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Bernese GPS Software Version 5.0 - Bernese GNSS Software

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9. Combination of Solutions<br />

files are combined to one set of parameters. If we want to stack the parameters pi and pi+1<br />

into one parameter pi, we can use following parameter transformation:<br />

⎛<br />

⎛ ⎞ 1 · · ·<br />

⎜ . ⎜<br />

⎟ ⎜ .<br />

⎜ ⎟ ⎜ . ..<br />

⎜ pi ⎟ ⎜<br />

⎜ ⎟ ⎜ 0 · · ·<br />

⎜ pi+1 ⎟ = ⎜<br />

⎜ ⎟ ⎜ 0 · · ·<br />

⎜ pi+2 ⎟ ⎜<br />

⎝ ⎠ ⎜ .<br />

⎝ . ..<br />

.<br />

0 · · ·<br />

.<br />

. ..<br />

1 · · ·<br />

1 · · ·<br />

.<br />

. ..<br />

⎞<br />

0<br />

⎟<br />

. ⎟<br />

0<br />

⎟<br />

0 ⎟<br />

. ⎠<br />

⎛ ⎞<br />

⎜ . ⎟<br />

⎜ ⎟<br />

⎜ pi ⎟<br />

⎜ ⎟ .<br />

⎜ pi+2 ⎟<br />

⎝ ⎠<br />

.<br />

(9.28)<br />

<br />

0 · · · 0 · · ·<br />

<br />

C<br />

1<br />

<br />

The transformation of the normal equation system is performed using Eqn. (9.22). Sometimes,<br />

parameters are stacked immediately after reading the normal equation system. But<br />

usually some type of parameter transformation precedes the stacking.<br />

Stacking is performed automatically for same parameters from different normal equation<br />

files, e.g., coordinates of the same station, troposphere parameters referring to the same<br />

station and the same epoch, or dynamic orbit parameters for the same satellite and the<br />

same osculating epoch.<br />

Stacking may be suppressed for station coordinates (e.g., in case of anomalous behavior) by<br />

marking the station as bad in the station information file (see Section 9.4.6). The coordinates<br />

for the marked station will then not be stacked but pre-eliminated before stacking for normal<br />

equation files within the time interval specified without any constraining.<br />

Orbital elements may be stacked after transformation to the same osculating epoch according<br />

to [Beutler et al., 1996]. For details see Section 15.3.2.<br />

9.3.7 Reduction of the Number of Parameters<br />

Stacking reduces the number of unknown parameters in the normal equations. An important<br />

application is the reduction of the number of parameters used to represent a piece-wise<br />

linear function, see example in Figure 9.2. The operation is performed in two steps: first, the<br />

validity interval of each parameter is adjusted to the new interval according to Section 9.3.5.<br />

Then transformed parameters are stacked according to Section 9.3.6.<br />

A typical example is the reduction of number of troposphere parameters. If you have, e.g.,<br />

estimated (and stored into normal equation files) 12 troposphere parameters per site and<br />

day, you have the possibility to reduce the number of parameters to 1, 2, 3, 4, or 6 values<br />

per day and site. See Section 9.4.5 for details on how to use this option.<br />

9.3.8 Introducing Additional Parameters<br />

The introduction of additional parameters is possible in some specific cases, even if these<br />

parameter types have not been set up in the individual normal equations. Site motion<br />

parameters, or site velocities, are an example for such parameter types. It is necessary that<br />

the influence of these parameters can be neglected within the individual normal equations.<br />

Page 190 AIUB

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