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Arctic Circle
(redirected from Circumpolar arctic)

   Also found in: Wikipedia, Hutchinson 0.02 sec.
Arctic Circle, imaginary circle on the surface of the earth at 66 1-2°N latitude, i.e., 23 1-2° south of the North Pole. It marks the northernmost point at which the sun can be seen at the winter solstice solstice (sŏl`stĭs) [Lat.
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 (about Dec. 22) and the southernmost point of the northern polar regions at which the midnight sun midnight sun, phenomenon in which the sun remains visible in the sky continuously for 24 hr or longer, occurring only in the polar regions. The midnight sun is due to the fact that the plane of the earth's equator is tilted about 23 1-2° to the plane of the
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 is visible.

Arctic Circle

Parallel of latitude approximately 66°30′ north of the Equator that circumscribes the northern frigid zone. It marks the southern limit of the area within which, for one day or more each year, the sun does not set or rise. The length of continuous day or night increases northward from the Arctic Circle, mounting to six months at the North Pole.


Arctic Circle
the imaginary circle round the earth, parallel to the equator, at latitude 66° 32ʹ N; it marks the northernmost point at which the sun appears above the level of the horizon on the winter solstice

Arctic Circle [¦ärd·ik ′sər·kəl]
(geodesy)
The parallel of latitude 66°32′N (often taken as 66½°N).


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Comparison of selected Indian viruses with representative rabies viruses recovered worldwide showed a close association of all Indian isolates with the circumpolar Arctic rabies lineage distributed throughout northern latitudes of North America and Europe and other viruses recovered from several Asian countries.
 
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