Issue 
A&A
Volume 558, October 2013



Article Number  A130  
Number of page(s)  5  
Section  The Sun  
DOI  https://doi.org/10.1051/00046361/201321485  
Published online  16 October 2013 
Helioseismology of sunspots: how sensitive are travel times to the Wilson depression and to the subsurface magnetic field?
^{1}
MaxPlanckInstitut für Sonnensystemforschung,
37191
KatlenburgLindau,
Germany
email:
schunker@mps.mpg.de
^{2}
Institut für Astrophysik, GeorgAugustUniversität Göttingen,
37077
Göttingen,
Germany
Received:
15
March
2013
Accepted:
21
June
2013
To assess the ability of helioseismology to probe the subsurface structure and magnetic field of sunspots, we need to determine how helioseismic travel times depend on perturbations to sunspot models. Here we numerically simulate the propagation of f, p_{1}, and p_{2} wave packets through magnetic sunspot models. Among the models we considered, a ±50 km change in the height of the Wilson depression and a change in the subsurface magnetic field geometry can both be detected above the observational noise level. We also find that the traveltime shifts due to changes in a sunspot model must be modeled by computing the effects of changing the reference sunspot model, and not by computing the effects of changing the subsurface structure in the quietSun model. For p_{1} modes, the latter is wrong by a factor of four. In conclusion, numerical modeling of MHD wave propagation is an essential tool for interpreting the effects of sunspots on seismic waveforms.
Key words: Sun: helioseismology / sunspots
© ESO, 2013
1. A numerical approach
Elucidating the subsurface processes of sunspot formation and evolution is important for understanding solar magnetism (Moradi et al. 2010; Rempel & Schlichenmaier 2011). Helioseismology is the only available tool for imaging the subsurface structure, magnetic field, and dynamics of sunspots (Gizon et al. 2010), all of which are largely unknown.
Early approaches interpreted the seismic signature of sunspots in terms of small perturbations to a quietSun reference model (Fan et al. 1995; Kosovichev 1996). However, the effects of the surface magnetic field and associated structural changes cause large perturbations in the wave speed (e.g., Lindsey & Braun 2005; Gizon et al. 2006). Recently, direct numerical simulations of magnetohydrodynamic (MHD) wave propagation through sunspot models have been used to capture the strong effects of the magnetic field on the waves (Gizon et al. 2010; Cameron et al. 2011).
A study by Liang et al. (2013) has measured the traveltime shifts caused by the sunspot in AR 9787. In an effort to understand and interpret these measurements, we numerically simulated the interaction of surfacegravity (f) and acoustic (p_{1} and p_{2}) wave packets with several sunspot models. With spectroscopy the height of the Wilson depression in sunspots is not known to better than 50 km (Solanki et al. 1993). Here we investigate whether seismic diagnostics can provide a stronger constraint. Furthermore, we study the seismic consequences of two subsurface magnetic field geometries below sunspots: a monolithic flux tube versus a weaker, spreadout magnetic field. Finally, we explore the sensitivity of waves to soundspeed perturbations at different depths along the axis of a sunspot model.
These parametric studies enable us to test the assumptions of existing approximation methods used in the interpretation of sunspot seismology. By comparing with measured noise in seismic travel times, we are able to draw conclusions about the detectability of different aspects of sunspot structure.
2. Sunspot models
2.1. Background quietSun model (QS)
Our sunspot models are embedded in the background solar model CSM_A described by Schunker et al. (2011). The CSM_A model is based on Model S from ChristensenDalsgaard et al. (1996), but was modified to be convectively stable so that linear waves can be propagated using the SLiM wave simulation code (Cameron et al. 2008). An indication of the sensitivity of the modes of oscillation in CSM_A as a function of height, z, is given by their kinetic energy density (see Fig. 1). Throughout this paper we define z as the height measured upward from the bottom of the photosphere.
