Abstract

Problem Statement: Ionospheric scintillations, which cause significant effects on satellite signals for communication and navigation, often takes place in equatorial region such as Malaysia. However, this disturbance are not fully understand due to few studies performed. This research reports the study and monitoring activity on Total Electron Content (TEC) and ionospheric scintillation in Malaysia using GPS measurements. Approach: One dual-frequency GPS receiver was positioned at the main station in Parit Raja, West Malaysia (1.86° N, 103.8° E) and Sipitang, East Malaysia (5.10° N, 115.56° E) respectively. Dual-frequency GPS data collected during the one-month ionospheric experimental campaign was used for TEC and scintillation computation and analysis. The TEC with 15 sec interval were computed from combined L1 and L2 code-pseudorange and carrier phase measurements. Whereas, the scintillation parameter S4 index was computed as a standard deviation of the received signal power normalized to average signal power every 60 sec on L1. A corrected S4 (without noise effects) was also computed and used in the analysis. Results: It was found that the daily maxima vTEC for Parit Raja (PR) ranged from 38-100 TECU, which is generally higher than those of Sipitang, which ranged from 30-42 TECU. However, a general consistency for both stations can be seen during the 1 month campaign period. Conclusions/Recommendations: In conclusion, these results show good agreement in the existence of the equatorial anomaly observed during moderate solar flux conditions and undisturbed geomagnetic condition. This will contributes to the knowledge of equatorial ionosphere and help in space weather condition. However, to better understand and characterize the ionosphere over Malaysia, more campaigns should be encouraged.

Highlights

  • The ionospheric disturbances cause significant effects on satellite signals for communication and navigation, which are dependent on the signal frequency and the ionospheric electron content

  • The ionospheric parameters were further compared to the main observatory at Wireless and Radio Science Centre (WARAS), Parit Raja, Batu Pahat, which is located at latitude 1.86° N and longitude 103.8° E at an altitude of 7.3 m

  • It is noted that the daily maxima vTEC for Parit Raja (PR) with values ranging from 38-100 TECU during the campaign period

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Summary

INTRODUCTION

The ionospheric disturbances cause significant effects on satellite signals for communication and navigation, which are dependent on the signal frequency and the ionospheric electron content. The ionosphere morphology is mainly due to the temporal and diurnal variability of the electron density This is dependent on the solar and geomagnetic activity of the earth. There are significant differences in the structure and effect on radio propagation of the ionosphere at these latitudes including the equatorial electrojet and accompanying equatorial anomaly, greater absorption and the geomagnetic field orientation being nearly horizontal. Not all these phenomena are completely understood because there are fewer observations here than at higher latitudes. The ionospheric parameters were further compared to the main observatory at Wireless and Radio Science Centre (WARAS), Parit Raja, Batu Pahat, which is located at latitude 1.86° N and longitude 103.8° E at an altitude of 7.3 m

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