For examples of local horizontal datums with
their underlying ellipsoid and difference in position (datum
shift) with respect to WGS84,
see image below.
Source: Knippers,
2002
Below, the situation in the Netherlands.
Source: Knippers,
2010
In the above case, the local horizontal
datum is realized through a so-called triangulation
network (or survey network). Such a network consists of monumented
points forming a network of triangular mesh element (figure
below). The angles in each triangle are measured in addition
to at least one side of a triangle; the fundamental point is
also a point in the triangulation network. The angle measurements
and the adopted coordinates of the fundamental point are then
used to derive geographic (or geodetic) coordinates
for all monumented points of the triangulation network.
Global horizontal datums
With increasing demands for global
surveying activities are underway to establish global reference
surfaces. The motivation is to make geodetic results mutually
comparable and to provide coherent results also to other disciplines
like astronomy and geophysics.
The most important global (or geocentric)
spatial reference system for the GIS community is the International
Terrestrial Reference System (ITRS). It is a three-dimensional
coordinate system with a well-defined origin (the centre of
mass of the Earth) and three orthogonal coordinate axes (X,Y,Z).
The Z-axis points towards a mean Earth north pole. The X-axis
is oriented towards a mean Greenwich meridian and is orthogonal
to the Z-axis. The Y-axis completes the righthanded reference
coordinate system.
The ITRS is realized through the
International Terrestrial Reference Frame (ITRF), a
distributed set of ground control stations that measure their
position continuously using GPS.
The trend is to use the ITRF everywhere
in the world for reasons of global compatibility. The World
Geodetic System of 1984 (WGS84) datum has been refined on several
occasions and is now aligned with the ITRF to within a few centimetres
worldwide. The Global Positioning System (GPS) uses the WGS84
as its reference system.
Global horizontal datums, such as the ITRF2000 or WGS84, are
also called geocentric datums because they are
geocentrically positioned with respect to the centre of mass
of the Earth. They became available roughly after the 1960's,
with advances in extra-terrestrial positioning techniques.