Flattening, Fundamental frequency, Geocentric – Leica Geosystems GPS Basics User Manual

Page 52: Geodesy, Geodetic datum, Geoid, Glossary

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52

GPS Basics -1.0.0en

Glossary

Flattening
Relating to Ellipsoids.

f = (a-b)/a = 1-(1-e

2

)

1/2

where a ... semimajor axis

b ... semiminor axis
e ... eccentricity

Fundamental frequency
The fundamental frequency used in GPS

is 10.23 MHz. The carrier frequencies L1

and L2 are integer multiples of the

fundamental frequency.

L1 = 154F = 1575.42 MHz
L2 = 120F = 1227.60 MHz

GDOP
Geometric dilution of precision
—> Dilution of precision

Geocentric
Relating to the centre of the earth.

Geodesy
The study of the earth’s size and shape

Geodetic Coordinates
Coordinates defining a point with

reference to an ellipsoid. Geodetic

Coordinates are either defined using

latitude, longitude and ellipsoidal height

or using Cartesian coordinates.

Geodetic Datum
A mathematical model designed to best

fit part or all of the geoid. It is defined by

an ellipsoid and the relationship be-

tween the ellipsoid and a point on the

topographic surface established as the

origin of datum. This relationship can

be defined by six quantities, generally

(but not necessarily) the geodetic

latitude, longitude, and the height of the

origin, the two components of the

deflection of the vertical at the origin, and

the geodetic azimuth of a line from the

origin to some other point.

Geoid
The particular equipotential surface

which coincides with mean sea level,

and which may be imagined to extend

through the continents. This surface is

everywhere perpendicular to the direc-

tion of the force of gravity.

Geoidal Height
See Geoid separation

Geoid separation
The distance from the surface of the

reference ellipsoid to the geoid mea-

sured outward along the normal to the

ellipsoid.

GPS
Global Positioning System

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