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Palabras clave – provistas por la editorial

electron temperature; topside ionosphere; ESA Swarm satellites; International Reference Ionosphere model; Langmuir Probes in-situ data; Incoherent Scatter Radar data; GNSS; GBAS; ionospheric gradient anomaly; one class support vector machine; earthquake; pre-earthquake anomalies; swarm satellites; ionospheric plasma; deep learning; physical mechanisms; τ; geomagnetic equator; magnetic storm; ionosphere; vertical pulse sounding; ionosonde; ionogram; software-defined radio; radar imaging; aspect angle; field-aligned plasma irregularities; mid-latitude E region; norm-constrained Capon; VHF radar; plasma turbulence; ionospheric irregularities; ionosphere F region; high latitude; pressure-gradient current; diamagnetic current; swarm measurements; oblique ionogram; automatic inversion; electron density profile; quasi-parabolic segments; the sporadic E layer; internal fine structure; high-resolution ionosphere imaging; frequency domain interferometry technique; auroral ionosphere; E × B plasma motion; ionospheric scintillation; GNSS-R; CYGNSS; earthquakes; polar ionosphere; VIPIR; Dynasonde; Jang Bogo Station (JBS); Antarctica; solar eclipse; precise point positioning; total electron content; rate of total electron content index; Swarm satellite measurements; electron density; main ionospheric trough; high latitude trough; ring ionospheric trough; low latitude trough; auroral diffuse precipitation; n/a