Issue 
A&A
Volume 506, Number 3, November II 2009



Page(s)  1415  1428  
Section  The Sun  
DOI  https://doi.org/10.1051/00046361/200811373  
Published online  03 September 2009 
A&A 506, 14151428 (2009)
The quiet Sun magnetic field observed with ZIMPOL on THEMIS^{}
I. The probability density function
V. Bommier^{1}  M. Martínez González^{1,}^{}  M. Bianda^{2,3}  H. Frisch^{4}  A. Asensio Ramos^{5}  B. Gelly^{6}  E. Landi Degl'Innocenti^{7}
1  LERMA, Observatoire de Paris, ENS, UPMC, UCP, CNRS, Place Jules Janssen, 92190 Meudon, France
2  Istituto Ricerche Solari Locarno, via Patocchi, 6605 LocarnoMonti, Switzerland
3  Institute of Astronomy, ETH Zurich, 8092 Zurich, Switzerland
4  Université de Nice, Observatoire de la Côte d'Azur, CNRS, Laboratoire Cassiopée,
BP 4229, 06304 Nice Cedex 4, France
5  Instituto de Astrofísica de Canarias, vía Láctea s/n, 38205 La Laguna, Tenerife, Spain
6  Télescope Héliographique pour l'Étude du Magnétisme et des
Instabilités Solaires, CNRS UPS 853  THEMIS, vía Láctea s/n, 38205 La
Laguna, Tenerife, Spain
7  Dipartimento di Astronomia e Scienza dello Spazio, Università degli
Studi di Firenze, Largo E. Fermi 2, 50125 Firenze, Italy
Received 18 November 2008 / Accepted 16 July 2009
Abstract
Context. The quiet Sun magnetic field probability density
function (PDF) remains poorly known. Modeling this field also
introduces a magnetic filling factor that is also poorly known. With
these two quantities, PDF and filling factor, the statistical
description of the quiet Sun magnetic field is complex and needs to be
clarified.
Aims. In the present paper, we propose a procedure that combines
direct determinations and inversion results to derive the magnetic
field vector and filling factor, and their PDFs.
Methods. We used spectropolarimetric observations taken with
the ZIMPOL polarimeter mounted on the THEMIS telescope. The target was
a quiet region at disk center. We analyzed the data by means of the
UNNOFIT inversion code, with which we inferred the distribution of the
mean magnetic field ,
being the magnetic filling factor. The distribution of
was derived by an independent method, directly from the spectropolarimetric data. The magnetic field PDF p(B)
could then be inferred. By introducing a joint PDF for the filling
factor and the magnetic field strength, we have clarified the
definition of the PDF of the quiet Sun magnetic field when the latter
is assumed not to be volumefilling.
Results. The most frequent local average magnetic field strength
is found to be 13 G. We find that the magnetic filling factor is
related to the magnetic field strength by the simple law
with B_{1}
= 15 G. This result is compatible with the Hanle weakfield
determinations, as well as with the stronger field determinations from
the Zeeman effect (kGauss field filling 12% of space). From linear
fits, we obtain the analytical dependence of the magnetic field PDF.
Our analysis has also revealed that the magnetic field in the quiet Sun
is isotropically distributed in direction.
Conclusions. We conclude that the quiet Sun is a complex medium
where magnetic fields having different field strengths and filling
factors coexist. Further observations with a better polarimetric
accuracy are, however, needed to confirm the results obtained in the
present work.
Key words: magnetic fields  polarization  turbulence  techniques: polarimetric  methods: data analysis  Sun: magnetic fields
1 Introduction
The solar magnetic field is divided into two classes: the network field, and the internetwork field. The network field is the one of sunspots and active regions (plages or faculae), but it appears also in quiet regions as pepperandsalt grains scattered in longitudinal magnetograms, indicating a stronger field than in their surroundings. These grains delineate the frontiers of a network of socalled supergranules, each supergranule having a width of about 30 000 km. The internetwork field lies inside the supergranules. A map of spectropolarimetric data, including active and quiet regions (and a filament) was analyzed by Bommier et al. (2007) in terms of vector magnetic field, by applying the UNNOFIT inversion code. It was found that these two classes of magnetic fields are characterized by different field strengths and directions: while the network field is found rather vertical with a field strength of 100 G or higher (spatially averaged), the internetwork is found to be far weaker (in spatial average) and turbulent in direction. In quiet regions, the solar magnetic field appears then as vertical trees standing in places (on the supergranules frontiers) out of the carpet of the turbulent internetwork field.
However, the internetwork magnetic field had already been investigated. The first attempt to measure the internetwork field comes from Stenflo (1982), who established the first and founding results: some lines observed near the solar limb are found linearly polarized, and this polarization stems from radiative scattering near the surface, because the incident radiation is anisotropic due to limb darkening. But the observed polarization degree is found to be lower than the theoretical one in a pure scattering model. Thus, Stenflo was led to introduce a possible magnetic depolarization, the Hanle effect. Stenflo (1982) evaluates the order of magnitudes, resulting in the range 10100 G for the internetwork field strength. This order of magnitude was later confirmed by a detailed theoretical calculation by FaurobertScholl (1992). The Hanle effect is sensitive to the magnetic field strength when the Larmor pulsation is comparable to the upperlevel inverse lifetime , i.e. when . For permitted visible lines where 10^{8} s (in the UV or IR domains, this order of magnitude differs), this leads to 10 G. For 100 times higher field strengths, the Hanle effect saturates and only the sensitivity to the field direction remains. In the Hanle field range, the sensitivity of the Zeeman effect is weak, and the Hanle effect observed in visible lines is then revealed as the welladapted tool for the weak field measurements. Moreover, the rotation of the polarization direction, which would also be observed for the Hanle effect in a deterministic field, has remained undetectable, leading Stenflo to conclude that there is a turbulent field (in direction). As the Hanle effect is highly nonlinear, it is also welladapted to the detection of a turbulent field, whereas the Zeeman effect would remain globally insensitive because it is linear.
Later on, however, strong kG fields were also detected in quiet regions (GrossmannDoerth et al. 1996), on small scales, smaller than the resolution element. Thus, a magnetic filling factor was to be introduced to interpret the observations, as earlier done in the network case (Stenflo 1973). And, time passing, the spatial resolution of both groundbased (VTT, THEMIS) and spaceborne (HINODE) instruments increased, raising the possibility of Zeeman detection of the weak fields. The IR window opened also, where the Zeeman effect is relatively more sensitive. We provide the references to the related new measurements later on in this paper. But, depending on the presence or absence of a magnetic filling factor in the models, the situation seems to us to be rather involved in discussions of the quiet Sun magnetic field probability density function (PDF), in particular with respect to its definition and evaluation.
From groundbased telescopes, the spatial resolution of spectropolarimetric data is about . At this stage, the only reliable results concerning the magnetic field strength in the quiet Sun have been performed in the nearIR (Martínez González et al. 2008a; Khomenko et al. 2003) or by using spectral lines with hyperfine structure (Ramírez Vélez et al. 2008; López Ariste et al. 2006) or spectral lines sensitive to the Hanle effect (Trujillo Bueno et al. 2004, and Refs. therein). The studies using the visible Fe I 6301.5 Å and 6302.5 Å spectral lines, which show stronger field in the kG range (Lites & SocasNavarro 2004; SocasNavarro & Sánchez Almeida 2002; Domínguez Cerdeña et al. 2003a; SocasNavarro et al. 2004), have been put in doubt (López Ariste et al. 2007; Khomenko & Collados 2007; Martínez González et al. 2006).
