Issue 
A&A
Volume 617, September 2018



Article Number  A111  
Number of page(s)  10  
Section  Stellar structure and evolution  
DOI  https://doi.org/10.1051/00046361/201730569  
Published online  27 September 2018 
Modeling and use of stellar oscillation visibilities
MaxPlanckInstitut für Sonnensystemforschung, JustusvonLiebigWeg 3, 37077
Göttingen, Germany
email: schou@mps.mpg.de
Received:
6
February
2017
Accepted:
28
May
2018
Context. Recently our ability to study stars using asteroseismic techniques has increased dramatically, largely through the use of space based photometric observations. Work has also been performed using ground based spectroscopic observations and more is expected in the near future from the SONG network. Unfortunately, the intensity observations have an inferior signaltonoise ratio and details of the observations do not agree with theory, while the data analysis used in the spectroscopic method has often been based on overly simple models of the spectra.
Aims. The aim is to improve the reliability of measurements of the parameters of stellar oscillations using spectroscopic observations and to enable the optimal use of the observations.
Methods. While previous investigations have used 1D models, I argue that realistic magnetohydrodynamic simulations, combined with radiative transfer calculations, should be used to model the effects of the oscillations on the spectra. I then demonstrate how to calculate the visibility of the oscillation modes for a variety of stellar parameters and fitting methods. In addition to the methods used in previous investigations, I introduce a singular value decomposition based technique. This new technique enables the determination of the information content available from spectral perturbations and allows this content to be expressed most compactly. Finally I describe how the time series obtained may be analyzed.
Results. It is shown that it is important to model the visibilities carefully and that the results deviate substantially from previous models, especially in the presence of rotation. Detailed spectral modeling may be exploited to measure the properties of a larger number of modes than possible via the commonly used crosscorrelation method. With moderate rotation, there is as much information in the line shape changes as in the Doppler shift and an outline of how to extract this is given.
Key words: asteroseismology / stars: oscillations / techniques: spectroscopic / line: profiles
© ESO 2018
1. Introduction
Most asteroseismic results have so far been obtained from photometric observations using a variety of spaceborne instruments, such as WIRE (Fletcher et al. 2006), MOST (Walker et al. 2003), CoRoT (Auvergne et al. 2009), and Kepler (Borucki et al. 2010). This will likely also be the case in the future with the launch of TESS (Ricker et al. 2014) and PLATO (Rauer et al. 2014). The main advantage of photometric observations is that it is possible to observe multiple stars simultaneously, as evidenced by the large number of main sequence stars for which results have been obtained (Stello et al. 2013; Chaplin et al. 2014; Lund et al. 2017a,b). However, Doppler velocity based observations have a superior signaltonoise ratio. Unfortunately, it is difficult to observe more than one star at a time with a spectrograph based instrument and it is difficult to obtain the required observing time, which is typically weeks to months at a high cadence and high duty cycle on a large telescope; therefore only a few stars have been observed this way, as reviewed by Bedding (2014). With the recent commissioning of the first SONG telescope (Grundahl et al. 2009, 2017) and the planned expansion of the SONG network, more stars will be observed in the future. Given this very limited resource and that the velocity observations are significantly different from photometric observations, it is essential that the maximum information is extracted from the observed stellar spectra and that the resulting power spectra are accurately modeled.
When extracting the oscillation signal from the observed spectra, Doppler shift algorithms developed for radial velocity planet searches (e.g., Bouchy et al. 2001) are often used and it is thus implicitly assumed that the oscillation signal is well represented by a Doppler shift. For fitting power spectra it is generally assumed that mode visibilities, as a function of the azimuthal order m, follow the description of Gizon & Solanki (2003), where it was assumed that the sensitivity only depends on the centertolimb distance on the stellar disk. Below I will show that, in the presence of modest stellar rotation, the Doppler shift approach discards a significant amount of information and that the use of the visibility expression of Gizon & Solanki (2003) can lead to significant systematic errors. The dependence of the visibilities on the spherical harmonic degree l is typically kept free or prescribed to follow a relationship based on simplified models, even though it is known that the observed visibilities for the Sun do not agree with the theoretically expected values for broadband photometry (Lund et al. 2014).
A few results, similar to those presented in the present paper, but using a different set of simulations were shown in Schou (2014). The present paper expands substantially on this by considering stars of different spectral types, the effects of magnetic fields, and a variety of analysis methods.
Models of the effects of oscillations on spectra and how the information can be extracted have been studied in the past; see for example Brown et al. (1998), Briquet & Aerts (2003), and particularly Zima (2006) in which several physical effects were included. However, these models have used simplified line models, rather than the results of 3D magnetohydrodynamic (MHD) models, such as those used in the present work and the effects of magnetic fields on the spectra were not considered. The use of a singular value decomposition (SVD) based analysis was also not discussed in those studies. Rather, Briquet & Aerts (2003), for example, used a moments based method, which does not result in as compact a representation as the SVD based method.
In Sect. 2, I start by discussing details of the models, the radiative transfer, and how the spectral perturbations can be calculated. In Sect. 3, I consider a variety of analysis methods, starting with the classic crosscorrelation. As that is shown to be suboptimal, I also discuss the option of performing leastsquares fits and describe an SVD based method. As these methods result in multiple time series, I finish Sect. 3 by outlining how multiple time series can be analyzed. Finally I discuss some of the issues still to be addressed and conclude.
Issues of how the methods may be applied to a given spectrograph, how they may be made more numerically efficient, and the analysis of simulated or real time series are deferred for later consideration.
2. Background
Before addressing the fitting of the spectra I will discuss, in the following subsections, the MHD models used, the radiative transfer performed, and how those are used to derive the perturbations to the spectra.
2.1. Convection models and radiative transfer
The convection models used in this work are snapshots from the simulations of Beeck et al. (2013) with surface properties corresponding to main sequence stellar models of types F3, G2, K0, K5, M0, and M2 and with sizes ranging from 30 Mm × 30 Mm × 9 Mm for the F3 model to 1.56 Mm × 1.56 Mm × 0.8 Mm for the M2 model. For each spectral type, models with injected magnetic fields of 0 G, 20 G, 100 G, and 500 G were made. Beeck et al. (2013) provide further details of the various simulations. For the radiative transfer, SPINOR (Frutiger et al. 2000) was used to synthesize various lines for a selection of the models discussed above.
The main line studied is FeI at 6173 Å, which is used by the HMI instrument (Schou et al. 2012) and has the advantage that it has simple atomic properties, a large Landé Factor, is relatively free of blends and that some of the results can be verified by observations. For selected models the FeI line at 5250 Å and the SiI line at 10 827 Å were also used. In addition to these real lines, the 6173 Å line was also modeled, assuming abundances of 0.1 and 10 times solar, to simulate weaker and stronger lines at otherwise fixed atomic physics. Finally a line synthesis (“500 H”) is performed for the 500 G case with the magnetic field artificially set to zero. This makes it possible to disentangle the effects of the field on the MHD simulations and on the final radiative transfer calculation.
The line profiles are synthesized for a number of viewing angles at a spectral resolution of 7.5 mÅ with 201 points covering ±0.75 Å (except for the SiI 10 827 Å line, where the spacing is 30 mÅ covering ±3 Å in order to accommodate the wider line) and the resulting profiles are averaged horizontally.
Figure 1 shows the profiles for the G2 star at 0 G. The limb darkening is clearly visible as a decrease of the continuum with viewing angle, as is the broadening of the line toward the limb. The line also becomes shallower and shifts to the red toward the limb because of convective blueshift. Of these quantities the limb darkening is the easiest to verify observationally and Fig. 2 shows a comparison between the observed limb darkening from HMI and that from various calculations. In general the correspondence is good, but there are also differences, especially very close to the limb where the point spread function (PSF) of HMI has not been taken into account. More importantly, the calculated limb darkening appears to be too steep, even far from the limb. Interestingly, the results of Pereira et al. (2013) are significantly closer to the observed results. These authors concluded that the key improvement in their calculations is that the radiative transfer within their MHD simulation was performed more accurately, resulting in structural changes near the surface. Such detailed radiative transfer is typically not performed as part of large MHD simulations due to computational cost, but was carried out by Pereira et al. (2013) to better model the centertolimb variations of various observed quantities. The radiative transfer used for the detailed line synthesis, given an MHD cube, is believed to be accurate for both their computations and those performed in the present study.
Fig. 1. Line profiles for the FeI 6173 Å line for the G2 star with 0 G. From top to bottom the viewing angles are 0°, 10°, … , 80°, 85°, and 87°. The profiles were normalized to the disk center continuum. The red line indicates the disk averaged line profile in the absence of rotation. 

