Abstract | ||
---|---|---|
Ionospheric scintillation can significantly degrade the performance and the usability of space-based communication and navigation signals. Characterization and prediction of ionospheric scintillation can be made from the Global Navigation Satellite System (GNSS) radio occultation (RO) technique using the measurement from a deep slant path where the RO tangent height (h(t)) is far below the ionospheric sources. In this study, the L-band S4 from the RO measurements ath(t)= 30 km is used to infer the amplitude scintillation on the ground. The analysis of global RO data ath(t)= 30 km shows that sporadic-E (Es), equatorial plasma bubbles (EPBs), and equatorial spread-F (ESF) produce most of the significant S4 enhancements, although the polar S4 is generally weak. The enhanced S4 is a strong function of local time and magnetic dip angle. The Es-induced daytime S4 tends to have a negative correlation with the solar cycle at low latitudes but a positive correlation at high latitudes. The nighttime S4 is dominated by a strong semiannual variation at low latitudes. |
Year | DOI | Venue |
---|---|---|
2020 | 10.3390/rs12152373 | REMOTE SENSING |
Keywords | DocType | Volume |
GPS radio occultation,ionospheric scintillation,electron density,plasma bubbles,polar scintillation,solar cycle | Journal | 12 |
Issue | Citations | PageRank |
15 | 0 | 0.34 |
References | Authors | |
0 | 1 |
Name | Order | Citations | PageRank |
---|---|---|---|
Dong L. Wu | 1 | 0 | 0.34 |