Khomenko et al. (2003) and Martínez González et al. (2008a) have derived the PDF of the magnetic field on the quiet Sun using the 1.5 m Fe I spectral lines. The magnetic field strengths inferred by both analyses were in the hG regime, with values around the equipartition field in the photosphere. They obtained a magnetic field PDF that could be reproduced by a decreasing exponential law. This exponential form for the PDF was then used by Trujillo Bueno et al. (2006,2004) to interpret second solar spectrum observations (from various authors and instruments) in terms of Hanle depolarization due to a turbulent field. From these observations, these authors propose that the mean magnetic field is 130 G.
The HINODE satellite has provided spectropolarimetric data in the 6302.5 Å spectral range with a spatial resolution of about 0.32 . The validity of the analysis of this kind of data has been studied by Orozco Suárez et al. (2007a). The inversion of quiet Sun HINODE data has resulted in a PDF containing hG fields, as pointed out by the infrared measurements but in disagreement with the previous 6302.5 Å studies mentioned above (Orozco Suárez et al. 2007b).
In this paper, we deal with 6302.5 Å spectropolarimetric data to infer the magnetic field PDF in the quiet Sun. The observations were taken with the ZIMPOL polarimeter mounted on the THEMIS telescope and are described in Sect. 2. To overcome the difficulties with the 6302.5 Å interpretation, we propose an analysis procedure that combines the results of the UNNOFIT inversion code (first step, determination of the local average field, Sect. 3) and direct observables of the polarized profiles (second step, direct determination of the magnetic filling factor, Sect. 4). It is then possible to derive the PDF (Sect. 5), but we had to return to the basic statistical definitions to clarify the role played by the magnetic filling factor in the PDF definition (see also Appendix A). In Sect. 5 we compare our results with the previous ones, which leads us to clarify the notion of PDF applied to the quiet Sun magnetic field and to reexamine the validity conditions of the Fe I 6302.5 Å inversion. Our analysis is compatible with previous quiet Sun studies, revealing that the greater the magnetic field strength the less the filling factor. We provide analytical fits of our histograms, leading to an analytical PDF.
Our aim in writing this paper is to get a statistical approach to the quiet Sun magnetic field and to disentangle the notions of magnetic field strength distribution and filling factor. Our main contribution is to directly determine the magnetic filling factor, which is independent of the data inversion.
2 Observations
The observations were performed on the 5 and 6 July 2008, with the ZIMPOL polarimeter mounted on the THEMIS telescope (ZIMPOL II, see Gandorfer & Povel 1997). The aim of these observations was to investigate the quiet Sun magnetic field at different atmospheric layers. In this prospect, two ZIMPOL cameras were installed, one observing the Cr I 5781.8 Å line (line center formation height 85 km), and the other one observing the Fe I 6301.5 Å and 6302.5 Å lines (line center formation height 330 km and 260 km, respectively). We recall that the ZIMPOL system requires one unmasked pixel every four pixels of the camera chip. The camera centered on the 6302 Å spectral range was equipped with a microlens system that focuses the solar light in the unmasked pixel. The 5782 Å camera was not equipped with this system. The integration time was thus significantly shorter for the 6302 Å camera. The unmasked pixelsize was 0.13 arcsec, but the observation pixelsize results in 0.53 arcsec because of the microlens system. The spectral pixel was 7.18 mÅ. The slit width was 0.5 arcsec.
The observations were performed with the slit fixed at disk center. The disk center was quiet. The slit was oriented solar north. The exposure time was 320 ms (per accumulation), but we determined that 10 accumulations were needed to get a polarimetric accuracy of . Due to the actuation (camera readout, analyzer plates rotation), the total duration was 0.9 s per accumulation. Several accumulations were averaged before being stored on the disk, the storage process taking about 4.5 s. Actually, the polarimetric accuracy of (for 10 accumulations) was insufficient to get a signal in linear polarization, so we were obliged to average series of images. The polarimetric accuracy level was derived from the noise level along the observed profiles. The detail of the observations (number of averaged images, resulting polarimetric accuracy, total duration) is given in Table 1. On 5 July the TIPTILT stabilization system was ON, but some jumps occurred and we averaged the images between the jumps. On 6 July the TIPTILT stabilization system was OFF but the seeing was excellent. We averaged the data by series of 15 images. Such a series corresponds to a total duration of less than 600 s. We retained this limit because we observed that the linear polarization signaltonoise ratio decreases if the total integration time is longer than the typical granule lifetime, which is around 600 s. When the TIPTILT was OFF, no alternative correction was applied for the seeing effect. We thus got a total of 12 different observations of the 140 pixels slit, which results in 1680 observed profiles on which we can perform a statistical analysis.
The magnetic field values given in the present paper were derived from the Fe I 6302.5 Å observations. The ZIMPOL data reduction package was used (Gandorfer et al. 2004).
Table 1: Information on the averaged data. Each line of the table corresponds to one average.
2.1 Evaluation of the line center height of formation
The temperature, electron pressure and gas pressure were taken from the Maltby et al. quiet Sun photospheric reference model (Maltby et al. 1986), extrapolated downwards beyond 70 km to 450 km below the level. Above 70 km, this model is very similar to the quiet Sun VAL C (Vernazza et al. 1981). The continuum absorption coefficient was evaluated as in the MALIP code of Landi Degl'Innocenti (1976), i.e. by including H^{} boundfree, H^{} freefree, neutral hydrogen atom opacity, Rayleigh scattering on H atoms and Thompson scattering on free electrons. The line absorption coefficient was derived from the Boltzmann and Saha equilibrium laws, taking the two first ions of iron into account. The atomic data were taken from Wiese or Moore and the partition functions from Wittmann. The iron abundance was assumed to be 7.60 (in the usual logarithmic scale where the abundance of hydrogen is 12). A depthindependent microturbulent velocity field of 1 km s^{1} was introduced. Finally, for layers above , departures from LTE in the ionization equilibrium were simulated by applying Saha's law with a constant ``radiation temperature'' of 5100 K instead of the electron temperature provided by the atmosphere model.
To get the result, the line center optical depth grid was scaled to the continuum one, by using their respective absorption coefficients. The continuum optical depth grid was the one provided with the atmosphere model and the transfer equation was not explicitely solved again. The height of formation of the line center (the one given above) was then determined as follows. Given the grid of line center optical depths, the height of formation of the line center is the one for which the optical depth along the line of sight is unity (EddingtonBarbier approximation), i.e. the one for which , where is the line center optical depth along the vertical, and the cosine of the heliocentric angle (here taken at 0).
3 First step: full Stokes inversion
3.1 Results on the quiet Sun magnetic field strength and direction
Figure 1: UNNOFIT fit (dotted line) of a typical observation (full line). The main spectral line (centered at pixel 38), that is polarized, is Fe I 6302.5 Å, and the other line, unpolarized, is a telluric line. 10 pixels are 72 mÅ and blue is towards the left. Derived magnetic field parameters: local average field strength 11.7 G, inclination 115 from the lineofsight, azimuth 123 from the slit direction which is the reference axis for the Stokes parameters. The line strength parameter is found to be 2.6, and the Doppler width 35.8 mÅ. 

