A&A 464, 1059-1067 (2007)
DOI: 10.1051/0004-6361:20066369
S. Leccia1 - H. Kjeldsen2 - A. Bonanno3 - R. U. Claudi4 - R. Ventura3 - L. Paternò5
1 - INAF - Astronomical Observatory of Capodimonte, Salita Moiariello 16, 80131 Napoli, Italy
2 -
Department of Physics and Astronomy, University of Aarhus, Ny Munkegade, Building 1520, 8000 Aarhus C, Denmark
3 -
INAF - Astrophysical Observatory of Catania, via S. Sofia 78, 95123 Catania, Italy
4 -
INAF - Astronomical Observatory of Padua, Vicolo Osservatorio 5, 35122 Padova, Italy
5 -
Department of Physics and Astronomy, Astrophysics Section, University of Catania, via S. Sofia 78, 95123 Catania, Italy
Received 8 September 2006 / Accepted 7 December 2006
Abstract
The F5 IV-V star Procyon A (
)
was observed in January 2001 by means of the high-resolution spectrograph SARG operating with the TNG
Italian telescope (Telescopio Nazionale Galileo) in the Canary Islands, exploiting the iodine cell technique. The time series of about 950 spectra carried out during 6 observation nights and a preliminary data analysis (Claudi et al. 2005) showed a significant power excess between 0.5 and
,
with
peak amplitude. Here we present a more detailed analysis of the time series, based on both radial velocity and line equivalent width analyses. From the power spectrum we found a typical p-mode frequency comb-like structure, identified 11 frequencies with a good margin of certainty in the interval
of modes with l=0,1,2 and
,
and determined large and small frequency separations,
and
,
respectively. The mean amplitude per mode (l=0,1) at peak power is
,
twice larger than the solar one, and the mode lifetime is
,
which indicates a non-coherent, stochastic source of mode excitation. Line equivalent width measurements do not show a significant excess in power in the examined spectral region but allowed us to infer an upper limit to the granulation noise.
Key words: stars: oscillations - stars: individual: Procyon A - techniques: spectroscopic - techniques: radial velocities
Owing to its proximity and brightness, Procyon has already
attracted the attention of stellar seismologists (Barban et al. 1999; Guenther & Demarque 1993; Brown et al. 1991; Eggenberger et al. 2004; Chaboyer et al. 1999; Martic et al. 1999,2004), causing an intense debate among scientists. The power excess in the range
found by Bouchy et al. (2004), Martic et al. (2004),
Eggenberger et al. (2004), and Claudi et al. (2005, hereinafter referred to as Paper I) seems to have a stellar origin and is consistent with a p-mode comb-like pattern.
However, data from the Canadian MOST satellite (Matthews et al. 2004) show no significant power excess in the same spectral region. In this regard, Bedding et al. (2005) suggest that the most likely explanation for the null detection could be a dominating non-stellar noise source in the MOST data, although Régulo & Roca Cortés (2005) make a claim for the presence of a signal in these data.
In Paper I we presented high precision radial velocity (RV) measurements
carried out during 6 observation nights
by means of the high resolution spectrograph SARG operating with the TNG
Italian telescope (Telescopio Nazionale Galileo) in the Canary Islands. The data showed a power excess
between
with a large separation of about
,
in agreement with previous measurements by Mosser et al. (1998), Barban et al. (1999), Martic et al. (2004,1999), and Eggenberger et al. (2004), who found values in the range
.
Here we deal with an improvement in the preliminary analysis presented in Paper I concerning an accurate time-series analysis of both radial velocities and line equivalent width (EW) measurements, from which mode frequencies, amplitudes, and lifetimes are determined and constraints on stellar granulation noise are deduced.
RV have already been determined by means of the AUSTRAL code (Endl et al. 2000) which
models instrumental profile, stellar, and iodine-cell spectra in order
to measure Doppler shifts (see also Paper I). This code also provides an estimate of the uncertainty in the
velocity measurements, .
These values were derived from the scatter of velocities measured from many (
)
small (
Å) segments of the echelle spectrum.
To perform a weighted Fourier analysis of the data, we first verified that these
values reflected the noise
properties of the velocity measurements, following the Butler et al. (2004) approach.
The high-frequency noise in the power spectrum (PS), well beyond the stellar
signal, reflects the properties of the noise in the data;
since we do expect the oscillation signal the dominant cause of variations in the velocity time series, we need to remove it before analyzing the noise. We do that iteratively by finding the highest peak in the PS of the velocity time-series and subtracting the corresponding sinusoid from the time-series.
