Sporadic-E layers, also known as Es or tidal ion layers (TIL), are enhanced ionization patches that can be observed mostly at the height from 90 to 120 km in the mesosphere and low thermosphere (MLT) region where the background wind varies drastically and ion-neutral particles collide violently. Es layers can significantly affect the propagation of radio waves in the ionosphere, hence playing an important role in the navigation systems, HF/ VHF communication, surveillance, etc. (Davies, 1990;McNamara, 1991).Formation of the middle-and low-latitude Es layers is generally explained by the Windshear Theory, in which the zonal and meridional winds provide vertical wind shear convergence nodes. As a result, long-lived metallic ions, derived from meteor ablation and deposition, are forced to converge toward the wind shear null to form a thin layer of enhanced metallic ionization (Mathews, 1998;Whitehead, 1989). The details of the Windshear Theory can be seen in the reviews by Whitehead (1970Whitehead ( ), (1989, Mathews (1998), Haldoupis (2012, and references therein.In the past 60 years, the mechanism of Es layer formation has been a subject of intense research based on observations from radiowave remote sensing techniques, such as ionosondes, radars, GNSS receivers, as well as in situ rocket measurements (e.g.