Geodesy and Surveying

Disciplines/professions aimed at measuring positions. Reading: Geodesy for the Layman


Purpose of Lecture:


Earth Measurement (Geodesy)

Ellipsoid (Spheroid) is the assumed surface of rotation ­ defines lat/long (horizontal spatial reference system)
The Geoid is the complex surface of gravity at "Mean Sea Level" (vertical reference)

Eratosthenes 250 BC estimated circumference at 46250km (only 15% high),
using two points of observation (angles of sun in wells at Aswan & Alexandria)
Ptolemy "corrected" it to a value which was 25% small.

 Selected Ellipsoids

 major axis [a] (meters)

 1/f (flattening)

[f= (a­b) /a]
 Bessel 1841

 6377397.2

 299.15
 Everest 1830

 6377276.3

 300.80
 Clarke 1866 (NAD27)

 6378206.4

 294.98
 Clarke 1880

 6378249.2

 293.47
 World Geodetic System 1972

 6378135.0

 298.26
 GRS-80 (NAD 83, etc.)

 6378137.0

 298.26

Terms you need to know:

More resources on Geodesy in 465 course notes...


What is measured: depends on collection system

Debriefing on Event 2: What errors can occur in triangulation?


Adjustment computations: data quality work

Basically, there was no "source of higher accuracy", all assessments from internal evidence

Early schemes had no cross-check (buried the topic)

Closure of traverse: apportioning error in getting back to the same point.

Resolve redundancy: (triangulation produces little triangles (big?), not points) What to pick?

Mathematical models (least squares now) used to apportion errors out along a traverse.

(Compass rule to Weighted Least Squares)

Modern systems are self-error-checking; massive systems of simultaneous equations.


Version of 23 January 2004