This procedure is carried out
for the strongest peaks in the oscillation spectrum in the frequency range
,
until the spectral leakage into high frequencies from the remaning power is
negligible. Thus we have a time series of residual velocities, ri, that
reflects the noise properties of the measurements. We then analyze the ratio
,
which is expected to be Gaussian-distributed, so that the outliers correspond to the suspected data points.
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Figure 1:
Upper panel: cumulative histograms of
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Figure 2:
The power spectrum of the weighted data. A power excess around ![]() ![]() |
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Figure 3:
The first-order spacing calculated over several frequency ranges, as determined from the comb-response analysis. The line shows the mean
value of
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Figure 4:
The cumulative comb-response obtained as the sum of the individual comb-responses for each central frequency ![]() ![]() |
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Figure 5: The echelle diagram as derived from the "standard'' extraction of frequencies. |
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Table 1:
Prominent peaks in the power spectrum of Procyon identified
as mode oscillation frequencies (in )
in terms of n and l.
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Figure 6: The echelle diagram as derived from the "modified'' extraction of frequencies. |
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Figure 7:
The mean power folded at the large-separation frequency as a function of frequency modulo of
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The amplitude of individual modes can be estimated from the power concentrated in the PS, on assuming that only l=0,1,2,3 modes are detected, owing to the full disc observations. It is then possible to estimate the amplitude per mode necessary for producing the observed power level. Following the procedure described in Kjeldsen et al. (2005), we found a mean amplitude of the p-mode peak power, for the modes with l=0,1 in the frequency interval
,
of
,
which is a value twice higher than the solar one and one in very good agreement with the amplitudes estimated by Brown et al. (1991). Our velocity amplitude can be transformed in intensity amplitude by using the Kjeldsen & Bedding (1995) method, and obtaining the value of
per mode (l=0,1) at
,
in good agreement with the WIRE (Bruntt et al. 2005) and upper-limit MOST (Matthews et al. 2004) measurements. The results are summarized in Fig. 8 where the velocity amplitude per mode is shown as a function of frequency, together with the intensity scale and the equispaced positions of l=0 modes, as derived from the relationship (1) into which the determined values of
and
were inserted.
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Figure 8:
Velocity amplitude per mode (l=0,1) as a function of frequency. The horizontal line at
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In order to perform the comparison with Eggenberger et al. (2004),
we applied the same least-square best fit
as applied to our frequency data to those of Eggenberger et al. (2004) and derived the
parameters of the asymptotic relationship which are:
,
.
In this procedure the value of
was taken fixed to the
value given by Eggenberger et al. (2004),
.
If one calculates the frequencies corresponding to the two
asymptotic solutions, the one in the present paper and the
one we obtained by fitting to the Eggenberger et al. (2004) data, we find that most of the
calculated frequencies, for l = 0, 1, agree within
.
We find that
l=0, n=9-24 modes from the Eggenberger et al. (2004) asymptotic relation
correspond to l=1, n=8-23 modes from the asymptotic relation in
the present study.
We also find that l=1, n=7-22 (Eggenberger et al. 2004) modes correspond to
l=0, n=7-22 modes identified by us.
We conclude that we and Eggenberger et al. (2004) are detecting signals
from the same underlying p-modes.
If we look at all the raw extracted frequencies given in Table 2
of Eggenberger et al. (2004), it appears striking that most of those
frequencies may be identified by using the asymptotic solution
deduced from the present study. In Table 2 we compare
the Eggenberger et al. (2004) raw frequencies with the asymptotic relation from
the present study (
,
,
).
Table 2:
Comparison between the Eggenberger et al. (2004) extracted raw frequencies
(in )
and the asymptotic relation from the present
study (
,
,
).
It is interesting to note that 8 out of 11 frequencies determined by us match,
within a few ,
those listed in the Table 2 of Eggenberger et al. (2004) well,
but with a different mode identification.
Therefore we detected signals from the same frequencies as Eggenberger et al. (2004), but
extracted the p-mode structure in a slightly different way, reaching two
different solutions, and therefore identifications, for the extracted frequencies.
If we use our solution,
,
,
,
to verify to what
extent it matches the Eggenberger et al. (2004) frequencies, we find that 16
frequencies match our solution, 5 need a shift of
,
4 need a shift
of
,
and only 2 do not match the solution. Otherwise, if we
use the Eggenberger et al. (2004) solution,
,
,
,
we find that 12
frequencies match this solution, 8 need a shift of
,
3
need a shift of
,
and 4 do not match the solution. This
means that the frequencies detected by Eggenberger et al. (2004) provide a slightly
better fit to our solution than to their solution.