2.2. Reference sunspot model (RS)
Cameron et al. (2011) constructed a parametric sunspot model that causes a seismic response consistent with what is observed for the sunspot in active region NOAA 9787 (Liang et al. 2013, Paper I). The vector magnetic field of the sunspot model is cylindrically symmetric; i.e., it only depends on the horizontal distance from the axis of the sunspot, ϖ = (x^{2} + y^{2})^{1/2}, and on height, z. The model of Cameron et al. (2011) is a selfsimilar and monolithic magnetic field model specified by the strength of the field on the axis of the sunspot (ϖ = 0) as a function of height. Here we adopt the same sunspot model with the parameters given in Table 1 of Cameron et al. (2011), except that the parameters controlling the inclination of the magnetic field are modified slightly (α_{1} = 1.5 Mm and α_{2} = 9.2 Mm) so that the magnetic field inclination at the umbrapenumbra boundary (50°) matches observed field inclinations in sunspots better (Schunker et al. 2008). Figure 1 shows a sample of the magnetic field lines. Throughout this paper we refer to this model as the reference sunspot model, abbreviated as “RS”.
2.3. Changes to the Wilson depression
The Wilson depression is a physical depression of the surface (optical depth unity) caused by strong magnetic fields in the umbra of a sunspot (Loughhead & Bray 1958). The Wilson depression of our reference sunspot model is at z = −550 km in the center of the umbra and at z = −300 km in the middle of the penumbra as in Cameron et al. (2011).
To assess the ability of helioseismology to measure the height of the Wilson depression, we considered two additional sunspot models in which the Wilson depression is shifted by ± 50 km with respect to the reference sunspot model. In these modified models, we translated the density, pressure, and soundspeed profiles in height by ± 50 km, while keeping the magnetic field unchanged. (Models are not in magnetohydrostatic equilibrium.)
Fig. 1 Reference sunspot model and perturbations to it. The magnetic field lines of the reference model are shown by the black curves (Sect. 2.2). The dashed black curves are the magnetic field lines of the alternative magnetic field model (Sect. 2.4). Two Wilson depressions modified by ± 50 km have been considered (red curves, Sect. 2.3). The ellipses along the axis of the sunspot indicate the locations of the various soundspeed perturbations (Sect. 2.5). The size of the ellipses corresponds to the full width at half maximum of the Gaussian perturbations. The uppermost soundspeed perturbation is shown in light blue to be easily distinguished from the perturbation half a megameter below. The right panel shows mode kinetic energy density, ρ ∥ v ∥ ^{2}, for the f mode at kR_{⊙} = 450 (black), for p_{1} at kR_{⊙} = 420 (blue), and for p_{2} at kR_{⊙} = 390 (red), where ρ is density and v is the velocity eigenfunction for quietSun model CSM_A. Mode kinetic energy density is a useful indicator of the vertical sensitivity of the modes. 

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2.4. Alternative magnetic field model
The monolithic reference sunspot model described in Sect. 2.2 is only one possibility among many. We considered a sunspot model with an alternative magnetic field below z = −1 Mm, which fans out as a function of depth. This alternative model is motivated by, e.g., the dynamical disconnection model of Schüssler & Rempel (2005) whereby the flux tube is disrupted by convective motions at depths greater than 2 Mm. In the alternative magnetic sunspot model, we keep the sound speed, pressure and density profiles unchanged from the reference sunspot model.
More precisely, the alternative magnetic field is modified so that the magnetic field becomes weaker below z_{t} = −1 Mm (above, it is identical to the reference sunspot model), smoothly transitioning to weak field strengths below z_{b} = −4 Mm. Along the axis of the sunspot, the zcomponent of the magnetic field, , is obtained from the reference field, B_{z}, as (1)where Π(z) is the fifthorder polynomial in z such that is continuous and has continuous first and secondorder derivatives; i.e., Π(z) = 1−0.9Z^{3}(6Z^{2}−15Z + 10) where Z = (z − z_{t})/(z_{b} − z_{t}). The same field lines as for the reference sunspot model are shown for the alternative magnetic field model in Fig. 1.