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The magnetic field vector was determined by applying the UNNOFIT inversion (Bommier et al. 2007; Landolfi et al. 1984), which is based on the MilneEddington approximation. A 2component atmosphere is assumed: one magnetic (with filling factor ) and one nonmagnetic (with filling factor ). These two atmospheres are assumed to have all their other parameters identical, except for the presence/absence of the magnetic field. Only the information of the 6302.5 Å spectral line is taken into account. The four Stokes parameters are inverted simultaneously. An example of observed profile and the best fit obtained with UNNOFIT is shown in Fig. 1. In the examination of the differences between the theoretical and observed profiles in this figure, it can first be pointed out that the noise level, measurable in the continuum, is non negligible with respect to the signal order of magnitude, especially in Q/I and U/I . Second, it has to be considered that the four Stokes profiles are simultaneously fitted, by using a rather simple atmosphere model (MilneEddington): thus, departures may not be surprising. However, we find that the theoretical profile shape corresponds to the observed one, in terms of sign and components. Thus we conclude that, under the ME hypothesis, we are able to retrieve the field vector within an uncertainty that is clarified in the following.
The neighboring Fe I 6301.5 Å line was also observed, but its
inversion fails in a number of pixels that we estimate too high. This comes
from its lower sensitivity to the magnetic field: first because its Landé
factors are smaller, and second because it is not a normal Zeeman triplet
line (
)
contrary to 6302.5. Its Zeeman polarization
is more entangled along the spectrum, resulting in a lower global
sensitivity. We applied UNNOFIT2, the inversion code adapted to lines that
are not normal Zeeman triplet and got this unsatisfactory result. Besides,
both lines 6302.5 and 6301.5 could be inverted together, but as pointed out
by Martínez González et al. (2006), they are not formed at the same depth, on the
one hand, and one line is enough for MilneEddington inversion in terms of
number of researched parameters, on the other.
Figure 2: Histogram of the local average longitudinal magnetic field (the product of the longitudinal magnetic field B_{z} with the magnetic filling factor ), from the UNNOFIT inversion. 

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Figure 3: Histogram of the local average magnetic field strength (the product of the magnetic field strength B with the magnetic filling factor ), from the UNNOFIT inversion. 

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Figure 4: Histogram of the magnetic field inclination with respect to the lineofsight, from the UNNOFIT inversion. The lineofsight is also the solar vertical with the observation performed at disk center. 

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As shown by Bommier et al. (2007), the 2component inversion of Fe I 6302.5 Å is unable to separately determine the magnetic filling factor and the magnetic field strength B, but only their product , which we call the local average magnetic field strength. Figures 25 display histograms constructed from the UNNOFIT inversion of the 1680 observed profiles. Figure 2 displays the histogram of the local average longitudinal magnegtic field , which is the magnetic flux. The unsigned average magnetic flux is found to be 11 Mx/cm^{2}. Figure 3 displays the histogram of the local average magnetic field strength for all the observed profiles. The most probable value is G, the probability for stronger fields decreasing very fast. The mean value is G and the standard deviation is 14 G.
Figure 4 displays the histogram of the magnetic field vector inclination. First we recall that an isotropic distribution of field directions leads to a histogram for the inclination that has a sinusoidal shape because the elementary surface on the unit sphere is . Such a shape was obtained in previous THEMIS observations (Bommier et al. 2007), but it was wrongly concluded that the magnetic field tends to be horizontal because the inclination angles were also predominantly ranging between and . Disregarding the central hollow, the histogram in Fig. 4 displays the sinusoidal shape expected for the inclination angles of an isotropic distribution. This central void is the result of the presence of V profiles in all the observed pixels. Simultaneous nonzero Q, U and V is not surprising if many magnetic fields with different inclinations actually coexist in each resolution element. The central hollow could stem from our modeling by a single magnetic field per element. Another explanation for the presence of Stokes V could be some misalignment problem in the data reduction. We note here that the inclination histogram of HINODE data by Ishikawa & Tsuneta (2009, see their Fig. 5) also displays a central hollow, although not as marked as here. From the accuracy test described further, the inclination angle is determined within . Considering also the small average number of analyzed profiles per bin (see the discussion in the next paragraph), it is impossible to ascertain a departure from the isotropic distribution in the last four bins at the extremities where the envelope tangent seems to be horizontal, in contrast to a envelope.
Figure 5 displays the histogram of the azimuth, which is defined with respect to the slit direction. As the fundamental ( ) ambiguity is not resolved, the azimuth is defined modulo between and . This histogram displays a flat shape on average, also corresponding to the azimuths of an isotropic distribution. More precisely, the average number of counts per bin is about . Assuming a Gaussian noise, the noise level per bin is . In the figure, the deviations from bin to bin generally agree with this value, except in some cases where it is higher. In these cases a positive deviation is, however, most often immediately followed by a negative one of the same order of magntitude, and there is no case where this deviation is greater than , which would be really significant. Thus, we conclude that in a first approximation our observations indicate an isotropic distribution of the quiet Sun magnetic field azimuths.
We conclude from the THEMIS observations (Bommier et al. 2007) and from these new ZIMPOL observations that the quiet Sun magnetic field has most likely an isotropic distribution of directions. Observations performed at different limb distances by Martínez González et al. (2008b) also conclude on an isotropic distribution of the quiet Sun magnetic field direction. Such observations at different limb distances are indeed needed to thoroughly investigate the field direction distribution. We performed them with ZIMPOL on THEMIS, and we shall discuss them in a future paper of this series. On the basis of our present observations, we do not confirm the horizontal trend of the internetwork magnetic field recently observed by HINODE (Lites et al. 2007,2008) and derived from HINODE inclination histograms by Orozco Suárez et al. (2007b) and Ishikawa & Tsuneta (2009), who could have also been unaware of the sinusoidal shape of the inclination histogram from an isotropical distribution.
Figure 5: Histogram of the magnetic field azimuth with respect to the slit direction, from the UNNOFIT inversion (ambiguity is not resolved). The observation was performed at disk center and the slit was solar north, so that this is also the histogram of the horizontal field component azimuth. 

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3.2 Accuracy of the inversion
Figure 6: Test of the determination of the local average magnetic field strength (the product of the magnetic field strength B with the magnetic filling factor ) by the UNNOFIT inversion. A series of theoretical profiles are computed under the conditions of the ZIMPOL observations (spectral and polarimetric resolutions), and then submitted to the inverter. In abscissae are the input known values, in ordonnae are the output recovered values. The bottom figure is a zoom of the top figure near the axis origin. 

