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Arc measurement, sometimes called degree measurement, is the astrogeodetic technique of determining the radius of Earth and, by extension, its circumference. More specifically, it seeks to determine the local Earth radius of curvature of the figure of the Earth, by relating the latitude difference and the geographic distance surveyed between two locations on Earth's surface. The most common variant involves only astronomical latitudes and the meridian arc length and is called meridian arc measurement; other variants may involve only astronomical longitude or both geographic coordinates .
Arc measurement campaigns in Europe were the precursors to the International Association of Geodesy (IAG).
Nowadays, the method is replaced by worldwide geodetic networks and by satellite geodesy.
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