2.5. Subsurface soundspeed perturbations
We also consider a set of sunspot models in which we modify the subsurface sound speed. In these models, the sound speed is given by (2)where c is the sound speed in the reference sunspot model, and (3)is a 3D Gaussian perturbation to the sunspot model. In the above expression, the relative amplitude of the perturbation is A, the height of the center of the perturbation is h, and the width of the perturbation is fixed to σ_{z} = 0.42 Mm, σ_{ϖ} = 2.12 Mm. For one experiment (Sect. 5.1) we used all the perturbations (shown by the ellipses in Fig. 1). For a second experiment (Sect. 5.2) we used only the perturbations associated with the light blue ellipse.
3. Numerical simulations of wave propagation
We used the SLiM code (Cameron et al. 2007, 2011) to simulate the propagation of wave packets through the sunspot models described above. We used a simulation domain that covers 145.77 Mm in each of the horizontal directions and extends from −25 Mm below to 2.5 Mm above the bottom of the photosphere. The depth of the simulation domain is sufficient to study acoustic modes with radial orders n ≤ 4. The spatial resolutions are 0.025 Mm per pixel vertically and 0.73 Mm per pixel horizontally. The time resolution is 0.13 s. We did a resolution study that showed that the numerical solutions are converged for the waves studied here.
We carried out simulations for individual wave packets with modes of fixed radial order, i.e. with either f, p_{1}, or p_{2} modes. The initial conditions (t = 0) for the simulations are specified by the displacement, ξ(x,y,z), and the velocity, v(x,y,z). This requires specifying the wave amplitude distribution, A_{k}, as a function of wavenumber, k (see Cameron et al. 2008, 2011). For each wave packet, A_{k} is chosen in such a way that the vertical velocity in the simulation (v_{z}) is directly comparable to an observed crosscovariance function. This comparison is justified because the crosscovariance is closely related to the Green’s function in the far field (e.g., Gizon et al. 2010).
The wave packets in our simulations are comparable to the Solar and Heliospheric Observatory’s Michelson Doppler Imager (SOHO/MDI) observed crosscovariance functions presented by Liang et al. (2013). The peak of wave power occurs at kR_{⊙} = 450 and ν = 2.1 mHz for the f modes, at kR_{⊙} = 420 and ν = 2.5 mHz for the p_{1} modes, and at kR_{⊙} = 390 and ν = 3.1 mHz for the p_{2} modes. At t = 0, each wave packet peaks at x = −43.73 Mm (at the left edge of Fig. 2), from where they propagate in the + x direction (to the right) and interact with the sunspot centered at x = y = 0 Mm.
Fig. 2 Spatial map of traveltime shifts Δ_{QS}τ of p_{1} modes through the reference sunspot model. The SLiM code numerically computes the waveform as a function of time through the reference sunspot model. The color bar indicates the traveltime shift in seconds. The ellipse encloses the region for which the spatial average of the traveltime shift (denoted with symbols ⟨ ⟩) is computed. The gray (black) circle indicates the penumbra (umbra) of the sunspot. 

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4. Travel times
4.1. Measuring travel times
Traveltime measurements are very useful for characterizing the sensitivity of seismic waveforms to subsurface perturbations. In this paper we explore how changes to the reference sunspot model affect travel times.
We define the traveltime shift, Δτ, as the time by which a sliding reference wavelet, w, must be shifted to best match the seismic waveform v_{z}(x,y,t) = v_{z}(x,y,z = 0.2 Mm,t). Following Gizon & Birch (2002) and Liang et al. (2013), Δτ is the time, τ, that maximizes the function (4)In practice, the reference wavelet w was chosen to be v_{z} from either the quietSun simulation or the reference sunspot simulation. To denote these two kinds of measurements (which give similar results, see Sect 5.2), we used the notations Δ_{QS}τ and Δ_{RS}τ, respectively. Furthermore, we used the notation Δτ(MODEL) to indicate the background model through which the seismic waveform is propagated, where “MODEL” is “RS”, “RS+pert”, or “QS+pert”. The time integrals in Eq. (4) are approximated by summations with a time discretization, of 6 s. With this time discretization travel times are accurate to 0.01 s, which is sufficient for our purpose.