This statement is supported by the fact that, if we only look at those 12 frequencies that fit, without shift, the Eggenberger et al. (2004) asymptotic relationship and compare them to the Eggenberger et al. (2004) 16 raw frequencies that fit the solution found in the present study, we see that the scatter for the 16 frequencies is about 10% lower when we use our asymptotic relation. Moreover, Eggenberger et al. (2004) identify the 50% of those 12 frequencies that fit its relation as l=2 modes, while the l=1 modes should instead show the highest amplitude. However, since the two solutions provide basically the same frequencies, one should of course be cautious before claiming that one solution is far better than the other one.
The method we use in the present analysis is based on the frequency scatter per identified mode (Kjeldsen et al. 2005; Bedding et al. 2004), as calculated in Sect. 3.2. We ran 8400 individual simulations to determine the rms scatter of the detected frequencies as a function of the mode lifetime, by using the De Ridder et al. (2006) simulator and neglecting rotational splittings both because Procyon is a slow rotator and the majority of modes used are radial. The simulations contain the correct amplitude of modes, noise level, and number of detected modes out of the total number of modes contained in the p-mode spectrum, as determined from the asymptotic relationship (1) in the observed frequency interval. The fit represents a model that contains two components: the frequency spread, which is essentially the width of the Lorentzian profile, and the scatter of coherent oscillations, which corresponds to an infinite mode lifetime. The results are reported in Fig. 9 where the rms scatter of the 10 considered frequencies, out of the 11 identified (see Sect. 3.2), is plotted vs. mode lifetime. Since the mode frequency scatter determined in Sect. 3.2 turns out to be
,
it is easily seen from Fig. 9 that the corresponding lifetime is
.
The observed frequency scatter in Procyon is noticeably larger than is consistent with coherent oscillations, ruling out this possibility, and the related mode lifetimes appear to be slightly shorter than those observed in the Sun, where the oscillations are excited by the surface turbulent convection. The present data strongly indicate that oscillations in Procyon are not coherent, but damped and re-excited by a mechanism similar to what is operating in the Sun, as expected.
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Figure 9:
The rms scatter of the 10 identified frequencies as a function of mode lifetime obtained by several thousand simulations. The intersection of the horizontal line of the observed scatter with the solid curve obtained by simulations indicates that the mode lifetime is
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The results of the previous method for determining the mode lifetimes are corroborated by a different analysis we performed based on the amplitude of the highest peaks in the PS, with the idea that the amplitude of modes are also affected by their lifetimes, in the sense that, when the peak amplitude is smaller, the mode lifetime is shorter, while when it is larger the mode lifetime is longer. However, since there is not a simple relationship between amplitude and lifetime, we used a data simulation based on several thousand runs that allows a direct comparison between the observed properties of the time-series and the properties of the oscillation modes in order to establish a calibrated relationship between the peak height and the mode lifetime (De Ridder et al. 2006). Compared to the previous one, this method has the advantage of being independent of mode identification but the disadvantage of being less accurate.
The result is reported in Fig. 10, where we show the amplitude, with
error bars, of the 6
largest-amplitude detected modes with l=0,1,2 as a function of the mode lifetime.
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Figure 10:
The amplitude of the 6 largest amplitude detected modes, for l=0,1,2 as a function of the mode lifetime. The bars indicate the ![]() |
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The effects of frequency scatter and mode amplitude on mode lifetime is evident in Figs. 11 and 12, where simulations concerning
continuous observation campaigns are reported for mode lifetimes of
and
,
respectively. In these two figures the upper panel shows the complete PS, while the lower one an enlarged portion of it from
to
.
From our simulations it is clear that the frequencies of long-lived modes are much better defined, or less scattered, and have larger amplitudes than those of short-lived modes.
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Figure 11:
Simulated Procyon p-mode power spectrum obtained by using the De Ridder et al. (2006) simulator, not including noise and rotational splittings. The length of the time-series is ![]() ![]() |
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Figure 12:
The same simulation as in Fig. 11, but for a mode lifetime of ![]() |
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Table 3: Spectral line wavelengths used for EW measurements.
