Issue 
A&A
Volume 527, March 2011



Article Number  A30  
Number of page(s)  7  
Section  The Sun  
DOI  https://doi.org/10.1051/00046361/201015491  
Published online  21 January 2011 
Nonlinear forcefree field extrapolation in spherical geometry: improved boundary data treatment applied to a SOLIS/VSM vector magnetogram
^{1}
MaxPlanckInstitut für Sonnensystemforschung,
MaxPlanckStrasse 2,
37191
KatlenburgLindau,
Germany
email: tadesse@mps.mpg.de; wiegelmann@mps.mpg.de; inhester@mps.mpg.de
^{2}
Addis Ababa University, College of Education, Department of
Physics Education, PO Box
1176, Addis Ababa,
Ethiopia
email: tilaye.tadesse@gmail.com
^{3}
National Solar Observatory, Sunspot, NM
88349,
USA
email: apevtsov@nso.edu
Received:
28
July
2010
Accepted:
23
November
2010
Context. Understanding the 3D structure of coronal magnetic field is important to understanding: the onset of flares and coronal mass ejections, and the stability of active regions, and to monitoring the magnetic helicity and free magnetic energy and other phenomena in the solar atmosphere. Routine measurements of the solar magnetic field are mainly carried out in the photosphere. Therefore, one has to infer the field strength in the upper layers of the solar atmosphere from the measured photospheric field based on the assumption that the corona is forcefree. Meanwhile, those measured data are inconsistent with the above forcefree assumption. Therefore, one has to apply some transformations to these data before nonlinear forcefree extrapolation codes can be applied.
Aims. Extrapolation codes in Cartesian geometry for modelling the magnetic field in the corona do not take the curvature of the Sun’s surface into account and can only be applied to relatively small areas, e.g., a single active region. Here we apply a method for nonlinear forcefree coronal magnetic field modelling and preprocessing of photospheric vector magnetograms in spherical geometry using the optimization procedure.
Methods. We solve the nonlinear forcefree field equations by minimizing a functional in spherical coordinates over a restricted area of the Sun. We extend the functional by an additional term, which allows us to incorporate measurement errors and treat regions lacking observational data. We use vector magnetograph data from the Synoptic Optical Longterm Investigations of the Sun survey (SOLIS) to model the coronal magnetic field. We study two neighbouring magnetically connected active regions observed on May 15 2009.
Results. For vector magnetograms with variable measurement precision and randomly scattered data gaps (e.g., SOLIS/VSM), the new code yields field models that satisfy the solenoidal and forcefree condition significantly better as it allows deviations between the extrapolated boundary field and observed boundary data within the measurement errors. Data gaps are assigned an infinite error. We extend this new scheme to spherical geometry and apply it for the first time to real data.
Key words: magnetic fields / Sun: corona / Sun: photosphere / methods: numerical
© ESO, 2011
1. Introduction
Observations have shown that physical conditions in the solar atmosphere are strongly controlled by the solar magnetic field. The magnetic field also provides the link between different manifestations of solar activity such as, for instance, sunspots, filaments, flares, or coronal mass ejections. Therefore, the information about the 3D structure of magnetic field vector throughout the solar atmosphere is crucially important. Routine measurements of the solar vector magnetic field are mainly carried out in the photosphere. Therefore, one has to use numerical modelling to infer the field strength into the upper layers of the solar atmosphere from the measured photospheric field based on the assumption that the corona is forcefree. Owing to the low value of the plasma β (the ratio of gas pressure to magnetic pressure) (Gary 2001), the solar corona is magnetically dominated. To describe the equilibrium structure of the coronal magnetic field when nonmagnetic forces are negligible, the forcefree assumption is then appropriate: (1)(2)(3)where B is the magnetic field and H_{obs} is the 2D observed surface magnetic field in the photosphere. Extrapolation methods have been developed for different types of forcefree fields: potential field