At low latitudes, the day-night temperature differences due to the solar irradiation causes a pressure gradient that is directed from noon to midnight. This drives the westward zonal wind during daytime and eastward wind at night. A fast zonal wind jet band is found along the magnetic equator, rather than along the geographic equator because of the reduced ion drag effect (Liu et al., 2009). Superrotation occurs when the daily average zonal wind in the thermosphere exceeds the Earth's rotational speed, and it has measurable effects on inclination changes of the satellite orbital plane.The first superrotation study was conducted by King-Hele (1964), who interpreted satellite drag data and reported that the rotation of the atmosphere was 20% faster than that of the Earth. Using Dynamic Explorer 2 (DE2) satellite observations during 1981and 1982, Wharton et al. (1984 then reported that the equatorial zonal wind velocity exceeded the Earth's rotation by ∼18 m/s at an altitude between 200 and 700 km, and Coley and Heelis (1989) found that superrotation attained a peak at the magnetic equator. Using Challenging Minisatellite Payload (CHAMP) zonal wind data from 2002 to 2004, Liu et al. (2006 revealed that the superrotation increased from 22 m/s at the solar medium (F10.7 = 100 sfu) to 63 m/s at the solar maximum (F10.7 = 190 sfu) because the eastward wind increased with the enhanced solar activity, whereas the westward wind decreased in velocity. Rishbeth ( 2002) reported a superrotation velocity of 47 m/s at an altitude of 400 km from a Thermosphere-Ionosphere Electrodynamics General Circulation