An important issue in the tomographic reconstruction of the solar poles is the relatively rapid evolution of the polar plumes. We demonstrate that it is possible to take into account this temporal evolution in the reconstruction. The difficulty of this problem comes from the fact that we want a 4D reconstruction (three spatial dimensions plus time) while we only have 3D data (2D images plus time). To overcome this difficulty, we introduce a model that describes polar plumes as stationary objects whose intensity varies homogeneously with time. This assumption can be physically justified if one accepts the stability of the magnetic structure. This model leads to a bilinear inverse problem. We describe how to extend linear inversion methods to these kinds of problems. Studies of simulations show the reliability of our method. Results for SOHO/EIT data show that we are able to estimate the temporal evolution of polar plumes in order to improve the reconstruction of the solar poles from only one point of view. We expect further improvements from STEREO/EUVI data when the two probes will be separated by about 60 degrees.
Deep Dive into A Time-Evolving 3D Method Dedicated to the Reconstruction of Solar plumes and Results Using Extreme Ultra-Violet Data.
An important issue in the tomographic reconstruction of the solar poles is the relatively rapid evolution of the polar plumes. We demonstrate that it is possible to take into account this temporal evolution in the reconstruction. The difficulty of this problem comes from the fact that we want a 4D reconstruction (three spatial dimensions plus time) while we only have 3D data (2D images plus time). To overcome this difficulty, we introduce a model that describes polar plumes as stationary objects whose intensity varies homogeneously with time. This assumption can be physically justified if one accepts the stability of the magnetic structure. This model leads to a bilinear inverse problem. We describe how to extend linear inversion methods to these kinds of problems. Studies of simulations show the reliability of our method. Results for SOHO/EIT data show that we are able to estimate the temporal evolution of polar plumes in order to improve the reconstruction of the solar poles from onl
arXiv:0802.0113v1 [astro-ph] 1 Feb 2008
Solar Physics
DOI: 10.1007/•••••-•••-•••-••••-•
A Time-Evolving 3D Method Dedicated to the
Reconstruction of Solar Plumes and Results
Using Extreme Ultra-Violet Data
Nicolas Barbey∗† · Frédéric Auchère∗·
Thomas Rodet† · Jean -Claude Vial∗
Received: 9 May 2007 / Accepted: 24 January 2008
c⃝Springer ••••
Abstract An important issue in the tomographic reconstruction of the solar poles
is the relatively rapid evolution of the polar plumes. We demonstrate that it is
possible to take into account this temporal evolution in the reconstruction. The
difficulty of this problem comes from the fact that we want a 4D reconstruction (three
spatial dimensions plus time) while we only have 3D data (2D images plus time).
To overcome this difficulty, we introduce a model that describes polar plumes as
stationary objects whose intensity varies homogeneously with time. This assumption
can be physically justified if one accepts the stability of the magnetic structure. This
model leads to a bilinear inverse problem. We describe how to extend linear inversion
methods to these kinds of problems. Studies of simulations show the reliability of our
method. Results for SOHO/EIT data show that we are able to estimate the temporal
evolution of polar plumes in order to improve the reconstruction of the solar poles
from only one point of view. We expect further improvements from STEREO/EUVI
data when the two probes will be separated by about 60◦.
1. Introduction
A method known as solar rotational tomography has been used to retrieve the 3D
geometry of the solar corona (Frazin 2000; Frazin and Janzen 2002). This method
assumes the stability of the structures during the time necessary to acquire the
data. Since we generally have only one point of view at our disposal, about 15
days are required to have data for half a solar rotation at the poles. Here, we focus
our study on solar polar plumes. They are bright, radial, coronal ray structures
located at the solar poles in regions of open magnetic field. The study of plumes is
of great interest since it may be the key to the understanding of the acceleration
of the fast component of the solar wind (Teriaca et al., 2003). However the three-
dimensional shape of these structures is poorly known and different assumptions have
∗Institut d’Astrophysique Spatiale, Université Paris-Sud, Orsay, France
email: nicolas.barbey@ias.u-psud.fr, frederic.auchere@ias.u-psud.fr, jean-claude.vial@ias.u-psud.fr
†Laboratoire des Signaux et Syst`emes, Supéléc, Gif-sur-Yvette, France
email: nicolas.barbey@lss.supelec.fr, thomas.rodet@lss.supelec.fr
N. Barbey et al.
been made, e.g. Gabriel et al., 2005; Llebaria, Saez, and Lamy, 2002. The plumes
are known to evolve with a characteristic time of approximately 24 hours on spatial
scales typical of Extreme ultra-violet Imaging Telescope (SOHO/EIT) data (2400
km) (DeForest, Lamy, and Llebaria, 2001). Consequently the stability assumption
made in rotational tomography fails. Fortunately, the Solar TErestrial RElations
Observatory (STEREO) mission consists of two identical spacecraft STEREOA and
STEREOB which take pictures of the Sun from two different points of view. With the
SOHO mission still operating, this results in three,simultaneous points of view. Three
viewpoints help to improve the reconstruction of the plumes, but they are still not
enough to use standard tomographic algorithms. The problem is underdetermined
and consequently one has to add a priori information in order to overcome the lack
of information. This leads to challenging and innovative signal analysis problems.
There are different ways to deal with underdetermination depending on the kind of
object to be reconstructed. Interestingly the field of medical imaging faces the same
kind of issues. In cardiac reconstruction, authors make use of the motion periodicity
in association with a high redundancy of the data (Grass et al., 2003; Kachelriess,
Ulzheimer, and Kalender, 2000). If one can model the motion as an affine transfor-
mation, and if one assumes that we know this transformation, one can obtain an
analytic solution (Ritchie et al., 1996; Roux et al., 2004).
In solar tomography, the proposed innovative approaches involve the use of ad-
ditional data such as magnetic-field measurements in the photosphere (Wiegelmann
and Inhester, 2003) or data fusion (Frazin and Kamalabadi, 2005). Attempts have
been made by Frazin et al. (2005) to treat temporal evolution using Kalman filtering.
Since polar plumes have apparently a local, rapid, and aperiodic temporal evo-
lution, we developed as in the previously referenced work, a model based on the
specifics of the object we intend to reconstruct (preliminary results can be found in
Barbey et
al., (2007). Plumes have an intensity which evolves rapidly with time,
but their position can be considered as constant. This hypothesis is confirmed by
previous studies of the plumes such as DeForest, Lamy, and Llebaria (2001). The
model is made u
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