extrapolation (Schmidt 1964; Semel 1967), linear forcefree field extrapolation (Chiu & Hilton 1977; Seehafer 1978, 1982; Semel 1988; Clegg et al. 2000), and nonlinear forcefree field extrapolation (Sakurai 1981; Wu et al. 1990; Cuperman et al. 1991; Demoulin et al. 1992; Mikic & McClymont 1994; Roumeliotis 1996; Amari et al. 1997, 1999; Yan & Sakurai 2000; Valori et al. 2005; Wheatland 2004; Wiegelmann 2004; Amari et al. 2006; Inhester & Wiegelmann 2006). Among these, the nonlinear forcefree field has the most realistic description of the coronal magnetic field. For a more complete review of existing methods for computing nonlinear forcefree coronal magnetic fields, we refer to the review papers by Amari et al. (1997), Schrijver et al. (2006), Metcalf et al. (2008), and Wiegelmann (2008).
The magnetic field is not forcefree in the photosphere, but becomes forcefree roughly 400 km above the photosphere (Metcalf et al. 1995). Nonlinear forcefree extrapolation codes can be applied only to low plasmaβ regions, where the forcefree assumption is justified. The preprocessing scheme used until now modifies observed photospheric vector magnetograms with the aim of approximating the magnetic field vector at the bottom of the forcefree domain (Wiegelmann et al. 2006; Fuhrmann et al. 2007; Tadesse et al. 2009). The resulting boundary values are expected to be more suitable for an extrapolation into a forcefree field than the original values. Preprocessing is important to NLFFcodes that use the magnetic field vector on the boundary directly. Consistent computations for the GradRubin method, which use B_{n} and J_{n} (or α) as boundary conditions were carried out by Wheatland & Régnier (2009).
In this paper, we use a larger computational domain that accommodates most of the connectivity within the coronal region. We also take the uncertainties of measurements in vector magnetograms into account as suggested in DeRosa et al. (2009). We implement the preprocessing procedure of Tadesse et al. (2009) to SOLIS data in spherical geometry by considering the curvature of the Sun’s surface within the large field of view containing two active regions. We use a spherical version of the optimization procedure implemented in Cartesian geometry in Wiegelmann & Inhester (2010) for synthetic boundary data.
2. Method
2.1. The SOLIS/VSM instrument
In this study, we use vector magnetogram observations from the Vector Spectromagnetograph (VSM, see Jones et al. 2002), which is part of the Synoptic Optical Longterm Investigations of the Sun (SOLIS) synoptic facility (SOLIS, see Keller et al. 2003). VSM/SOLIS currently operates at the Kitt Peak National Observatory, Arizona, and has provided magnetic field observations of the Sun almost continuously since August 2003.
VSM is a full disk Stokes polarimeter. As part of daily synoptic observations, it takes four different observations in three spectral lines: Stokes I (intensity), V (circular polarization, Q, and U (linear polarization) in photospheric spectral lines FeI630.15 nm and FeI630.25 nm, Stokes I and V in FeI630.15 nm and FeI630.25 nm, similar observations in chromospheric spectral line CaII854.2 nm, and Stokes I in the HeI1083.0 nm line and the near by SiIspectral line. Observations of I, Q, U, and V are used to construct full disk vector magnetograms, while I − V observations are employed to create separate full disk longitudinal magnetograms in the photosphere and the chromosphere.
In this study, we use a vector magnetogram observed on 15 May 2009. The data were taken with 1.125 arcsec pixel size and 2.71 pm spectral sampling. In December 2009, SOLIS/VSM upgraded its cameras from Rockwell (90 Hz, 18 micron pixels) to Sarnoff (300 Hz, 16 micron pixels). This camera upgrade has resulted in improved spatial and spectral sampling. The noise level for a lineofsight component is about 1 Gauss. However, noise due to atmospheric seeing may be much higher, and the final measurement error depends on the measured flux, its spatial distribution, as well as the seeing conditions. A rough estimate suggests a noise level of a few tens of Gauss for areas with a strong horizontal gradient of magnetic field and about 1 arcsec atmospheric seeing.
Fig.1 Surface contour plot of radial magnetic field vector, and vector field plot of transverse field indicated by black arrows. 

