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Estimation of the total electron content of the Martian ionosphere using radar sounder surface echoes
DOI: 10.1029/2007GL032154 Bibcode: 2007GeoRL..3423204S

Gim, Yonggyu; Kofman, Wlodek; Herique, Alain +5 more

The Martian ionosphere's local total electron content (TEC) and the neutral atmosphere scale height can be derived from radar echoes reflected from the surface of the planet. We report the global distribution of the TEC by analyzing more than 750,000 echoes of the Mars Advanced Radar for Subsurface and Ionospheric Sounding (MARSIS). This is the fi…

2007 Geophysical Research Letters
MEx 109
Mobility and topographic effects for large Valles Marineris landslides on Mars
DOI: 10.1029/2007GL029835 Bibcode: 2007GeoRL..3410201L

Mangeney, A.; Lucas, A.

Recent experiments on dry granular flows over horizontal plane bare some similarities with large Martian landslides observed in Valles Marineris (VM). However, Martian normalized runout are twice as large as those that observed in dry granular flow experiments. Numerical simulations on theoretical 2D and real 3D topographies reconstructed from rem…

2007 Geophysical Research Letters
MEx 62
Stability of hydrated minerals on Mars
DOI: 10.1029/2007GL031267 Bibcode: 2007GeoRL..3420202C

Mustard, John F.; Bibring, Jean-Pierre; Poulet, François +7 more

The validity of recent identification of various hydrated minerals (kieserite, gypsum, hexahydrite, nontronite, chamosite, and montmorillonite) on Mars was assessed by exposing these minerals to simulated Martian surface conditions of atmospheric composition and pressure, temperature, and ultraviolet light irradiation. When exposed to such conditi…

2007 Geophysical Research Letters
MEx 45
Absorption of MARSIS radar signals: Solar energetic particles and the daytime ionosphere
DOI: 10.1029/2006GL028829 Bibcode: 2007GeoRL..34.9101E

Espley, Jared R.; Plaut, Jeffrey J.; Farrell, William M. +5 more

We present observations from the subsurface sounding mode of the MARSIS instrument onboard Mars Express that imply radar wave absorption because of increased amounts of ionization in the upper Martian atmosphere during the fall of 2005. On at least two occasions these radar disruptions lasted for several days and we find that these periods are cor…

2007 Geophysical Research Letters
MEx 39
On Martian nitrogen dayglow emission observed by SPICAM UV spectrograph/Mars Express
DOI: 10.1029/2006GL028437 Bibcode: 2007GeoRL..34.2206L

Leblanc, F.; Bertaux, J. L.; Chaufray, J. Y.

SPICAM UV spectrograph on board Mars Express has reported, for the first time, the identification of the N2 VK (0,5) and (0,6) band emissions in the Martian dayglow. The derived exospheric temperature of the N2 species in the upper Martian atmosphere is equal to 190 +/- 51 K for areocentric longitudes between 100° and 171° an…

2007 Geophysical Research Letters
MEx 31
Numerical modeling of the magnetic topology near Mars auroral observations
DOI: 10.1029/2007GL031806 Bibcode: 2007GeoRL..3424202L

Barabash, S.; Lundin, R.; Winningham, J. D. +6 more

Magnetohydrodynamic (MHD) simulations of the Mars magnetic field topology are presented for the auroral observations reported from the Mars Express SPICAM instrument. It is found that the field lines closest to the assumed emission location are open. That is, they are connected to the interplanetary magnetic field, thus allowing access for solar w…

2007 Geophysical Research Letters
MEx 26