South Magnetic Pole

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Locations of South Magnetic Pole from direct observation and model prediction.[1]

The South Magnetic Pole is the wandering point on the Earth's Southern Hemisphere where the geomagnetic field lines are directed vertically upwards. It should not be confused with the lesser known South Geomagnetic Pole described later.

For historical reasons, the "end" of a freely hanging magnet that points (roughly) north is itself called the "north pole" of the magnet, and the other end, pointing south, is called the magnet's "south pole". Because opposite poles attract, the Earth's South Magnetic Pole is physically actually a magnetic north pole (see also Script error: The function "formatLink" does not exist.).

The South Magnetic Pole is constantly shifting due to changes in the Earth's magnetic field. As of 2005 it was calculated to lie at Lua error in package.lua at line 80: module 'strict' not found.,[2] placing it off the coast of Antarctica, between Adelie Land and Wilkes Land. In 2015 it lay at Lua error in package.lua at line 80: module 'strict' not found. (est).[3] That point lies outside the Antarctic Circle. Due to polar drift, the pole is moving northwest by about 10 to 15 kilometers per year. Its current distance from the actual Geographic South Pole is approximately 2860 km.[1] The nearest permanent science station is Dumont d'Urville Station. Wilkes Land contains a large gravitational mass concentration.

North Magnetic Pole[4] (2001) Lua error in package.lua at line 80: module 'strict' not found. (2004 est) Lua error in package.lua at line 80: module 'strict' not found. (2007) Lua error in package.lua at line 80: module 'strict' not found. (2015) Lua error in package.lua at line 80: module 'strict' not found.[3][5]
South Magnetic Pole (1998) Lua error in package.lua at line 80: module 'strict' not found. (2004 est) Lua error in package.lua at line 80: module 'strict' not found. (2007) Lua error in package.lua at line 80: module 'strict' not found.[6] (2015) Lua error in package.lua at line 80: module 'strict' not found.[3]

Expeditions

Early unsuccessful attempts to reach the magnetic south pole included those of French explorer Dumont d'Urville (1837–40), American Charles Wilkes (expedition of 1838–42) and Briton James Clark Ross (expedition of 1839 to 1843).[7]

The first calculation of the magnetic inclination to locate the magnetic South Pole was made on January 23, 1838 by the hydrographer fr (Clément Adrien Vincendon-Dumoulin), a member of the Dumont d'Urville expedition in Antarctica and Oceania on the corvettes "L'Astrolabe" and "Zélée" in 1837-1840, which discovered Adelie Land.

On 16 January 1909 three men (Douglas Mawson, Edgeworth David, and Alistair Mackay) from Sir Ernest Shackleton's Nimrod Expedition claimed to have found the South Magnetic Pole,[8] which was at that time located on land. However, there is now some doubt as to whether their location was correct.[9] The approximate position of the pole on 16 January 1909 was Lua error in package.lua at line 80: module 'strict' not found..[10]

Fits to global data sets

The South Magnetic Pole has also been estimated by fits to global sets of data such as the World Magnetic Model (WMM) and the International Geomagnetic Reference Model (IGRF).[1] For earlier years back to about 1600, the model GUFM1 is used, based on a compilation of data from ship logs.[11]

South Geomagnetic Pole

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The Earth's geomagnetic field can be approximated by a tilted dipole (like a bar magnet) placed at the center of the Earth. The South Geomagnetic Pole is the point where the axis of this best-fitting tilted dipole intersects the Earth's surface in the southern hemisphere. As of 2005 it was calculated to be located at Lua error in package.lua at line 80: module 'strict' not found.,[12] near the Vostok Station. Because the field is not an exact dipole, the South Geomagnetic Pole does not coincide with the South Magnetic Pole. Furthermore, the South Geomagnetic Pole is wandering for the same reason its northern magnetic counterpart wanders.

See also

References

  1. 1.0 1.1 1.2 Lua error in package.lua at line 80: module 'strict' not found.
  2. Lua error in package.lua at line 80: module 'strict' not found.
  3. 3.0 3.1 3.2 British Geological Survey - Magnetic Poles
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  6. Lua error in package.lua at line 80: module 'strict' not found.
  7. Antarctic Treaty System: an Assessment, p. 90, US National Research Council, 1986
  8. Lua error in package.lua at line 80: module 'strict' not found.
  9. Lua error in package.lua at line 80: module 'strict' not found.
  10. Shackleton, Roland Huntford
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  12. Lua error in package.lua at line 80: module 'strict' not found.
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External links