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To create a single magnetogram, the solar disk image is scanned from terrestrial south to north; it takes about 20 min to complete one vector magnetogram. After the scan is done, the data are sent to an automatic data reduction pipeline that includes dark and flat field correction. Once the spectra are properly calibrated, full disk vector (magnetic field strength, inclination, and azimuth) magnetograms are created using two different approaches. Quicklook (QL) vector magnetograms are created based on an algorithm by Auer et al. (1977). The algorithm uses the MilneEddington model of solar atmosphere, which assumes that the magnetic field is uniform (no gradients) through the layer of spectral line formation (Unno 1956). It also assumes symmetric line profiles, disregards magnetooptical effects (e.g., Faraday rotation), and does not distinguish the contributions of magnetic and nonmagnetic components in spectral line profiles (i.e., magnetic filling factor is set to unity). A complete inversion of the spectral data is performed later using a technique developed by Skumanich & Lites (1987). This latter inversion (called ME magnetogram) also employs MilneEddington model of atmosphere, but solves for magnetooptical effects and determines the magnetic filling factor i.e., (the fractional contribution of magnetic and nonmagnetic components to each pixel). The ME inversion is only performed for pixels with spectral line profiles above the noise level. For pixels below the polarimetric noise threshold, the magnetic field parameters are set to zero.
From the measurements, the azimuths of transverse magnetic field can be determined with 180degree ambiguity. This ambiguity is resolved using the nonpotential field calculation (NPFC, see Georgoulis 2005). The NPFC method was selected on the basis of a comparative investigation of several methods for 180degree ambiguity resolution (Metcalf et al. 2006). Both QL and ME magnetograms can be used for potential and/or forcefree field extrapolation. However, in strong fields inside sunspots, the QL field strengths may exhibit an erroneous decrease inside the sunspot umbra due to socalled magnetic saturation. For this study, we choose to use fully inverted ME magnetograms. Figure 1 shows a map of the radial component of the field as a contour plot with the transverse magnetic field depicted as black arrows. For this particular dataset, about 80% of the data pixels are undetermined and as a result the ratio of data gaps to total number of pixels is large.
2.2. Preprocessing of SOLIS data
The preprocessing scheme of Tadesse et al. (2009) involves minimizing a twodimensional functional of quadratic form in spherical geometry similar to (4)where H is the preprocessed surface magnetic field from the input observed field H_{obs}. Each of the constraints L_{n} is weighted by an as yet undetermined factor μ_{n}. The first term (n = 1) corresponds to the forcebalance condition, the next (n = 2) to the torquefree condition, and the last term (n = 4) controls the smoothing. The explicit form of L_{1}, L_{2}, and L_{4} can be found in Tadesse et al. (2009). The term (n = 3) ensures that the optimized boundary condition agrees with the measured photospheric data. In the case of SOLIS/VSM data, we modified L_{3} with respect to the one in Tadesse et al. (2009), to treat those data gaps, to become (5)In this integral, W(θ,φ) = diag(w_{radial},w_{trans},w_{trans}) is a diagonal matrix which gives different weights to the different observed surface field components depending on their relative measurement accuracy. A careful choice of the preprocessing parameters μ_{n} ensures that the preprocessed magnetic field H does not deviate from the original observed field H_{obs} by more than the measurement errors. As a result of the parameter study in this work, we found that μ_{1} = μ_{2} = 1.0, μ_{3} = 0.03, and μ_{4} = 0.45 as optimal values.
2.3. Optimization principle
Equations (1) and (2) can be solved with the help of an optimization principle, as proposed by Wheatland et al. (2000) and generalized by Wiegelmann (2004) for Cartesian geometry. The method minimizes a joint measure of the normalized Lorentz forces and the divergence of the field throughout the volume of interest, V. Throughout this minimization, the photospheric boundary of the model field B is matched exactly to the observed H_{obs} and possibly preprocessed magnetogram values H. Here, we use the optimization approach for functional (L_{ω}) in spherical geometry (Wiegelmann 2007; Tadesse et al. 2009) along with the new method, which instead of an exact match enforces a minimal deviation between the photospheric boundary of the model field B and the magnetogram field H_{obs} by adding an appropriate surface integral term L_{photo} (Wiegelmann & Inhester 2010). These terms are given by (6)where L_{f} and L_{d} measure how well the forcefree Eqs. (1) and divergencefree (2) conditions are fulfilled, respectively, and both ω_{f}(r,θ,φ) and ω_{d}(r,θ,φ) are weighting functions. The third integral, L_{photo}, is the surface integral over the photosphere which allows us to relax the field on the photosphere towards forcefree solution without too much deviation from the original surface field data, and the term W(θ,φ) is the diagonal matrix in Eq. (5).
Numerical tests of the effect of the new term L_{photo} were performed by Wiegelmann & Inhester (2010) in Cartesian geometry for a synthetic magnetic field vector generated from Low & Lou model (Low & Lou 1990). They showed that this new means of incorporating the observed boundary field allows us to cope with data gaps as they appear in SOLIS and other vector magnetogram data. Within this work, we use a spherical geometry for the full disk data from SOLIS. We adopt a spherical grid r, θ, φ with n_{r}, n_{θ}, n_{φ} grid points in the direction of radius, latitude, and longitude, respectively. The method works as follows:

