Siple Dome Explained

Siple Dome Field Camp
Settlement Type:Camp
Mapsize:270px
Pushpin Map:Antarctica
Pushpin Mapsize:270
Pushpin Relief:yes
Coordinates:-81.6543°N -149.0051°W
Subdivision Type:Country
Subdivision Name:
Subdivision Type1:Location in Antarctica
Subdivision Name1:Siple Dome
Marie Byrd Land
Antarctica
Subdivision Type3:Administered by
Subdivision Name3:National Science Foundation
Established Title:Established
Blank Name Sec1:Type
Blank Info Sec1:Seasonal
Blank Name Sec2:Status
Elevation M:730
Population Total:Up to 60

Siple Dome (-81.6543°N -149.0051°W) is an ice dome approximately 100 km wide and 100 km long, located 130 km east of Siple Coast in Antarctica. Charles Bentley and Robert Thomas established a "strain rosette" on this feature to determine ice movement in 1973–74. They referred to the feature as Siple Dome because of its proximity to Siple Coast.

Siple Dome ice core

The Siple Dome ice core project (79.468° S 112.086° W) was conducted by the United States National Science Foundation. The deepest ice was recovered in 1999 from 974 m, with an age of 97,600 years.[1]

It is best known for the poorly-explained steps in water isotopes during the deglacial, which are unique to this core and may indicate a rapid decrease in the surface elevation of the adjoining ice streams during the deglacial[2] and a record of atmospheric carbon dioxide.[3] The Chief Scientist was Kendrick Taylor.

Radar surveys of internal ice structure

In the 1990s a team from the University of Washington and St Olaf College surveyed the ice, measuring thickness and determining internal structure, [4] finding evidence for the operation of the Raymond Effect. They also found that the ice had a maximum thickness of around 1000 m.

In popular culture

Climate

The climate is ice cap (Köppen: ET), as is most of the continent. Without marine moderation and a few hundred meters above sea level, it has one of the harshest winters on the continent outside the Antarctic plateaus. Unlike Alert, NU at slightly higher latitude and positive high averages during summer, in Siple Dome temperatures remain below freezing during the afternoon of the warmer months on average.[5]

See also

Siple Dome Skiway
Type:government
Owner-Oper:US Antarctic Program
Location:Marie Byrd Land
Elevation-F:1,994
Elevation-M:607
Coordinates:-81.6581°N -148.9974°W
Pushpin Map:Antarctica
Pushpin Mapsize:270
Pushpin Map Caption:Location of airfield in Antarctica
R1-Length-F:10,940
R1-Length-M:3,330
R1-Surface:Ice

Further reading

Notes and References

  1. Brook, E. J., White, J. W., Schilla, A. S., Bender, M. L., Barnett, B., Severinghaus, J. P., ... & Steig, E. J. (2005). Timing of millennial-scale climate change at Siple Dome, West Antarctica, during the last glacial period. Quaternary Science Reviews, 24(12), 1333-1343.
  2. Taylor, K. C., White, J. W. C., Severinghaus, J. P., Brook, E. J., Mayewski, P. A., Alley, R. B., ... & Lamorey, G. W. (2004). Abrupt climate change around 22ka on the Siple Coast of Antarctica. Quaternary Science Reviews, 23(1), 7-15.
  3. Ahn, J., Wahlen, M., Deck, B. L., Brook, E. J., Mayewski, P. A., Taylor, K. C., & White, J. W. (2004). A record of atmospheric CO2 during the last 40,000 years from the Siple Dome, Antarctica ice core. Journal of Geophysical Research: Atmospheres, 109(D13)
  4. Nereson. N.A.. Raymond. C.F.. Jacobel. R.W.. Waddington. E.D.. 2. The accumulation pattern across Siple Dome, West Antarctica, inferred from radar-detected internal layers . Journal of Glaciology. 2000. 46. 152. 75–87. 10.3189/172756500781833449. 2000JGlac..46...75N. 10.1.1.367.2532. 18864009.
  5. Web site: World Maps of Köppen-Geiger climate classification. koeppen-geiger.vu-wien.ac.at. en. 2019-07-24.