Abstract

Single-frequency Global Positioning System (GPS) receivers do not accurately compensate for the ionospheric delay imposed upon a GPS signal. They rely upon models to compensate for the ionosphere. This delay compensation can be improved by measuring it directly with a dual-frequency receiver, or by monitoring the ionosphere using real-time maps. This investigation uses a 4D tomographic algorithm, Multi Instrument Data Analysis System (MIDAS), to correct for the ionospheric delay and compares the results to existing single and dualfrequency techniques. Maps of the ionospheric electron density, across Europe, are produced by using data collected from a fixed network of dual-frequency GPS receivers. Single-frequency pseudorange observations are corrected by using the maps to find the excess propagation delay on the GPS L1 signals. Days during the solar maximum year 2002 and the October 2003 storm have been chosen to display results when the ionospheric delays are large and variable. Results that improve upon the use of existing ionospheric models are achieved by applying MIDAS to fixed and mobile single-frequency GPS timing solutions. The approach offers the potential for corrections to be broadcast over a local region, or provided via the internet and allows timing accuracies to within 10 ns to be achieved.

Highlights

  • The Global Positioning System (GPS) allows a user to solve for their position and time virtually anywhere in the world

  • The aim of this paper is to show that the accuracy of a single-frequency GPS timing solution can be improved by using 4D tomographic mapping to reduce the ionospheric delay

  • These figures illustrate the performance of Multi Instrument Data Analysis System (MIDAS) in comparison to other GPS timing solutions and in increasing order, the general accuracy is: no correction, Klobuchar, International Reference Ionosphere (IRI) 2001, MIDAS and dual-frequency

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Summary

Introduction

The Global Positioning System (GPS) allows a user to solve for their position and time virtually anywhere in the world. Civilians commonly use GPS receivers for satellite navigation. They operate on a singlefrequency, the L1 channel and are compact and affordable. Their accuracy is hindered by the ionospheric delay, which is the cause of the largest error in a single-frequency solution (Langley, 1997). This delay is largely removed by dual-frequency GPS receivers, J.A.R. Rose, D.J. Allain and C.N. Mitchell which provide more accurate solutions and are used by the scientific community towards atmospheric monitoring for example. Dual-frequency receivers are more expensive than standard single-frequency receivers and in extreme ionospheric conditions, are susceptible to losses of lock on the L2 signal, which corrupts the GPS solution

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