We compute an initial source surface potential field in thecomputational domain fromH_{robs}, the normal component of the surface field at the photosphere at r = 1 R_{⊙}. The computation is performed by assuming that a currentless (J = 0 or ∇ × B = 0) approximation holds between the photosphere and some spherical surface S_{s} (source surface where the magnetic field vector is assumed radial). We computed the solution of this boundaryvalue problem in a standard form of harmonic expansion in terms of eigensolutions of the Laplace equation written in a spherical coordinate system, (r,θ,φ).

We minimize L_{ω} (Eqs. (6)) iteratively without constraining H_{obs} at the photosphere boundary as in a previous version of Wheatland algorithm (Wheatland et al. 2000). The model magnetic field B at the surface is gradually driven towards the observations, while the field in the volume V relaxes to be forcefree. If the observed field is inconsistent, the difference B − H_{obs} or B − H (for preprocessed data) remains finite depending on the control parameter ν. At data gaps in H_{obs}, we set w_{radial} = 0 and w_{trans} = 0, and the respective field value is automatically ignored.

The state L_{ω} = 0 corresponds to a perfect forcefree and divergencefree state and exact agreement of the boundary values B with observations H_{obs} in regions where w_{radial} and w_{trans} are greater than zero. For inconsistent boundary data, the forcefree and solenoidal conditions can still be fulfilled, but the surface term L_{photo} will remain finite. This results in some deviation of the bottom boundary data from the observations, especially in regions where w_{radial} and w_{trans} are small. The parameter ν is tuned so that these deviations do not exceed the local estimated measurement error.

The iteration stops when L_{ω} becomes stationary as ΔL_{ω} / L_{ω} < 10^{4}.
3. Results
We use the vector magnetograph data from the Synoptic Optical Longterm Investigations of the Sun survey (SOLIS) to model the coronal magnetic field. We extrapolate by means of Eq. (6) both the observed field H_{obs} measured above two active regions observed on May 15 2009 and preprocessed surface field (H obtained from H_{obs} applying our preprocessing procedure). We compute 3D magnetic field in a wedgeshaped computational box V, which includes an inner physical domain V′ and the buffer zone (the region outside the physical domain), as shown in Fig. 3 of the bottom boundary on the photosphere. The wedgeshaped physical domain V′ has its latitudinal boundaries at θ_{min} = 3° and θ_{max} = 42°, longitudinal boundaries at φ_{min} = 153° and φ_{max} = 212°, and radial boundaries at the photosphere (r = 1 R_{⊙}) and r = 1.75 R_{⊙}.
Fig.2 Left: full disc vector magnetogram of May 15 2009 at 16:02UT. Middle: SOHO/EIT image of the Sun on the same day at 16:00 UT. Right: potential magneticfield line plot of SOLIS vector magnetogram at 16:02 UT, which has been computed from the observed radial component. 

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Fig.3 Top row: radial surface vector field difference between a) modelled B without preprocessing and H_{obs}, b) modelled B^{pre} and H_{obs}, c) initial potential and H_{obs}. Middle row: latitudinal surface vector field difference between d) modelled B without preprocessing and H_{obs}, e) modelled B^{pre} and H_{obs}, and f) initial potential and H_{obs}. Bottom row: longitudinal surface vector field difference between g) modelled B without preprocessing and H_{obs}, h) modelled B^{pre} and H_{obs}, and i) initial potential and H_{obs}. The vertical and horizontal axes show latitude, θ and longitude, φ in degree on the photosphere respectively. 

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Fig.4 a) Some field lines for the potential field reconstruction. b) Nonlinear forcefree reconstruction from SOLIS data without preprocessing. c) Nonlinear forcefree reconstruction from preprocessed SOLIS data. The panels show the same FOV as in Fig. 2 (right panel). 

