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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
Dawn: A journey in space and time
DOI: 10.1016/j.pss.2003.06.013 Bibcode: 2004P&SS...52..465R

Russell, C. T.; Jaumann, R.; Keller, H. U. +18 more

By successively orbiting both 4 Vesta and 1 Ceres the Dawn mission directly addresses the long-standing goals of understanding the origin and evolution of the solar system. Ceres and Vesta are two complementary terrestrial protoplanets (one apparently ;wet; and the other ;dry;), whose accretion was probably terminated by the formation of Jupiter. …

2004 Planetary and Space Science
eHST 87
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
Recent advances in the long-wavelength radio physics of the Sun
DOI: 10.1016/j.pss.2004.09.016 Bibcode: 2004P&SS...52.1399G

Gopalswamy, N.

Solar radio bursts at long wavelengths provide information on solar disturbances such as coronal mass ejections (CMEs) and shocks at the moment of their departure from the Sun. The radio bursts also provide information on the physical properties (density, temperature and magnetic field) of the medium that supports the propagation of the disturbanc…

2004 Planetary and Space Science
SOHO 30
CASSINI/VIMS-V at Jupiter: Radiometric calibration test and data results
DOI: 10.1016/j.pss.2003.11.005 Bibcode: 2004P&SS...52..661C

Brown, R. H.; Gondet, B.; Langevin, Y. +5 more

During the Cassini-Huygens flyby of Jupiter in December 2000, VIMS-V acquired multispectral data cubes of Jupiter's atmosphere. The visual and infrared imaging spectrometer-visual channel (VIMS-V) is one of the principal contributions of Italian Space Agency (ASI) to the Cassini-Huygens mission to Saturn. VIMS-V is an imaging spectrometer operatin…

2004 Planetary and Space Science
Cassini 29
Influence of wall impacts on the Ulysses dust detector on understanding the interstellar dust flux
DOI: 10.1016/j.pss.2004.07.022 Bibcode: 2004P&SS...52.1287A

Krüger, H.; Grün, E.; Altobelli, N. +2 more

The Ulysses spacecraft orbits the Sun on a highly inclined orbit, and the impact ionization dust detector on board continuously measures interstellar dust grains with masses up to 10-13kg, penetrating deep into the Solar System. The flow direction is close to the mean apex of the Sun's motion through the local interstellar cloud (LIC), …

2004 Planetary and Space Science
Ulysses 25
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
Quasi-periodic emissions (15- 80 min) from the poles of Jupiter as a principal source of the large-scale high-latitude magnetopause boundary layer of energetic particle
DOI: 10.1016/j.pss.2003.10.002 Bibcode: 2004P&SS...52..543K

Preka-Papadema, P.; Anagnostopoulos, G. C.; Karanikola, I. +2 more

In this study, we concentrate on the examination of the quasi-periodic behavior of 0.5-1.6 MeV(∼40-400 keV) protons (electrons) and of relativistic (>16 MeV) electrons, observed at Jupiter by two different experiments onboard Ulysses, the HI-SCALE and COSPIN, respectively, within the large-scale south duskside magnetopause boundary layer (MPBL)…

2004 Planetary and Space Science
Ulysses 19
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