4.2. Estimating traveltime noise
While the numerical simulations performed in this paper are used to estimate the expectation value of a traveltime measurement (the signal), we also need to estimate the noise level in order to determine whether a signal is detectable.
We used the traveltime maps measured by Liang et al. (2013) covering seven independent days of SOHO/MDI observations of AR9787 (Gizon et al. 2009; Moradi et al. 2010). To decrease noise, we further averaged these traveltime maps over a region behind the sunspot where scattering phase shifts are large. This elliptical portion of the traveltime maps is shown in Fig. 2. We use angle brackets ⟨ · ⟩ to denote this spatial averaging of the travel times.
For one day of observations, the spatially averaged traveltime shift introduced by the sunspot is ⟨ Δ_{QS}τ ⟩ ≃ 75 s for the p_{1} modes. To estimate the noise in these measurements, we compute ⟨ Δ_{QS}τ ⟩ for each of the seven days of observations. We define the observed noise level as the standard error in the mean of the spatially averaged traveltime shifts. The observed noise level decreases with radial order: it is 3.8 s for the f modes, 3.5 s for p_{1} modes, and 1.6 s for p_{2} modes.
5. Results
We carried out two sets of numerical experiments. In the first set, we propagated f, p_{1}, and p_{2} waves independently through different sunspot models to predict the traveltime shifts caused by various perturbations to the reference sunspot model and to determine whether they are above the observed noise level. In the second set of experiments we looked at the sensitivity of p_{1} wave travel times to changes in the amplitude of the subsurface sound speed. We considered soundspeed perturbations to both the quietSun model and to the reference sunspot model. The results of these experiments are described in the sections below.
5.1. Is it possible to distinguish between sunspot models?
One way to measure the effect of a change in the sunspot model on the waves is to look at the change in the traveltime shifts measured with respect to the waves in the quietSun reference model, i.e. by computing the difference ⟨ Δ_{QS}τ(RS + pert) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩. Table 1 shows these changes in traveltime shifts for the perturbations to the reference sunspot model described in Sects. 2.3, 2.4, and 2.5. For the case where the Wilson depression is moved deeper (shallower) by 50 km, we find that the f wave packet travels slower (faster) and the p_{1} and p_{2} wave packets travel faster (slower). Because the traveltime shifts for these two cases do not have the same amplitude, perturbation theory that is linear in the height of the Wilson depression will not fully capture this result. The physical cause of these effects is not clear. We note, however, that a change in the Wilson depression implies a change in the density, soundspeed, and Alfvén speed, which all affect the wave speed (Hanasoge et al. 2012). For the case of the p_{2} wave packet, the change in the traveltime shift is roughly twice the noise level, implying that the p_{2} travel times are useful for constraining the height of the Wilson depression to an accuracy better than 50 km (assuming the other sunspot parameters are well constrained).
Reducing the strength of the subsurface magnetic field causes a change in the traveltime shift of roughly 3 s for all wave packets. The physical process governing the interaction of the wave with the subsurface magnetic field is not clear. We recall that this change in the magnetic field is only below z = −1 Mm. As for the case of changes to the height of the Wilson depression, the change in the traveltime shift is about twice that of the observed noise level for the p_{2} wave packet. Assuming that the Wilson depression was well constrained (and all other sunspot parameters), the subsurface magnetic field may also be constrained.
Inserting subsurface soundspeed enhancements causes the p_{1} and p_{2} mode wave packets to travel faster than expected. The f wave packet is not sensitive to the subsurface sound speed at all, which is also not surprising since it is a surface gravity wave. Unless the observed signaltonoise can be increased for the p_{1} and p_{2} wave packets by a factor of at least 4, soundspeed perturbations of this type will not be able to be detected with the spatially averaged traveltime shifts of these modes.
Spatially averaged traveltime shift introduced by the perturbation to the sunspot model, ⟨ Δ_{QS}τ(RS + pert) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩.