Open with DEXTER 
Fig. 2. Continuum limb darkening near the FeI line at 6173 Å. Results are shown both as a function of the fractional solar radius r (on the top axis) and (on the bottom axis). Red: From the simulations shown in Fig. 1, including a number of additional angles. Black: An estimate from the HMI instrument. Green: An estimate from Pereira et al. (2013) courtesy of R. Trampedach. Vertical dotted lines indicate 1.0, 2.0, and 5.0 pixels from the limb. The results were not corrected for the PSF of the HMI instrument. 

Open with DEXTER 
In any case, the limb darkening is well modeled, giving confidence in the accuracy of the simulations and radiative transfer. For other stars Dravins et al. (2017), recently demonstrated that the accuracy of the line profile calculations may be checked by using spectroscopic observations during planetary transits.
2.2. Effects of oscillations on spectra
To calculate the effect of the oscillations on the observed spectra, it is necessary to integrate the oscillations over the stellar disk (⊙) as follows:(1)
where λ is the wavelength, t time, x and y are the coordinates relative to disk center (in units of the stellar radius), r = (x, y), μ^{2} = 1 − x^{2} − y^{2} = 1 − r^{2}, r is the fractional radius, I_{m} the model intensity, , V_{0} the background stellar LOS velocity (assumed in this work to be due to solid body rotation), V′ is the LOS velocity induced by the mode (assumed small), k = dλ/dV = λ/c, and c is the speed of light. For simplicity the dependencies of V_{0} and V′ on x and y and the fact that λ is in reality discretized are suppressed here and in the rest of this article. Similarly time variations of V_{0} have been ignored. An obvious source of such variations is the orbital motion of the Earth. This causes variations in V_{0}, which are far outside of the linear range and which have to be dealt with by shifting the spectra or fitting templates. It has been assumed that the only change to the spectrum, at a given spatial location, caused by the mode is that resulting from Doppler shift. In other words intensity, linewidth, and other thermodynamic changes are not taken into account.
To calculate the effect of a given mode, it is necessary to calculate the LOS velocity caused by it. Assuming that the modes have unit amplitude, are undistorted by asphericities (such as rotation or starspots), are undamped, and that only the radial component is significant, the induced velocity is given by(2)
where the factor μ accounts for the velocity projection factor, is a spherical harmonic, an associated Legendre function, x = sin ϕ cos θ, y = sin θ sin i − cos ϕ cos θ cos i, ϕ is longitude, θ is latitude, i is the inclination of the rotation axis, and ω_{lm} is the mode frequency. With the convention chosen and . Without loss of generality the coordinate system was chosen to have the stellar rotation axis aligned with the y axis.
Substituting Eq. (2) into Eq. (1),(3)
is obtained. It is important to note that and and that in the absence of EW asymmetries (e.g., rotation) the term vanishes.
While I have, for simplicity, assumed that the only background velocity is that from uniform rotation and that the modes are undistorted, the formalism can easily accommodate the more general case. For some details of how this can be carried out, see Zima (2006). Similarly it is straightforward to include thermodynamic changes, when known.
3. Fitting methods
In this section I describe the results of three methods for extracting information from the observed spectra: a simple crosscorrelation, a fit of the expected perturbations, and an SVD based analysis.
3.1. Crosscorrelation analysis
A simple and common method used to extract the Doppler shift is to crosscorrelate the reference spectrum with the observed spectrum, as described by, for example, Bouchy et al. (2001). In principle the wavelength dependence of the noise should be taken into account, but for simplicity I start by assuming a uniform noise and discuss the effect of the wavelength dependence of the noise in the next subsection.
As the oscillation velocities are small and do not cause a significant smearing of the line (relative to the zero oscillation case) the reference spectrum can be taken as I_{0}. Given that the perturbations are small, the crosscorrelation is equivalent to a fit of δI at each time, to the derivative of I_{0} with respect to λ, assuming a uniform error, using the following equation:(4)
where V_{fit} is the fitted velocity. Given Eq. (3), and since a unit amplitude oscillation was assumed, the visibilities, S , can be defined by fitting the perturbations to the derivative, that is,(5)
As discussed later, only is significant.
To illustrate how well these profiles match, Fig. 3 shows for various modes together with fits to . For the lowest degrees the fit of is very good but it starts to disagree more as the degree is increased. Still, the approximation used for Eq. (4) is perhaps adequate to justify using the crosscorrelation method for this case. The decrease of the visibility at higher l is also evident.
Fig. 3. Perturbations (black) for the 6173 Å line for the G2 star with 0 G, i = 0° and no rotation. The values of (l, m) are (0, 0) (solid), (1, 0) (dotted), (2, 0) (dashed), and (3, 0) (dashdotted). Also shown (in red) is the derivative scaled to best fit each perturbation. The shape (but not magnitude) of the perturbations do not depend on i and m in the absence of rotation. 

