Experimental Determination of the Ionospheric Effects and Cycle Slip Phenomena for Galileo and GPS in the Arctic

S. S. Beeck, C. N. Mitchell, A. B.O. Jensen, L. Stenseng, T. Pinto Jayawardena, D. H. Olesen

Research output: Contribution to journalArticlepeer-review

1 Citation (SciVal)

Abstract

The ionosphere can impair the accuracy, availability and reliability of satellite-based positioning, navigation and timing. The Arctic region is particularly affected by strong ionospheric gradients and phase scintillation, posing a safety issue for critical infrastructure and operations. Ionospheric warning and impact maps can provide support to Arctic operations, but to produce such maps threshold values have to be determined. This study investigates how such thresholds can be derived from the GPS and Galileo satellite signals. Rapid changes in total electron content (TEC) or scintillation-induced receiver tracking errors could result in cycle slips or even loss of lock. Cycle slips and data outages are used as a measure of impact on the receiver in this paper. For Galileo, 73.6% of the impacts were cycle slips and 26.4% were outages, while for GPS, 29.3% of the impacts were cycle slips and 70.7% were outages. Considering the sum of cycle slips and outages, it is worth noting that the sum of impacts for Galileo signals is larger than for GPS. A range of possible explanations have been examined through hardware-in-the-loop simulations. The simulations showed that the GPS L2 signal was not adequately tracked during rapid TEC changes and TEC changes were underestimated, thus the GPS cycle slips, derived from L1 and L2 derived TEC changes, were not all registered. These results are important in designing threshold values for TEC and for scintillation impact maps as well as for the operation of GNSS equipment in the Arctic. In particular, the results show that ionospheric changes could be underestimated if GPS L1 and L2 were used in isolation from other dual frequency combinations. It is the first time this analysis has been made for Greenland and the first time that the dual frequency derivation of ionospheric delay using GPS L1 and L2 has been shown to underestimate large TEC gradients. This has important implications for informing GNSS operations that rely on GPS to provide reliable estimates of the ionosphere.

Original languageEnglish
Article number5685
JournalRemote Sensing
Volume15
Issue number24
DOIs
Publication statusPublished - 11 Dec 2023

Bibliographical note

Publisher Copyright:
© 2023 by the authors.

Funding

C.N.M. has received funding from NERC grant number NE/W003074/1. C.N.M. acknowledges support from a Royal Society Industry Fellowship. S.S.B. acknowledges DALO for funding part of her PhD studies. This study was made possible by access to data from the SWADO network which is operated by DTU on behalf of the Danish Defence and from the GNET owned by SDFI. Also important was access to the Spirent GSS7000 simulator at the University of Bath which made it possible to test the response of the GPS and Galileo signals to the same ionospheric disturbance under the exact same environment conditions. UNAVCO is acknowledged for developing and making the TEQC software version 2019Feb25 available.

FundersFunder number
DALO
Natural Environment Research CouncilNE/W003074/1
Royal Society

Keywords

  • Arctic
  • cycle slip
  • Galileo
  • GNSS
  • Greenland
  • ionosphere
  • scintillation
  • sigma phi
  • signal tracking
  • space weather

ASJC Scopus subject areas

  • General Earth and Planetary Sciences

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