Sublimation of Mars's southern seasonal CO2 ice cap and the formation of spiders
By S. Piqueux, S. Byrne, Mark Richardson. 2003
158 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science, Environmental Chemistry
View Paper: https://www.semanticscholar.org/paper/e91216597c1b25a26954d5fe294649d03f32849f
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In Astronomy and Astrophysics
- S. Byrne
- Ralph E. Milliken
- Francois Forget
- John P. Grotzinger
- J. Bibring
- Yves Langevin
- B. Gondet
- A. S. McEwen
In Atmospheric Science
- Francois Forget
- S. Byrne
- A. S. McEwen
- Ralph E. Milliken
- Nicolas Gonzalez Thomas
- S. Squyres
- C. Dundas
- M. Mellon
Citations in the corpus
- 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): “The low albedo of the cryptic region results from extensive dust contamination of the surface [Langevin et al., 2006], which could result to a large extent to venting of sub-ice gas bubbles as proposed by Kieffer [2000], Piqueux et al. [2003] , and Kieffer et al. [2006].”
- The High Resolution Imaging Science Experiment (HiRISE) during MRO’s Primary Science Phase (PSP) (2010, background): “Unique spider-like channels are eroded into the surface, most likely by CO2 gas escaping from under the ice (Kieffer, 2000, 2007; Piqueux et al., 2003; Christensen et al., 2005a; Kieffer et al., 2006) and entraining loose material.”