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Figure 7: Fit of the local average longitudinal magnetic field histogram of Fig. 2 by a Gaussian of halfwidth w = 13.5 G. 

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To determine the accuracy of the magnetic inversion, we performed the same test as in Bommier et al. (2007), but for the ZIMPOL/THEMIS polarimetric accuracy ( in the continuum under the conditions described in Sect. 2) and spectral sampling. As in that paper, a series of theoretical profiles was generated from the UnnoRachkovsky solution applied to the 2component atmosphere, for a set of magnetic field strength, inclination, azimuth, and filling factor values. These profiles were then noised at the observed level and submitted to the UNNOFIT inversion. The test consists in comparing the output values with the known input ones. The main result is presented in Fig. 6, which is analogous to Fig. 4 of Bommier et al. (2007), and it shows analogously that the local average magnetic field strength (the product of the field strength by the filling factor) is correctly determined by the inversion. The bottom figure is a zoom of the top figure near the axis origin, and shows the dispersion of the results about the first diagonal that represents equal input and output. This dispersion is on the order of 10 G, which we retain as the accuracy on the local average magnetic field strength determination. This dispersion includes both longitudinal and transverse fields. Moreover, the bottom figure shows that, when the input local average magnetic field strength decreases to zero, the output saturates at 10 G. In Fig. 4 of Bommier et al. (2007), the saturation level is 25 G for a polarimetric accuracy of only . It thus appears that the saturation level is directly related to the polarimetric accuracy. The regular pattern detectable in the lower part of Fig. 6 is a consequence of the regular spacing of the input theoretical data. The number of input points is 183 600 and the number of output points that depart from more than about 10 G from the diagonal is about 5% of the total number of points.
The observed profile asymmetries, which are visible in Fig. 1, are taken into account neither in the test nor in the inversion. Such asymmetries may be due to vertical gradient of the radial velocity. A new version of our inversion code UNNOFIT is under development, which takes into account such gradients and is able to properly fit asymmetric profiles. At first sight the magnetic field strength would not be highly modified. Besides, it may be noted that the asymmetries' order of magnitude is comparable to the polarimetric noise in Fig. 1, at least in Q/I and U/I.
Figures 7 and 8 display Gaussian
fits of the histograms of Figs. 2 and 3,
corresponding respectively to the local average longitudinal magnetic field
and to the local average magnetic field strength. The histogram of Fig. 2 can be fitted with the usual Gaussian
.
The histogram in Fig. 3 can be fitted
by the Maxwell distribution
.
These fits show
that the magnetic field vector has a Gaussian distribution, since a Gaussian
distribution leads to a Maxwell distribution after angle averaging. The
width w of the Gaussian and Maxwellian are 13.5 G and 11 G, respectively.
Since these values are not significantly higher than the 10 G corresponding
to the inversion accuracy, we cannot conclude that the local average
magnetic field truly has a Gaussian PDF, so we attribute the Gaussian shape
of these histogram envelopes to the polarimetric noise.
Figure 8: Fit of the local average magnetic field strength histogram of Fig. 3 by a Maxwellian of halfwidth w = 11 G. 

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4 Second step: direct determination of the magnetic filling factor
From the weak field laws, which express the emerging polarization Stokes
parameters in terms of the derivatives of the intensity profile,
Landi Degl'Innocenti & Landolfi (2004, pp. 405407) derive the approximate expressions
We have introduced here the magnetic filling factor , which is not in Landi Degl'Innocenti & Landolfi (2004, pp. 405407). Here, is the Doppler width and the magnetic field vector inclination with respect to the lineofsight. is the Zeeman splitting in wavelength units, defined by
(3) 
where is the Larmor frequency (Landi Degl'Innocenti & Landolfi 2004, p. 78). In numerical values, this is
(4) 
where is in mÅ, is in Å and B in G. is the effective Landé factor, and is the second order effective Landé factor introduced by Landi Degl'Innocenti & Landolfi (2004), that is equal to in the case of Zeeman triplet lines like Fe I 6302.5 Å. is the line depth
(5) 
where is the continuum intensity near the line and I_{0} is the line center intensity.
We now note that the linear polarization depends quadratically on the
magnetic field strength and direction, but linearly on the magnetic filling
factor. Taking the square of Eq. (1) and dividing by Eq. (2), we find
Figure 9 displays a test of this approximation. The Stokes parameters are first computed with the UnnoRachkovsky solution applied to a 2component atmosphere with a given value of ( input). The other parameters needed to compute the line profile are taken from the average values resulting from the UNNOFIT inversion applied to our Fe I 6302.5 Å data. In particular the line strength is . The output values of are computed with Eq. (6 ). Figure 9 was plotted for a series of magnetic field strengths and inclinations. The field strengths are given in Doppler width units . The different values 0.25, 0.50, 1, and 2 Doppler widths correspond to 236, 472, 944, and 1888 G, respectively, in the case of the Fe I 6302.5 Å line formed in the quiet Sun. This figure is the same for any input value.
Figure 9: Test of the determination of the magnetic filling factor by applying Eq. (6) to the polarimetric data. For the test, the polarimetric data were theoretical profiles computed from the UnnoRachkovsky solution, weighted by a theoretical input magnetic filling factor (input). Equation (6) is then applied, leading to (output). The figure displays their ratio, for a series of magnetic field inclination angles and strengths (in Doppler width units). This plot is valid for any value. 

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Figure 10: Histogram of the filling factor, determined from the polarization data complemented by the UNNOFIT inversion results on the field inclination (see Eq. (6)). The abscissa is in logarithmic scale. 

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In Fig. 10, we plotted the histogram derived from the application of Eq. (6) to our data. The inclination angle value was taken from the UNNOFIT inversion results. We thus obtain a filling factor ranging between and , with a maximum probability at . The mean value is . The standard deviation of is 0.5. The values higher than unity have no physical meaning and come from the fact that for a quasihorizontal field, when is close to , becomes very large.
From the polarimetric accuracy
of our
ZIMPOL/THEMIS data (S being any of the Stokes parameters I,Q,U,V), we
find that the relative error predicted by Eq. (6) is
(7) 
Because , we find that the inaccuracy is not negligible but nevertheless lower than the standard deviation of the values displayed in the histogram of Fig. 10. We conclude that the dispersion we observe has a physical meaning, but that further observations with better polarimetric accuracy are needed to confirm this result.
5 The magnetic field probability density function
Figure 11: Histogram of the magnetic field strength, derived by dividing the local average magnetic field strength by the independently determined magnetic filling factor , in each solar pixel. The envelope of this histogram is the magnetic field probability density function (PDF), apart from a normalization factor. Actually, this PDF is a marginal density function of the joint density function of the two random variables and B, represented in Fig. 13. The abscissa is on a linear scale. 

