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Revision as of 09:59, 15 August 2018 by Kevin McE(talk | contribs)(→top: False causality; it is basis of IDL because it is diametrically opposite Greenwich meridian. Note deviations of IDL from this line.)
The 180th meridian or antimeridian[1] is the meridian 180° east or west of the Prime Meridian, with which it forms a great circle dividing the earth into the Western and Eastern Hemispheres. It is common to both east longitude and west longitude. It mostly passes through the open waters of the Pacific Ocean, but passes across land in Russia, Fiji and Antarctica. This meridian is used as the basis for the International Date Line, but the latter deviates from it to maintain date consistency within the territories of Russia, USA, Kiribati, Fiji and New Zealand.
Starting at the North Pole and heading south to the South Pole, the 180th meridian passes through:
The only place where roads cross this meridian, and where there are buildings very close to it, is in Fiji.
Software representation problems
Many geographic software libraries or data formats project the world to a rectangle; very often this rectangle is split exactly at the 180th meridian. This often makes it non-trivial to do simple tasks (like representing an area, or a line) over the 180th meridian. Some examples:
The GeoJSON specification strongly suggests splitting geometries so that neither of their parts cross the antimeridian.[2]
In OpenStreetMap, areas (like the boundary of Russia) are split at the 180th meridian.