Abstract

We have analyzed the total electron content (TEC) derived from dual-frequency GPS receivers (GPS TEC) at the Chumpon station, Thailand, during the period 2004–2006. The diurnal, monthly, and seasonal variation in the measured TEC is compared with the TEC derived from the IRI-2007 model as well as the TEC obtained from the International GNSS service (IGS). To date, TEC data at equatorial latitudes are limited. The Chumphon station (10.72°N, 99.37°E) is located at the equatorial latitude and the dip latitude of 3°N. The TEC from the IRI-2007 model is based on the actual F2 plasma frequency (foF2) measurement. The results of our study show that the TEC derived from the IRI-2007 model agrees with the GPS TEC data mostly in the morning hours, but that it generally underestimates the GPS TEC. The maximum differences are about 15 TECU during the daytime and 5 TECU during the nighttime. The underestimation is more evident at daytime than at nighttime. The noon-bite out phenomena are clearly seen for the IRI-2007 TEC, but not on the IGS TEC and GPS TEC. The general underestimation of the IRI-2007 model can be explained from the exclusion of the plasmasphere, whereas the large difference during noon bite-outs is caused by the difference in the slab thickness in the ionosphere between the IRI-2007 model and the actual measurement. When compared with the TEC from the IGS model, the TEC measurements at Chumpon appear to be quite similar.

Highlights

  • The Global Position System (GPS), low-orbit navigation satellites, such as TRANSIT, and space technologies set the need to improve our understanding of the structure and activities of both the topside and bottomside ionospheres

  • Results of the Analysis 3.1 Diurnal variation of the GPS total electron content (TEC) and TEC from the International Reference Ionosphere (IRI)-2007 model Figure 1 shows the comparison between the diurnal median values of Global Position System TEC (GPS TEC) and IRI-2007 TEC at Chumphon station from 2004 to 2006, a period of low solar activity

  • The GPS TEC values differ from IRI-2007 TEC values at about 15 TECU

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Summary

Introduction

The Global Position System (GPS), low-orbit navigation satellites, such as TRANSIT, and space technologies set the need to improve our understanding of the structure and activities of both the topside and bottomside ionospheres. At the equatorial latitudes, such as at Chumphon station, Thailand, comparisons between TEC based on observation and that of the IRI models are scarce.

Results
Conclusion
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