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Figure 12: Behavior of the magnetic filling factor as a function of the magnetic field strength B. The linear fit can also be expressed as , with B_{1} = 15 G. 

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Figure 13: 2D histogram of the magnetic filling factor and of the magnetic field strength B, each pair of them known in each solar pixel. This figure is a 3D representation of the number of points in Fig. 12. The joint PDF is the envelope of the 2D histogram. The two marginal density functions and p(B) for each of the two random variables and B are the envelopes of the two histograms given in Figs. 10 and 11 respectively. 

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For each of the 1680 observed solar pixels (determined by the slit width and the camera pixel size along the slit), the local average magnetic field strength was obtained from the UNNOFIT inversion (Sect. 3), and the magnetic filling factor was directly and independently determined from the spectropolarimetric data (Sect. 4). The magnetic field strength value is then obtained by performing the ratio for each pixel, and the magnetic field strength B histogram follows (Fig. 11). The PDF of the magnetic field strength is then the envelope of this histogram. The tail of very strong fields that appears in the histogram stems from the noise contribution, but detecting strong fields associated to small filling factors is not new (see for instance SocasNavarro & Sánchez Almeida 2002; Domínguez Cerdeña et al. 2003b,a; GrossmannDoerth et al. 1996). Khomenko et al. (2003) obtained a B histogram similar in shape to ours, but with lower field strengths. Their histogram is devoid of any filling factor effect, because it results from direct Zeeman splitting measurement in IR profiles, where the Zeeman effect is stronger. However, as clearly shown by their Figs. 2 and 4, the Zeeman components are not yet completely resolved (in the near IR range), so that the real situation is probably inbetween the weak field approximation described by our Eq. (1) where the component separation does not depend on the field strength but instead on the derivative of the intensity profile and the completely resolved Zeeman effect. This circumstance could explain the lowest field strengths reported by these authors.
Thus, for each pixel, we find one
and one B value. These
values can be used to place a point representing the pixel in the

axes, thus giving a scatter plot where all the 1680 pixels are represented (Fig. 12). We find that these data are
wellfitted (in the loglog coordinates) by the linear function
(8) 
which is
with B_{1}=15 G. The form of this very simple relation partly comes from the histogram of Fig. 3 being rather narrow, whereas the histogram of Fig. 10 has a fairly extended range.
A 2D histogram can be built from Fig. 12 by defining 2D bins and
counting the number of points falling inside each 2D bin. This histogram is
represented in Fig. 13. Its envelope is the joint PDF of the two
random variables
and B, that we denote as
.
The
shape of the envelope (and Fig. 12) shows that these two variables
are strongly correlated. The magnetic field PDF (the envelope of the
histogram of Fig. 11) is the marginal PDF
(10) 
Similarly, the envelope of Fig. 10 is the other marginal PDF, .
For the benefit of the reader, we give the definition of the joint PDF of two random variables in Appendix A, and the related marginal PDFs (see also Papoulis 1965, Chap. 6).
5.1 Discussion of the magnetic field PDF
Figure 14: Weighted histogram of the magnetic field strength. For each bin of the magnetic field strength histogram of Fig. 11, the count number has been multiplied by the average magnetic field filling factor for this magnetic field strength , with B_{1} = 15 G following the linear fit in Fig. 12. The envelope of this histogram is then , where is the average filling factor conditioned by B, and p(B) is the magnetic field PDF of Fig. 11. The linear fit corresponds to an exponential decrease of as , with B_{0} = 660 G. 

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Confusion is encountered in the literature about the definition of the magnetic field PDF. This comes from the quiet Sun magnetic field being a complex quantity, having a PDF for both its field strength and magnetic filling factor, at least in data interpretation where these two quantities are determined in each pixel, the magnetic filling factor representing the fraction of the resolution element covered by the magnetic field B. From the modeling point of view, the necessity of introducing the magnetic filling factor is less evident, and one has to carefully examine the modeling conditions, i.e. with or without filling factor, before comparing the magnetic field PDFs. Thus, the following discussion will be divided into several parts corresponding to different approaches.
5.1.1 Comparison with Sánchez Almeida's definition
For the interpretation of observations concerning the solar internetwork,
Sánchez Almeida et al. (2003) introduce a quantity referred to as
magnetic field PDF and defined as being
proportional to the sum of filling factors of all those
measurements (i.e. of field strength B) in the bin
. In Sánchez Almeida (2007), this definition is rephrased
as the fraction of quiet Sun occupied by magnetic field of
each strength. The same definition is used in
Domínguez Cerdeña et al. (2006b,a). An explicit definition of
this quantity is given in Eq. (14) of Martínez González et al. (2008a). Starting
from this equation, we find that this socalled PDF can be written as
,
with p(B) the magnetic field marginal PDF introduced
above and
(11) 
Here, is the PDF of , conditioned by the value of B. Hence, is the average magnetic filling factor, conditioned by the value of B. We recall that we have the relation
Martínez González et al. (2008a) rightly mention that their PDF takes into account the filling factor. We think that it is not a good idea to call the product a PDF. It certainly does not have the normalization property that one expects from a PDF.
We now explain why this quantity
is very useful for
solar polarization modeling, although it is not a true magnetic field PDF.
For this purpose, let us recall that the first Stokes parameter I is the
specific intensity of radiation in erg/cm^{2}/s/sr/Hz. This means that the
energy
emitted by the elementary surface
during
the elementary time interval
in the elementary solid angle
and frequency interval
is
(13) 
The other Stokes parameters Q,U,V have the same unit. For this reason, when computing, say, the average emitted , starting from the known Q(B) corresponding to the magnetic field B, we must take into account that only a fraction of the elementary surface is occupied by the magnetic field, leading to
(14) 
For simplicity we assume that Stokes Q only depends on the magnetic field strength. Using Eq. (12), we obtain
which demonstrates the exact physical meaning of the quantity . But as discussed above this quantity is not the magnetic field PDF, a denomination that has to be reserved to p(B). We suggest calling the product the magnetic field contribution function and denoting it as C(B) (see also Appendix A).
5.1.2 Analytical fit giving the magnetic field PDF
In Fig. 14 we have plotted the histogram that has
as envelope, for comparison with Fig. 6 (right) of
Martínez González et al. (2008a) and with Fig. 3 of Sánchez Almeida et al. (2003)
(although this last figure concerns longitudinal magnetic fields). It can be
seen that the agreement with the IR data recommended by
Martínez González et al. (2008a) is fairly good, although our field strengths are
a bit higher. We agree with Martínez González et al. (2008a) on the linear
behavior of the histogram (in loglin coordinates). The linear fit of our
data is
where A is a constant to be determined by normalization, and B_{0}=660 G. Assuming that (see Eq. (9)), imposing , i.e. , since is unphysical, we obtain
(17) 
so that finally
with B_{1}=15 G, B_{0}=660 G, and . Figure 15 displays the histogram of Fig. 11 fitted with this function.
Figure 15: Fit of magnetic field strength histogram of Fig. 11 by the magnetic field PDF p(B) derived from the linear fits of Figs. 12 and 14. This magnetic field PDF is given by Eq. (18). 

