Arc measurement

Arc measurement, sometimes degree measurement, is the astrogeodetic technique of determining the radius of Earth – more specifically, the local Earth radius of curvature of the figure of the Earth – by relating the latitude difference (sometimes also the longitude difference) and the geographic distance (arc length) 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 (parallel arc measurement) or both geographic coordinates (oblique arc measurement).
Arc measurement campaigns in Europe were the precursors to the International Association of Geodesy (IAG).
History
The first known arc measurement was performed by Eratosthenes (240 BC) between Alexandria and Syene in what is now Egypt, determining the radius of the Earth with remarkable correctness.
In the early 8th century, Yi Xing performed a similar survey.
The French physician Jean Fernel measured the arc in 1528. The Dutch geodesist Snellius (~1620) repeated the experiment between Alkmaar and Bergen op Zoom using more modern geodetic instrumentation (Snellius' triangulation).
Later arc measurements aimed at determining the flattening of the Earth ellipsoid by measuring at different geographic latitudes. The first of these was the French Geodesic Mission, commissioned by the French Academy of Sciences in 1735–1738, involving measurement expeditions to Lapland (Maupertuis et al.) and Peru (Pierre Bouguer et al.).
Struve measured a geodetic control network via triangulation between the Arctic Sea and the Black Sea, the Struve Geodetic Arc.
Bessel compiled several meridian arcs, to compute the famous Bessel ellipsoid (1841).
Nowadays, the method is replaced by worldwide geodetic networks and by satellite geodesy.
List of other instances
Al-Ma'mun's arc measurement
Posidonius' arc measurement
Swedish–Russian Arc-of-Meridian Expedition
Picard's arc measurement
Dunkirk-Collioure arc measurement (Cassini, Cassini, and de La Hire)
Dunkirk-Collioure arc measurement (Cassini de Thury and de Lacaille)
Meridian arc of Delambre and Méchain
West Europe-Africa Meridian-arc
De Lacaille's arc measurement
Fernel's arc measurement
Norwood's arc measurement
Boscovich and Maire's arc measurement
Maclear's arc measurement
Hopfner's arc measurement
Determination
Assume the astronomic latitudes of two endpoints, (standpoint) and (forepoint), are precisely determined by astrogeodesy, observing the zenith distances of sufficient numbers of stars (meridian altitude method). The empirical Earth's meridional radius of curvature at the midpoint of the meridian arc can then be determined as:
where is the arc length on mean sea level (MSL).
Historically, the distance between two places has been determined at low precision by pacing or odometry.
High precision land surveys can be used to determine the distance between two places at nearly the same longitude by measuring a baseline and a triangulation network linking fixed points. The meridian distance from one end point to a fictitious point at the same latitude as the second end point is then calculated by trigonometry. The surface distance is reduced to the corresponding distance at MSL, (see: Geographical distance#Altitude correction).
Two arc measurements at different latitudinal bands serve to determine Earth's flattening.
See also
Astrogeodesy
Earth ellipsoid
Geodesy
Gradian#Relation to the metre
History of geodesy
Spherical Earth#History
Meridian arc#History
Earth's circumference#History
Meridian arc
Paris Meridian
References
Geodetic surveys