Antarctic Circle
Southernmost major latitude circle marking the Antarctic region.
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via Wikipedia: Antarctic Circle · see source
The Antarctic Circle is the southernmost of Earth’s five main latitude lines. Land and sea south of this circle make up the Antarctic region, while the area just north of it is the Southern Temperate Zone. Its location shifts over time; currently, ignoring the slight wobble called nutation, it sits at 66°33′51.0″ south of the Equator. That number isn’t exact because nutation—which can shift the line by up to 10 arcseconds—isn’t factored in.
Midnight sun and polar night
The circle’s latitude depends on Earth’s axial tilt, which varies by more than 2° over a 41,000-year cycle due to tidal forces from the Moon’s orbit. As a result, the Antarctic Circle is slowly moving south at about 14.5 meters (48 feet) each year. Within the Antarctic Circle, the Sun stays above the horizon for a full 24 hours at least once a year—meaning it’s visible at midnight—and also stays below the horizon for a full 24 hours at least once a year, so it’s not seen at noon.
The same happens inside the Arctic Circle, its northern counterpart. Right on the circle itself, these events occur exactly once per year: the midnight sun at the December solstice and the polar night at the June solstice. But because of atmospheric refraction, mirages, and the fact that the Sun appears as a disk rather than a point, the midnight sun can be glimpsed up to about 50 arcminutes (roughly 90 kilometers or 56 miles) north of the circle on the summer solstice.
Similarly, part of the Sun may be visible up to 50 arcminutes south of the circle on the winter solstice. These limits apply at sea level; higher elevations extend them, though mountains often block a clear view of the horizon. Mirages in Antarctica are often more dramatic than in the Arctic, sometimes creating a series of false sunsets and sunrises while the Sun stays below the horizon. No one lives permanently south of the Antarctic Circle, but several nations run research stations there, staffed by rotating teams of scientists.
Human habitation
In past centuries, semi-permanent whaling stations were set up on the continent, and some whalers stayed for a year or more. At least eleven children have been born in Antarctica, though all at stations north of the circle. The Antarctic Circle’s circumference is roughly 16,000 kilometers (9,900 miles). The area south of it covers about 20,000,000 square kilometers (7,700,000 square miles), or roughly 4% of Earth’s surface.
Sites along the Circle
Most of Antarctica lies within the circle. Starting at the prime meridian and moving east, the circle passes through various points ( as a table). Related concepts include the Antarctic Convergence, the Tropic of Cancer, and the Tropic of Capricorn.
Quick Facts
- Type
- Circle of latitude
- Current latitude
- 66°33 ft 51.0 in (11.4 m) south of the Equator
- Area south of circle
- About 20,000,000 km² (7,700,000 sq mi), covering roughly 4% of Earth's surface
- Drift speed
- Currently drifting southwards at about 14.5 m (48 ft) per year
- Axial tilt variation
- Fluctuates within a margin of more than 2° over a 41,000-year period
Facts from the source article.
Lore & Background
South of the Antarctic Circle, the Sun is above the horizon for 24 continuous hours at least once per year (and therefore visible at solar midnight) and the centre of the Sun (ignoring refraction) is below the horizon for 24 continuous hours at least once per year (and therefore not visible at solar noon); this is also true within the Arctic Circle, the Antarctic Circle’s counterpart in the Northern Hemisphere. Directly on the Antarctic Circle these events occur, in principle, exactly once per year: at the December and June solstices, respectively. However, because of atmospheric refraction and mirages, and because the sun appears as a disk and not a point, part of the midnight sun may be seen on the night of the southern summer solstice up to about 50 minutes (′) (90 km (56 mi)) north of the Antarctic Circle; similarly, on the day of the southern winter solstice, part of the sun may be seen up to about 50′ south of the Antarctic Circle. That is true at sea level; those limits increase with elevation above sea level, although in mountainous regions there is often no direct view of the true horizon.
Mirages on the Antarctic continent tend to be even more spectacular than in Arctic regions, creating, for example, a series of apparent sunsets and sunrises while in reality the sun remains below the horizon. There is no permanent human population south of the Antarctic Circle, but there are several research stations in Antarctica operated by various nations that are inhabited by teams of scientists who rotate on a seasonal basis. In previous centuries some semi-permanent whaling stations were established on the continent, and some whalers would live there for a year or more. At least eleven children have been born in Antarctica, albeit in stations north of the Antarctic Circle.
Reader's Guide
The Antarctic Circle is the northernmost latitude in the Southern Hemisphere at which the centre of the sun can remain continuously above the horizon for twenty-four hours; as a result, at least once each year at any location within the Antarctic Circle the centre of the sun is visible at local midnight, and at least once the centre of the sun is below the horizon at local noon. The circumference of the Antarctic Circle is roughly 16,000 kilometres (9,900 mi). The area south of the Circle is about 20,000,000 km2 (7,700,000 sq mi) and covers roughly 4% of Earth's surface. Most of the continent of Antarctica is within the Antarctic Circle.
The circle's latitude depends on the Earth's axial tilt, which fluctuates within a margin of more than 2° over a 41,000-year period, due to tidal forces resulting from the orbit of the Moon. Consequently, the Antarctic Circle is currently drifting southwards at a speed of about 14.5 m (48 ft) per year. Its position is not fixed and, not taking account of the nutation, currently runs 66°33′51.0″ south of the Equator, though this figure may be slightly inaccurate because it does not allow for the effects of astronomical nutation, which can be up to 10″.
Frequently Asked Questions
Where is the Antarctic Circle located and how big is it?
It currently runs at roughly 66°33′51.0″ south of the Equator, with a circumference of about 16,000 kilometres. The exact latitude can wobble slightly due to astronomical nutation.
Is the Antarctic Circle's position fixed over time?
No — it is slowly migrating southward at a rate of about 14.5 metres per year. Over a 41,000-year cycle, Earth's axial tilt can shift by more than two degrees, which would move the circle's latitude even further.
More in Physical Geography & Elevation
Related in Physical Geography & Elevation
Links follow this subject's own source article.
Sources
Compiled from Wikipedia and the sources listed below. Text from Wikipedia is available under CC BY-SA 4.0; this entry is adapted from it.
- Wikipedia: Antarctic Circle (CC BY-SA 4.0).
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