- ED50
ED 50 ("European Datum 1950") is a geodetic datum which was defined after
World War II for the international connection ofgeodetic network s.Some of the important battles of World War II were fought on the borders of
Germany , theNetherlands ,Belgium andFrance , and the mapping of these countries had incompatiblelatitude andlongitude positioning. This led to the setting up of ED50 as a consistent mapping datum for much ofWestern Europe . It was, and still is, used in much of Western Europe apart fromGreat Britain ,Ireland ,Sweden andSwitzerland , which have their own datums.It was based on the
International Ellipsoid of 1924 ("Hayford-Ellipsoid" of 1909) (radius of the Earth'sequator 6378.388 km,flattening 1:297) and widely used all over the world up to the 1980s, whenGRS80 andWGS84 were established.Many national coordinate systems of Gauss-Krüger are defined by ED50 and oriented by means of
Geodetic astronomy . Up to now it has been used indata base s of gravity field,cadastre , smallsurveying networks in Europe and America, and by some developing countries with no modern baselines.The geodetic datum of ED50 is centred at the
Munich Frauenkirche in southernGermany , where the approximate centre of the Western Europenational network s was situated in the years of thecold war . ED50 was also part of the fundamentals of theNATO coordinates (Gauss-Krüger andUTM ) up to the 1980s.Datum shift between ED50 and WGS84
The longitude and latitude lines on the two datums are the same in the Archangel region of north-west
Russia . As one moves westwards across Europe, the longitude "lines" on ED50 gradually become further west than their WGS84 equivalents, and are around 100 metres west inSpain andPortugal . Moving southwards, the latitude "lines" on ED50 gradually become further south than the WGS84 lines, and are around 100 m south in theMediterranean Sea . (NB. If the "lines" are further west, the longitude "value" of any given point becomes more easterly. Similarly, if the "lines" are south, the "values" become northerly.)The datum shift for the
Universal Transverse Mercator grid is different. The eastings vary between 0 m in Eastern Europe and 100 m in the far west of the continent, roughly similar to the longitude shift, but the northings are about 200 m different across Europe, with the ED50 UTM northing "lines" south of the WGS84 UTM northing lines, as UTM northings are measured from the Equator, and the theoretical ED50 Equator is about 200 m south of the WGS84 one.ee also
* The Great Britain datum
OSGB36 .
* For Ireland, theIrish Transverse Mercator .
* The Sweden datumRT90 .
* The Switzerland datumCH1903 .
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