The ionized layer of the terrestrial atmosphere from ∼90 to 600 km above sea level called ionosphere affects radio propagation due to the presence of free electrons and ions (Hargreaves, 1992). With our ever-growing technological dependence on satellites for many applications related to navigation and communication, forecasting and nowcasting of ionosphere is becoming crucial for precise positioning and navigation. However, due to unsteady primary source of its ionization, which is Sun, ionosphere is variable and exhibits normal hour-to-hour, day-to-day, seasonal, 11-year, and transient variations. Apart from the well-established solar and geomagnetic influences under space weather, it has been more or less established during the last two decades that meteorological processes also perturb the ionosphere significantly, accounting for ∼20% of daytime ionospheric variations on average (Forbes et al., 2000). This percentage share becomes more