Abstract
Universal Time UT variations in many magnetospheric state indicators and
indices have recently been reviewed by (Lockwood and Milan, 2023). Key
effects are introduced into magnetospheric dynamics by the eccentric
nature of Earth’s magnetic field, features that cannot be reproduced by
a geocentric field model. This paper studies the UT variation in the
occurrence of substorm onsets and uses a simple Monte-Carlo model to
show how it can arise for an eccentric field model from the effect of
the diurnal motions of Earth’s poles on the part of the geomagnetic tail
where substorms are initiated. These motions are in any reference frame
that has an X axis that points from the center of the Earth to the
center of the Sun and are caused by Earth’s rotation. The premise behind
the model is shown to be valid using a super-posed epoch study of the
conditions leading up to onset. These studies also show the surprising
degree of preconditioning required, ahead of the growth phase, for onset
to occur. A key factor is the extent to which pole motions caused by
Earth’s rotation influence the near-Earth tail at the relevant X
coordinate. Numerical simulations by a global MHD model of the
magnetosphere reveal the required effect to generate the observed UT
variations and with right order of amplitude, albeit too small by a
factor of about one third. Reasons why this discrepancy may have arisen
for the simulations used are discussed.