High‐time resolution measurements of upstream magnetic field and plasma conditions during flux transfer events at the Earth's dayside magnetopause

We present preliminary results of a study of upstream magnetic field and plasma conditions measured by IRM during flux transfer events observed at the Earth's magnetopause by CCE. This study was designed to determine the importance of various upstream factors in the formation of bipolar magnetic field signatures called flux transfer events (FTEs). Six FTE encounters were examined. Three cases were when the two satellites were on similar magnetic field lines. Preliminary investigation showed that fluctuations occurred in the B_z component of the interplanetary magnetic field (IMF) resulting in a southward field preceding the FTE in all three of these cases. In two of these cases, the changes were characterized by a distinct rotation from a strong southward to a strong northward field. There were also accompanying changes in the dynamic and thermal pressure in the solar wind immediately before the FTE was encountered. Examination of the 3d plasma distributions showed that these pulses were due to the addition of energetic upstreaming foreshock particles, There were no consistent changes in either B_z or the plasma pressure at IRM for the three events when the satellites were not connected by the IMF.