Ionosphere products that are relatively precise are available thanks to the efforts of the International GNSS Service (IGS), and it might be possible to obtain a high success rate for the fixed integer ambiguities for medium- or longer-baseline ambiguity resolution (AR) using the ionosphere products as a priori information constraints. In this study, we used the IGS precise ionosphere products as a priori information before forming double-difference (DD) measurement equations using only original observables in a mid-range relative positioning and estimated the ionosphere residuals explicitly after DD. Furthermore, we proposed a sequential and partial ambiguity resolution (SPAR) strategy under the integer least square condition to realize fast and reliable AR. To demonstrate our proposed strategy, we randomly selected seven baselines ranging from 30 to 111 km and undertook positioning in a post-processing mode using real GPS dual-frequency data. According to the results, the SPAR strategy has a faster convergence process compared with batch AR. For instance, the convergence time with >90 % cumulative frequency percentage (probability) for 30, 40, 56, 66, 80, 95, and 111 km baselines was advanced by 55, 50, >75, 85, >110, 65, and >35 epochs, respectively, with a 30-s sample interval. By considering ionospheric correction before DD, we found further improvement in the initialization performance with the use of the SPAR strategy.
Keywords
GPSMedium-range relative positioningSequential and partial ambiguity resolutionConvergence timePrecise ionosphere consideration
Background
Real-time kinematic (RTK) positioning, which is known for its precision, has been used widely as positioning technology in many fields of engineering and science. The situation is relatively simple for short-baseline (<10 km) RTK under 10 km. The double difference (DD) of satellite observables between rover and base stations mostly eliminates atmospheric delay errors, and the ambiguity resolution process usually employs the least squares ambiguity decorrelation adjustment (LAMBDA) method (Teunissen 1995) that is efficient in delivering reliable fixed integer ambiguities. After comparison of four ambiguity resolution (AR) methods: LAMBDA, geometry-free models for three-carrier ambiguity resolution (TCAR) (Forssell et al. 1997; Vollath et al. 1998), geometry-based TCAR (Teunissen et al. 2002; Feng and Li 2008, 2009), and GIF-TCAR (TCAR based on a geometry-free and ionosphere-free combination) (Wang and Rothacher 2013), Zhang and He (2015) highlighted that the LAMBDA method is optimal in both short- and medium-baseline (10–100 km) cases. Li et al. (2015) developed a reliable AR strategy that efficiently resolves ambiguities sequentially under the integer least square (ILS) condition (Teunissen 1995) for the case of short-range RTK. However, for medium or long baselines (>100 km), large ionospheric delay residuals remain after DD. The conventional method for overcoming this problem is to use ionosphere-free linear combinations (LCs) of the original observables and to accommodate AR using a sequential rounding process of wide-lane (WL) and narrow-lane (NL) ambiguities (Takasu and Yasuda 2010). Unfortunately, the LCs of the original measurements amplify the observable noise and lead to the inevitable addition of positioning error. Therefore, for longer-baseline RTK, it is better to use original observables to limit the propagation of measurement noise. Li et al. (2014) developed efficient procedures for improved float solutions and ambiguity fixing over long-baseline RTK without using ionosphere-free measurements, although the WL AR process remained a rounding process. In fact, simple rounding schemes for WL and NL ambiguities cannot ensure high reliability of fixed integer ambiguities. Teunissen (1999) provided proof that an ILS estimator of the carrier-phase ambiguities is best for maximizing the probability of correct integer estimation. Hence, the AR process should be performed under an ILS condition to ensure the reliability of the fixed integer ambiguities. Nevertheless, validation of the batch AR mode by the LAMBDA method might still fail because of biases in some estimated float ambiguities (Takasu and Yasuda 2010), especially in the case of long baselines. Therefore, the partial AR technique was developed, which resolves a subset of the ambiguities to overcome this condition (Teunissen et al. 1999).
Ionosphere products that are relatively precise are available owing to the efforts of the International GNSS Service (IGS), and it might be possible to obtain a high success rate for the fixed integer ambiguities for medium- or longer-baseline AR using the ionosphere products as a priori information constraints. Considering the problems mentioned above, we used the IGS precise ionosphere products as a priori information before forming the DD measurement equations using only original observables in a mid-range RTK and estimated the ionosphere residuals explicitly after DD. Furthermore, we propose a sequential and partial ambiguity resolution (SPAR) strategy under the ILS condition to realize fast and reliable AR. In the following, we offer a detailed description of the proposed SPAR strategy. We compare the initialization performances of the SPAR and batch AR strategies and investigate the influence of a priori ionosphere information on the efficiency of the SPAR strategy.
