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1.a line of latitude near but to the south of the north pole; it marks the northernmost point at which the sun is visible on the northern winter solstice and the southernmost point at which the midnight sun can be seen on the northern summer solstice
cercle (généricité) (fr)[Classe]
parallel; latitude; line of latitude; parallel of latitude[Classe]
région froide du monde (fr)[ClasseParExt.]
zone géographique supra-continentale de la Terre (fr)[Classe...]
polar circle[ClasseHyper.]
pole[Classe]
(pole), (polar circle)[Thème]
geography[Domaine]
Region[Domaine]
latitude, line of latitude, parallel, parallel of latitude - Frigid Zone, polar region, polar zone[Hyper.]
Nord (fr)[Thème]
Grand Nord (fr)[Situé]
Arctic, north-polar[Dérivé]
polar circle[Hyper.]
Arctic Circle (n.)
The Arctic Circle is one of the five major circles of latitude that mark maps of the Earth. For Epoch 2012, it is the parallel of latitude that runs 66° 33′ 44″ (or 66.5622°) [1] north of the Equator.
The region north of this circle is known as the Arctic, and the zone just to the south is called the Northern Temperate Zone. The equivalent polar circle in the Southern Hemisphere is called the Antarctic Circle.
The Arctic Circle marks the southern extremity of the polar day (24-hour sunlit day, often referred to as the "midnight sun") and polar night (24-hour sunless night). North of the Arctic Circle, the sun is above the horizon for 24 continuous hours at least once per year and below the horizon for 24 continuous hours at least once per year. On the Arctic Circle those events occur, in principle, exactly once per year, at the June and December solstices, respectively. In fact, because of atmospheric refraction 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 northern summer solstice up to about 50′ (90 km (56 mi)) south of the Arctic Circle; similarly, on the day of the northern winter solstice, part of the sun may be seen up to about 50′ north of the Arctic 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.
The position of the Arctic Circle is not fixed, but directly depends on the Earth's axial tilt, which fluctuates within a margin of 2° over a 40,000 year period,[2] notably due to tidal forces resulting from the orbit of the Moon. The Arctic Circle is currently drifting northwards at a speed of about 15 m (49 ft) per year, see Circle of latitude for more information.
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Relatively few people live north of the Arctic Circle due to the Arctic climate. The three largest communities above the Arctic Circle are situated in Russia: Murmansk (population 325,100), Norilsk (135,000), and Vorkuta (85,000). Tromsø (in Norway) has about 68,000 inhabitants. In contrast, the largest North American community north of the circle, Sisimiut (Greenland), has approximately 5,000 inhabitants, while between Canada and the USA, Barrow, Alaska is the largest settlement with circa 4,000 inhabitants. Rovaniemi (in Finland), which lies slightly south of the line, has a population of approximately 58,000, and is the largest settlement in the immediate vicinity of the Arctic Circle.
The Arctic Circle passes through the Arctic Ocean, the Scandinavian Peninsula, North Asia, Northern America and Greenland. The land on the Arctic Circle is divided among eight countries: Norway, Sweden, Finland, Russia, the United States (Alaska), Canada, Denmark (Greenland), and Iceland (where it passes through the small offshore island of Grímsey).
Starting at the Prime Meridian and heading eastwards, the Arctic Circle passes through:
| Wikimedia Commons has media related to: Arctic Circle |
| Look up arctic circle in Wiktionary, the free dictionary. |
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