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The age of Phobos and its largest crater, Stickney
DOI: 10.1016/j.pss.2014.04.009 Bibcode: 2014P&SS..102..152S

Neukum, G.; Michael, G. G.; Murray, J. B. +2 more

We derived crater production functions and chronology functions of Phobos for two scenarios, which likely represent the end-members of its dynamical evolution. Case A assumes that Phobos has been in its current orbit about Mars since its formation. Case B assumes a recent capture of Phobos and the impact history of an average Main Belt Asteroid. W…

2014 Planetary and Space Science
MEx 32
Drainage systems of Lonar Crater, India: Contributions to Lonar Lake hydrology and crater degradation
DOI: 10.1016/j.pss.2013.05.011 Bibcode: 2014P&SS...95...45K

Sekine, Yasuhito; Matsui, Takafumi; Komatsu, Goro +3 more

Lonar, a 1.8-km-diameter impact crater in India, is a rare example of terrestrial impact craters formed in basaltic bedrock. The estimated age of the crater ranges widely from less than 12 ka to over 600 ka, but the crater preserves a relatively pristine morphology. We conducted a study of various drainage systems of Lonar Crater. The crater floor…

2014 Planetary and Space Science
MEx 31
Spectroscopy and detectability of liquid brines on mars
DOI: 10.1016/j.pss.2014.01.018 Bibcode: 2014P&SS...92..136M

Pommerol, A.; Schmitt, B.; Massé, M. +5 more

Recent geomorphological observations as well as chemical and thermodynamic studies demonstrate that liquid water should be stable today on the Martian surface at some times of the day. In Martian conditions, brines would be particularly more stable than pure water because salts can depress the freezing point and lower the evaporation rate of water…

2014 Planetary and Space Science
MEx 30
The variable extension of Saturn's electron radiation belts
DOI: 10.1016/j.pss.2014.03.021 Bibcode: 2014P&SS..104....3R

Krupp, N.; Roussos, E.; Krimigis, S. M. +4 more

Contrary to the permanent MeV ion belts which are relatively stable in intensity over both short and long time scales and are modulated by a single Galactic Cosmic Ray driven source, the electron belts of Saturn appear to be much more complex in both structure and temporal evolution. In order to understand the responses of this system to the diffe…

2014 Planetary and Space Science
Cassini 28
Floor-Fractured Craters on Mars - Observations and Origin
DOI: 10.1016/j.pss.2013.09.017 Bibcode: 2014P&SS...98..146B

Jaumann, R.; Michael, G. G.; Kneissl, T. +2 more

Floor-Fractured Craters (FFCs) represent an impact crater type, where the infilling is separated by cracks into knobs of different sizes and shapes. This work focuses on the possible processes which form FFCs to understand the relationship between location and geological environment. We generated a global distribution map using new High Resolution…

2014 Planetary and Space Science
MEx 27
A non-monotonic eddy diffusivity profile of Titan's atmosphere revealed by Cassini observations
DOI: 10.1016/j.pss.2013.10.009 Bibcode: 2014P&SS..104...48L

Kammer, Joshua A.; Zhang, Xi; Li, Cheng +3 more

Recent measurements from the limb-view soundings of Cassini/CIRS and the stellar occultations from Cassini/UVIS revealed the complete vertical profiles of minor species (e.g., C2H2 and C2H4) from 100 to 1000 km in the atmosphere of Titan. In this study, we developed an inversion technique to retrieve the…

2014 Planetary and Space Science
Cassini 26
Geometry, stratigraphy and evidences for fluid expulsion within Crommelin crater deposits, Arabia Terra, Mars
DOI: 10.1016/j.pss.2013.12.013 Bibcode: 2014P&SS...92...34F

Rossi, A. P.; Pondrelli, M.; Franchi, F. +1 more

Conical mounds and furrows are widely interpreted as the morphological evidences of fluids expulsion on the martian surface. In the Crommelin crater (equatorial Arabia Terra) furrows and conical mounds are exhumed within light-toned equatorial layered deposits (ELDs). Aim of this paper is to describe these landforms and discuss their potential rel…

2014 Planetary and Space Science
MEx 25
The water production rate of Rosetta target Comet 67P/Churyumov-Gerasimenko near perihelion in 1996, 2002 and 2009 from Lyman α observations with SWAN/SOHO
DOI: 10.1016/j.pss.2013.11.006 Bibcode: 2014P&SS...91...14B

Schmidt, W.; Bertaux, J. -L.; Combi, M. R. +1 more

We report here the observations of the hydrogen cloud in Lyman alpha emission of Comet 67P/Churyumov-Gerasimenko at the last three passages through its perihelion, in 1996, 2002 and 2009. This comet became the target of ESA space mission Rosetta in 2003, and is therefore of particular interest. The data were collected with the SWAN instrument on b…

2014 Planetary and Space Science
Rosetta SOHO 25
Phobos: Observed bulk properties
DOI: 10.1016/j.pss.2014.01.004 Bibcode: 2014P&SS..102...86P

Pätzold, Martin; Dehant, Véronique; Rosenblatt, Pascal +2 more

This work is a review of the mass determinations of the Mars moon Phobos by spacecraft close flybys, by solving for the Martian gravity field and by the analysis of secular orbit perturbations. The absolute value and accuracy is sensitive on the knowledge and accuracy of the Phobos ephemeris, of the spacecraft orbit, other perturbing forces acting…

2014 Planetary and Space Science
MEx 25
Processing OMEGA/Mars Express hyperspectral imagery from radiance-at-sensor to surface reflectance
DOI: 10.1016/j.pss.2013.11.007 Bibcode: 2014P&SS...90....1B

Bakker, W. H.; van Ruitenbeek, F. J. A.; van der Werff, H. M. A. +4 more

OMEGA/Mars Express hyperspectral imagery is an excellent source of data for exploring the surface composition of the planet Mars. Compared to terrestrial hyperspectral imagery, the data are challenging to work with; scene-specific transmission models are lacking, spectral features are shallow making them difficult to detect, and field data for val…

2014 Planetary and Space Science
MEx 24