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Guidelines for the use of GNSS in surveying and mapping

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6.3.1 Ellipsoidal to cartesian<br />

trans<strong>for</strong>mations <strong>and</strong> reverse<br />

The follow<strong>in</strong>g <strong>for</strong>mulae are suitable <strong>for</strong> conversion<br />

<strong>of</strong> ellipsoidal co-ord<strong>in</strong>ates (φ <strong>and</strong> λ) to cartesian coord<strong>in</strong>ates<br />

(x, y <strong>and</strong> z). In <strong>the</strong>se <strong>for</strong>mulae, <strong>the</strong> x-axis<br />

is def<strong>in</strong>ed as be<strong>in</strong>g parallel to <strong>the</strong> conventional zero<br />

meridian <strong>of</strong> Greenwich, <strong>the</strong> z-axis parallel to <strong>the</strong><br />

CIO <strong>and</strong> <strong>the</strong> y-axis at right angles to <strong>the</strong>se two<br />

(eastwards). The cartesian system may be<br />

geocentric or referred to <strong>the</strong> vertical at some<br />

specified po<strong>in</strong>t.<br />

6.1<br />

where:<br />

6.6<br />

(e’) 2 <strong>the</strong> second<br />

eccentricity 2 6.6a<br />

6.6b<br />

6.6c<br />

6.2<br />

6.7<br />

6.3<br />

Or<br />

(us<strong>in</strong>g Bom<strong>for</strong>d’s notation)<br />

6.7a<br />

Notice that <strong>the</strong> height <strong>of</strong> <strong>the</strong> po<strong>in</strong>t is (N+h) above<br />

<strong>the</strong> ellipsoid. Thus, equations 6.1, 6.2 <strong>and</strong> 6.3<br />

presuppose knowledge <strong>of</strong> <strong>the</strong> geoid/ellipsoid<br />

separation (N).<br />

The reverse trans<strong>for</strong>mation, from cartesian to<br />

ellipsoidal co-ord<strong>in</strong>ates, does not produce such<br />

closed <strong>for</strong>mulae. The <strong>for</strong>mulae <strong>for</strong> this reverse<br />

trans<strong>for</strong>mation are:<br />

Approximate values <strong>of</strong> φ <strong>and</strong> λ are <strong>use</strong>d <strong>and</strong><br />

iteration gives rapid convergence.<br />

6.4<br />

6.5<br />

Ano<strong>the</strong>r alternative is <strong>the</strong> closed <strong>for</strong>mula due to<br />

Bowr<strong>in</strong>g:<br />

It is important to note that aga<strong>in</strong> N needs to be<br />

known (see paragraph 6.3.4), <strong>and</strong> that (N+h) is<br />

determ<strong>in</strong>ed when us<strong>in</strong>g equation 6.7. (N+h) is<strong>the</strong><br />

ellipsoidal height <strong>and</strong> is not a height obta<strong>in</strong>ed by<br />

spirit levell<strong>in</strong>g.<br />

In summary, to convert from:<br />

+ ellipsoidal to cartesian: <strong>use</strong> equations 6.1, 6.2<br />

<strong>and</strong> 6.3<br />

+ cartesian to ellipsoidal: <strong>use</strong> equations 6.4, 6.5<br />

<strong>and</strong> 6.7.<br />

Evidently, different ma<strong>the</strong>matical models can exist<br />

<strong>for</strong> <strong>the</strong> trans<strong>for</strong>mations, hence <strong>the</strong> small differences<br />

that may occur when us<strong>in</strong>g different manufacturers’<br />

methods <strong>of</strong> trans<strong>for</strong>mation. These differences will<br />

manifest as small systematic <strong>of</strong>fsets between two<br />

groups <strong>of</strong> local co-ord<strong>in</strong>ates when trans<strong>for</strong>med by<br />

two different methods. The most important issue<br />

when work<strong>in</strong>g on high-accuracy projects is to be<br />

consistent <strong>and</strong> <strong>use</strong> <strong>the</strong> same method <strong>of</strong><br />

trans<strong>for</strong>mation <strong>and</strong> s<strong>of</strong>tware. Thus any small<br />

differences <strong>in</strong> co-ord<strong>in</strong>ates will not be propagated<br />

<strong>in</strong>to a project <strong>and</strong> distort <strong>the</strong> geometry <strong>of</strong> a survey<br />

undertaken us<strong>in</strong>g <strong>GNSS</strong>.<br />

GUIDELINES FOR THE USE OF <strong>GNSS</strong> IN LAND SURVEYING AND MAPPING |45

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