The Thermosphere-Ionosphere (TI) system of the Earth is externally forced by waves from the lower atmosphere and energy and momentum inputs from the sun through solar irradiance and solar wind energetic particles. The solar irradiance controls the thermospheric background neutral density and temperature through heating by the extreme ultraviolet radiation, one form of solar forcing. Another form of solar forcing comes from solar energetic charged particles from coronal mass ejection, high-speed streams, and corotating interaction regions. These charged particles behave like a plasma and are termed as the solar wind. The solar wind magnetic field, depending on its directionality, reconnects with Earth's magnetic field, transporting the solar wind energetic charged particles into the Earth's magnetosphere. Due to magnetosphere and ionosphere coupling through precipitation and electric fields, currents and resulting joule heating are produced, which perturbs the TI system. These perturbations then spread globally transporting energy and momentum. The transport happens through a high to lower latitude circulation induced by the heating and through Traveling Atmospheric Disturbance, that transports energy into the mid-to low-latitudes (Burns et al., 1995). Depending on the storm strength it can take from ∼3 hr