Open with DEXTER 
If the star is rotating and not observed from the pole (i = 0°) the results change substantially, as illustrated in Fig. 4. While is still moderately well fitted by is now nonzero and shows a very different profile, corresponding to a narrowing and widening of the line, which is not well fitted by the derivative. I return to this issue below.
Fig. 4. Similar to Fig. 3 this shows the perturbations (black) and (blue) for the G2 star with i = 90° and solid body rotation with an equatorial rotation velocity of 4 km s^{−1}. The values of (l, m) are (0, 0) (solid), (1, 1) (dotted), (2, 0) (dashed), and (2, 2) (dashdotted). Also shown (in red) is the derivative scaled to best fit each of the . The unperturbed line, and thus the derivative, is different from that in Fig. 3 because of rotational broadening. 

Open with DEXTER 
Examples of the visibilities are shown in Fig. 5 for a variety of spectral lines. As can be seen the differences are modest, especially in the visible, even if the abundances are changed substantially. The SiI line shows a slightly different behavior, likely because it is a much broader line and in the nearinfrared. As such it should be possible to model only selected lines and interpolate the results. For different stars (Fig. 6) there is a modest trend with stellar type, but the overall trend remains the same. Again it would appear that while the variations should not be neglected, it should be possible to interpolate between the spectral types, avoiding the need to run large simulations for each star.
Fig. 5. Visibilities for the m = 0 modes for the G2 star as a function of l and spectral line, for the 0 G case and an inclination angle of 0°. In addition to the regular lines, profiles were synthesized with larger and smaller abundances of Fe for the 6173 Å line (using the same simulations). For clarity the visibilities have, for each spectral line, been divided by the visibility of l = 0. The visibilities of the other m values are zero at i = 0°. 

Open with DEXTER 
Fig. 6. Similar to Fig. 5 for different stars. All cases are for the 6173 Å line without a magnetic field, no rotation, i = 0°, and m = 0, and the visibilities have been divided by that for m = l = 0. 

Open with DEXTER 
Adding a modest magnetic field also does not have a dramatic effect as shown in Fig. 7. For the, possibly unrealistic, 500 G case the change is more significant. It is interesting that the changes in the structure dominates over the radiative transfer, as can be seen by turning off the field in the 500 H case, which changes the result by much less than the introduction of the magnetic field in the MHD simulations. As such it appears that the presence of magnetic fields can probably be ignored unless the fields are very strong.
Fig. 7. Similar to Fig. 5 for the different field strength cases in Beeck et al. (2013). The “500 H” case used the “500 G” simulation but with the field set to zero in the radiative transfer calculations. All cases are for the G2 star using the 6173 Å line, no rotation, i = 0° and m = 0 and the visibilities have been divided by the one for m = l = 0. 

Open with DEXTER 
The inclination dependence of the visibilities shown in Fig. 8 is much more interesting. Without rotation the inclination dependence follows the prediction by (Gizon & Solanki 2003; not shown). But even for a modest rotation rate of 4 km s^{−1} (roughly twice solar) the deviations are dramatic. For an equatorial observation (i = 90°) the ratio of the visibility of the (l, m) = (3, 3) mode relative to that of the (3, 1) mode changes from −1.29 in the absence of rotation to −2.71.
Fig. 8. Visibilities of the l = 0 through l = 3 modes for the G2 star as a function of inclination angle and equatorial rotation velocity for the case with 0 G and using the 6173 Å line. For clarity the values have been divided by the visibility of the corresponding m = 0 mode at i = 0°. The corresponding values, which are not shown, go up to 0.02, but are generally less than 0.01. 

Open with DEXTER 
That the rotation has a significant effect on the visibilities is is not too surprising. As the rotation increases, the line emitted far from the central meridian moves far away from that at the center (and the average) and so the measurement ceases to be sensitive to the oscillations near the edges. This also explains why the changes become significant when the Doppler shift at the east and west limbs becomes comparable to the linewidth; the full width half maximum (FWHM) of the average 6173 Å line in the nonrotating case corresponds to about 5.3 km s^{−1}.
This issue is illustrated in Fig. 9, in which the sensitivity as a function of position on the stellar disk is shown for an edgeon (i = 90°) view. As the rotation rate increases the sensitivity becomes more and more concentrated toward the central meridian. Beyond about 4 km s^{−1} the sensitivity becomes negative at the east and west limbs as the shift becomes comparable to the linewidth. While barely visible it is also the case that the sensitivity is not exactly eastwest symmetric as a consequence of the combination of the rotation and convective blueshift.
Fig. 9. Sensitivity as a function of position on the disk for the 6173 Å line for the G2 star with 0 G and i = 90°. The rotation rates for panels a through d are 0 km s^{−1}, 2 km s^{−1}, 4 km s^{−1}, and 6 km s^{−1}. The maps are normalized to have the same integrated sensitivity for the four cases. Grayscale goes from −0.15 times the maximum sensitivity to the maximum. 

