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Equator, great circle around the Earth that is everywhere equidistant from the geographic poles and lies in a plane perpendicular to the Earth’s axis. This geographic, or terrestrial, Equator divides the Earth into the Northern and Southern hemispheres and forms the imaginary reference line on the Earth’s surface from which latitude is reckoned; in other words, it is the line with 0° latitude.
In astronomy, the celestial equator is the great circle in which the plane of the terrestrial Equator intersects the celestial sphere; it consequently is equidistant from the celestial poles. When the Sun lies in its plane, day and night are everywhere of equal length, a twice-per-year occurrence known as equinox.
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geomagnetic field: Characteristics of Earth’s magnetic field…around until they cross Earth’s Equator pointing geographically northward. They curve still more reentering Earth in northern latitudes, finally returning to the south pole of the magnet. At the present time, the north geographic pole corresponds to the south pole of the equivalent bar magnet. This has not always been…
geomagnetic field: Cause of magnetic storms…roughly parallel to Earth’s magnetic equator. Small departures from this average orientation are caused by rotation of the tilted dipole magnetic field once per day and by revolution of Earth around the Sun once per year. Large departures are caused by changes in the direction of the IMF relative to…
navigation: Latitude measurements…navigators got close to the Equator, these stars fell below the horizon; there it became necessary to rely on observing the altitude of the noonday Sun and calculating latitude with the aid of an almanac.…