As we know
from
reading the previous page, in Geodesy an ellipsoid is a mathematical
model of the earth as a slightly flattened shape. There are several
different ellipsoidal models used in defining the shape of the Earth,
and these are used for defining
geodetic
coordinates, three-dimensional coordinate systems defined in
terms of latitude and longitude.
In order to navigate with an ellipsoid model, we have to know where the
ellipsoid is tied to defined points on the Earth's surface. A
datum defines how an ellipsoidal
model of the Earth's shape relates to its actual surface. Places where
the Earth and the ellipsoid are "attached" to each other are called
Realisation Points (or "Realization
Points"), and tend to be marked with a small construction such as a
concrete post in the ground. Traditionally, these were used by
cartographers to
triangulate
as an accurate point of reference when making maps.
Unfortunately, many different datums were developed over time, each
applying to a different country or part of the world. This means that
it is not possible to translate a latitude and longitude position to an
exact location on the Earth's surface unless you are aware of which
datum is being used. Examples of different datums include:
i)
Ordnance Survey
1936
- British, based on Airy's 1830 ellipsoid
ii)
Hjorsey
1955
- Icelandic, based on the 1924 International ellipsoid
iii)
Bogota
Observatory
- Colombian, based on the 1924 International ellipsoid
iv)
North American
Datum of 1983 (NAD83)
- Based on the GRS80 ellipsoid
v) World
Geodetic
System of 1984 (WGS84)
- Global, developed by US Department of Defense, based on GRS80 and its
own ellipsoid.
The differences in these datums and ellipsoids mean that you may
sometimes be given a set of coordinates for a location which do not
match other ones you may have. This commonly occurs between NAD83, in
North America, and WGS84, as much US geographical data is based on
NAD83, and most GPS devices use WGS84.
A2B
always uses the
World Geodetic System of 1984 (WGS84) for defining coordinates. If
uploading from a GPS or entering a position manually, not using WGS84
can lead to errors in the hundreds of metres.
You can find out more about navigation and geodesic datums on our
links page.