The ionosphere is an ionized part of the upper atmosphere, spanning from 60 to around 1,000 km in altitude (Hargreaves, 1992). It arises mainly due to the photoionization effects from the solar extreme ultraviolet (EUV) radiation and charged energetic-particle precipitation (Kivelson & Russell, 1995). Generally, the ionosphere is strongly coupled with the thermosphere (Astafyeva, 2019). The latter supplies the neutral particles that can be ionized, and plays a crucial role in the interplay between the production (source) and recombination (loss) processes. The ionosphere affects the propagation of the Global Navigation Satellite System (GNSS) signals by introducing frequency-dependent delays. Unlike the neutral atmosphere, which can cause errors in navigation and positioning in the order of several meters, ionospheric effects can yield uncertainties of up to E 100 m (e.g., Hernández-Pajares et al., 2011;Petit & Luzum, 2010). Ionospheric delays are inversely related to the square of carrier frequency, and directly proportional to electron density integrated along the ray path (e.g., Goss et al., 2019;Hobiger & Jakowski, 2017).Electron density distribution in the ionosphere strongly depends on altitude and can be divided into several layers, originally identified from ionograms: the D-layer (60-90 km altitude), E-layer (90-130 km), and F-layer (above 130 km), which can be subdivided into F1 and F2 layers (e.g., Astafyeva, 2019). The dominant contribution to electron density profiles comes from the peak of the F2 layer, generally located between