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5.1.3 Comparison with volumefilling PDFs
Let us call volumefilling PDF, the PDF of a magnetic field present everywhere in the medium. In this case and the PDFs proposed in the literature have to be compared with the envelope of our local average magnetic field histograms. One also has to carefully examine whether the proposed PDF concerns the absolute field strength or the longitudinal field that is one component only of the field vector. We note that the consideration of the volumefilling longitudinal field is quite relevant, because this is the magnetic flux. We also note that in the case of a volumefilling magnetic field, the magnetic field PDF p(B) is indeed the fraction of the solar surface occupied by fields with values between B and (see the detailed discussion in Appendix A).
In this category, one finds the determination of the magnetic flux PDF by Stenflo & Holzreuter (2003). As the flux distribution is derived from magnetograms, it has to be compared with our Figs. 2 and 7. The widths of the distributions (13.5 G ours, 17.0 G theirs) are comparable and in good agreement with the polarimetric accuracy of the corresponding measurements. The authors consider the wings of the distribution in detail. Probably, the wings are caused by network pixels that bear a stronger field and are visible in their magnetograms (Fig. 1). Such pixels cannot be avoided in the measurements. Our distribution also has broader wings than Gaussian, visible in logarithmic scale in Fig. 16, but we have a much lower pixel number in our analysis. In the same category one finds the theoretical study by Berrilli et al. (2008). This is also a longitudinal flux PDF to be compared with our Figs. 2 and 7. As is visible in Fig. 16, we do not have enough pixels to validate or invalidate this model with our observations.
We now turn to the field strength distribution. Inspired by the exponential
PDF obtained by Martínez González et al. (2008a), Trujillo Bueno et al. (2004)
introduced an exponential distribution for the volumefilling field
strength,
,
to fit a series of Hanle effect
measurements of the turbulent quiet Sun magnetic field. In addition, the
field is assumed to be microturbulent with an isotropic angular
distribution. With B_{0}=130 G, the fit is rather satisfactory. It should
also be mentioned that the same data can be fitted almost equally well with
a singlevalued magnetic field (PDF in the form of a Dirac distribution)
with a strength of B=60 G. Our B_{0} value of 660 G differs notably,
however, from this 130 G value, because they assume (volumefilling magnetic field) in their simulation. This may also be due to
the shape of our PDF that decreases towards zero at the axis origin, as well
as our
histogram in Figs. 3 and 8, as does the Maxwellian distribution function, whereas their
theoretical distribution does not. Considering our result of
with B_{1}=15 G, the filling factor remains close to unity for
weak fields as those detected by Hanle effect interpretation, so that their
hypothesis of volumefilling may be found coherent with our results for weak
fields. As mentioned in our conclusion, the derived PDF may depend on the
sensitivity of the magnetic field measurement method (Hanle effect is
sensitive to weak and unresolved fields, Zeeman effect is sensitive to the
strongest fields). The mean value B=60 G that they derive under the
hypothesis of volumefilling and singlevalued microturbulent field remains
comparable to our mean value
G.
Figure 16: Same as Fig. 7, but with the number of pixels per bin (counts) plotted on a logarithmic scale to highlight the distribution in the wings. 