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The weighting functions ω_{f} and ω_{d} in L_{f} and L_{d} in Eq. (6) are chosen to be unity within the inner physical domain V′ and decline with a cosine profile in the buffer boundary region (Wiegelmann 2004; Tadesse et al. 2009). They reach a zero value at the boundary of the outer volume V. The distance between the boundaries of V′ and V is chosen to be nd = 10 grid points wide. The framed region in Figs. 3a − i corresponds to the lower boundary of the physical domain V′ with a resolution of 132 × 196 pixels in the photosphere. The original full disc vector magnetogram has a resolution of 1788 × 1788 pixels out of which we extracted 142 × 206 pixels for the lower boundary of the computational domain V, which corresponds to 550 Mm × 720 Mm on the photosphere.
The main reason for the implementation of the new term L_{photo} in Eq. (6) is that we need to work with boundary data of different noise levels and qualities or even neglect some data points completely. SOLIS/VSM provides fulldisk vectormagnetograms, but for some individual pixels the inversion from line profiles to field values may not have been successfully inverted and field data there will be missing for these pixels. Since the old code without the L_{photo} term requires complete boundary information, it cannot be applied to this set of SOLIS/VSM data. In our new code, these data gaps are treated by setting W = 0 for these pixels in Eq. (6). For those pixels, for which H_{obs} was successfully inverted, we allow deviations between the model field B and the input fields either observed H_{obs} or preprocessed surface field H using Eq. (6), so that the model field can be iterated closer to a forcefree solution even if the observations are inconsistent. This balance is controlled by the Lagrangian multiplier ν as explained in Wiegelmann & Inhester (2010), where we used w_{radial} = 100w_{trans} for the surface fields both from data with preprocessing and without.
Figure 2 shows the position of the active region on the solar disk for both the SOLIS fulldisk magnetogram^{1}, and the SOHO/EIT image of the Sun observed at 195 Å on the same day at 16:00 UT^{2}. As stated in Sect. 2.3, the potential field is used as the initial condition for iterative minimization required in Eq. (6). The respective potential field is shown in the rightmost panel of Fig. 2. During the iteration, the code forces the photospheric boundary of B towards observed field values H_{obs} or H (for preprocessed data) and ignores data gaps in the magnetogram. A deviation between surface vector field from model B and either H_{obs} or H (for preprocessed data) occurs where H_{obs} is inconsistent with a forcefree field. In this sense, the term L_{photo} in Eq. (6) acts on H_{obs} as in the preprocessing, generating a surface field B instead of H from H_{obs}, which is close to H_{obs}, but consistent with a forcefree field above the surface. In Fig. 3, we therefore compare the difference between the preprocessing procedure and the new extrapolation code (Eq. (6)) on H_{obs}. The figure shows the surface magnetic field differences of the preprocessed, unpreprocessed, and potential surface fields.
To identify the similarity of vector components on the bottom surface, we calculate their pixelwise correlations. The correlation were calculated from (7)where v_{i} and u_{i} are the vectors at each grid point i on the bottom surface. If the vector fields are identical, then C_{vec} = 1; if v_{i} ⊥ u_{i}, then C_{vec} = 0. Table 1 shows the correlations between the surface fields from B^{pre} − H_{obs}, (where B^{pre} is the model field obtained from the preprocessed surface field H using Eq. (6)) and B^{unpre} − H_{obs}, where B^{unpre} is the model field the obtained from observed surface field H_{obs} using Eq. (6). We computed the vector correlations of the two surface vector fields for the three components at each grid points to compare how well they are aligned in each direction. From those values in Table 1, one can see that the preprocessing and extrapolation with Eq. (6) act on H_{obs} in a similar way. In Fig. 4, we plot magnetic field lines for the three configurations in which the vector correlations of potential field lines in the 3D box for both the extrapolated NLFF with and without preprocessing data are 0.741 and 0.793, respectively.
The correlations between the components of surface fields from (B^{pre} − H_{obs}) and (B^{unpre} − H_{obs}).
The magnetic energy associated with extrapolated NLFF field configurations with and without preprocessing.
The electric current density calculated from Ampère’s law, J = ▿ × B / 4π, on the basis of spatially sampled transverse magnetic fields varies widely over an active region. To investigate how errors in the vector magnetograph measurements produce errors in the vertical electric current densities, Liang et al. (2009) numerically simulated the effects of random noise on a standard photospheric magnetic configuration that is produced by electric currents and satisfies the forcefree field conditions. Even if the current density can be estimated on the photosphere, it is not intuitively clear how the change in the current density distribution affects a coronal magnetic configuration. Régnier & Priest (2007b) studied these modifications in terms of the geometry of field lines, the storage of magnetic energy, and the amount of magnetic helicity. Figure 5 shows isosurface plots of current density above the volume of the active region. There are strong current configurations above each active regions. This becomes clear if we compare the total current inbetween each active region with the current moving from the left to the right active region. These currents were added up from the surface normal currents emanating from the pixels that are magnetically connected inside or across active regions, respectively. The result is shown in Table 3. The active regions share a decent amount of magnetic flux compared to their internal flux from one polarity to the other. In terms of the electric current, they are much more isolated. The ratio of shared to intrinsic magnetic flux is of the order of unity, while for the electric current those ratios are much less, 1.58 / 49.6 and 1.58 / 32.17, respectively. We can similarly calculate the average value of α on the field lines with the respective magnetic connectivity. The averages are shown in the second row of Table 3. The two active regions are magnetically connected but are much less by electric currents.
Fig.5 Isosurfaces (ISs) of the absolute current density vector J = 100 mA m^{2} computed above the active regions. 

