TES mapping of Mars' north seasonal cap
By Hugh H. Kieffer, T. Titus. 2001
153 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/97adadbcf9ad9abc3e0a937a794504747430dbe1
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In Aerospace Engineering
- Francois Forget
- Michael J. Wolff
- Michael D. Smith
- R. Clancy
- F. Montmessin
- Ehouarn Millour
- Philip R. Christensen
- Jean-Baptiste Madeleine
In Astronomy and Astrophysics
- Francois Forget
- Michael D. Smith
- Ehouarn Millour
- James W. Head III
- Michael J. Wolff
- R. Clancy
- Jean-Baptiste Madeleine
- A. Spiga
Citations in the corpus
- The Polar Deposits of Mars (2009, background): “F or p er so na l u se o nl y. example, although dominated by CO2 ice (Leighton & Murray 1966), the northern seasonal ice cap is now known to have an annulus of water frost that tracks its outer edge (Kieffer & Titus 2001, Wagstaff et al. 2008).”
- Miniature thermal emission spectrometer for the Mars Exploration Rover (2002, background): “Mars Global Surveyor was launched in 1996, and the MGS TES has been returning excellent data since the spacecraft arrived at Mars in September, 1997 [Christensen et al., 2001a, 2001b; Bandfield et al., 2000; Bandfield, 2002; Smith et al., 2001a, 2001b; Kieffer et al., 2000; Kieffer and Titus, 2001].”
- Observations of the south seasonal cap of Mars during recession in 2004–2006 by the OMEGA visible/near‐infrared imaging spectrometer on board Mars Express (2007, background): “[25] H2O ice has been observed at the boundary of the receding north seasonal cap first as a bright and moderately cold ring [Kieffer and Titus, 2001], then with a direct spectral identification by OMEGA [Bibring et al., 2005].”
- Amazonian northern mid-latitude glaciation on Mars: A proposed climate scenario (2009, background): “…2002, Bibring et al., 2005, and Langevin et al., 2005 ) during this period revealed the recession of a seasonal CO 2 frost (James and Cantor, 2001; Kieffer and Titus, 2001) followed by a fine-grained H 2 O ice edge, whose sublimation finally exposes the perennial H 2 O cap to summer insolation.”
- Mars high resolution gravity fields from MRO, Mars seasonal gravity, and other dynamical parameters (2011, methodology): “Piqueux and Christensen, 2008), thermal imaging (TES, Kieffer et al., 2000; Kieffer and Titus, 2001), the high energy neutron detection (HEND, Litvak et al.”
- Sublimation of Mars's southern seasonal CO2 ice cap and the formation of spiders (2003, background): “An extreme example is the observed evolution of the ‘‘cryptic’’ region, primarily in the southern hemisphere [Kieffer et al., 2000] but also recently recognized in the north [Kieffer and Titus, 2001].”
- CRISM multispectral summary products: Parameterizing mineral diversity on Mars from reflectance (2007, result): “These results reproduce findings from past missions that identified a large water-rich, CO 2 -ice-free, residual polar cap [Kieffer et al., 1976; Kieffer and Titus, 2001; Bibring et al., 2005; Figure 9.”
- THE MARTIAN ATMOSPHERIC BOUNDARY LAYER (2011, background): “The polar caps and their growth, extent, and retreat have been surveyed with several instruments, and their extent, seasonal changes, and composition are presently very well known [James and Cantor, 2001; Kieffer and Titus, 2001; Langevin et al., 2005; Douté et al., 2007].”