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Bernese GPS Software Version 5.0 - Bernese GNSS Software

Bernese GPS Software Version 5.0 - Bernese GNSS Software

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6.2 Preprocessing on the RINEX Level<br />

the arc with a maximum RMS value specified by the user. Outliers are only temporarily<br />

removed in this step. The difference between the two (clean) parts is estimated and the arcs<br />

are connected using the estimated cycle slip. All points that were considered outliers during<br />

the cycle slip detection are included again. The RMS is recomputed to check whether there<br />

are more cycle slips in this observation arc.<br />

After the detection of all cycle slips, the observations are screened for outliers. Outliers are<br />

removed (using a 4σ-threshold) until the RMS of the observation arc is below the specified<br />

maximum. The specified maximum RMS is typically 0.4–0.6 wide-lane cycles (34–52 cm).<br />

If an outlier is detected, all four observation types (code and phase on two frequencies) are<br />

rejected.<br />

6.2.2 Data Screening Based on Geometry-Free Linear Combination<br />

Only those observation arcs in which cycle slips have been detected are screened using the<br />

geometry-free combination of the phase observations (see Eqn. (2.46)). At this stage the size<br />

of the wide-lane cycle slip (n1 − n2) is known. The geometry-free linear combination (L4)<br />

allows us to compute the size of the n1 and n2 cycle slips because it gives us: L4 = L1 −L2.<br />

To determine the size of the cycle slip on the L4 linear combination two linear polynomials<br />

are fitted through m points (m is defined by the user in option “Number of L4 observations for<br />

fit” in panel “RNXSMT 2.3: Options”), before and after the cycle slip. The difference between<br />

the two polynomials at the time of the cycle slip is computed. If the fractional part of<br />

the difference is smaller than a user specified limit (option “RMS of L4 for fit and cycle slip<br />

correction” in panel “RNXSMT 2.3: Options”) the n4 cycle slip is accepted and the cycle slips n1<br />

and n2 are computed. Typically a value of m = 10 is used and a difference smaller than<br />

10 mm. This procedure is executed to be able to connect the code observations during the<br />

code smoothing step. Because cycle slips occur rarely, no attempt is made to connect the<br />

phase observations. For the phase observations a new ambiguity is set up at the epoch of<br />

the detected cycle slip.<br />

6.2.3 Data Screening Based on Ionosphere-Free Linear Combination<br />

Sometimes the described procedure is not fully successful to clean the data due to systematic<br />

errors in the Melbourne-Wübbena combination. These systematic errors are most likely<br />

caused by the filtering and smoothing procedures employed in the receivers. Therefore, an<br />

additional data screening step is necessary.<br />

The difference between ionosphere-free linear combinations of the phase and code observations,<br />

Eqns. (2.41) and (2.42), i.e., L3 − P3, is used in this step. As in the case of the<br />

Melbourne-Wübbena combination this linear combination should consist of noise only, too.<br />

The disadvantage is an amplified noise (about 3 times the noise of the P1 observations),<br />

which is about 4 times larger than the noise of the Melbourne-Wübbena combination. Nevertheless,<br />

the check is useful for removing errors caused by systematic effects. It consists of an<br />

outlier rejection scheme very similar to the one used for screening the Melbourne-Wübbena<br />

combination. The starting value for the maximum RMS is larger (typically 1.6–1.8 meters<br />

for option “RMS of an arc in ionosphere free LC (L3-P3)” in panel “RNXSMT 2.3: Options”) to<br />

account for the higher noise of these observations.<br />

<strong>Bernese</strong> <strong>GPS</strong> <strong>Software</strong> <strong>Version</strong> <strong>5.0</strong> Page 105

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