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Figure 13: Time series of EW measurements as derived from the combination of all the lines reported in Table 3. |
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Figure 14:
The weighted power spectrum
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To evaluate the power generated by the granulation of the star in the
PS of the EW's and to make a comparison with data obtained with different
methods we need to define a quantity independent of the temporal length of the data, which is obtained by computing the power density spectrum (PDS), a measure of the power per frequency resolution element that
is therefore independent of the length and sampling of the time-series:
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(4) |
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Figure 15:
Smoothed power density spectra (PDS) of Procyon granulation noise as obtained from SARG (dashed line, this project) and AAT/ESO EW 1999, squares, (Kjeldsen et al. 1999) spectroscopy, and MOST (Matthews et al. 2004) and WIRE (Bruntt et al. 2005) space photometry (continuous lines). The PDS derived from the PS of Fig. 14 is shown in the background. Power density is expressed in
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While our measurements are directly comparable with the spectroscopic ones of Kjeldsen et al. (1999), in order to compare them with the photometric ones, we need to pass from intensities I to temperatures T and from there to EW's. This is accomplished by using appropriate sensitivity indices; for intensity, we used
(Kjeldsen & Bedding 1995), and
for EW, as deduced from the analysis of Bedding et al. (1996) for Fe I lines at
.
The results are shown in Fig. 15, where MOST and WIRE PDF curves are plotted together with Kjeldsen et al. (1999) data and our curve.
It appears that, while WIRE and our distribution of power are mutually consistent, at least in the frequency interval
,
and corroborated by the few data of Kjeldsen et al. (1999), MOST shows a power density level higher by a factor of four or more. Uncertainties in sensitivity index calibration of I and EW with respect to T may lead to some discrepancies, but they are not enough large to explain such a significant disagreement between MOST and other data. In order to render the MOST data comparable with ours, it should be
and
.
This is unlikely because the value of
adopted here has been derived by observations of the same lines we use here at the same temperature of Procyon (Bedding et al. 1996) and a value of
disagrees with the models of Bedding et al. (1996). This seems to imply that MOST did not detect granulation noise, probably because of some instrumental or stellar spurious signal, as suggested by Bruntt et al. (2005).
In contrast to the first spectroscopic determinations of Kjeldsen et al. (1999) relative to a few points in the high frequency side of the granulation noise PDS, our EW determinations constitute the first spectroscopic measurements of Procyon granulation in the frequency range
,
so providing an independent measure of and establishing an upper limit to granulation noise power. The fact that at low frequencies, below
,
our power level is higher than the one shown by WIRE might be caused partially because we did not correct the WIRE data at low frequencies for the effect of high-pass filter and partially because of the possible effect of stellar activity in Procyon that affects spectral lines but not the continuum.
Table 4: Properties of the p-mode oscillations in Procyon.
We identified 11 individual p-mode frequencies with l=0,1,2 and
with a good margin of certainty in the frequency range
,
as reported in Table 1,
which are largely consistent with those found by Eggenberger et al. (2004).
The large frequency separation deduced from the fit of 10, out of the 11 identified frequencies, to the asymptotic relationship (1) is consistent with the results from the comb response analysis, both individual and cumulative, and its value agrees fairly well with
determined by Eggenberger et al. (2004); but it shows some discrepancy with what was determined by Martic et al. (2004),
,
although in a previous article (Martic et al. 1999) the authors found
,
as is evident from their Fig. 12.
The large frequency separation we have determined is consistent with an evolutionary model for Procyon, constructed with solar chemical abundance, elemental diffusion, and mass loss, having a mass of
,
an age of
,
a luminosity of
,
a radius of
,
and a surface convection zone that is
of the stellar radius (Bonanno et al. 2007).
This is in very good agreement with other
theoretical studies of Procyon A (Eggenberger et al. 2005; Barban et al. 1999; Chaboyer et al. 1999).
The small frequency separation we determined from one l=2 and
three l=1 modes is larger by
than what was determined by Martic et al. (2004),
,
and what we derived from Eggenberger et al. (2004) data,
,
but our value is not strongly constrained by our measurements, as only a few modes with
were identified.
The mean amplitude per mode, for modes with l=0,1, is about 0.45, twice larger than the solar one.
The mode lifetime was determined by means of two independent methods whose results are mutually consistent and give a lifetime of about .
This short lifetime rules out the possibility of a coherent, over-stable excitation of modes in Procyon, but it indicates that oscillations are excited stochastically by turbulent convection as in the case of the Sun.
We used the red part of the observed spectrum and the measurement of the EW's to determine an upper limit to granulation noise-power that turned out to agree with previous spectroscopic (Kjeldsen et al. 1999) and space photometric (Bruntt et al. 2005) measurements, but significantly contrasting with MOST data (Matthews et al. 2004).
Our RV data are available upon request from the first author of the present article.
Acknowledgements
This work was partially supported by the Italian Ministry of University and Scientific Research, under the contract PRIN 2004024993.