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Performance and surface scattering models for the Mars Advanced Radar for Subsurface and Ionosphere Sounding (MARSIS)
DOI: 10.1016/j.pss.2003.08.020 Bibcode: 2004P&SS...52..149P

Gurnett, D. A.; Johnson, W. T. K.; Orosei, R. +10 more

The primary scientific objective of the Mars Advanced Radar for Subsurface and Ionosphere Sounding (MARSIS), which will be on board Mars Express mission scheduled for launch in 2003, is to map the distribution and depth of the liquid water/ice interface in the upper kilometres of the crust of Mars. MARSIS will also provide unique information to he…

2004 Planetary and Space Science
MEx 97
Ion loss on Mars caused by the Kelvin Helmholtz instability
DOI: 10.1016/j.pss.2004.06.001 Bibcode: 2004P&SS...52.1157P

Kallio, E.; Barabash, S.; Gunell, H. +8 more

Mars Global Surveyor detected cold electrons above the Martian ionopause, which can be interpreted as detached ionospheric plasma clouds. Similar observations by the Pioneer Venus Orbiter electron temperature probe showed also extreme spatial irregularities of electrons in the form of plasma clouds on Venus, which were explained by the occurrence …

2004 Planetary and Space Science
MEx 67
Evolution of the Martian atmosphere and hydrosphere: Solar wind erosion studied by ASPERA-3 on Mars Express
DOI: 10.1016/j.pss.2004.07.020 Bibcode: 2004P&SS...52.1059L

Lundin, Rickard; Barabash, Stanislav

The evolution of the Martian atmosphere and the potential existence of a past hydrosphere is a scientific issue of great interest in planetary research. Although the first missions to Mars had a focus on surface features and atmospheric properties, some of the missions (e.g., The Soviet Mars 2, 3 and 5) also carried instruments addressing the sola…

2004 Planetary and Space Science
MEx 24
Visible and infrared spectroscopy of minerals and mixtures with the OMEGA/MARS-EXPRESS instrument
DOI: 10.1016/j.pss.2003.08.014 Bibcode: 2004P&SS...52..133B

Gendrin, Aline; Bibring, Jean-Pierre; Langevin, Yves +4 more

We present the reflectance measurements made with OMEGA during ground calibration on a selection of minerals and mixtures considered as candidates for constituents of the Mars surface. OMEGA is the visible and infrared mapping spectrometer designed to fly on-board the ESA/MARS-EXPRESS probe. These measurements allow to evaluate the instrument perf…

2004 Planetary and Space Science
MEx 18
The microscope for Beagle 2
DOI: 10.1016/j.pss.2004.02.008 Bibcode: 2004P&SS...52..853T

Keller, H. U.; Hviid, S. F.; Thomas, N. +13 more

The microscope for the Beagle 2 lander, which was launched as part of the European Space Agency's Mars Express mission on 2 June 2003, will provide images of the Martian surface at around 6 µm resolution. It will provide optical images of the surface of Mars at a resolution 5 times higher than any other experiment currently planned. The devi…

2004 Planetary and Space Science
MEx 17
The Beagle 2 environmental sensors: science goals and instrument description
DOI: 10.1016/j.pss.2004.07.015 Bibcode: 2004P&SS...52.1141T

Patel, M. R.; Zarnecki, J. C.; Wilson, C. F. +12 more

A suite of instruments on the Beagle 2 Mars lander was designed and built in order to investigate the environmental conditions at the landing site. The sensor suite was capable of measuring air temperature at two heights, surface level pressure, wind speed and direction, saltated particle momentum, UV flux (diffuse and direct at five wavelengths),…

2004 Planetary and Space Science
MEx 16
Martian northern polar cap: Layering and possible implications for radar sounding
DOI: 10.1016/j.pss.2004.08.002 Bibcode: 2004P&SS...52.1195I

Ilyushin, Yaroslaw A.

The propagation of electromagnetic waves in the northern polar ice sheet of Mars is considered. It is shown that the dispersion and attenuation of radio waves in the polar sheet are regulated by two groups of factors: the physical and chemical composition of the ice, and the geometrical parameters of the layered structure of polar sheet. Both anal…

2004 Planetary and Space Science
MEx 9
Visualization and topographical analysis of the Mars surface
DOI: 10.1016/j.pss.2003.08.017 Bibcode: 2004P&SS...52..249D

Dorninger, P.; Jansa, J.; Briese, Ch.

The Institute of Photogrammetry and Remote Sensing has more than 30 years of experience in computation, visualization and analysis of digital terrain data. Most of the developed methods and algorithms are implemented in the software application SCOP++ and tested on Earth datasets. Due to the institute's involvement into Mars Express, these methods…

2004 Planetary and Space Science
MEx 5
Beagle-2 position determination from the returned camera panoramas using MOLA data
DOI: 10.1016/j.pss.2003.11.002 Bibcode: 2004P&SS...52..271M

Michael, G. G.

After the Beagle-2 lander of the Mars Express mission comes to rest on the surface of Isidis Planitia in late December 2003 to carry out a range of geochemistry and exobiology experiments, there will be considerable interest in determining its exact location. This work considers the feasibility of identifying topographic features seen in the Mars …

2004 Planetary and Space Science
MEx 1
Environmental predictions for the Beagle 2 lander, based on GCM climate simulations
DOI: 10.1016/j.pss.2003.12.001 Bibcode: 2004P&SS...52..259B

Newman, C. E.; Lewis, S. R.; Read, P. L. +1 more

The Mars climate database (MCD) is a database of statistics based on output from physically consistent numerical model simulations which describe the climate and surface environment of Mars. It is used here to predict the meteorological environment of the Beagle 2 lander site. The database was constructed directly on the basis of output from multi…

2004 Planetary and Space Science
MEx 0