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5.1.4 Comparison with HINODE results
We now discuss the results by Orozco Suárez et al. (2007b) and Ishikawa & Tsuneta (2009). Both papers show a magnetic field strength PDF with a maximum in the hG range. A careful examination shows that their PDF definition is correct and is the same as ours, and that the differences in the results (our PDF peaks at higher field strengths) have to be assigned to a difference in the measurement of the magnetic filling factor. All these studies apply a MilneEddington inversion to the spectropolarimeteric data, with filling factor. As mentioned in Bommier et al. (2007), only the local average magnetic field strength can be retrieved from this inversion. It can be verified that both works agree when looking at this product : their field strengths are lower than ours, but their filling factor are higher than ours, so that the order of magnitude of their product is the same. We emphasize that their filling factor is defined by the rate of stray light, which is also assumed to be the proportion of light coming from the unmagnetic region (note that their corresponds to our )
The question lies in the filling factor method of measurement. Ours is described above and is performed independently of the MilneEddington inversion. They derive the filling factor by comparing, in a first step, local intensity profiles (no polarization at that step) with average intensity profiles assumed to represent the zero field situation. This is the method introduced by Skumanich & Lites (1987) and discussed by Lites & Skumanich (1990). Depending of the activity level of the map under study, this average profile is evaluated either by a global average or by a local average on the less active part on the map. In the present case of quiet Sun studies, this profile is determined by a local average evaluated around the pixel of interest. Considering that this approach gives a different result from ours, we are led to raise the question to know whether such a method really determines the nonmagnetic profile. If this average profile is taken from the whole map (global average) or from a less active but wide part of it, we note that the local physical parameters at the pixel under study (temperature, density) may not be fully taken into account in the nonmagnetic global profile. And if this average is performed on the neighbor pixels only as in the abovementioned studies, we raise the question: is the local average really nonmagnetic with respect to the considered pixel?
5.1.5 What can be expected from Fe I 6302.5 measurements?
When the quiet Sun magnetic field strength B is discussed, this magnetic field also has a magnetic filling factor . The question is how to determine and B separately. As discussed in Bommier et al. (2007), it is not possible to determine and Bseparately from inversion of Fe I 6302.5 Å data, but only their product . This is because, for solar magnetic field strengths and for a visible line like Fe I 6302.5 Å, the Zeeman splitting unit remains smaller or close to the Doppler width . This behavior can be expected for any line in the visible range. On the contrary, when the Zeeman components are separated, determining and B separately, by inversion, becomes possible. This is partly true at infrared wavelengths (see the discussion at the beginning of Sect. 5). That is why Martínez González et al. (2008a) are able to get reliable results by inverting infrared lines, and we get results in agreement with theirs by applying our direct determination complementing the inversion of the visible Fe I 6302.5 Å line. Examining the work of Martínez González et al. (2008a), it can be seen that they are not confident in the Fe I 6302.5 Å results in separate and B, because they find that these results depend on the initialization of the inversion; however, it can be seen in their paper that the magnetic flux, which is the longitudinal counterpart of the product , remains unchanged whatever the initialization be. This confirms that the inversion of visible Fe I 6302.5 Å data accurately recovers the local average magnetic field strength , though it is not able to recover and Bseparately.
6 Conclusions
We find that the magnetic field filling factor is related to the magnetic field strength B by the simple approximate law with B_{1}=15 G. Moreover, we find that the magnetic field PDF can be expressed by the analytical law of Eq. (18). This means that the medium is complex and various field strengths may be encountered: (i) the 1500 Gauss field filling 1% of space as seen in the tails of the magnetic field distributions by Khomenko et al. (2003), Martínez González et al. (2006), Orozco Suárez et al. (2007b), Martínez González et al. (2008a), as also detected by Domínguez Cerdeña et al. (2003b,2006b,2003a,2006a) ; (ii) the 150 Gauss field filling 10% of space as seen from incomplete PaschenBack effect interpretation by López Ariste et al. (2007) and Sánchez Almeida et al. (2008); (iii) 2050 Gauss field filling the major part of space, as seen from the Hanle effect interpretation (see the measurement review by Trujillo Bueno et al. (2004) and Trujillo Bueno et al. (2006) for the Sr I 4607 line, see also Bommier et al. (2006) for a series of MgH lines).
Because the kG internetwork field with very small filling factors were previously detected (Sánchez Almeida & Lites 2000; GrossmannDoerth et al. 1996), recent magnetoconvection modeling (Bushby et al. 2008) shows that fields stronger than the equipartition value could result from localized concentrations due to convective intergranular downflows. However, it should be noted that our results have to be taken with care because our field determination is based on a 2component inversion, whereas we arrive at the vision of a complex medium where all the field strengths coexist.
Actually, each magnetic field determination (Zeeman, hyperfine structure, Hanle) has its own sensitivity domain. Because it is a linear effect, the Zeeman effect detects the stronger fields better even if they do not fill the whole space. In contrast, the Hanle effect, being highly nonlinear, cannot detect the strong fields. To prove this point, let us assume a 2component atmosphere with a 2000 Gauss field filling 2% of space: 98% of the scattered radiation will not be depolarized, while 2% will only be depolarized by the Hanle effect. As a 2000 G field corresponds to the saturation regime of the Hanle effect, the corresponding linear polarization is 1/5 of the zero field one. As a result, the global polarization remains almost insensitive to strong intermittent magnetic fields. In contrast, the Hanle effect is sensitive to weak field filling the major part of space. The incomplete PaschenBack effect is sensitive to hG fields, but also is unable to detect kG fields. The result of our paper is that the strong, intermediate, and weak fields cohabit, with different filling factors obeying the simple approximate law with B_{1}=15 G.
In a later paper of this series, we will analyze the centertolimb variation of the quiet Sun polarization with ZIMPOL on THEMIS observations, in order to thoroughly investigate the field direction distribution function. Further observations with a better polarimetric accuracy are, however, needed to confirm the results obtained in the present work.
AcknowledgementsThe authors are grateful and indebted to D. Gisler and A. Feller for having provided the ZIMPOL data reduction package adapted to THEMIS, and to the whole ZIMPOL and THEMIS teams and to J.O. Stenflo for having given them the possibility of using ZIMPOL on THEMIS. They are also grateful to the anonymous referee for the kind and very helpful comments. Thanks also to J. Adams for the excellent english language corrections. The ZIMPOL campaign at THEMIS was financed by the SNF grant 200020117821. A.A.R. acknowledges financial support by the Spanish Ministry of Education and Science through project AYA200763881.
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Appendix A: Statistical definitions
The question of the magnetic field PDF of the solar internetwork is still a hot subject of discussion, with different observations leading to somewhat different answers. The meaning of magnetic field PDF is not always clear, in particular when the magnetic field is not present everywhere in the medium. We show here how an unambiguous definition of the magnetic field PDF can be given in this latter case.
We assume that we have some area at our disposal on the solar surface divided into a number N of pixels. In each pixel, a value for the magnetic field vector and a value for a filling factor , with , were determined by some inversion method. In each pixel, this factor yields the fraction of the surface where the magnetic field is present. In a quiet internetwork region, the values of and are changing from pixel to pixel in a way that cannot be predicted with certainty. This suggests treating these two quantities as random variables. If the value of N is sufficiently high, we can hope to deduce from the data set statistical properties of the magnetic field and of the filling factor. This type of analysis is the purpose of the present paper, based on spectropolarimetric data obtained with ZIMPOL on THEMIS. In the following we would like to give an overall picture of the basic definitions. All the concepts that are introduced below are standard elements in probability theory. We recommend Papoulis (1965) for a rigorous, yet easily readable, introduction to probability theory.
For simplicity in notation, we consider amplitude B of the magnetic field instead of vector . We also assume that the random variables Band have a continuous range of values with and . Henceforth, random variables are denoted with boldface characters to distinguish them from the outcome values of a given event. The continuity assumption implies that N is infinite. The case of finite Nis considered below. We introduce the joint PDF defined by
(A.1) 
As is clear from the definition,
is the probability
that
has a value in the interval
and
a value in the interval
.
We recall
that
is the second derivative, assumed to exist, of the joint
probability distribution function
,
i.e.
(A.2) 
with
(A.3) 
The joint distribution function satisfies and .
The function
satisfies
and the
normalization condition
(A.4) 
Starting from , we can define the two marginal PDFs
(A.5)  
(A.6) 
These functions are the PDFs of B and . It is easy to verify that they are normalized to unity, namely
(A.7)  
(A.8) 
They can be used to define the mean values
(A.9)  
(A.10) 
Very useful are the conditional PDFs and , which are the PDF of , knowing B, and the PDF of B, knowing . They are defined by
(A.11)  
(A.12) 
With these conditional PDFs, one can define conditional averages,
It is easy to verify that
(A.15)  
(A.16) 
The conditional average yields the mean value of the filling factor for magnetic fields with a value between B and . The product can be interpreted as the fraction of the surface occupied by magnetic fields between B and .
The concepts of joint PDF and conditional PDF are easy to grasp with a graphic representation. We introduce a rectangular coordinate system , with the axes and B defining the horizontal plane and z the vertical axis. The joint PDF defines a surface . If we intersect this surface by the vertical plane B=B_{1}, we obtain the profile of the conditional PDF , as a function of . Similarly, a cut by the vertical plane yields the profile of the conditional PDF , as a function of B.
In some spectropolarimetric analysis one considers that the magnetic field is present everywhere in the medium. In this case the random variable takes only the value . All the expressions given above hold with , being the Dirac distribution. The conditional PDFs become and . For the Hanle effect, it is always assumed that and often that the magnetic strength has a single value B=B_{0} . The corresponding joint PDF reduces to .
For simplicity in the notation, we have retained the strength B of the magnetic field as random variable. It is clear that all the definitions remain the same if we replace B by the magnetic field vector . The vector corresponds actually to three random variables, one for the strength and two for the direction. The differential element should be replaced , with and the polar angles of the magnetic field direction in an appropriate reference frame.
An interesting quantity for the understanding of the Sun global energy
budget is the mean magnetic energy density in the quiet internetwork. If the
magnetic field is present everywhere, this mean energy is
with
(A.17) 
If the field is not volumefilling, one should use
(A.18) 
This expression can be written
with
C(B)  =  
=  (A.20)  
= 
Here, is the conditional mean value of defined in Eq. (A.13). The function C(B) also appears in the calculation of the mean Stokes parameters Q, U, and V, when the magnetic field is not volumefilling (see Sect. 5). If the random variable only takes the value 1, C(B) is simply the PDF of the random variable . If not, as suggested by Eq. ( A.19), C(B) could be referred to as the magnetic field contribution function. The name magnetic field PDF should be reserved for the marginal PDF p(B). One reason for not calling C(B) a magnetic field PDF is that it is not normalized to unity. It is easy to check that the integral of C(B) over Bis equal to the mean value .
In the analysis of real data, the number N of pixels is not infinite. Also the magnetic field and filling factor are determined with some error bar. What is usually inferred from the data are histograms of the count number, i.e. of the number of pixels n(B_{i}) in which the magnetic field strength takes a value between B_{i} and . Similarly histograms are being constructed with the number of pixels in which the filling factor takes a value between and . The envelopes of these histograms, divided by and , yield the marginal PDFs p(B) and , in the limit , , with and constants. One can also construct 2Dhistograms corresponding to the joint PDF . In each cell , one plots on the vertical axis, the number of pixels in which B has a value in the interval and has a value in the interval . As in the continuous case, the conditional histograms are obtained by cutting the 2Dhistogram with vertical planes. Examples of 1D and 2D histograms can be found in the present paper.
The mean magnetic energy takes the form
(A.21) 
with
where is the number of pixels in which and . The definition of C(B_{i}) in Eq. (A.23) is identical to the definition of the magnetic field PDF given in Eq. (14) in Martínez González et al. (2008a). We note here that is the discrete version of the conditional PDF , whereas , is the discrete version of the marginal PDF p(B). The summation over j in the first square bracket of Eq. (A.23) yields the conditional mean value of with B in the interval . When takes only the value , is the fraction of the surface occupied by magnetic fields in the bin , and this ratio is the discrete version of the magnetic field PDF. When the magnetic field is not present everywhere in the medium, the fraction of the surface occupied by magnetic fields with a value of B in the bin is given by C(B_{i}). As already stressed above, this function is not a PDF.
Footnotes
 ... THEMIS^{}
 Based on observations made with the FrenchItalian telescope THEMIS operated by the CNRS and CNR on the island of Tenerife in the Spanish Observatorio del Teide of the Instituto de Astrofísica de Canarias.
 ...^{}
 Present address: Instituto de Astrofísica de Canarias, vía Láctea s/n, 38205 La Laguna, Tenerife, Spain.
All Tables
Table 1: Information on the averaged data. Each line of the table corresponds to one average.
All Figures
Figure 1: UNNOFIT fit (dotted line) of a typical observation (full line). The main spectral line (centered at pixel 38), that is polarized, is Fe I 6302.5 Å, and the other line, unpolarized, is a telluric line. 10 pixels are 72 mÅ and blue is towards the left. Derived magnetic field parameters: local average field strength 11.7 G, inclination 115 from the lineofsight, azimuth 123 from the slit direction which is the reference axis for the Stokes parameters. The line strength parameter is found to be 2.6, and the Doppler width 35.8 mÅ. 

