مدار'۳۳ ْ۶۶ جنوبی که منطقهٔ قطبی جنوب زمین را مشخص میکند مدار جنوبگان (نام قدیمیتر: مدار قطب جنوب) مینامند.
این مدار، یکی از پنج مدار مهم زمین است که در نقشهها غالباً نمایش داده میشود. در سال ۲۰۰۰، این مدار موازی با عرض جغرافیایی "۳۹ '۳۳ °۶۶ جنوب استوا بودهاست. در سال ۲۰۱۱، این مدار به عرض جغرافیایی "۴۴ '۳۳ °۶۶ (°۶۶٬۵۶۲۲) جنوبی رانده شدهاست.
محدوده جنوبی این مدار، جنوبگان و محدوده شمال آن تا مدار رأسالجَدی، منطقه معتدل جنوبی نام دارد. مدار شمالگان مدار مقابل آن در نیمکره شمالی زمین است.
پیوند به بیرون[ویرایش]
The Antarctic Circle is the most southerly of the five major circles of latitude that mark maps of the Earth. The region south of this circle is known as the Antarctic, and the zone immediately to the north is called the Southern Temperate Zone. South of the Antarctic Circle, the sun is above the horizon for 24 continuous hours at least once per year (and therefore visible at midnight) and the centre of the sun is below the horizon for 24 continuous hours at least once per year (and therefore not visible at noon); this is also true within the equivalent polar circle in the Northern Hemisphere, the Arctic Circle.
The position of the Antarctic Circle is not fixed; as of 22 August 2019, it runs 66°33′47.7″ south of the Equator. Its 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 15 m (49 ft) per year.
Midnight sun and polar night
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 obscured at local noon.
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 under 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 three children have been born in Antarctica, albeit in stations north of the Antarctic Circle.
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.
Sites along the Circle
Starting at the prime meridian and heading eastwards, the Antarctic Circle passes through: