Search Publications

An improvement to the volcano-scan algorithm for atmospheric correction of CRISM and OMEGA spectral data
DOI: 10.1016/j.pss.2009.03.007 Bibcode: 2009P&SS...57..809M

Seelos, Frank P.; Murchie, Scott L.; Mustard, John F. +12 more

The observations of Mars by the CRISM and OMEGA hyperspectral imaging spectrometers require correction for photometric, atmospheric and thermal effects prior to the interpretation of possible mineralogical features in the spectra. Here, we report on a simple, yet non-trivial, adaptation to the commonly-used volcano-scan correction technique for at…

2009 Planetary and Space Science
MEx 167
The Circum-Hellas Volcanic Province, Mars: Overview
DOI: 10.1016/j.pss.2008.08.010 Bibcode: 2009P&SS...57..895W

McCord, Thomas B.; HRSC Co-Investigator Team; Xiao, Long +13 more

Building on previous studies of volcanoes around the Hellas basin with new studies of imaging (High-Resolution Stereo Camera (HRSC), Thermal Emission Imaging System (THEMIS), Mars Orbiter Camera (MOC), High-Resolution Imaging Science Experiment (HiRISE), Context Imager (CTX)), multispectral (HRSC, Observatoire pour la Minéralogie, l'Eau, les Glace…

2009 Planetary and Space Science
MEx 126
The Mars express MARSIS sounder instrument
DOI: 10.1016/j.pss.2009.09.016 Bibcode: 2009P&SS...57.1975J

Gurnett, D.; Orosei, R.; Picardi, G. +16 more

The Mars advanced radar for subsurface and ionospheric sounding (MARSIS) on Mars Express is the first high-frequency sounding radar operating from orbital altitudes since the Apollo 17 Lunar Sounder flown in 1972. The radar operates from a highly elliptical orbit but acquires data only from altitudes lower than 1200 km. The periapsis altitude is 2…

2009 Planetary and Space Science
MEx 117
Pingos on Earth and Mars
DOI: 10.1016/j.pss.2008.11.003 Bibcode: 2009P&SS...57..541B

Burr, Devon M.; Tanaka, Kenneth L.; Yoshikawa, Kenji

Pingos are massive ice-cored mounds that develop through pressurized groundwater flow mechanisms. Pingos and their collapsed forms are found in periglacial and paleoperiglacial terrains on Earth, and have been hypothesized for a wide variety of locations on Mars. This literature review of pingos on Earth and Mars first summarizes the morphology of…

2009 Planetary and Space Science
MEx 72
Sedimentary deposits in Xanthe Terra: Implications for the ancient climate on Mars
DOI: 10.1016/j.pss.2008.06.009 Bibcode: 2009P&SS...57..944H

Jaumann, R.; Scholten, F.; Neukum, G. +7 more

A variety of sedimentary deposits is observed in Xanthe Terra, Mars, including Gilbert-type deltas, fan deltas dominated by resedimentation processes, and alluvial fans. Sediments were provided through deeply incised valleys, which were probably incised by both runoff and groundwater sapping. Mass balances based on High-Resolution Stereo Camera (H…

2009 Planetary and Space Science
MEx 66
Automatic detection of sub-km craters in high resolution planetary images
DOI: 10.1016/j.pss.2009.03.009 Bibcode: 2009P&SS...57..880U

Stepinski, Tomasz F.; Urbach, Erik R.

Impact craters are among the most studied geomorphic planetary features because they yield information about the past geological processes and provide a tool for measuring relative ages of observed geologic formations. Surveying impact craters is an important task which traditionally has been achieved by means of visual inspection of images. The s…

2009 Planetary and Space Science
MEx 66
Dayglow on Mars: Kinetic modelling with SPICAM UV limb data
DOI: 10.1016/j.pss.2008.08.012 Bibcode: 2009P&SS...57.1008S

Bertaux, J. -L.; Leblanc, F.; Witasse, O. +2 more

The UV spectrometer experiment SPICAM onboard ESA Mars Express has been orbiting Mars since December 2003. We present here some comparisons between airglow data that have been newly interpreted with the advanced kinetic model Trans-Mars. A series of numerical one-dimensional kinetic models, in the Trans-* family [Lilensten, J., Blelly. P.L., 2002.…

2009 Planetary and Space Science
MEx 50
Multi-resolution topographic data extraction from Martian stereo imagery
DOI: 10.1016/j.pss.2009.09.024 Bibcode: 2009P&SS...57.2095K

Muller, J. -P.; Kim, J. R.

The acquisition of high resolution topographic data such as Digital Terrain Models (DTMs) and orthoimages from various Martian stereo imagery is now readily available. The very successful European Space Agency (ESA) Mars Express mission includes the High Resolution Stereo Camera (HRSC) which has provided, since March 2004, an increasingly global s…

2009 Planetary and Space Science
MEx 40
Regional differences in gully occurrence on Mars: A comparison between the Hale and Bond craters
DOI: 10.1016/j.pss.2008.09.008 Bibcode: 2009P&SS...57..958R

Hiesinger, H.; Hauber, E.; Reiss, D. +1 more

The observation of gullies on Mars raised questions about the presence of liquid water in the recent past. In some regions like Hale and Bond crater, gullies occur in one crater (Hale) but do not in another crater nearby (Bond). These regional differences have been interpreted as an argument for a formation of the gullies related to groundwater. T…

2009 Planetary and Space Science
MEx 39
Investigation of water signatures at gully-exposed sites on Mars by hyperspectral image analysis
DOI: 10.1016/j.pss.2008.10.011 Bibcode: 2009P&SS...57...93F

Schulze-Makuch, Dirk; Fan, Chaojun; Xie, Hongjie +1 more

High-resolution images from the Mars Obiter Camera (MOC) onboard the Mars Global Surveyor (MGS) show a variety of gully features on sloped surfaces of Mars. The mechanism of gully formation is still under debate, although a majority of studies tend to favor a mechanism related to liquid water flow based on geomorphology and fluid mechanics conside…

2009 Planetary and Space Science
MEx 36