Mars Orbiter Laser Altimeter: Experiment summary after the first year of global mapping of Mars
By David E. Smith, Maria T. Zuber, Herbert Frey, J. Garvin, James W. Head III, D. Muhleman, G. Pettengill, Roger J. Phillips, Sean C. Solomon, H. Zwally and 14 more. 2001
1,675 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/2671eb431e2389cecf6a42e5623987586ecb9845
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In Astronomy and Astrophysics
- James W. Head III
- Mark A. Wieczorek
- E. Kite
- Francois Forget
- V. Hamilton
- Michael D. Smith
- Philip R. Christensen
- J. Bandfield
Citations in the corpus
- Lunar Reconnaissance Orbiter Overview: The Instrument Suite and Mission (2007, methodology): “2) is similar to the designs of the Mars Orbiter Laser Altimeter (Smith et al. 2001) and the Mercury Laser Altimeter (Solomon et al. 2001); however, it has five laser beams and five receiver channels.”
- The High Resolution Imaging Science Experiment (HiRISE) during MRO’s Primary Science Phase (PSP) (2010, background): “This variation in strategy has allowed for more complete coverage of different scientific themes, sub-topics, and types of features, allowing us to address a wide spectrum of Martian surface science.”
- Geologic Constraints on Early Mars Climate (2018, background): “Williams, R. M. E.; Phillips, R. J., 2001, Morphometric measurements of martian valley networks from Mars Orbiter Laser Altimeter (MOLA) data, J. Geophys.”
- High-resolution thermal inertia derived from the Thermal Emission Imaging System (THEMIS): Thermal model and applications (2006, methodology): “TES atmospheric 336 dust opacity was used for the first Martian year of MGS 337 mapping when there were no global dust storms [Smith et 338 al., 2000; M. D. Smith et al., 2001].”
- Formation timescales of large Martian valley networks (2011, methodology): “Volumes within the valleys were measured using ArcGIS software and Mars Global Surveyor (MGS) Mars Global Laser Altimeter (MOLA) topographic data (~463 m/pix) (Smith et al., 2001) and, where available, Mars Express High Resolution Stereo Camera (HRSC) topographic data (~75 m/pix) (Jaumann et al.”
- Planetary Spectrum Generator: An accurate online radiative transfer suite for atmospheres, comets, small bodies and exoplanets (2018, methodology): “03 degrees) by employing the MOLA topographic data [39].”
- Temperature inversions, thermal tides, and water ice clouds in the Martian tropics (2003, methodology): “The true surface topography [Smith et al., 2001] is shown by contour lines at intervals of 3 km.”
- The Polar Deposits of Mars (2009, background): “Mars Reconnaissance Orbiter (MRO) CRISM Compact Reconnaissance Imaging Spectrometer for Mars (Murchie et al. 2007a) HiRISE High Resolution Imaging Science Experiment (McEwen et al. 2007) SHARAD Mars Shallow Subsurface Radar (Seu et al. 2007b) Mars Express (MEX) MARSIS Mars Advanced Radar for Subsurf”