Sequential and partial ambiguity resolution (SPAR) strategy
For clarity, a flowchart of this strategy is presented in Fig. 1.
Fig. 1
Flowchart of the sequential and partial ambiguity resolution strategy (amb ambiguity)
After the ordinary least square adjustment stage in relative positioning, we can obtain the real-value estimates and their variance–covariance matrix (dual-frequency case):
where \(\hat{B}_{1}\) and \(\hat{B}_{2}\) are the DD carrier-phase ambiguity estimates on carrier waves L1 and L2, respectively, which should be integers, and \(\hat{X}\) represents the estimates of the remaining unknowns, including the baseline components (coordinates), tropospheric parameters, and ionospheric parameters.
For medium- or longer-baseline RTK, because of the biases in some float ambiguities, batch AR by the LAMBDA method might still not pass the validation step. Therefore, the partial AR technique, which resolves a subset of the ambiguities, is implemented to obtain a high success rate (Teunissen et al. 1999; Zinas et al. 2013; Wang and Feng 2013). The success rate and ratio test are different indicators with which to assess the reliability of the fixed ambiguities (Euler and Schaffrin 1990; Teunissen 1998; Hassibi and Boyd 1998; Teunissen and Verhagen 2008; Wang and Feng 2013). The selection of the ambiguity subset, however, is not unique, and it could be based on the float ambiguity variance, elevation angle, and LCs (Mowlam and Collier 2004). Parkins (2011) described an algorithm for resolving a subset of ambiguities with validation from previous epochs in single-epoch RTK positioning (Wang and Feng 2013). Takasu and Yasuda (2010) employed a very simple criterion involving the satellite elevation angle for long-baseline RTK. Li et al. (2015) chose a subset that comprised all the extra-WL or WL ambiguities in a multi-frequency case, because the extra-WL or WL ambiguities suffer relatively low effects from noise and they can be easily resolved reliably. They also indicated the possibility of resolving the ambiguities sequentially when the corresponding success rate is very close to the batch AR mode and they proposed a multi-carrier fast partial ambiguity resolution strategy that they tested with short baselines.
For longer baselines, WL ambiguity resolution will be affected inevitably by the biases in the measurements. Thus, a subset that contains all the WL float ambiguities without distinction might not be the best choice, and consequently, there is a need to optimize the subset. Here, we propose an optimization method that works in an iterative scheme to fix the float ambiguities with low variance. The ratio test (Euler and Schaffrin 1990) is used here for ambiguity validation. The ratio test in fact calculates the closeness of the float ambiguity \(\hat{B}\) to its nearest integer \(\bar{B}\) compared to the second nearest integer \(\bar{B}^{{\prime }}\), and it reads as:
where \(q\left( B \right) = \left( {\hat{B} - B} \right)^{\text{T}} Q_{{\hat{B}}}^{ - 1} \left( {\hat{B} - B} \right)\), and c is a tolerance value, to be determined by user. In general, c can be chosen 1.5, 2, 3 (Leick 2004; Wang and Feng 2013). In our validation step, we chose the critical value 3.
Different from the direct batch AR mode, we first conduct a transformation:
After transformation, the ambiguity types are \(\hat{B}_{\text{WL}}\) and \(\hat{B}_{1}\) instead of the previous \(\hat{B}_{1}\) and \(\hat{B}_{2}\). This transformation is fundamental in our proposed strategy for introducing the WL ambiguity type.
According to the law of error propagation, the variance–covariance matrix of \(\hat{Y}\) is:
Based on this, we propose the SPAR strategy, outlined below.
Step 1 Resolve the WL ambiguities first using the LAMBDA method; the validation technique used here is the popular ratio test with a critical threshold value of 3. Actually, this is the partial AR idea that resolves a subset of the entire float ambiguities. As the biases in the measurements have the least effect on the resolution of WL ambiguities, a subset that comprises all the WL float ambiguities is reasonable (Li et al. 2015). However, for a longer baseline, WL AR could be disturbed by measurement noise, meaning that it is not possible to select all the float WL ambiguities without distinction. When the validation test fails, our optimizing method deletes the float WL ambiguity with the maximum variance (which is considered the one disturbing the WL AR process) from \(\hat{B}_{\text{WL}}\), and then repeats the resolution and test until the validation test is passed, which provides the integer solution \(\bar{B}_{\text{WL}}\).
Step 2 Update \(\hat{X}\), \(\hat{B}_{1}\), and their variance–covariance matrix together with the fixed solution \(\bar{B}_{\text{WL}}\). In this step, the remaining float ambiguities on the L1 frequency and other parameters are not distinguished. The formula for the update is as below (Teunissen 1995):
Step 3 Resolve the remaining ambiguities on the L1 frequency using the LAMBDA method and repeat the entire process from Step 1 to obtain the remaining integer ambiguities \(\bar{B}_{1}\).