Open with DEXTER  
In the text 
Figure 2: Histogram of the local average longitudinal magnetic field (the product of the longitudinal magnetic field B_{z} with the magnetic filling factor ), from the UNNOFIT inversion. 

Open with DEXTER  
In the text 
Figure 3: Histogram of the local average magnetic field strength (the product of the magnetic field strength B with the magnetic filling factor ), from the UNNOFIT inversion. 

Open with DEXTER  
In the text 
Figure 4: Histogram of the magnetic field inclination with respect to the lineofsight, from the UNNOFIT inversion. The lineofsight is also the solar vertical with the observation performed at disk center. 

Open with DEXTER  
In the text 
Figure 5: Histogram of the magnetic field azimuth with respect to the slit direction, from the UNNOFIT inversion (ambiguity is not resolved). The observation was performed at disk center and the slit was solar north, so that this is also the histogram of the horizontal field component azimuth. 

Open with DEXTER  
In the text 
Figure 6: Test of the determination of the local average magnetic field strength (the product of the magnetic field strength B with the magnetic filling factor ) by the UNNOFIT inversion. A series of theoretical profiles are computed under the conditions of the ZIMPOL observations (spectral and polarimetric resolutions), and then submitted to the inverter. In abscissae are the input known values, in ordonnae are the output recovered values. The bottom figure is a zoom of the top figure near the axis origin. 

Open with DEXTER  
In the text 
Figure 7: Fit of the local average longitudinal magnetic field histogram of Fig. 2 by a Gaussian of halfwidth w = 13.5 G. 

Open with DEXTER  
In the text 
Figure 8: Fit of the local average magnetic field strength histogram of Fig. 3 by a Maxwellian of halfwidth w = 11 G. 

Open with DEXTER  
In the text 
Figure 9: Test of the determination of the magnetic filling factor by applying Eq. (6) to the polarimetric data. For the test, the polarimetric data were theoretical profiles computed from the UnnoRachkovsky solution, weighted by a theoretical input magnetic filling factor (input). Equation (6) is then applied, leading to (output). The figure displays their ratio, for a series of magnetic field inclination angles and strengths (in Doppler width units). This plot is valid for any value. 

Open with DEXTER  
In the text 
Figure 10: Histogram of the filling factor, determined from the polarization data complemented by the UNNOFIT inversion results on the field inclination (see Eq. (6)). The abscissa is in logarithmic scale. 

Open with DEXTER  
In the text 
Figure 11: Histogram of the magnetic field strength, derived by dividing the local average magnetic field strength by the independently determined magnetic filling factor , in each solar pixel. The envelope of this histogram is the magnetic field probability density function (PDF), apart from a normalization factor. Actually, this PDF is a marginal density function of the joint density function of the two random variables and B, represented in Fig. 13. The abscissa is on a linear scale. 

Open with DEXTER  
In the text 
Figure 12: Behavior of the magnetic filling factor as a function of the magnetic field strength B. The linear fit can also be expressed as , with B_{1} = 15 G. 

Open with DEXTER  
In the text 
Figure 13: 2D histogram of the magnetic filling factor and of the magnetic field strength B, each pair of them known in each solar pixel. This figure is a 3D representation of the number of points in Fig. 12. The joint PDF is the envelope of the 2D histogram. The two marginal density functions and p(B) for each of the two random variables and B are the envelopes of the two histograms given in Figs. 10 and 11 respectively. 

Open with DEXTER  
In the text 
Figure 14: Weighted histogram of the magnetic field strength. For each bin of the magnetic field strength histogram of Fig. 11, the count number has been multiplied by the average magnetic field filling factor for this magnetic field strength , with B_{1} = 15 G following the linear fit in Fig. 12. The envelope of this histogram is then , where is the average filling factor conditioned by B, and p(B) is the magnetic field PDF of Fig. 11. The linear fit corresponds to an exponential decrease of as , with B_{0} = 660 G. 

Open with DEXTER  
In the text 
Figure 15: Fit of magnetic field strength histogram of Fig. 11 by the magnetic field PDF p(B) derived from the linear fits of Figs. 12 and 14. This magnetic field PDF is given by Eq. (18). 

Open with DEXTER  
In the text 
Figure 16: Same as Fig. 7, but with the number of pixels per bin (counts) plotted on a logarithmic scale to highlight the distribution in the wings. 

Open with DEXTER  
In the text 
Copyright ESO 2009
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