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Basics

Meridian

meridian

Definition

A meridian is a half of a great circle on the Earth's surface, connecting the North Pole and the South Pole. Every point on Earth lies on exactly one meridian, and the angle between that meridian and the Prime Meridian (longitude 0°) defines the point's longitude. The term derives from the Latin 'meridies' (midday), since the sun crosses a given meridian at local noon.

The Prime Meridian

The Prime Meridian is the meridian designated as 0° longitude. It was established at the 1884 International Meridian Conference as the line passing through the Royal Observatory in Greenwich, England. This decision set the global reference point for the longitude and time zone systems. Today the international standard is the IERS Reference Meridian, which passes approximately 102 meters east of the historical Greenwich line.

Relationship to Time

Because the Earth rotates 360° in 24 hours, every 15° of longitude (15 meridians) corresponds to a one-hour time difference. All locations on the same meridian share the same solar time and observe the sun culminating at the same moment. Time zones are theoretically 15° wide, but in practice their boundaries follow national borders and administrative divisions rather than exact meridian lines.

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