Swiss cheese features

Swiss cheese features (SCFs) are curious pits in the south polar ice cap of Mars (Mare Australe quadrangle) named from their similarity to the holes in Swiss cheese. They were first seen in 2000 using Mars Orbiter Camera imagery.[1]

Pits in south polar ice cap, taken in consecutive southern hemisphere summers, the first of which was in 1999, the second in 2001. Mars Global Surveyor, NASA

Description

They are typically a few hundred meters across and 8 metres deep, with a flat base and steep sides. They tend to have similar bean-like shapes with a cusp pointing towards the south pole, indicating that insolation is involved in their formation. The angle of the Sun probably contributes to their roundness. Near the Martian summer solstice, the Sun can remain continuously just above the horizon; as a result the walls of a round depression will receive more intense sunlight, and sublimate much more rapidly than the floor. The walls sublimate and recede, while the floor remains the same.[2][3] As the seasonal frost disappears, the pit walls appear to darken considerably relative to the surrounding terrain. The SCFs have been observed to grow in size, year by year, at an average rate of 1 to 3 meters, suggesting that they are formed in a thin layer (8 m) of carbon dioxide ice lying on top of water ice.[4][5] Later research with HiRISE showed that the pits are in a 1–10-meter-thick layer of dry ice that is sitting on a much larger water ice cap. Pits have been observed to begin with small areas along faint fractures. The circular pits have steep walls that work to focus sunlight, thereby increasing erosion. For a pit to develop, a steep wall of about 10 cm and a length of over 5 meters is necessary.[6]

Halo features

Bright transient halo features around the carbon dioxide pits were found during the southern hemisphere's summer, during Mars year 28 (Earth year 2007). However, this was the only time these features have ever been seen. The data to understand these halos were taken from the MRO (Mars Reconnaissance Orbiter) Context Camera, the HiRISE (High Resolution Imaging Science Experiment) camera, and the MOC (Mars Orbiter Camera). The halo features were only visible during the solar longitudes (position of Mars around the Sun) of 279 degrees and 331 degrees. The halo's appearance correlates to the global dust storm that began earlier in the same Martian year. The lifetime of the halos was broken into trimesters; the first was 285–295 degrees Ls (Solar Longitude, time in the Martian Year), the second was 295–305 degrees Ls, and the final was counted at 305–340 degrees Ls. The average width of the high albedo area around the Swiss cheese features changes throughout its lifetime. In the first trimester the width was calculated to be 12.14 ± 1.44 meters wide, the second trimester was 32.96 ± 4.02 meters wide, and in the final trimester the average width was 55.48 ± 6.98 meters. The Hapke's reflectance theory was used to calculate the brightness of the features.[7] During the first trimester, the halos were 4 +/- .3% brighter than the non-halo areas. Then in the second trimester the halos became more prominent at 7 +/- .7% brighter. Toward the end of their life they were the brightest recorded at 8 +/- .6% brighter than the surrounding topography. The halos are brighter than the surrounding region due to the impurities in the ice. The global dust storm filled the CO2 ice with sand and increased the grain size of the ice crystals.[8]

  • Swiss cheese-like ice formations as seen by Mars Global Surveyor
  • Swiss cheese-like ice formations as seen by Mars Global Surveyor showing layers
  • Close-up of Swiss cheese terrain, as seen by Mars Global Surveyor
gollark: Also, the compiler is slow and 250 dependencies constantly.
gollark: I would use Rust but it takes somewhat more time to do things than I'd like sometimes.
gollark: Anyway, I would use Python but due to things I've become disillusioned with using it for webapps.
gollark: It isn't automatic. The mailing list server has to process it all.
gollark: I would use JS, if JS wasn't awful in all ways.

See also

References
  1. Thomas, P. C.; et al. (2000). "North-south geological differences between the residual polar caps on Mars". Nature. 404 (6774): 161–4. Bibcode:2000Natur.404..161T. doi:10.1038/35004528. PMID 10724162.
  2. Hartmann, W. 2003. A Traveler's Guide to Mars. Workman Publishing. NY NY.
  3. Mangold, Nicolas (2011). "Ice sublimation as a geomorphic process: A planetary perspective". Geomorphology. 126 (1–2): 1–17. Bibcode:2011Geomo.126....1M. doi:10.1016/j.geomorph.2010.11.009.
  4. Byrne, S.; Ingersoll, A. P. (2002). "A Sublimation Model for the Formation of the Martian Polar Swiss-cheese Features". American Astronomical Society. 34: 837. Bibcode:2002DPS....34.0301B.
  5. "HiRISE - South Pole Residual Cap Swiss-Cheese Terrain Monitoring (PSP_005095_0935)". hirise.lpl.arizona.edu. Archived from the original on 2015-02-12.
  6. Buhler, Peter B.; Ingersoll, Andrew P.; Ehlmann, Bethany L.; Fassett, Caleb I.; Head, James W. (2017). "How the martian residual south polar cap develops quasi-circular and heart-shaped pits, troughs, and moats". Icarus. 286: 69–93. Bibcode:2017Icar..286...69B. doi:10.1016/j.icarus.2017.01.012.
  7. Hapke, Bruce (2012-01-19). Theory of Reflectance and Emittance Spectroscopy. Cambridge University Press. ISBN 978-0-521-88349-8.
  8. Becerra, Patricio; Byrne, Shane; Brown, Adrian J. (2015-05-01). "Transient bright "halos" on the South Polar Residual Cap of Mars: Implications for mass-balance". Icarus. Dynamic Mars. 251: 211–225. Bibcode:2015Icar..251..211B. doi:10.1016/j.icarus.2014.04.050. ISSN 0019-1035.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.