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South magnetic pole
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South magnetic pole
The south magnetic pole, also known as the magnetic south pole, is the point on Earth's Southern Hemisphere where the geomagnetic field lines are directed perpendicular to the nominal surface. The Geomagnetic South Pole, a related point, is the south pole of an ideal dipole model of Earth's magnetic field that most closely fits Earth's actual magnetic field.
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, Earth's south magnetic pole is physically actually a magnetic north pole (see also North magnetic pole § Polarity).
The south magnetic pole is constantly shifting due to changes in Earth's magnetic field.
As of 2005, it was calculated to lie at 64°31′48″S 137°51′36″E / 64.53000°S 137.86000°E, placing it off the coast of Antarctica, between Adélie Land and Wilkes Land. In 2015 it lay at 64°17′S 136°35′E / 64.28°S 136.59°E (est). That point lies outside the Antarctic Circle. Due to polar drift, the pole is moving northwest by about 10 to 15 kilometres (6 to 9 mi) per year. Its current distance from the actual Geographic South Pole is approximately 2,860 km (1,780 mi). The nearest permanent science station is Dumont d'Urville Station. While the north magnetic pole began wandering very quickly in the mid 1990s, the movement of the south magnetic pole did not show a matching change of speed.
Early unsuccessful attempts to reach the magnetic south pole included those of French explorer Jules Dumont d'Urville (1837–1840), American Charles Wilkes (expedition of 1838–1842) and Briton James Clark Ross (expedition of 1839–1843).
The first calculation of the magnetic inclination to locate the magnetic South Pole was made on 23 January 1838 by the hydrographer Clément Adrien Vincendon-Dumoulin, a member of the Dumont d'Urville expedition in Antarctica and Oceania on the corvettes Astrolabe and Zélée in 1837–1840, which discovered Adélie 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, which was at that time located on land. They planted a flagpole at the spot and claimed it for the British Empire. However, there is now some doubt as to whether their location was correct. The approximate position of the pole on 16 January 1909 was 72°15′S 155°09′E / 72.25°S 155.15°E.[full citation needed]
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 Field (IGRF). For earlier years back to about 1600, the model GUFM1 is used, based on a compilation of data from ship logs.
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South magnetic pole AI simulator
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South magnetic pole
The south magnetic pole, also known as the magnetic south pole, is the point on Earth's Southern Hemisphere where the geomagnetic field lines are directed perpendicular to the nominal surface. The Geomagnetic South Pole, a related point, is the south pole of an ideal dipole model of Earth's magnetic field that most closely fits Earth's actual magnetic field.
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, Earth's south magnetic pole is physically actually a magnetic north pole (see also North magnetic pole § Polarity).
The south magnetic pole is constantly shifting due to changes in Earth's magnetic field.
As of 2005, it was calculated to lie at 64°31′48″S 137°51′36″E / 64.53000°S 137.86000°E, placing it off the coast of Antarctica, between Adélie Land and Wilkes Land. In 2015 it lay at 64°17′S 136°35′E / 64.28°S 136.59°E (est). That point lies outside the Antarctic Circle. Due to polar drift, the pole is moving northwest by about 10 to 15 kilometres (6 to 9 mi) per year. Its current distance from the actual Geographic South Pole is approximately 2,860 km (1,780 mi). The nearest permanent science station is Dumont d'Urville Station. While the north magnetic pole began wandering very quickly in the mid 1990s, the movement of the south magnetic pole did not show a matching change of speed.
Early unsuccessful attempts to reach the magnetic south pole included those of French explorer Jules Dumont d'Urville (1837–1840), American Charles Wilkes (expedition of 1838–1842) and Briton James Clark Ross (expedition of 1839–1843).
The first calculation of the magnetic inclination to locate the magnetic South Pole was made on 23 January 1838 by the hydrographer Clément Adrien Vincendon-Dumoulin, a member of the Dumont d'Urville expedition in Antarctica and Oceania on the corvettes Astrolabe and Zélée in 1837–1840, which discovered Adélie 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, which was at that time located on land. They planted a flagpole at the spot and claimed it for the British Empire. However, there is now some doubt as to whether their location was correct. The approximate position of the pole on 16 January 1909 was 72°15′S 155°09′E / 72.25°S 155.15°E.[full citation needed]
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 Field (IGRF). For earlier years back to about 1600, the model GUFM1 is used, based on a compilation of data from ship logs.
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