Modeling The 3D Density Structure and White-Light Appearance of CME Events
ROSES ID: NNH05ZDA001N Selection Year: 2006
Program Element: Independent Investigation
Principal Investigator: Ward Manchester
Affiliation(s): University of Michigan
Project Member(s):
Vourlidas, Angelos Co-I JHU/APL
Roussev, Ilia Iankov Collaborator University of Hawaii
Summary:
We propose to examine the propagation of solar eruptive events to 1 AU
in a realistic heliosphere using a global magnetohydrodynamic (MHD) model.
The main focus of this study will be the evolution of the 3D density
structure of the CME and how it relates to Thomson-scattered white
light images. The University of Michigan's BATSRUS code will used to
perform the proposed simulations. CME initiation will follow from
both flux ropes and (Gibson & Low, 1998) and imposed shearing motions.
Our earlier simulations have produced many important results. We have
shown that the mass of fast CMEs increases by as much as a factor of
four as they propagate to Earth because of plasma swept up by the
CME-driven shock. We have also shown that line-of-sight measurements
of CME mass may significantly underestimate the mass swept up by a
CME if a dense spherical shell encases a low density cavity. Expansion
of the CME flux rope has also been shown to cause the dense core to
evolve to a density depletion. These results have been published a
series of papers: Manchester el al. (2004a, 2004b) Lugaz, Manchester
and Gombosi (2005). This proposal seeks funds to significantly
advance this research in 4 ways: (1) incorporate a more realistic
MHD model of the inner heliosphere based on solar magnetograms,
(2) investigate the pre-eruption conditions at the Sun based on
magnetic data for chosen active regions and use this data to direct
CME initiation, (3) comparing the CME synthetic white light images
with LASCO observations near the Sun and images obtained near 1 AU
with STEREO. We will examine the 3D model density structure of CME
disturbances and line-of-sight images to determine what may be
accurately inferred about the density, velocity and energy of
CMEs from single and stereoscopic views. Understanding the CME
morphology will allow us to separate the shock from the driver and
will lead to more accurate measurements of the physical parameters such
as the compression ratio, speed, mass, and location. In the case of
shocks, the compression ratio and speed are necessary inputs
in models of particle acceleration. Understanding how the various
CME structures evolve through the heliosphere will enhance the
scientific return from the numerous in-situ instruments. It will
also help us investigate what causes some CME to be geoeffective.
Obtaining realistic CME models throughout the heliosphere will greatly
enhance the return from the SECCHI observations by (1) providing
examples of how certain CME structures (shock, flux rope) will look
at different heliocentric distances and perspectives, and (2) act
as a controlled data set upon which to test the fidelity of the 3D
reconstruction algorithms.
Presentations:
Performance Year | Reference | Actions |
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1 | Cohen, Ofer; Sokolov, Igor; Gombosi, Tamas; Roussev, ...
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