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Thesis - Leigh Moody.pdf - Bad Request - Cranfield University

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Appendix B / Frames of Reference<br />

_ _<br />

by the poles and Greenwich (London). Z E passes through the north pole. In<br />

1984 the International Earth Rotation Service created the WGS 84 standard<br />

comprising the zero reference meridian and axis of rotation that define X C<br />

and Z C .<br />

C<br />

X<br />

15.5 Alignment Frame<br />

s<br />

O<br />

Z<br />

EQUATORIAL<br />

PLANE<br />

S A T E L L I T E O R B I T A L<br />

P L A N E<br />

Ω<br />

15-5<br />

N'<br />

Z E<br />

C<br />

Z<br />

r<br />

N<br />

X O<br />

Figure 15-2 : Celestial and GPS Satellite Orbital Frames<br />

The Alignment Frame (A), shown in Figure 15-3, is fixed with respect to the<br />

Earth at point (o). X A is an easterly tangent to the Earth’s surface parallel to<br />

the equatorial plane. Z A lies along the ray from the Earth geometric centre<br />

(r) through point (o). Y A lies in the local meridian plane spanned by Z E and<br />

Z A pointing in a northerly direction.<br />

15.6 Local Geodetic Axes<br />

Generic LGA (G), an example of which is shown in Figure 15-3, are located<br />

a general point (p) above the Earth’s surface. Z G points away from the Earth<br />

along the bi-normal vector to the tangent plane at the Earth’s equipotential<br />

surface. X G lies parallel to an easterly tangent at the Earth’s surface. Y G<br />

points north in the local meridian plane spanned by Z E and Z G . The geodetic<br />

vertical of the LGA located at point (m) passes through point (d) on the<br />

WGS-84 geoid, and point (f) on the Earth’s surface.<br />

Μ<br />

ι<br />

s

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