“…The former, m1Es, is the type which represents a sharply stratified and highly ionized cloud while the latter, m2Es, is the type of sporadic-E layer which consists of many small size blobs not highly ionized. Rocket observation of the electron density profile has supported this classification of m1Es and m2Es [Seddon, 1962;Smith, 1965Smith, , 1966Bowlill, 1966]. The theoretical base for formation of m1Es has mainly been the wind shear mechanisms as discussed by many authors [Dungey, 1958;Axford, 1961, 1963, 1964, Whitehead, 1961Layser,1964 ;Hines, 1964;Axf ord and Cunnold, 1966].…”