Abstract

Ionospheric scintillation frequently occurs in equatorial, auroral and polar regions, posing a threat to the performance of the global navigation satellite system (GNSS). Thus, the detection of ionospheric scintillation is of great significance in regard to improving GNSS performance, especially when severe ionospheric scintillation occurs. Normal algorithms exhibit insensitivity in strong scintillation detection in that the natural phenomenon of strong scintillation appears only occasionally, and such samples account for a small proportion of the data in datasets relative to those for weak/moderate scintillation events. Aiming at improving the detection accuracy, we proposed a strategy combining an improved eXtreme Gradient Boosting (XGBoost) algorithm by using the synthetic minority, oversampling technique and edited nearest neighbor (SMOTE-ENN) resampling technique for detecting events imbalanced with respect to weak, medium and strong ionospheric scintillation. It outperformed the decision tree and random forest by 12% when using imbalanced training and validation data, for tree depths ranging from 1 to 30. For different degrees of imbalance in the training datasets, the testing accuracy of the improved XGBoost was about 4% to 5% higher than that of the decision tree and random forest. Meanwhile, the testing results for the improved method showed significant increases in evaluation indicators, while the recall value for strong scintillation events was relatively stable, above 90%, and the corresponding F1 scores were over 92%. When testing on datasets with different degrees of imbalance, there was a distinct increase of about 10% to 20% in the recall value and 6% to 11% in the F1 score for strong scintillation events, with the testing accuracy ranging from 90.42% to 96.04%.

Highlights

  • The ionosphere, the atmosphere at about 60 to 1000 km from the ground, is modulated by the ionizing effects of solar radiation, particle precipitation and the geomagnetic field.There are some typical ionospheric phenomena, such as the equatorial ionization anomaly (EIA) and equatorial plasma bubbles at low attitudes [1,2,3], as well as the tongue of ionization at high latitudes [4,5], by which radio waves such as global navigation satellite system (GNSS) signals may be severely affected

  • Was taken into consideration in the manual detection process. This manual labelled approach combined with personal knowledge and experience can reserve the transient phases of the events and reduce the missed detections, significantly enhancing the labelling accuracy and detection performance. The goal of this approach was to propose an improved eXtreme Gradient Boosting (XGBoost) algorithm combined with the synthetic minority oversampling technique and edited nearest neighbor (SMOTE-ENN), comparing the performance with that of the decision tree and random forest algorithms, which have been successfully used in recent research [16]

  • Severe ionospheric scintillation is an adverse factor influencing the amplitude and carrier phase of a GNSS signal; its detection is a prerequisite in the design of an advanced receiver with greater accuracy, reliability and efficiency

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Summary

Introduction

The ionosphere, the atmosphere at about 60 to 1000 km from the ground, is modulated by the ionizing effects of solar radiation, particle precipitation and the geomagnetic field.There are some typical ionospheric phenomena, such as the equatorial ionization anomaly (EIA) and equatorial plasma bubbles at low attitudes [1,2,3], as well as the tongue of ionization at high latitudes [4,5], by which radio waves such as global navigation satellite system (GNSS) signals may be severely affected. When passing through the ionospheric irregularities, the signals are plagued with rapid fluctuation, phase shifts, delay, multipath, and even loss of tracking loop. This phenomenon of ionospheric scintillation occurs more frequently and severely in both low-latitude regions and polar regions, compromising positioning accuracy and continuity [6,7]. In high-latitude regions, the occurrence of ionospheric scintillation is more apparent during geomagnetic storms, and the formation of irregular structures and ionospheric scintillation activities appears to 4.0/).

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