Abstract

Global navigation satellite sensors can transmit three frequency signals. When the classical three-carrier ambiguity resolution (TCAR) is applied to long baselines of hundreds of kilometres, the narrow-lane integer ambiguity resolution (IAR) is affected by the remaining double-differenced (DD) ionospheric delays. As such, large amounts of observational data are typically needed for successful recovery. To strengthen ionospheric delays, we analysed the combination of three frequency signals and a new ambiguity-free ionospheric combination where the least amount of noise is defined, which is enhanced with epoch-differenced ionospheric delays to provide better absolute ionospheric delay and temporal change. To optimize ionosphere estimations, we propose defining the optimal smoothing length, and also propose a strategy to diagnose wrongly determined ionospheric estimations. With such ionospheric information, we can obtain the ionosphere-weighted model by incorporating the ionospheric information to the geometry-based model and use the real triple-frequency observations to evaluate our method. Our results show that the precision of ionospheric estimations from our new ionospheric model is 25% higher than that from the current combination method and that it can provide real-time smoothed ionospheric delay with magnitudes defined to the nearest centimetre. Additionally, using ionospheric estimation as a constraint, the ionosphere-weighted model requires 20% less time to generate the first-fixed solution (TFFS) than the geometry-based model.

Highlights

  • Modern navigation satellite systems can transmit three or more frequency signals

  • The standard deviation of the ionospheric delays estimated from the new method is 20% less than that from the combination method

  • Using theoretical derivations and sensitivity tests, we found that the most suitable smoothing length is 16 epochs and that the smoothed ionospheric delay could reach a magnitude of precision defined to the nearest centimetre

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Summary

Introduction

Modern navigation satellite systems can transmit three or more frequency signals. GPS and QZSS introduced the L5 signal, in addition to the current L1 and L2 signals. In real-time positioning applications, the ionospheric delay that is treated as an ionospheric constraint should be estimated with the filtering process; for the ionosphere-weighted TCAR, a crucial question is how to shorten the time to obtain more accurate ionospheric estimates In view of this requirement, we modified the previously mentioned method. Compared with other navigation systems, the GPS system has the highest observation quality and the most precise orbit/clock estimations, in addition to some Block IIF satellites in orbit that can transmit triple-frequency signals. Based on these results, we use the GPS system as an example to illustrate our method along with other systems.

On the Fundamental Combinations Concerning TCAR
The Current TCAR Method
EWL and WL Resolutions
NL Resolution
New Ionosphere-Weighted Model
New Model of Estimating DD Ionospheric Delay
Smoothed
NL Ambiguity Resolution
Experiments and Analysis
Evaluate the Precision of the Ionospheric Estimates
Findings
Value Percentage
Full Text
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