Open with DEXTER 
In solarlike stars the spacing between modes with different m (which is essentially equal to the rotation frequency) is often small or comparable to the linewidth (Bazot et al. 2007; Nielsen et al. 2014), resulting in the modes blending together. In this case, it is therefore necessary to rely on a model of the visibilities and any errors in that can lead to incorrect mode parameter estimates. This is illustrated in Fig. 10. In this figure, limit spectra calculated with the correct visibilities (those including the effects of rotation) were fitted assuming the incorrect visibilities (those not including the effects of rotation). As is shown, both the inclinations and splittings, that is, the spacing between adjacent m values, which is essentially equal to the rotation frequency for Sunlike stars, are misestimated; in some cases this results in values far from the input values. Also, the values determined from different values of l are inconsistent, which may or may not be noticeable. When the peaks corresponding to the different values of m are well separated, the error is obvious and would make it clear that there is a problem. If the correct visibilities are used, the parameters are, of course, correctly estimated. On the other hand the errors are suboptimal, as discussed in Sect. 3.3.
Fig. 10. Results of fitting power spectra constructed with sensitivities calculated including the effects of rotation, but using a model calculated assuming sensitivities ignoring the effects of rotation. Results are shown for the G2 star with no field, the 6173 Å line, and a rotation velocity of 6 km s^{−1}. The ratio of the FWHM of the modes to the rotation rate is set to 1.0. The symbols show the results of fitting the spectrum of one l at a time. The solid blue line shows the results of fitting the spectra of all l with 0 ≤ l ≤ 3 together. In all cases a global search was performed to ensure that the global minimum has been found. 

Open with DEXTER 
Taking into account the effects of rotation does not mean that it is necessary to fit for additional parameters. The visibilities are given by the rotation rate (and thus the splittings) and inclination, both of which are already fitted for. The only required change to a fitting code is thus to replace the use of the expressions in Gizon & Solanki (2003) by a parametrization of the visibilities (e.g., the results shown in Fig. 8), for example by interpolating the values.
3.2. Leastsquares fit
As mentioned in the previous subsection, the crosscorrelation analysis suffers from several problems. Among others, the effects of rotation can be substantial and the implicit assumption that the derivative of the line is a good approximation to the perturbation is thus poor. Also, it is assumed that the noise is independent of wavelength. These approximations can be addressed by performing a maximumlikelihood fit, which is considered in this subsection.
That the noise is independent of the wavelength is unlikely to be correct, as discussed in Bouchy et al. (2001). A better approximation is to assume that photon noise is the dominant noise term. Assuming that the number of photons is >> 1 and that the perturbation is small, the photon noise can be approximated by a normal distribution with a variance proportional to the signal. A fairly benign consequence of this is that an internal estimate of the noise on the derived velocity, assuming that the noise equals that in the continuum, is wrong relative to that using the photon noise estimate. In the case of the 6173 Å line by an lindependent factor around 1.2.
A more significant problem is that the estimate is statistically suboptimal, in other words that an estimate with a better signaltonoise ratio can be constructed. The optimal (maximumlikelihood) estimate can be obtained by performing an error weighted leastsquares fit, writing the observed spectrum as(7)
thereby obtaining a time series x_{c} of the cosine component and another x_{s} of the sine component.
The error weighted fit is equivalent to an unweighted fit in which both the data and model are divided by the error estimate, which is in this case given by the square root of the model. A downside of the leastsquares fitting is that a different function should ideally be fitted for each mode. This is discussed in the next subsection.
A comparison between the crosscorrelation estimates and the fits of only the cosine component (which is dominant at low rotational velocity) is shown in Fig. 11. In this figure, the signaltonoise ratio is shown, rather than the visibility. As the noise is independent of the mode in the crosscorrelation case, this is proportional to the absolute value of the visibility. For the polar (i = 0°) case, which is unaffected by rotation, the effect is modest. But for an equatorial (i = 90°) view the difference is significant, especially at higher degree. At l = 4 the improvement is roughly a factor of 1.6 and at l = 5 it is 2.2.
Fig. 11. Signal to noise for various cases. Solid is crosscorrelation is m = 0 for i = 0° and dashed the corresponding fits. The dotted line indicates the crosscorrelation for m = l, 4 km s^{−1} equatorial rotation and i = 90° while the dashdotted line indicates the corresponding fit. In all cases the absolute value of the signaltonoise ratio is shown divided by the corresponding l = 0 crosscorrelation value. 

Open with DEXTER 
Results of fitting for both the sine and cosine components are shown in Fig. 12. At modest rotation rates the visibility of the real part drops and the visibility of the imaginary part increases. At higher degrees the two visibilities become similar. In other words the broadening and narrowing of the line caused by the sin component becomes as significant as the shift of the line caused by the cos component, which among other things allows for separating prograde and retrograde modes. In general the ability to observe two separate time series opens up the possibility of deriving significantly more information about the modes, but requires a somewhat more complex analysis, as described in Sect. 3.4.
Fig. 12. Signal to noise for the real (cos) and imaginary (sin) components for m = l, i = 90° for various equatorial rotation velocities. The signaltonoise ratios were normalized to the l = 0 case without rotation. 

