Search Publications

Identification of hydrated silicate minerals on Mars using MRO-CRISM: Geologic context near Nili Fossae and implications for aqueous alteration
DOI: 10.1029/2009JE003339 Bibcode: 2009JGRE..114.0D08E

Murchie, Scott L.; Ehlmann, Bethany L.; Mustard, John F. +9 more

The Noachian terrain west of the Isidis basin hosts a diverse collection of alteration minerals in rocks comprising varied geomorphic units within a 100,000 km2 region in and near the Nili Fossae. Prior investigations in this region by the Observatoire pour l'Minéralogie, l'Eau, les Glaces, et l'Activité (OMEGA) instrument on Mars Expre…

2009 Journal of Geophysical Research (Planets)
MEx 435
Density and temperatures of the upper Martian atmosphere measured by stellar occultations with Mars Express SPICAM
DOI: 10.1029/2008JE003086 Bibcode: 2009JGRE..114.1004F

Montmessin, Franck; Bertaux, Jean-Loup; González-Galindo, Francisco +6 more

We present one Martian year of observations of the density and temperature in the upper atmosphere of Mars (between 60 and 130 km) obtained by the Mars Express ultraviolet spectrometer Spectroscopy for Investigation of Characteristics of the Atmosphere of Mars (SPICAM). Six hundred sixteen profiles were retrieved using stellar occultations techniq…

2009 Journal of Geophysical Research (Planets)
MEx 167
Composition, Morphology, and Stratigraphy of Noachian Crust around the Isidis basin
DOI: 10.1029/2009JE003349 Bibcode: 2009JGRE..114.0D12M

Mangold, N.; Bibring, J. -P.; Mustard, J. F. +5 more

Definitive exposures of pristine, ancient crust on Mars are rare, and the finding that much of the ancient Noachian terrain on Mars exhibits evidence of phyllosilicate alteration adds further complexity. We have analyzed high-resolution data from the Mars Reconnaissance Orbiter in the well-exposed Noachian crust surrounding the Isidis basin. We fo…

2009 Journal of Geophysical Research (Planets)
MEx 138
Mineralogy of Juventae Chasma: Sulfates in the light-toned mounds, mafic minerals in the bedrock, and hydrated silica and hydroxylated ferric sulfate on the plateau
DOI: 10.1029/2009JE003352 Bibcode: 2009JGRE..114.0D09B

Murchie, Scott L.; Mustard, John F.; Brown, Adrian J. +10 more

Juventae Chasma contains four light-toned sulfate-bearing mounds (denoted here as A-D from west to east) inside the trough, mafic outcrops at the base of the mounds and in the wall rock, and light-toned layered deposits of opal and ferric sulfates on the plateau. Hyperspectral visible/near-infrared Compact Reconnaissance Imaging Spectrometer for M…

2009 Journal of Geophysical Research (Planets)
MEx 131
Structure of the Venus neutral atmosphere as observed by the Radio Science experiment VeRa on Venus Express
DOI: 10.1029/2008JE003204 Bibcode: 2009JGRE..114.0B36T

Tellmann, Silvia; Tyler, G. Leonard; Pätzold, Martin +2 more

The European Space Agency Venus Express Radio Science experiment (VeRa) obtained 118 radio occultation measurements of the Venusian atmosphere between July 2006 and June 2007. Southern latitudes are uniformly sampled; measurements in the northern hemisphere are concentrated near the pole. Radial profiles of neutral number density derived from the …

2009 Journal of Geophysical Research (Planets)
VenusExpress 122
A ground-to-exosphere Martian general circulation model: 1. Seasonal, diurnal, and solar cycle variation of thermospheric temperatures
DOI: 10.1029/2008JE003246 Bibcode: 2009JGRE..114.4001G

Forget, F.; López-Valverde, M. A.; González-Galindo, F. +2 more

We present the extension to the thermosphere of a Martian general circulation model, the first able to self-consistently study the whole Martian atmosphere from the surface to the exosphere. We describe the parameterizations developed to include physical processes important for thermospheric altitudes. The results of a simulation covering 1 full M…

2009 Journal of Geophysical Research (Planets)
MEx 121
A new model to simulate the Martian mesoscale and microscale atmospheric circulation: Validation and first results
DOI: 10.1029/2008JE003242 Bibcode: 2009JGRE..114.2009S

Forget, François; Spiga, Aymeric

The Laboratoire de Météorologie Dynamique (LMD) Mesoscale Model is a new versatile simulator of the Martian atmosphere and environment at horizontal scales ranging from hundreds of kilometers to tens of meters. The model combines the National Centers for Environmental Prediction(NCEP)-National Center for Atmospheric Research (NCAR) fully compressi…

2009 Journal of Geophysical Research (Planets)
MEx 113
Characterization of phyllosilicates observed in the central Mawrth Vallis region, Mars, their potential formational processes, and implications for past climate
DOI: 10.1029/2008JE003301 Bibcode: 2009JGRE..114.0D10M

Murchie, Scott L.; Ehlmann, Bethany L.; Mustard, John F. +7 more

Mawrth Vallis contains one of the largest exposures of phyllosilicates on Mars. Nontronite, montmorillonite, kaolinite, and hydrated silica have been identified throughout the region using data from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM). In addition, saponite has been identified in one observation within a crater. These …

2009 Journal of Geophysical Research (Planets)
MEx 103
Altimetry of the Venus cloud tops from the Venus Express observations
DOI: 10.1029/2008JE003320 Bibcode: 2009JGRE..114.0B43I

Roatsch, Th.; Drossart, P.; Piccioni, G. +6 more

Simultaneous observations of Venus by Visible and Infrared Thermal Imaging Spectrometer and Venus Monitoring Camera onboard the Venus Express spacecraft are used to map the cloud top altitude and to relate it to the ultraviolet (UV) markings. The cloud top altitude is retrieved from the depth of CO2 absorption band at 1.6 µm. In l…

2009 Journal of Geophysical Research (Planets)
VenusExpress 84
Testing evidence of recent hydration state change in sulfates on Mars
DOI: 10.1029/2008JE003245 Bibcode: 2009JGRE..114.0D02R

Bibring, J. -P.; Mustard, J. F.; Forget, F. +6 more

The East Candor Interior Layered Deposit (ILD) has signatures of mono- and polyhydrated sulfate in alternating layers that give insight into the processes which formed these layered deposits and on the environmental conditions acting on them since then. We use orbital data to explore multiple hypotheses for how these deposits formed: (1) sulfate-b…

2009 Journal of Geophysical Research (Planets)
MEx 73