The South Magnetic Pole is the point on Earth's Southern Hemisphere where the geomagnetic field lines are directed vertically upwards. It should not be confused with the South Geomagnetic Pole described later. For historical reasons, the "end" of a freely hanging magnet that points 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, Earth's South Magnetic Pole is physically actually a magnetic north pole. The South Magnetic Pole is constantly shifting due to changes in Earth's magnetic field. As of 2005 it was calculated to lie at, placing it off the coast of Antarctica, between Adélie Land and Wilkes Land. In 2015 it lay at . That point lies outside the Antarctic Circle. Due to polar drift, the pole is moving northwest by about per year. Its current distance from the actual Geographic South Pole is approximately. The nearest permanent science station is Dumont d'Urville Station.
North Magnetic Pole
South Magnetic Pole
Expeditions
Early unsuccessful attempts to reach the magnetic south pole included those of French explorerDumont d'Urville, American Charles Wilkes and Briton James Clark Ross. The first calculation of the magnetic inclination to locate the magnetic South Pole was made on January 23, 1838 by the hydrographer, 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 from Sir Ernest Shackleton's Nimrod Expedition claimed to have found the South Magnetic Pole, which was at that time located on land. They planted a flagpole at the spot and claimed it for the British Empire. The three men began the expedition to the South Magnetic Pole in a motor car specially adapted for the cold conditions, but abandoned it when it proved useless on soft surfaces. They then walked a total of 1260 miles to reach the South Magnetic Pole while pulling sledges and supplies that weighed approximately 670 lbs. Walking on foot across the coldest place on earth was perilous, and the men faced many dangers such as falling in concealed snow crevasses and acquiring frostbite and snow-blindness. Fearing starvation, they strictly rationed their biscuits down to the crumbs, and hunted seals and penguins. However, there is now some doubt as to whether their location was correct. The approximate position of the pole on 16 January 1909 was.
The South Magnetic Pole has also been estimated by fits to global sets of data such as the World Magnetic Model and the International Geomagnetic Reference Model. For earlier years back to about 1600, the model GUFM1 is used, based on a compilation of data from ship logs.
South Geomagnetic Pole
Earth's geomagnetic field can be approximated by a tilted dipole placed at the center of Earth. The South Geomagnetic Pole is the point where the axis of this best-fitting tilted dipole intersects Earth's surface in the southern hemisphere. As of 2005 it was calculated to be located at, 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. While the north magnetic pole began wandering very quickly in the mid 1990s, the movement of the southmagnetic pole did not show a matching change of speed.
