It is shown that the intensification of electric field dominated auror
al electrojets in the morning and evening sectors of the amoral oval o
n be understood in a self-consistent fluid model as the ionospheric re
sponse to enhanced magnetospheric plasma convection. Starting from a s
elf-consistently calculated equilibrium characterized by current-closu
re in the partially ionized ionosphere we perform fluid simulations to
study the dynamics of the ionospheric current system in response to e
nhanced magnetospheric convection.