Based on the coordinated observations by the incoherent scatter radar (ISR), ionosonde, magnetometers, and GPS receivers, the electrodynamic effects on the equatorial and low-latitude ionosphere have been investigated during the intense solar flare (X1.5/2B) on 13 September 2005. In the initial stage of the flare, the ISR and ionosonde measurements at Jicamarca show the decreases of 10.14 m/s and 20 km in the upward vertical E × B drift velocity and the F 2 region peak height, respectively, while equatorial electrojet (EEJ) strength over American sector indicates a sudden increase of 53.7 nT. The decrease of the upward vertical E × B drift velocity reveals the weakening of eastward electric field during the flare, which is firstly and directly observed by instrument. It is well known that the variation of equatorial electric field is mainly attributed to the ionospheric dynamo electric field and partially affected by the penetration of interplanetary electric field. The observations during this flare suggest that the flare-induced increase of Cowling conductivity changes the ionospheric dynamo electric field and further results in the weakening of eastward electric field and the decrease of the upward vertical E × B drift velocity. Meanwhile, the upward vertical E × B drift velocity and the EEJ strength during the flare are negatively correlated, which is contrary to the knowledge established by Anderson et al. (2002) based on 10 days of observations in the Peruvian longitude sector. The difference may be caused by the flare-induced enhancement of Cowling conductivity. In addition, GPS total electron content (TEC) observations from six stations in the American equator and low latitudes show an enhancement of 1.47-3.09 TEC units. The measurements of GPS and ISR indicate that the contribution of the enhanced photoionization to the increase of TEC is more than that of electrodynamic effect during the initial stage of the intense flare.
IntroductionAs one of the severest solar events, the solar flare is an important topic of solar-terrestrial relations and current space weather research. During a flare, the large and rapid increases of solar X-ray and extreme ultraviolet (EUV) enhance the ionization of the upper atmosphere and cause many kinds of sudden ionospheric disturbances (SIDs). Since 1960s, many researchers have studied different kinds of SIDs, such as sudden cosmic noise absorption (SCNA), sudden enhancement of atmospheric (SEA), sudden phase anomaly (SPA), short wave fadeout (SWF), sudden frequency deviation (SFD), and sudden increase of total electron content (SITEC) [Garriott et al., 1967;Sao et al., 1970;Stonehocker, 1970;Donnelly, 1971;Jones, 1971;Ohshio, 1971;Deshpande and Mitra, 1972;Davies, 1980;Wan et al., 2005]. Previous works have suggested that different disturbed phenomena are attributed to the increase of electron density at different altitudes of ionosphere during flares [e.g., Mendillo and Evans, 1974;Le et al., 2007;Xiong et al., 2011]. The SCNA, SEA, SPA, and SWF are closely relat...