We analyze the injections of tailward flowing O+ ions measured by PROG
NOZ-8 in the magnetospheric lobes using three-dimensional single-parti
cle codes. These injections are shaped as ''inverted Vs'' and unexpect
edly well correlated with AE variations during a time interval of abou
t 7 hours. Such a correlation leads us to consider the effect of trans
ient intensification of the large-scale magnetospheric convection. Usi
ng a simple model of time-varying electric field, we show that the sou
rce of the Of lies near the dayside cusp. This source extends over a n
arrow (a few degrees) latitudinal interval in the vicinity of the last
closed field line, likely involving ions expelled into the magnetosph
ere after being transversely accelerated. We demonstrate that, downstr
eam of the ejection site, impulsive convection leads to prominent stru
cturing of the tailward streaming particles with abrupt energy variati
ons on small length scales. A good agreement is obtained between the n
umerical results and the observations which supports our impulsive con
vection based interpretation framework.