Open with DEXTER 
While the leastsquares fitting does provide significant advantages over the crosscorrelation approach, the SVD based approached, discussed in the next subsection, provides significant advantages, and so the practicalities of implementing the leastsquares fitting are not discussed further.
3.3. SVD analysis
The fact that the perturbations caused by different modes are different raises a number of questions. Is it necessary to fit a given spectrum multiple times with functions designed to fit each mode? Is it possible to separate more than the cos and sin components, like different l and m values? A way to address these questions is to perform an SVD (Principal Component) analysis, writing the perturbations as(8)
where the division by accounts for the variation of the photon noise, j encodes the mode ID, σ_{k} are the singular values, U the singular vectors in mode ID, and V are the singular vectors in wavelength. The mode ID could, for example, be j = (l, m, p), where p is c or s as defined in Eq. (3) at some fixed inclination and rotation rate. The properties of the SVD ensure that the U vectors are orthonormal, as are the V vectors. By convention, the singular values σ are ordered by descending value. Their squares give the amount of variance of the lefthand side of Eq. (8) that is captured by the corresponding term (having implicitly assumed that the inherent mode amplitudes are independent l and m, as expected for solarlike oscillations on a Sunlike star). An important property of the SVD is that the variance captured by the first N terms is the maximum possible. No other vectors, such as the moments used by Briquet & Aerts (2003), can capture more information using N terms.
The vectors V are fitted to the spectra using an unweighted leastsquares fit of(9)
for some suitable k_{max} (see discussion later in this subsection), resulting in several time series y_{k}. As the V vectors are orthonormal, the noise on each term is the same and the y_{k} are given by dot products(10)
in the case where the fits are performed over the same wavelengths as the SVD. It also follows that the σU are the corresponding visibilities of the various modes.
Figure 13 shows the singular vectors in wavelength for three different cases and as can be seen the vectors are very similar. As expected given the earlier results, the vectors look roughly like the first, second, and third derivatives of the spectral line with wavelength.
Fig. 13. Singular vectors in wavelength for three cases. Black: i = 90° with 4 km s^{−1} equatorial rotation rate. Red: All inclinations (i = 0°, 10°, … , 90°) combined with 4 km s^{−1} equatorial rotation rate. Green: All inclinations combined with all equatorial rotation rates (0 km s^{−1}, 1 km s^{−1}, … , 6 km s^{−1}). Solid, dotted, and dashed lines indicate the first, second, and third vectors, respectively. The signs of some of the vectors were inverted; they are arbitrary in an SVD. All cases are for the 6173 Å line at 0 G. 

Open with DEXTER 
On the other hand the singular values σ are somewhat different for the different cases. A way to quantify this is to ask how much of the variance (i.e., information in the spectra) is covered by the lowest few terms. For an equatorial view and a 4 km s^{−1} rotation rate the numbers are 66.3%, 94.7%, 98.7%, and 99.8%, for one through four terms. For a single (4 km s^{−1}) rotation rate, but different viewing angles, the corresponding numbers are 84.6%, 97.4%, 99.5%, and 99.9%. For the case with different angles and rotation rates the numbers are 89.3%, 97.7%, 99.5%, and 99.8%.
Given these results it appears that one only needs to fit two or three terms to the observed spectra to extract the vast majority of the available information. Exactly how many terms are needed to extract all the statistically significant information depends on the signaltonoise ratio, resolution, and spectral coverage. The similarity of the spectra also means that there is little need to know the inclination and rotation rate in order to fit the spectra, which greatly simplifies the fitting. The analysis of the multiple resulting time series is discussed in Sect. 3.4.
The singular vectors in mode ID (U) give the relative visibility of a given V to various modes, as shown in Fig. 14. Given that V_{1} is very close to the wavelength derivative it is not surprising that the corresponding U vector is dominated by the cos component. Similarly the second vector is dominated by the sin component and so forth.
Fig. 14. First four (from left to right) singular vectors in l, m, and p for the case shown in red in Fig. 13. Top row shows the cos component and the bottom row shows the sin component. Each block shows the mean over i of the absolute value of the singular vectors as a function of l (horizontal) and m (vertical) for 0 ≤ m ≤ l ≤ 10. The blocks have been individually normalized to have identical maximum values. 

Open with DEXTER 
To further illustrate this Fig. 15 shows σ_{2}U_{2,j} for the sin term as a function of σ_{1}U_{1,j} for the cos term. As can be seen the ratios of the two visibilities are different for different modes, indicating that it may be possible to partially identify the modes based on this ratio. Interestingly the ratio depends mostly on the rotation rate and (l, m) and less on the inclination.
Fig. 15. Visibility of the sin component for the second term in the SVD as a function of the visibility of the cos component for the first term for the case shown with black in Fig. 13. The modes with the largest visibilities are identified by their l, m values. The steepest dotted line roughly represents the largest ratio, the middle line represents half of that ratio, and the third line represents zero. 

