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Bernese GPS Software Version 5.0 - Bernese GNSS Software

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Example 2<br />

6.5 Preprocessing Phase Observations<br />

The second example is based on the very short baseline (only 14 meters) between the two<br />

stations in Zimmerwald (ZIMJ−ZIMM) available in the example campaign (see Chapter 20).<br />

We used the strategy BOTH in this case. All other options are identical to those in Example 1<br />

with one exception: “Maximum ionospheric change from epoch to epoch” in panel “MAUPRP 8:<br />

Cycle Slip Detection/Correction” was set to 30%. The strategy BOTH should not be used for<br />

baselines longer than about 10 km. However, this strategy may be superior to the COM-<br />

BINED strategy if the baseline is very short and the receiver is of poor quality and provides<br />

measurements with a high noise level (not the case in this example). The output from the<br />

program is similar to that of Example 1. The only difference is the cycle slip detection flag<br />

used: here it is SNG (instead of DUA in Example 1).<br />

------------------------------------------------------------------------<br />

CYCLE SLIPS ACCEPTED IN THIS RUN<br />

------------------------------------------------------------------------<br />

NUMBER OF SLIPS IN L1: 70<br />

NUMBER OF SLIPS IN L2: 124<br />

NUMB TYP N EPOCH SAT FRQ WLF SLIP FRAC RES.L3 IONOS<br />

(M) (M)<br />

------------------------------------------------------------------------<br />

1 CLK * 18 ALL 1 1 51988847.<br />

2 CLK * 18 ALL 2 1 40510790.<br />

3 SNG * 51 18 2 1 -8442034. 0.12<br />

4 SNG * 87 18 2 1 52. 0.08<br />

5 SNG * 87 14 2 1 4106575. 0.06<br />

You may compare the correction for cycle slip 3 (second frequency for satellite 18 at<br />

epoch 51) in the second example with the correction for the corresponding cycle slip in<br />

the first example. It is the same event that can be attributed to the data of the station Zimmerwald<br />

(ZIMM) that was used in both baselines. The small difference in the correction for<br />

the clock jump between the two examples does not matter because finally double-differences<br />

of the observations without access to the clock parameters are analyzed.<br />

Example 3<br />

The third example demonstrates the program output of MAUPRP for screening zerodifference<br />

files. Again the station Zimmerwald (ZIMM) is used. A satellite clock file produced<br />

by the program CLKEST was introduced. To preprocess zero-difference observation files we<br />

have to use the COMBINED mode. The option “Do not accept cycle slip corrections” is marked<br />

and the “Maximum ionospheric change from epoch to epoch” is 400% (see panel “MAUPRP 8: Cycle<br />

Slip Detection/Correction”).<br />

As mentioned in Section 6.5.3 the change of the receiver clock correction is estimated epochwise<br />

before the residuals for the cycle slip detection are computed (Eqns. (6.4)). The program<br />

output contains a summary of these epoch solutions:<br />

<strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> <strong>Version</strong> <strong>5.0</strong> Page 127

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