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The currents and average α calculated from those pixels which are magnetically connected.
4. Conclusion and outlook
We have investigated the coronal magnetic field associated with the AR 11017 on 2009 May 15 and a neighbouring active region by analysing SOLIS/VSM data. We have used the optimization method for the reconstruction of nonlinear forcefree coronal magnetic fields in spherical geometry by restricting the code to limited parts of the Sun (Wiegelmann 2007; Tadesse et al. 2009). In contrast to previous implementation, our new code allows us to deal with a lack of data and regions with poor signaltonoise ratio in the extrapolation in a systematic manner because it produces a field that is closer to a forcefree and divergencefree field and tries to match the boundary only where it has been reliably measured (Wiegelmann & Inhester 2010).
For vector magnetograms with a lack of data points and where zero values have been replaced for the signal below a certain threshold value, the new code relaxes the boundary and allows us to fulfill the solenoidal and forcefree conditions more reliably as it allows deviations between the extrapolated boundary field and an inconsistent observed boundary data. With the new term, L_{photo} extrapolation from H_{obs} and H yields almost the same 3D field. However, in the latter case the iteration to minimize Eq. (6) saturates in fewer iteration steps. At the same time, preprocessing does not affect the overall configuration of magnetic field and its total energy content.
We plan to use this newly developed code for upcoming data from SDO (Solar Dynamics Observatory)/HMI (Helioseismic and Magnetic Imager) when full disc magnetogram data become available.
Acknowledgments
SOLIS/VSM vector magnetograms are produced cooperatively by NSF/NSO and NASA/LWS. The National Solar Observatory (NSO) is operated by the Association of Universities for Research in Astronomy, Inc., under cooperative agreement with the National Science Foundation. Tilaye Tadesse acknowledges a fellowship of the International MaxPlanck Research School at the MaxPlanck Institute for Solar System Research and the work of T. Wiegelmann was supported by DLRgrant 50 OC 453 0501.
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All Tables
The correlations between the components of surface fields from (B^{pre} − H_{obs}) and (B^{unpre} − H_{obs}).
The magnetic energy associated with extrapolated NLFF field configurations with and without preprocessing.
The currents and average α calculated from those pixels which are magnetically connected.
All Figures
Fig.1 Surface contour plot of radial magnetic field vector, and vector field plot of transverse field indicated by black arrows. 

Open with DEXTER  
In the text 
Fig.2 Left: full disc vector magnetogram of May 15 2009 at 16:02UT. Middle: SOHO/EIT image of the Sun on the same day at 16:00 UT. Right: potential magneticfield line plot of SOLIS vector magnetogram at 16:02 UT, which has been computed from the observed radial component. 

Open with DEXTER  
In the text 
Fig.3 Top row: radial surface vector field difference between a) modelled B without preprocessing and H_{obs}, b) modelled B^{pre} and H_{obs}, c) initial potential and H_{obs}. Middle row: latitudinal surface vector field difference between d) modelled B without preprocessing and H_{obs}, e) modelled B^{pre} and H_{obs}, and f) initial potential and H_{obs}. Bottom row: longitudinal surface vector field difference between g) modelled B without preprocessing and H_{obs}, h) modelled B^{pre} and H_{obs}, and i) initial potential and H_{obs}. The vertical and horizontal axes show latitude, θ and longitude, φ in degree on the photosphere respectively. 

Open with DEXTER  
In the text 
Fig.4 a) Some field lines for the potential field reconstruction. b) Nonlinear forcefree reconstruction from SOLIS data without preprocessing. c) Nonlinear forcefree reconstruction from preprocessed SOLIS data. The panels show the same FOV as in Fig. 2 (right panel). 

Open with DEXTER  
In the text 
Fig.5 Isosurfaces (ISs) of the absolute current density vector J = 100 mA m^{2} computed above the active regions. 

Open with DEXTER  
In the text 
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