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The Arctic Circle

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The Arctic Circle, at approximately 66° 34' N, is a major circle of latitude defining the Earth's northern polar region. It experiences unique solar phenomena like the midnight sun and polar night, and is home to diverse human settlements and natural wonders. The region's climate, geography, and cultural importance are crucial for scientific studies, particularly in understanding global climate patterns and the impacts of climate change.

Defining the Arctic Circle

The Arctic Circle is one of the five major circles of latitude that mark maps of the Earth. It is an imaginary line located at approximately 66° 34' N that defines the southernmost boundary of the Arctic, a region at the top of the planet. The position of the Arctic Circle is not static; it shifts slightly due to the axial tilt of the Earth, which is subject to a 41,000-year cycle influenced by gravitational forces, primarily from the Moon. As a result of this axial precession, the Arctic Circle is currently drifting northward at a rate of about 15 meters per year.
Arctic landscape with polar bear in the foreground, people on sled pulled by huskies and icebergs in the background under the midnight sun.

Unique Solar Phenomena of the Arctic Circle

The Arctic Circle is known for distinctive solar phenomena: the midnight sun and the polar night. During the summer solstice, areas inside the Arctic Circle experience at least one day when the sun remains above the horizon for 24 hours, known as the midnight sun. Conversely, during the winter solstice, there is at least one day when the sun does not rise at all, termed the polar night. These occurrences become more extreme as one moves closer to the North Pole. For example, the city of Murmansk in Russia, just north of the Arctic Circle, endures a polar night that can last for over a month.

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Arctic Circle latitude coordinates

Approximately 66° 34' N

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Southernmost boundary definition

Arctic Circle marks the southernmost part of the Arctic region

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Arctic Circle's axial precession impact

Shifts due to Earth's axial tilt, moving northward at about 15 meters per year

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