5.2. Can we avoid using numerical simulations?
In the second experiment, we further investigated the sensitivity of traveltime shifts to changes in the subsurface soundspeed. Fan et al. (1995), Kosovichev (1996), and Birch et al. (2004) explored this problem using perturbation theory around quietSun reference models. Here we go beyond the smallamplitude perturbation theory and look at finite amplitude perturbations to the subsurface sound speed. In addition, we look at the effects of identical soundspeed changes to a reference sunspot model and in the quietSun model.
We insert Gaussian soundspeed perturbations of various amplitudes into the reference sunspot model (i.e., Eq. (3) with A = −0.01 to 0.5 and h = −1.5 Mm). To assess the significance of the reference model, we also insert identical soundspeed perturbations into the background quietSun model so that (5)where c_{0} is the quietSun sound speed, and Δc(ϖ,z) is the perturbation to the reference sunspot model defined by Eq. (3). We simulated the propagation of p_{1} wave packets through these models.
Fig. 3 Traveltime perturbations versus soundspeed perturbation amplitudes A, for p_{1} wave packets. The results from two SLiM numerical experiments are shown. In the first procedure, the red diamonds show the traveltime perturbations resulting from soundspeed perturbations to a background model that includes the reference sunspot, ⟨ Δ_{QS}τ(RS + δc) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩. In the second procedure, the black diamonds show the traveltime perturbations resulting from the same soundspeed perturbations to a quietSun background model, ⟨ Δ_{QS}τ(QS + δc) ⟩. In both experiments, the travel times (diamonds) are measured using sliding quietSun waveforms. For the first experiment, the red asterisks show the results using a different measurement procedure, ⟨ Δ_{RS}τ(RS + δc) ⟩. The solid lines show linear fits to the three smallest perturbations with A = −1%, 0, and 1%. The inset shows a zoom around the origin of the plot. The dashed curves are parabolic fits. The p_{1} traveltime noise level for 7 days of observation is 3.5 s as indicated by the arrow. 

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Figure 3 shows the change in the spatially averaged traveltime shifts, ⟨ Δ_{QS}τ(RS + δc) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩, as a function of the amplitude of the soundspeed perturbation. The ensuing changes to the traveltime shift are not linear with the amplitude of the soundspeed perturbation. The deviation from linearity for a soundspeed perturbation with a 10% amplitude is 5% – a parabolic fit describes the change in the traveltime shifts with respect to soundspeed perturbation amplitude better. For all amplitudes, even up to 50%, the change in the traveltime shift is well below the observed noise level. Thus, these subsurface soundspeed perturbations are not detectable using only the p_{1} wave packet.
Another way to measure the traveltime shift due to the soundspeed perturbations is to directly compute the traveltime shift with respect to the reference sunspot model, i.e., ⟨ Δ_{RS}τ(RS + δc) ⟩ (see Fig. 3). This gives a different, but qualitatively similar, result to the previous method. This shows that the general behavior of the change in the traveltime shifts with amplitude is not just a consequence of the measurement procedure.
Figure 3 also shows the traveltime shifts, ⟨ Δ_{QS}τ(QS + δc) ⟩, caused by imposing the same soundspeed perturbations in the quietSun model. In this case, the linear approximation is incorrect by more than 10% when the amplitude of the soundspeed perturbation is 10%. More importantly, these traveltime shifts are roughly four times larger than the traveltime shifts caused by imposing the same soundspeed perturbation in the reference sunspot model. As a result, the quietSun model cannot be used to predict the traveltime shifts caused by soundspeed perturbations to a sunspot model because the sunspot substantially changes the p_{1} wave packet, and thus its sensitivity to subsurface perturbations. Therefore, it is necessary to use numerical simulations for a better understanding of the effects of a sunspot on the waves.
6. Summary and prospects
We have shown that it should be possible to constrain the height of the Wilson depression to within 50 km and to distinguish between the two models for the subsurface magnetic field structure (a monolithic and a weaker spreading field) using seven days of SOHO/MDI observations of one sunspot. Using only the spatial average of the traveltime shifts, it is not possible to detect 10% soundspeed changes with a length scale of 5 Mm at depths between 1.5 and 4 Mm with the same observations. We expect that including more information, such as the spatial distribution of the traveltime shifts, the amplitude of the crosscorrelations, and higher order modes, will improve the ability of helioseismic measurements to constrain the subsurface structure of sunspots.