Open with DEXTER 
The other two lines studied give similar results. The singular vectors in wavelength are different for the IR line, but the behavior of the singular vectors in ID and the singular values are similar. Considering the three lines simultaneously does not lead to a significant improvement in the ability to separate modes.
It is not practical to perform a bruteforce calculation of the perturbations for the entire spectrum. The radiative transfer calculations are extremely expensive given the size of the computation boxes and the number of lines present in a typical spectrum. On the other hand the majority of lines behave in a similar way and their properties vary slowly with atomic parameters, so it is only necessary to perform a detailed radiative transfer calculation for a subset. Also, the number of spatial points needed to sample the convection adequately can likely be reduced dramatically.
Whether it is possible to determine the singular vectors in wavelength empirically (e.g., by performing an SVD of a number of observed spectra) is unclear as there are many other sources of variations, such as spectrograph drift and differential extinction. Also, such an empirical determination does not directly identify the modes.
Another way to determine the vectors without having to perform the radiative transfer would be to use the method of Dravins et al. (2017), which has the advantage of automatically taking into account the spectrograph PSF, but the obvious disadvantage is that it only works directly for stars with large transiting planets.
Similarly, the fact that the SVD represents the most compact representation does not mean that this method has to be employed. Other parameterizations, such as moments (Briquet & Aerts 2003), can also be used, but it must be realized that more terms may be needed and/or that some information is lost.
It is possible that the addition of the thermodynamic perturbations caused by the modes or some of the other neglected effects increases the ability to discriminate between modes, but this will have to await 3D simulations capable of predicting these effects reliably.
Implementing the fits in practice will require a number of steps. Ideally this would start by obtaining an (M)HD model for the specific stellar type, synthesizing the spectrum as a function of viewing angle, convolving with the spectrograph PSF, integrating up the perturbations caused by each mode, performing the SVD, determining how many terms to retain, fitting the spectra using the relevant number of terms, and fitting the resulting timeseries, as described in the next subsection. Unfortunately, many of these steps have complications.
The simulation and spectral synthesis are extremely costly if carried out with brute force. However, as demonstrated the resulting visibilities only depend weakly on stellar type and most of the spectral lines of interest are expected to depend only slowly on the properties of the lines, making it possible to interpolate the results. Indeed, simply interpolating the results shown in this paper, possibly supplemented with a few extra stellar models and spectral lines may be adequate, given the limited signal to noise of the currently available spectra.
The effects of the spectrograph PSF have not been discussed here. If the PSF is well known it is straightforward to convolve by it after the line synthesis and to check how the results are affected. If the PSF is poorly known, more research will obviously be needed.
Integrating up the contributions for each mode and performing the SVD should similarly not present a problem. Once the signaltonoise ratio for the spectrograph is known, determining the number of terms to retain is also straightforward to estimate, although of course, adjacent values could be attempted to test the significance. The fitting of the individual spectra is a linear fit of nearly orthonormal vectors and should thus be stable and easy to implement.
3.4. Analysis of multiple simultaneous timeseries
In asteroseismology only a single time series has generally been available for a given star and analysis methods initially developed for Sun as a star observations have been used. For an introduction to the basics, see Anderson et al. (1990).
Clearly, these analysis methods will not be optimal for the multiple simultaneous time series generated using the methods described in Sects. 3.2 and 3.3. Using the leastsquares analysis described in Sect. 3.2, two time series (x_{c} and x_{s}) are obtained, while in Sect. 3.3 there can be several time series, depending on the signaltonoise ratio. Thus the question arises of how to go about the case where each mode appears in multiple series, but with different visibilities. This issue has been addressed extensively in helioseismology and details can be found in, for example, Schou (1992) and Larson & Schou (2015). I briefly outline the general idea and how it might be applied to the present case. I restrict my case to stochastically driven solarlike oscillations.
In the case of stochastically driven solarlike oscillations, the Fourier transform of a single mode of oscillation has real and imaginary parts with a mean of zero and a variance given by(11)
where V is the variance, v the frequency , v_{0} the mode frequency, P is proportional to the mode power, and w is the HWHM of the mode. Under certain assumptions, most importantly that the mode excitations are frequent and that there are no gaps in the time series, it may be shown that the values of the Fourier transforms are normally distributed and are independent across frequencies and real/imaginary.
When a mode is observed with one of the methods described above, the result is that the resulting Fourier transform are multiplied by complex constants C_{jk}, where j identifies the time series and k encodes the mode. The real part of the constant is the sensitivity to the cos(mϕ) component and the imaginary part the sensitivity to the sin(mϕ) component, as discussed earlier. For simplicity, and consistent with the rest of the paper, it is assumed that these constants are independent of frequency and thus the radial order n of the mode.
As it has been assumed that the amplitudes are small, it follows that the observed transforms are the sum over the transforms of the individual modes(12)
An important consequence of the fact that a given mode, in general, appears in more than one time series is that fitting their power spectra (as opposed to Fourier transforms) is suboptimal. Specifically, the fact that the phases are correlated between the Fourier transforms is ignored resulting in a loss of information when the power spectra are made from the Fourier transforms.
While it is possible to continue using complex numbers (e.g., through the use of crossspectra), it is perhaps simpler and more intuitive to rearrange the equations to be purely real. To this end the complex spectra are split into twice as many real spectra to give(13)
where j and k now both run over the real and imaginary parts of the observed and mode transforms.
As the are sums of normally distributed variables with zero mean, they are themselves normally distributed with zero mean and a covariance matrix with elements given by(14)
where the vector a containing the parameters describing the modes has been made explicit and where a noise term has been added. It is important to note that E depends on the parameter vector a through both C′ and V.
The probability density for such a multivariate normal distribution is given by(15)
where  indicates the determinant.
To obtain the maximumlikelihood estimate it is necessary to minimize the negative of the logarithm of the product of the probabilities, that is(16)
where the sum only needs to be made over positive frequencies, given the lack of independent information in the negative part of the transforms. It is important to note that, despite the superficial similarity, this is not a leastsquares fit. In a leastsquares fit, one fits for the mean with a known variance, here the mean is known (zero) and the fit is for the variance. This results in a nonlinear fit, but one that is straightforward to implement from a numerical point of view using standard numerical routines. Equivalent Bayesian estimates should be straightforward to calculate.