Step 4 Obtain the fixed solution of the remaining unknowns using the formulas below:
Step 5 Change back. Conduct the inverse transformation of (3).
The fundamental concepts of this strategy involve resolving the WL ambiguities and the ambiguities on the L1 frequency sequentially, and optimizing the selected ambiguity subset circularly based on the estimated ambiguity variance, as long as the validation test fails.
Experiment demonstration
Figure 2 displays the distribution of our experimental stations. We randomly selected seven baselines of the EUREF Permanent Network (EPN) and used their 3-day GPS dual-frequency observational data with a 30-s sampling interval, starting from day-of-year (DOY) 152 to DOY 154 in 2015. The detailed information of the data is presented in Table 1.
Fig. 2
Station distribution
Table 1
Information of selected baselines in EUREF
Approximate length (km)
Base station ID
Rover station ID
31
EIJS
WARE
40
DOUR
REDU
56
GOPE
CTAB
66
CRAK
MARJ
80
BRUX
DOUR
95
CLIB
CPAR
111
CPAR
KUNZ
In the positioning process, we tested our strategy in a post-processing mode. We estimated the residual ionospheric and tropospheric delay errors explicitly after determining the DD of the satellite observables between the rover and base stations. The relative positioning system was reset every 2 h to obtain a sufficient number of initialization samples; thus, there were almost 36 initializations for each baseline during the study period. For each initialization, we were interested in the corresponding convergence time. A simple representation of the convergence time adopted here is the time (measured in epochs) at which no less than 90 % of the ambiguities are resolved, with the restriction that the components of the positioning errors are <10 cm. Because of noise in the observations, these 36 initializations do not perform consistently. Therefore, for both the batch AR and SPAR strategies, we drew pictures of the cumulative distribution histograms of the convergence time corresponding to the 36 initializations of one baseline (Figs. 3, 4, 5, 6, 7, 8, 9).
Fig. 3
Cumulative distribution histograms of the convergence time for EIJS–WARE (30 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 4
Cumulative distribution histograms of the convergence time for DOUR–REDU (40 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 5
Cumulative distribution histograms of the convergence time for GOPE–CTAB (56 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 6
Cumulative distribution histograms of the convergence time for CRAK–MARJ (66 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 7
Cumulative distribution histograms of the convergence time for BRUX–DOUR (80 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 8
Cumulative distribution histograms of the convergence time for CLIB–CPAR (95 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
Fig. 9
Cumulative distribution histograms of the convergence time for CPAR–KUZE (111 km) baseline: (left) batch ambiguity resolution strategy and (right) sequential and partial ambiguity resolution strategy
It is obvious that the SPAR strategy demonstrates amazing efficiency. Taking the 31-km baseline as an example, it can be seen that the cumulative frequency percentage (probability) of the convergence time under 55 epochs is >90 % when using the SPAR strategy. Conversely, under the batch AR strategy, the probability of the convergence time under 55 epochs is only 50 % and actually 110 epochs are needed to achieve the probability of the convergence time of >90 %. For each baseline, we recorded the corresponding convergence time when the probability in the cumulative distribution histogram was >90 % for both strategies and the results are listed in Table 2. It can be seen that the SPAR strategy is always faster than the batch AR strategy. Interestingly, for the baselines GOPE–CTAB, BRUX–DOUR, and CPAR–KUNZ, the probabilities of the convergence time are all <90 % during the 2-h interval purposely designed in our program when using the batch AR strategy, whereas the probabilities of the convergence time are all >90 % when using the SPAR strategy, corresponding to 165, 130, and 205 epochs, respectively. We speculate that this is mainly due to the large ionosphere delay residuals after DD in the case of these baselines. Since SPAR strategy inherently suffers relatively low effect in the biases of observables, it will perform still faster even toward large ionosphere residuals.