We have also demonstrated that the wave traveltime shifts caused by changes in sound speed to our sunspot model are different than the wave traveltime shifts caused by the same change in sound speed of the quietSun model. This is due to the effect of the sunspot on the wavefield, and this effect is not captured by the traditional approximations of local helioseismology (Fan et al. 1995; Kosovichev 1996; Birch et al. 2004). Computational helioseismology, however, provides a clear path forward. These simulations may also be used to test the magnetoghydrodynamic ray approximation (e.g. Cally 2000; Schunker & Cally 2006).
Other avenues to explore are the use of vector magnetograms and intensity images to further constrain the surface properties
of sunspots and the use of SDOHMI Doppler observations (Scherrer et al. 2012) for helioseismic measurements.
Acknowledgments
H.S. and L.G. acknowledge research funding by Deutsche Forschungsgemeinschaft (DFG) under grant SFB 963/1 “Astrophysical flow instabilities and turbulence” (Project A18, WP “Seismology of magnetic activity”). The German Data Center for SDO, funded by the German Aerospace Center (DLR), provided the IT infrastructure.
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All Tables
Spatially averaged traveltime shift introduced by the perturbation to the sunspot model, ⟨ Δ_{QS}τ(RS + pert) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩.
All Figures
Fig. 1 Reference sunspot model and perturbations to it. The magnetic field lines of the reference model are shown by the black curves (Sect. 2.2). The dashed black curves are the magnetic field lines of the alternative magnetic field model (Sect. 2.4). Two Wilson depressions modified by ± 50 km have been considered (red curves, Sect. 2.3). The ellipses along the axis of the sunspot indicate the locations of the various soundspeed perturbations (Sect. 2.5). The size of the ellipses corresponds to the full width at half maximum of the Gaussian perturbations. The uppermost soundspeed perturbation is shown in light blue to be easily distinguished from the perturbation half a megameter below. The right panel shows mode kinetic energy density, ρ ∥ v ∥ ^{2}, for the f mode at kR_{⊙} = 450 (black), for p_{1} at kR_{⊙} = 420 (blue), and for p_{2} at kR_{⊙} = 390 (red), where ρ is density and v is the velocity eigenfunction for quietSun model CSM_A. Mode kinetic energy density is a useful indicator of the vertical sensitivity of the modes. 

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In the text 
Fig. 2 Spatial map of traveltime shifts Δ_{QS}τ of p_{1} modes through the reference sunspot model. The SLiM code numerically computes the waveform as a function of time through the reference sunspot model. The color bar indicates the traveltime shift in seconds. The ellipse encloses the region for which the spatial average of the traveltime shift (denoted with symbols ⟨ ⟩) is computed. The gray (black) circle indicates the penumbra (umbra) of the sunspot. 

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In the text 
Fig. 3 Traveltime perturbations versus soundspeed perturbation amplitudes A, for p_{1} wave packets. The results from two SLiM numerical experiments are shown. In the first procedure, the red diamonds show the traveltime perturbations resulting from soundspeed perturbations to a background model that includes the reference sunspot, ⟨ Δ_{QS}τ(RS + δc) ⟩ − ⟨ Δ_{QS}τ(RS) ⟩. In the second procedure, the black diamonds show the traveltime perturbations resulting from the same soundspeed perturbations to a quietSun background model, ⟨ Δ_{QS}τ(QS + δc) ⟩. In both experiments, the travel times (diamonds) are measured using sliding quietSun waveforms. For the first experiment, the red asterisks show the results using a different measurement procedure, ⟨ Δ_{RS}τ(RS + δc) ⟩. The solid lines show linear fits to the three smallest perturbations with A = −1%, 0, and 1%. The inset shows a zoom around the origin of the plot. The dashed curves are parabolic fits. The p_{1} traveltime noise level for 7 days of observation is 3.5 s as indicated by the arrow. 

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In the text 
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