“…The low-latitude ionospheric response to sudden stratospheric warmings (SSWs) has been an area of extreme interest in recent years [e.g., Vineeth et al, 2009;Chau et al, 2009Chau et al, , 2010Sridharan et al, 2009;Goncharenko et al, 2010a, b;Fejer et al, 2010Fejer et al, , 2011Yue et al, 2010;Rodrigues et al, 2011;Liu et al, 2011;Park et al, 2012;Yamazaki et al, 2012a, b]. These events are characterized by large-scale metereological changes in the winter polar atmosphere, driven by the rapid growth of upward propagating quasi-stationary planetary (Rossby) waves, rapid growth of waves from the polar troposphere, and their interaction with the mean circulation, that last for several days or even a few weeks [e.g., Matsuno, 1971;Andrews et al, 1987;Liu and Roble, 2002;Holton, 2004].…”