Table 2
Comparison of initialization performance for the two strategies and comparison of initialization performance for two ionosphere correction models applied in SPAR strategy
Baseline length (km)
Convergence time (epoch) with cumulative frequency percentage ≥90 %
Convergence time (epoch) with cumulative frequency percentage ≥90 % for SPAR strategy
Batch AR
SPAR
Broadcast model
IONEX TEC model
31
110
55
55
55
40
130
80
60
60
56
>240
165
175
160
66
230
145
110
110
80
>240
130
75
75
95
130
65
60
60
111
>240
205
190
170
Currently, relatively precise ionosphere products are available owing to the efforts of the IGS, and it is possible to obtain a high success rate for the fixed integer ambiguities for medium- or longer-baseline AR using the ionosphere products as a priori information constraints in a post-processing mode. Therefore, we considered performing the ionosphere correction first to further reduce the ionospheric delay errors and then to estimate the ionosphere residuals explicitly in the DD equations. We applied two ionosphere models: the broadcast ionosphere model and the precise IGS ionosphere vertical total electron content (TEC) products which is in ionosphere exchange (IONEX) format to former seven baselines and performed the experiment again using the proposed SPAR strategy. The cumulative distribution histograms of the convergence time for both models are presented in Figs. 10, 11, 12, 13, 14, 15, and 16. Again, we recorded the convergence time when the probability in the cumulative distribution histogram was >90 % and the results are listed in Table 2. For the baseline of 31 km, there appears to be no improvement in the convergence time after considering the ionosphere correction. This is because the DD operation eliminates most of the ionospheric delay errors, which makes the correction redundant at this relatively short range. However, for longer baselines, dramatic improvements in the convergence time can be seen. For instance, the convergence time with >90 % cumulative frequency percentage is only 75 epochs for the baseline BRUX–DOUR (80 km), after applying the ionosphere correction models in the SPAR strategy, which is a considerable improvement on the original 130 epochs. But for the baseline GOPE–CTAB (56 km), broadcast ionosphere model correction seems not to bring improvement on the convergence time. We think this probably results from the low precision in the broadcast model. Interestingly, there appears to be no obvious difference between the two ionosphere models applied in the SPAR strategy for these baselines, except the 56 km and the 111 km baselines. From the convergence time results of the GOPE–CTAB (56 km) and the CPAR–KUNZ (111 km) baselines, it seems that the more precise IONEX TEC model leads to faster AR in comparison with the broadcast model when using our SPAR strategy.
Fig. 10
Cumulative distribution histograms of the convergence time for EIJS–WARE (30 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model (right) correction in sequential and partial ambiguity resolution strategy
Fig. 11
Cumulative distribution histograms of the convergence time for DOUR–REDU (40 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Fig. 12
Cumulative distribution histograms of the convergence time for GOPE–CTAB (56 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Fig. 13
Cumulative distribution histograms of the convergence time for CRAK–MARJ (66 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Fig. 14
Cumulative distribution histograms of the convergence time for BRUX–DOUR (80 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Fig. 15
Cumulative distribution histograms of the convergence time for CLIB–CPAR (95 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Fig. 16
Cumulative distribution histograms of the convergence time for CPAR–KUZE (111 km) baseline: (left) broadcast ionosphere model correction and (right) IONEX TEC model correction in sequential and partial ambiguity resolution strategy
Conclusions
In this work, we proposed a SPAR strategy for a dual-frequency case with estimation of atmosphere residuals for medium- and longer-baseline relative positioning. The fundamental concepts of this strategy involve resolving the WL ambiguities and the ambiguities on the L1 frequency sequentially, and optimizing the selected ambiguity subset circularly based on the estimated ambiguity variance, as long as the validation test fails. Tested using real GPS dual-frequency data of seven mid-range baselines in a post-processing mode, our strategy was shown always to be faster than the batch AR mode. The convergence time with >90 % cumulative frequency percentage in our samples for randomly chosen 30, 40, 56, 66, 80, 95, and 111 km baselines was advanced by 55, 50, >75, 85, >110, 65, and >35 epochs, respectively, with a 30-s sample interval. We undertook ionosphere corrections for each baseline before considering the DD of the satellite observables with the intention of reducing the ionospheric delay errors further. The results showed that after considering ionosphere correction, our proposed strategy worked faster; however, differences between the ionosphere models applied with our strategy were not obvious, which means it is acceptable to use the broadcast model with our SPAR strategy in such mid-range circumstances. Further investigation is necessary to do to test our proposed strategy in different positioning modes.
Notes
Declarations
Authors’ contributions
All the authors contributed to the design of the proposed algorithm. SZ came up with the idea of partial optimization in the algorithm. XL and BC participated in the experimental analysis. LZ carried out the experiments and drafted the manuscript. All authors read and approved the final manuscript.
Acknowledgements
This work is supported by Grants from the National Natural Science Foundation of China (Nos. 41304027 and 41274033) and the National Basic Research Program of China (973 Program) (Grant No. 2013CB733301). The authors are also very grateful to the open source software RTKLIB and EPN for providing GPS dual-frequency data.
Competing interests
The authors declare that they have no competing interests.
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
Authors’ Affiliations
(1)
School of Geodesy and Geomatics, Wuhan University
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