The interaction of CMEs and associated shocks with the
Earth's bow shock, magnetosheath, and magnetopause
will be studied. CMEs and
associated shocks arrive at the Earth as magnetic clouds [8].
It is important to study how the geo-effective properties of
magnetic clouds depend on the properties of initial coronal
structures and how they are changed during propagation towards the
Earth (see above). The interaction of arriving magnetic clouds with the
Earth's bow shock will be studied. The interaction with the
magnetopause and the connection with the ionosphere will be
included in a second phase, while in a first phase the attention
will be focused on changes in the bow shock location and in the
magnetosheath flow. Special attention will be given to the
possible formation of secondary slow shock structures behind the
bow shock and the corresponding change of the magnetic topology in
the magnetosheath will be studied
.
Although it is known that the MHD approximation is not fully
justified in large parts of the magnetosphere
,
we intend to use it
as a first approximation, and to explore its limitations. In this
respect, we intend to develop the boundary conditions describing
the coupling to the ionosphere, which are crucial for realistic
simulations. A second topic would be the extension of the MHD code
to include the Hall-MHD terms (reflecting some aspects of plasma
kinetic theory). Low-resolution simulations of the overall
magnetosphere will be conducted under prescribed solar wind
conditions, including the effect of sector boundaries and an
impacting CME, in order to investigate the response of the bow
shock and the magnetopause (which are believed to be reasonably
well modeled in the MHD approach). Also, high-resolution 3D
simulations are planned of the impulsive penetration for typical
conditions, both in the MHD and Hall-MHD approaches. Finally, the
predictions of coupled solar wind-magnetosphere simulations will
be compared with Cluster II observations.