2 lander was designed to:

  • Study the meteorology and climatology of Mars
  • Explore the geology, mineralogy and geochemistry at the landing site
  • Analyse the physical properties of the atmosphere and surface layers
  • Search for signs of life (exobiology)

Beagle 2 was scheduled to land on the Martian surface at the end of 2003. The lander was considered lost after it failed to make contact with the orbiter or with radio telescopes on Earth.

Contact

Falk Dambowsky

Head of Media Relations, Editor
German Aerospace Center (DLR)
Corporate Communications
Linder Höhe, 51147 Cologne
Tel: +49 2203 601-3959

Daniela Tirsch

Principal Investigator HRSC
German Aerospace Center (DLR)
Institute of Space Research
Rutherfordstraße 2, 12489 Berlin

Ulrich Köhler

German Aerospace Center (DLR)
Institute of Space Research
Public relations
Rutherfordstraße 2, 12489 Berlin