On the Low-Latitude Ionospheric Irregularities under Geomagnetically Active and Quiet Conditions using NavIC observables: A Spectral Analysis Approach

TL;DR

This study analyzes low-latitude ionospheric irregularities using spectral analysis of NavIC signals, revealing irregularity scales, propagation characteristics, and their evolution during different geomagnetic conditions.

Contribution

It introduces a spectral analysis approach to estimate irregularity scale sizes and propagation patterns using NavIC data during various geomagnetic conditions.

Findings

Irregularity scales range from hundreds of meters to a few kilometers.

Strong geomagnetic events show poleward and westward propagation of irregularities.

Continuous satellite data aids in understanding irregularity evolution and propagation.

Abstract

Ionospheric irregularities and associated scintillations under geomagnetically active/quiet conditions have detrimental effects on the reliability and performance of space- and ground-based navigation satellite systems, especially over the low-latitude region. The current work investigates the low-latitude ionospheric irregularities using the phase screen theory and the corresponding temporal Power Spectral Density (PSD) analysis to present an estimate of the outer irregularity scale sizes over these locations. The study uses simultaneous L5 signal C/N$_o$ observations of NavIC (a set of GEO and GSO navigation satellite systems) near the northern crest of EIA (Indore: 22.52$^\circ$N, 75.92$^\circ$E, dip: 32.23$^\circ$N) and in between the crest and the dip equator (Hyderabad: 17.42$^\circ$N, 78.55$^\circ$E, dip: 21.69$^\circ$N). The study period (2017-2018) covers disturbed and quiet-time conditions in the declining phase of the solar cycle 24. The PSD analysis brings forward the presence of irregularities, of the order of a few hundred meters during weak-to-moderate and quiet-time conditions and up to a few km during the strong event, over both locations. The ROTI values validate the presence of such structures in the Indian region. Furthermore, only for the strong event, a time delay of scintillation occurrence over Indore, with values of 36 minutes and 50 minutes for NavIC satellites (PRNs) 5 and 6, respectively, from scintillation occurrence at Hyderabad is observed, suggesting a poleward evolution of irregularity structures. Further observations show a westward propagation of these structures on this day. This study brings forward the advantage of utilizing continuous data from the GEO and GSO satellite systems in understanding the evolution and propagation of the ionospheric irregularities over the low-latitude region.