Title: COORDINATE SYSTEMS
1CO-ORDINATE SYSTEMS DATUMS IN AFRICA
CHARLES L MERRY SCHOOL OF ARCHITECTURE,
PLANNING GEOMATICS UNIVERSITY OF CAPE TOWN
2- Definitions
- Classical Datums
- Datums and Projections in Africa
- Problems
- The Future
3- A three-dimensional cartesian co-ordinate
system, where the origin and scale are
defined, as are the directions of the
three axes.
- An example is the ITRS
- geocentric - centre of mass of the Earth,
including oceans and atmosphere - orientation given by the BIH orientation (mean
pole, mean Greenwich meridian)
4- Practical realisation of a reference system,
using co-ordinates (and velocities) of a
number of sites
An example is the ITRF2000, where the
co-ordinates and velocities are given for some
200 tracking stations distributed around the
world.
5- Type of co-ordinate used to describe the
position of a point
Examples are Cartesian (3D) -
X, Y, Z
(2D) - y, x or E, N
Ellipsoidal (geographical) - f, l,
h Polar -
r, a, q
6- Solid body formed by rotating an ellipse
around its minor axis
There are many geodetic reference ellipsoids,
defined by either a, b or by a, f.
Examples Clarke 1866Clarke 1880
(modified)Bessel 1841International 1924WGS84
7- Spheroid is a sphere-like body
- In Europe and elsewhere, Spheroid generally
means a more complex body than an
Ellipsoid. - In England, Spheroid is identical to
Ellipsoid.
8- A specific ellipsoid in a specific position
and orientation with respect to the Earth.
Generally NOT geocentric, but with axes
nearly parallel to those of the ITRS.
There are many examples, to be discussed
later.Normally, the co-ordinate system
associated with this datum is the ellipsoidal (f,
l, h).
9- There are many ellipsoids and many (more)
datums. There is not a one-to-one
correspondence between them. One
ellipsoid can be used for several datums.
Datum 1
Datum 2
Ellipsoid A
Datum 3
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11- A geometrical or mathematical projection of
the surface of the ellipsoid onto a plane.
2D cartesian co-ordinates (y, x or E, N) on the
surface of the plane are used for mapping and
surveying tasks.
12- There are many projections and many datums.
- Applying the same projection to two different
datums will result in two different sets
of plane co-ordinates for the same
points. - Applying two different projections to the
same datum will result in two different
sets of plane co-ordinates for the same
points.
13- Choose a specific ellipsoid
- Choose it's orientation three translations,
three rotations
14- CLASSICAL DATUM DEFINITION
- Choose a specific ellipsoid
- Define an initial point, and the orientation
of the ellipsoid wrt the geoid
Position f, l, N Orientation x, h, a
15- CLASSICAL DATUM DEFINITION - 2
- Generally, deflections of the vertical (x, h)
and geoidal height (N) are chosen to be
zero at initial point - This implies that ellipsoidal position is set
equal to astronomic position at initial
point, and ellipsoidal height is set equal
to orthometric height (above (MSL) - This leads to a datum which is non-geocentric
16- A legacy of the Colonial era - datums based
upon ellipsoids determined by European
geodesists - Classical approach used astronomically-define
d origin ellipsoid from Europe classical
triangulation - Many so-called "datums" are just
re-computations of all or part of existing
networks, using the same initial point
e.g. the Arc 1950, Arc 1960, Circuit datums
17- Bessel 1841 Eritrea, Namibia
- Clarke 1866 Angola, Mozambique
- Clarke 1880 Algeria, Botswana, Burkina
Faso, Burundi, Cameroon, Chad, Congo,
DRC, Ethiopia, Gabon, Ghana, Guinea,
Kenya, Lesotho, Liberia, Malawi, Mali, Morocco,
Niger, Nigeria, Senegal, Tanzania, Tunisia,
Zambia, Zimbabwe - International 1924 Bissau, Egypt,
Guinea-Bissau, Libya, Madagascar, Tunisia - Krassovsky 1940 Somalia
18Sources NIMA TR8350.2 C Mugnier
(PERS) EPSG Database
19- Mapping of ellipsoidal co-ordinates (f, l) to
a plane - Common Projections
- Universal Transverse Mercator (UTM)
- Transverse Mercator / Gauss Conform / Gauss
Krüger - Lamberts Conformal Conic
- Labordes
20- PROJECTIONS IN AFRICA - 2
- Remember that the same projection applied to
two different ellipsoids will yield two
different sets of plane co-ordinates - The same projection applied to the same
ellipsoid, on different datums, will
yield two different sets of plane
co-ordinates
21- PROJECTIONS IN AFRICA - 3
- Example Gauss Conform projection on Cape datum
yields co-ordinates for the same point that
differ by up to 300m from Gauss Conform
projection on the Hart94 datum
Acknowledgements Chief Directorate of Surveying
Mapping
22A multitude of different datums, different
ellipsoids and different projections
? Variations on the same datum Point 58
/ Adindan / Blue Nile Cape / Arc 1950 / Arc
1960 / Circuit ? Variations on the same
ellipsoid Clarke 1880 (modified) - Arc /
IGN / RGS ? Variations on the same projection
Transverse Mercator different origins and
false origins, different scale factors
23- Confusion within countries as to appropriate
datums, projections and transformations to
use - Confusion and conflict regarding
international borders - Confusion and delays in cross-border projects
- boundary definition, transport
corridors, mapping, exploitation of
mineral resources
24- AFREF - a single consistent co-ordinate
frame - Establishment of a network of permanent GNSS
stations is only the FIRST step - The next step is to tie the existing networks
into this frame, establishing the
necessary transformations between the
local datum at the ITRF - Ideally, also converting all co-ordinated
points and maps to the ITRF