Detector based in carrier phase data: The geometry-free combination

Fundamentals
Title	Detector based in carrier phase data: The geometry-free combination
Author(s)	J. Sanz Subirana, J.M. Juan Zornoza and M. Hernández-Pajares, Technical University of Catalonia, Spain.
Level	Advanced
Year of Publication	2011

With two frequency signals it is possible to make the carrier phase geometry free combination, in order to remove the geometry, including clocks, and all non dispersive effects in the signal. This very precise (with very low noise) test signal performs as a smooth function, driven by the ionospheric refraction, with very few changes between closely epochs. Indeed, although, for instance, the jump produced by a simultaneous 1-cycle slip in both signal components is smaller in this combination than in the original signals , it can provide a reliable detection, also for small jumps.

Figure 1: Effect of 1-cycle jump in GPS [math]\displaystyle{ \Phi_{L_1} }[/math] carrier phase signal on the ionosphere free combination. The horizontal axis is seconds of day. The vertical axis is in meters.

The easiest way to build a cycle-slip detector is just to consider the differences in time of consecutive samples (see figure 1). A refinement of this procedure is the use of the n-order differences to take benefit of the jumps amplitude enlargement produced by the differencing process (see Table 1 from [Hofmann-Wellenhof et al., 2008] ).

Table 1: Scheme of differences computation: A jump of amplitude [math]\displaystyle{ \epsilon }[/math] happens at time [math]\displaystyle{ t_4 }[/math] and its effect is propagated and amplified by the n-order differences.

Table 2: Wide-lane and Narrow-lane combinations of signals for different frequencies of GPS, GLONASS (only the channel k = 0) and Galileo. The Galileo E5 and E6 signals have not been included to simplify the table.

This approach allows making a reasonable enough detector for many applications. Nevertheless, it must be taken into account that as the jumps are enlarged also the signal noise (i.e., signal instabilities) is amplified, which can lead to false detections in some scenarios (for instance with low signal to noise ratios, ionospheric scintillation…).

A way to mitigate the impact of these effects is to use a low order polynomial fit, reducing the test signal noise. This concept is the basis of the detector's example presented as follows:

Algorithm description:

The detection is based on fitting a second degree polynomial over a sliding window of [math]\displaystyle{ N_I }[/math] samples (e.g., [math]\displaystyle{ N_I=10 }[/math]). The predicted value from this polynomial is compared with the observed value to detect the cycle-slip. As the geometry-free combination is affected by the ionospheric refraction, a sampling rate dependent threshold is considered.

Input data: Geometry-free combination of carrier phase measurements. [math]\displaystyle{ \Phi_{L_I}(s;k)=\Phi_1(s;k)-\Phi_2(s;k) }[/math]

Output: satellite (PRN), time, cycle-slip flag

For each epoch ([math]\displaystyle{ k }[/math])

For each tracked satellite ([math]\displaystyle{ s }[/math])

• Declare cycle-slip when data hole greater than [math]\displaystyle{ tol_{\Delta t} }[/math]
• Fit a second degree polynomial [math]\displaystyle{ P(s;x) }[/math] to the previous values (after the last cycle-slip) [math]\displaystyle{ \Phi_{L_I}(s;k-N_I),\dots,\Phi_{L_I}(s;k-1)] }[/math].
• Compare the measured [math]\displaystyle{ \Phi_{L_I}(s;k) }[/math] and the predicted value [math]\displaystyle{ P(s;k) }[/math] at the epoch [math]\displaystyle{ k }[/math]. If the discrepancy is over a given [math]\displaystyle{ threshod }[/math], thence declare cycle-slip. That is:

If [math]\displaystyle{ |\Phi_{L_I}(s;k)-P(s;k)| \gt Threshold }[/math],

Thence, cycle-slip.

• Reset algorithm after cycle slip.

End

End

Comments:

The relative variation between two consecutive epochs [math]\displaystyle{ t_1 }[/math] and [math]\displaystyle{ t_2 }[/math] depends of the elapsed time interval in between (i.e., [math]\displaystyle{ \Delta t=t_2-t_1 }[/math]), due to the ionospheric refraction variation. Thence, a [math]\displaystyle{ \Delta t }[/math]-dependent threshold is recommended to account for the measurement sampling rate. For instance: [math]\displaystyle{ Threshod=a_0-a_1 \, \exp(-\Delta t/T_0) }[/math] can be used.

Notice that [math]\displaystyle{ a_0 }[/math] is the maximum threshold. On the other hand, taking for instance [math]\displaystyle{ a_1=a_0/2 }[/math], thence the threshold is [math]\displaystyle{ a_0 [1-\frac{e^{-\Delta t/T_0}}{2}] }[/math], which, for [math]\displaystyle{ T_0=60 }[/math] seconds, corresponds to about [math]\displaystyle{ a_0/2 }[/math] for [math]\displaystyle{ 1 }[/math] second sampling rate and about [math]\displaystyle{ 2a_0/3 }[/math] for [math]\displaystyle{ 30 }[/math] seconds sampling rate data. In this way, if [math]\displaystyle{ a_0 }[/math] is set as [math]\displaystyle{ a_0=\frac{3}{2}(\lambda_2-\lambda_1) }[/math], the minimum detectable jump, between two contiguous measurements, will be [math]\displaystyle{ \frac{3}{4}(\lambda_2-\lambda_1) }[/math] or [math]\displaystyle{ \lambda_2-\lambda_1 }[/math] for [math]\displaystyle{ 1 }[/math] second or [math]\displaystyle{ 30 }[/math] seconds sampling rate, respectively

Figure 2: The effect of a jump in the integer ambiguities is given in the equations above.