As for implementing such a fit in practice, several things need to be considered. First of all I have not explicitly stated the exact list of parameters in the parameter vector a used to describe the modes, as a large variety of parameterizations can and have been used, depending on the star and preferences of various investigators. Having said that, one would expect that parameterizations similar to those in current use (e.g., Nielsen et al. 2014) should work here, which some parameters added to deal with the noise covariance.
Similarly, I have not specified how the noise term could be parameterized, but likely the form of the covariance matrix can be determined from data away from the peaks, as done in helioseismology, given that it would be expected to depend slowly on frequency.
It may be noted that a brute force implementation of the above is actually somewhat inefficient. In particular many of the coefficients in C′ may be almost purely real or imaginary and the covariance matrix E has many identical entries and zeros. However, given that that there are only a few time series, the time saved for a maximumlikelihood estimate by a more efficient computation is unlikely to be worth the effort. For an MCMC calculation this may not be the case.
4. Discussion
The analysis described in this paper is, of course, incomplete and many effects have been neglected. For example the stars have been assumed to have no differential rotation in latitude, the distortion of the eigenfunctions by rotation has been neglected, the displacement has been assumed to be purely radial and independent of height, and it has been assumed that there are no thermodynamic perturbations accompanying the oscillations. For a discussion of some of these effects see Zima (2006). The assumptions of height independence and lack of thermodynamic perturbations are difficult to address numerically, as the signaltonoise ratio of the oscillations in the MHD simulations is very small because of their limited size and short simulation time. For the Sun there is a noticeable height dependent effect (Zhao et al. 2012) in the observations and Baldner & Schou (2012) have shown that the height dependence in the simulations is far from that predicted by simple theoretical models. The thermodynamic perturbations are difficult to address by the MHD models due to the signaltonoise limitations, but given the discrepant visibilities reported by Lund et al. (2014) in intensity and the complexity of the physics it should not be assumed that the simple analytical models often used give reliable results. However, for slowly rotating Sunlike stars the effects considered almost certainly dominate over those neglected, at least for spectroscopic observations.
For photometric observations the situation is different. The present method predicts essentially no perturbations and to obtain reliable estimates the details of the thermodynamic perturbations with height have to be understood in detail, as discussed above. It should also be mentioned that the issues discussed in this paper are also highly relevant for Doppler imaging and that the two areas have many similarities.
5. Conclusions
In summary it is clear that significant improvements can be made by careful modeling and analysis of the data and that while some of the changes are modest they should nonetheless be taken into account in the analysis of stellar spectra. Having said that, it is also clear that future work is needed in order to understand some of the remaining uncertainties and it would be useful to determine if the observed mode visibilities agree with those predicted in this work.
Acknowledgments
I would like to thank Benjamin Beeck, Regner Trampedach, Martin Bo Nielsen, and Björn Löptien for useful discussions and help with various calculations. The HMI data used are courtesy of NASA/SDO and the HMI science team.
References
 Anderson, E. R., Duvall, Jr., T. L., & Jefferies, S. M. 1990, ApJ, 364, 699 [NASA ADS] [CrossRef] [Google Scholar]
 Auvergne, M., Bodin, P., Boisnard, L., et al. 2009, A&A, 506, 411 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Baldner, C. S., & Schou, J. 2012, ApJ, 760, L1 [NASA ADS] [CrossRef] [Google Scholar]
 Bazot, M., Bouchy, F., Kjeldsen, H., et al. 2007, A&A, 470, 295 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Bedding, T. R. 2014, in Asteroseismology, eds. P. L. Pallé, & C. Esteban (Cambridge, UK: Cambridge University Press), 60 [Google Scholar]
 Beeck, B., Cameron, R. H., Reiners, A., & Schüssler, M. 2013, A&A, 558, A48 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Borucki, W. J., Koch, D., Basri, G., et al. 2010, Science, 327, 977 [NASA ADS] [CrossRef] [PubMed] [Google Scholar]
 Bouchy, F., Pepe, F., & Queloz, D. 2001, A&A, 374, 733 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Briquet, M., & Aerts, C. 2003, A&A, 398, 687 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Brown, T. M., Kotak, R., Horner, S. D., et al. 1998, ApJS, 117, 563 [NASA ADS] [CrossRef] [Google Scholar]
 Chaplin, W. J., Basu, S., Huber, D., et al. 2014, ApJS, 210, 1 [NASA ADS] [CrossRef] [Google Scholar]
 Dravins, D., Ludwig, H.G., Dahlén, E., & Pazira, H. 2017, A&A, 605, A91 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Fletcher, S. T., Chaplin, W. J., Elsworth, Y., Schou, J., & Buzasi, D. 2006, MNRAS, 371, 935 [NASA ADS] [CrossRef] [Google Scholar]
 Frutiger, C., Solanki, S. K., Fligge, M., & Bruls, J. H. M. J. 2000, A&A, 358, 1109 [NASA ADS] [Google Scholar]
 Gizon, L., & Solanki, S. K. 2003, ApJ, 589, 1009 [NASA ADS] [CrossRef] [Google Scholar]
 Grundahl, F., ChristensenDalsgaard, J., Arentoft, T., et al. 2009, Commun. Asteroseismol., 158, 345 [NASA ADS] [Google Scholar]
 Grundahl, F., Fredslund Andersen, M., ChristensenDalsgaard, J., et al. 2017, ApJ, 836, 142 [NASA ADS] [CrossRef] [Google Scholar]
 Larson, T. P., & Schou, J. 2015, Sol. Phys., 290, 3221 [NASA ADS] [CrossRef] [Google Scholar]
 Lund, M. N., Kjeldsen, H., ChristensenDalsgaard, J., Handberg, R., & Silva Aguirre, V. 2014, ApJ, 782, 2 [NASA ADS] [CrossRef] [Google Scholar]
 Lund, M. N., Silva Aguirre, V., Davies, G. R., et al. 2017a, ApJ, 835, 172 [NASA ADS] [CrossRef] [Google Scholar]
 Lund, M. N., Silva Aguirre, V., Davies, G. R., et al. 2017b, ApJ, 850, 110 [NASA ADS] [CrossRef] [Google Scholar]
 Nielsen, M. B., Gizon, L., Schunker, H., & Schou, J. 2014, A&A, 568, L12 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Pereira, T. M. D., Asplund, M., Collet, R., et al. 2013, A&A, 554, A118 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
 Rauer, H., Catala, C., Aerts, C., et al. 2014, Exp. Astron., 38, 249 [NASA ADS] [CrossRef] [Google Scholar]
 Ricker, G. R., Winn, J. N., Vanderspek, R., et al. 2014, in Space Telescopes and Instrumentation 2014: Optical, Infrared, and Millimeter Wave, Proc. SPIE, 9143, 914320 [CrossRef] [Google Scholar]
 Schou, J. 1992, PhD Thesis, Aarhus University, Aarhus, Denmark [Google Scholar]
 Schou, J. 2014, in Precision Asteroseismology, eds. J. A. Guzik, W. J. Chaplin, G. Handler, & A. Pigulski, IAU Symp., 301, 481 [NASA ADS] [Google Scholar]
 Schou, J., Scherrer, P. H., Bush, R. I., et al. 2012, Sol. Phys., 275, 229 [NASA ADS] [CrossRef] [Google Scholar]
 Stello, D., Huber, D., Bedding, T. R., et al. 2013, ApJ, 765, L41 [NASA ADS] [CrossRef] [Google Scholar]
 Walker, G., Matthews, J., Kuschnig, R., et al. 2003, PASP, 115, 1023 [NASA ADS] [CrossRef] [Google Scholar]
 Zhao, J., Nagashima, K., Bogart, R. S., Kosovichev, A. G., & Duvall, Jr., T. L. 2012, ApJ, 749, L5 [NASA ADS] [CrossRef] [Google Scholar]
 Zima, W. 2006, A&A, 455, 227 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
All Figures
Fig. 1. Line profiles for the FeI 6173 Å line for the G2 star with 0 G. From top to bottom the viewing angles are 0°, 10°, … , 80°, 85°, and 87°. The profiles were normalized to the disk center continuum. The red line indicates the disk averaged line profile in the absence of rotation. 

