SA31D-2369
Long Duration Enhancement And Depletion Observed In The Topside Ionospheric Electron Content During The March 2015 Strong Storm

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Jiahao Zhong1, Wenbin Wang2, Xinan Yue3, Alan Geoffrey Burns4, Xiankang Dou1 and Jiuhou Lei5, (1)University of Science and Technology of China, Hefei, China, (2)High Altitude Observatory, Boulder, CO, United States, (3)UCAR, Boulder, CO, United States, (4)National Center for Atmospheric Research, Boulder, CO, United States, (5)USTC University of Science and Technology of China, Hefei, China
Abstract:
Up-looking total electron content (TEC) measurements from multiple low Earth orbit (LEO) satellites have been utilized to study the topside ionospheric response to the 17 March 2015 great storm. The combined up-looking TEC observations from these LEO satellites are valuable in addressing the local time and altitudinal dependences of the topside ionospheric response to geomagnetic storms from a global perspective, especially over the southern hemisphere and oceans. In the evening sector, the up-looking TEC showed an obvious long-duration of positive storm effect during the main phase and a long duration of negative storm effect during the recovery phase of this storm. The increases of the topside TEC during the main phase were symmetric with respect to the magnetic equator, which was probably associated with penetration electric fields. Additionally, the up-looking TEC from different orbital altitudes suggested that the negative storm effect at higher altitudes was stronger in the evening sector. In the morning sector, the up-looking TEC also showed increases at low and middle latitudes during the storm main phase. Obvious TEC enhancement can be also seen over the Pacific Ocean in the topside ionosphere during the storm recovery phase. These results imply that the topside ionospheric responses significantly depend on local time. Thus, the LEO-based up-looking TEC provides an important database to study the possible physical mechanisms of the topside ionospheric response to storms.