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Sulfates in Martian Layered Terrains: The OMEGA/Mars Express View
DOI: 10.1126/science.1109087 Bibcode: 2005Sci...307.1587G

Le Mouélic, Stéphane; Gendrin, Aline; Mangold, Nicolas +8 more

The OMEGA/Mars Express hyperspectral imager identified hydrated sulfates on light-toned layered terrains on Mars. Outcrops in Valles Marineris, Margaritifer Sinus, and Terra Meridiani show evidence for kieserite, gypsum, and polyhydrated sulfates. This identification has its basis in vibrational absorptions between 1.3 and 2.5 micrometers. These m…

2005 Science
MEx 840
Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations
DOI: 10.1126/science.1108806 Bibcode: 2005Sci...307.1576B

Sotin, Christophe; Fouchet, Thierry; Drossart, P. +39 more

The Observatoire pour la Minéralogie, l'Eau, les Glaces, et l'Activité (OMEGA) investigation, on board the European Space Agency Mars Express mission, is mapping the surface composition of Mars at a 0.3- to 5-kilometer resolution by means of visible-near-infrared hyperspectral reflectance imagery. The data acquired during the first 9 months of the…

2005 Science
MEx 834
Sulfates in the North Polar Region of Mars Detected by OMEGA/Mars Express
DOI: 10.1126/science.1109091 Bibcode: 2005Sci...307.1584L

Bibring, Jean-Pierre; Langevin, Yves; Gondet, Brigitte +1 more

The Observatoire pour la Minéralogie, l'Eau, les Glaces, et l'Activité (OMEGA) imaging spectrometer observed the northern circumpolar regions of Mars at a resolution of a few kilometers. An extended region at 240°E, 85°N, with an area of 60 kilometers by 200 kilometers, exhibits absorptions at wavelengths of 1.45, 1.75, 1.94, 2.22, 2.26, and 2.48 …

2005 Science
MEx 428
Olivine and Pyroxene Diversity in the Crust of Mars
DOI: 10.1126/science.1109098 Bibcode: 2005Sci...307.1594M

Mangold, N.; Bibring, J. -P.; Gendrin, A. +6 more

Data from the Observatoire pour la Minéralogie, l'Eau, les Glaces, et l'Activité (OMEGA) on the Mars Express spacecraft identify the distinct mafic, rock-forming minerals olivine, low-calcium pyroxene (LCP), and high-calcium pyroxene (HCP) on the surface of Mars. Olivine- and HCP-rich regions are found in deposits that span the age range of geolog…

2005 Science
MEx 358
Ion Neutral Mass Spectrometer Results from the First Flyby of Titan
DOI: 10.1126/science.1110652 Bibcode: 2005Sci...308..982W

Ip, Wing-Huen; McNutt, Ralph L.; Waite, J. Hunter +19 more

The Cassini Ion Neutral Mass Spectrometer (INMS) has obtained the first in situ composition measurements of the neutral densities of molecular nitrogen, methane, molecular hydrogen, argon, and a host of stable carbon-nitrile compounds in Titan's upper atmosphere. INMS in situ mass spectrometry has also provided evidence for atmospheric waves in th…

2005 Science
Cassini 357
Deflection of the Interstellar Neutral Hydrogen Flow Across the Heliospheric Interface
DOI: 10.1126/science.1107953 Bibcode: 2005Sci...307.1447L

Bertaux, J. L.; Lallement, R.; Quémerais, E. +3 more

Using an absorption cell, we measured the Doppler shifts of the interstellar hydrogen resonance glow to show the direction of the neutral hydrogen flow as it enters the inner heliosphere. The neutral hydrogen flow is found to be deflected relative to the helium flow by about 4°. The most likely explanation of this deflection is a distortion of the…

2005 Science
SOHO 315
Radar Soundings of the Subsurface of Mars
DOI: 10.1126/science.1122165 Bibcode: 2005Sci...310.1925P

Gurnett, Donald A.; Johnson, William T. K.; Stofan, Ellen R. +31 more

The martian subsurface has been probed to kilometer depths by the Mars Advanced Radar for Subsurface and Ionospheric Sounding instrument aboard the Mars Express orbiter. Signals penetrate the polar layered deposits, probably imaging the base of the deposits. Data from the northern lowlands of Chryse Planitia have revealed a shallowly buried quasi-…

2005 Science
MEx 280
Titan's Atmospheric Temperatures, Winds, and Composition
DOI: 10.1126/science.1111150 Bibcode: 2005Sci...308..975F

Strobel, D. F.; Showalter, M. R.; Lellouch, E. +42 more

Temperatures obtained from early Cassini infrared observations of Titan show a stratopause at an altitude of 310 kilometers (and 186 kelvin at 15°S). Stratospheric temperatures are coldest in the winter northern hemisphere, with zonal winds reaching 160 meters per second. The concentrations of several stratospheric organic compounds are enhanced a…

2005 Science
Cassini 277
Solar Wind Origin in Coronal Funnels
DOI: 10.1126/science.1109447 Bibcode: 2005Sci...308..519T

Wilhelm, Klaus; Marsch, Eckart; Wang, Jing-Xiu +4 more

The origin of the solar wind in solar coronal holes has long been unclear. We establish that the solar wind starts flowing out of the corona at heights above the photosphere between 5 megameters and 20 megameters in magnetic funnels. This result is obtained by a correlation of the Doppler-velocity and radiance maps of spectral lines emitted by var…

2005 Science
SOHO 271
Composition and Dynamics of Plasma in Saturn's Magnetosphere
DOI: 10.1126/science.1106151 Bibcode: 2005Sci...307.1262Y

Lewis, G. R.; Coates, A. J.; Linder, D. R. +40 more

During Cassini's initial orbit, we observed a dynamic magnetosphere composed primarily of a complex mixture of water-derived atomic and molecular ions. We have identified four distinct regions characterized by differences in both bulk plasma properties and ion composition. Protons are the dominant species outside about 9 RS (where R

2005 Science
Cassini 259