Open with DEXTER  
In the text 
Fig. 2. Continuum limb darkening near the FeI line at 6173 Å. Results are shown both as a function of the fractional solar radius r (on the top axis) and (on the bottom axis). Red: From the simulations shown in Fig. 1, including a number of additional angles. Black: An estimate from the HMI instrument. Green: An estimate from Pereira et al. (2013) courtesy of R. Trampedach. Vertical dotted lines indicate 1.0, 2.0, and 5.0 pixels from the limb. The results were not corrected for the PSF of the HMI instrument. 

Open with DEXTER  
In the text 
Fig. 3. Perturbations (black) for the 6173 Å line for the G2 star with 0 G, i = 0° and no rotation. The values of (l, m) are (0, 0) (solid), (1, 0) (dotted), (2, 0) (dashed), and (3, 0) (dashdotted). Also shown (in red) is the derivative scaled to best fit each perturbation. The shape (but not magnitude) of the perturbations do not depend on i and m in the absence of rotation. 

Open with DEXTER  
In the text 
Fig. 4. Similar to Fig. 3 this shows the perturbations (black) and (blue) for the G2 star with i = 90° and solid body rotation with an equatorial rotation velocity of 4 km s^{−1}. The values of (l, m) are (0, 0) (solid), (1, 1) (dotted), (2, 0) (dashed), and (2, 2) (dashdotted). Also shown (in red) is the derivative scaled to best fit each of the . The unperturbed line, and thus the derivative, is different from that in Fig. 3 because of rotational broadening. 

Open with DEXTER  
In the text 
Fig. 5. Visibilities for the m = 0 modes for the G2 star as a function of l and spectral line, for the 0 G case and an inclination angle of 0°. In addition to the regular lines, profiles were synthesized with larger and smaller abundances of Fe for the 6173 Å line (using the same simulations). For clarity the visibilities have, for each spectral line, been divided by the visibility of l = 0. The visibilities of the other m values are zero at i = 0°. 

Open with DEXTER  
In the text 
Fig. 6. Similar to Fig. 5 for different stars. All cases are for the 6173 Å line without a magnetic field, no rotation, i = 0°, and m = 0, and the visibilities have been divided by that for m = l = 0. 

Open with DEXTER  
In the text 
Fig. 7. Similar to Fig. 5 for the different field strength cases in Beeck et al. (2013). The “500 H” case used the “500 G” simulation but with the field set to zero in the radiative transfer calculations. All cases are for the G2 star using the 6173 Å line, no rotation, i = 0° and m = 0 and the visibilities have been divided by the one for m = l = 0. 

Open with DEXTER  
In the text 
Fig. 8. Visibilities of the l = 0 through l = 3 modes for the G2 star as a function of inclination angle and equatorial rotation velocity for the case with 0 G and using the 6173 Å line. For clarity the values have been divided by the visibility of the corresponding m = 0 mode at i = 0°. The corresponding values, which are not shown, go up to 0.02, but are generally less than 0.01. 

Open with DEXTER  
In the text 
Fig. 9. Sensitivity as a function of position on the disk for the 6173 Å line for the G2 star with 0 G and i = 90°. The rotation rates for panels a through d are 0 km s^{−1}, 2 km s^{−1}, 4 km s^{−1}, and 6 km s^{−1}. The maps are normalized to have the same integrated sensitivity for the four cases. Grayscale goes from −0.15 times the maximum sensitivity to the maximum. 

Open with DEXTER  
In the text 
Fig. 10. Results of fitting power spectra constructed with sensitivities calculated including the effects of rotation, but using a model calculated assuming sensitivities ignoring the effects of rotation. Results are shown for the G2 star with no field, the 6173 Å line, and a rotation velocity of 6 km s^{−1}. The ratio of the FWHM of the modes to the rotation rate is set to 1.0. The symbols show the results of fitting the spectrum of one l at a time. The solid blue line shows the results of fitting the spectra of all l with 0 ≤ l ≤ 3 together. In all cases a global search was performed to ensure that the global minimum has been found. 

Open with DEXTER  
In the text 
Fig. 11. Signal to noise for various cases. Solid is crosscorrelation is m = 0 for i = 0° and dashed the corresponding fits. The dotted line indicates the crosscorrelation for m = l, 4 km s^{−1} equatorial rotation and i = 90° while the dashdotted line indicates the corresponding fit. In all cases the absolute value of the signaltonoise ratio is shown divided by the corresponding l = 0 crosscorrelation value. 

Open with DEXTER  
In the text 
Fig. 12. Signal to noise for the real (cos) and imaginary (sin) components for m = l, i = 90° for various equatorial rotation velocities. The signaltonoise ratios were normalized to the l = 0 case without rotation. 

Open with DEXTER  
In the text 
Fig. 13. Singular vectors in wavelength for three cases. Black: i = 90° with 4 km s^{−1} equatorial rotation rate. Red: All inclinations (i = 0°, 10°, … , 90°) combined with 4 km s^{−1} equatorial rotation rate. Green: All inclinations combined with all equatorial rotation rates (0 km s^{−1}, 1 km s^{−1}, … , 6 km s^{−1}). Solid, dotted, and dashed lines indicate the first, second, and third vectors, respectively. The signs of some of the vectors were inverted; they are arbitrary in an SVD. All cases are for the 6173 Å line at 0 G. 

Open with DEXTER  
In the text 
Fig. 14. First four (from left to right) singular vectors in l, m, and p for the case shown in red in Fig. 13. Top row shows the cos component and the bottom row shows the sin component. Each block shows the mean over i of the absolute value of the singular vectors as a function of l (horizontal) and m (vertical) for 0 ≤ m ≤ l ≤ 10. The blocks have been individually normalized to have identical maximum values. 

Open with DEXTER  
In the text 
Fig. 15. Visibility of the sin component for the second term in the SVD as a function of the visibility of the cos component for the first term for the case shown with black in Fig. 13. The modes with the largest visibilities are identified by their l, m values. The steepest dotted line roughly represents the largest ratio, the middle line represents half of that ratio, and the third line represents zero. 

Open with DEXTER  
In the text 
Current usage metrics show cumulative count of Article Views (fulltext article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 4896 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.