A&A 463, 297-308 (2007)
DOI: 10.1051/0004-6361:20041953
R. Samadi1,2 - D. Georgobiani3 - R. Trampedach4 - M. J. Goupil2 - R. F. Stein5 - Å. Nordlund6
1 - Observatório Astronómico UC, Coimbra, Portugal
2 - Observatoire de Paris, LESIA, CNRS UMR 8109, 92195 Meudon, France
3 - Center for Turbulence Research, Stanford University NASA Ames Research Center, Moffett Field, USA
4 - Research School of Astronomy and Astrophysics, Mt. Stromlo Observatory, Cotter Road, Weston ACT 2611, Australia
5 - Department of Physics and Astronomy, Michigan State University, Lansing, USA
6 - Niels Bohr Institute for Astronomy Physics and Geophysics, Copenhagen, Denmark
Received 6 September 2006 / Accepted 14 November 2006
Abstract
Aims. We extend semi-analytical computations of excitation rates for solar oscillation modes to those of other solar-like oscillating stars to compare them with recent observations
Methods. Numerical 3D simulations of surface convective zones of several solar-type oscillating stars are used to characterize the turbulent spectra as well as to constrain the convective velocities and turbulent entropy fluctuations in the uppermost part of the convective zone of such stars. These constraints, coupled with a theoretical model for stochastic excitation, provide the rate
at which energy is injected into the p-modes by turbulent convection. These energy rates are compared with those derived directly from the 3D simulations.
Results. The excitation rates obtained from the 3D simulations are systematically lower than those computed from the semi-analytical excitation model.
Key words: convection - turbulence - Sun: oscillations - Hertzsprung-Russell (HR) and C-M - stars: variables: general - methods: numerical
Stars with masses
have upper convective zones where stochastic excitation of p-modes by turbulent convection takes place as in the case of the Sun. As such, these stars are often referred to as solar-like oscillating stars. One of the major goals of the future space seismology mission CoRoT (Baglin & The Corot Team 1998), is to measure the amplitudes and the line-widths of these stochastically driven modes. From the measurements of the
mode line-widths and amplitudes, it is possible to infer the rates at
which acoustic modes are excited (see e.g. Baudin et al. 2005).
Such measurements will then provide valuable constraints on the theory of stellar oscillation excitation and damping. In turn, improved models of excitation and damping will provide valuable information about convection in the outer layers of solar-like stars.
The mechanism of stochastic excitation has been modeled by several authors
(e.g. Osaki 1990; Samadi & Goupil 2001; Balmforth 1992; Goldreich et al. 1994; Goldreich & Keeley 1977, for a review see Stein et al. 2004).
These models yield the energy rate,
,
at which p-modes are excited by turbulent convection but require an accurate knowledge of the time averaged and
- above all - the dynamic properties of turbulent convection.
All the related physical processes are complex and difficult to model. The present excitation model therefore uses a number of approximations such as the assumption of incompressibility, and the scale length separation between the modes and the turbulent eddies exciting the modes. It has been shown that the current excitation model is valid in the case of the Sun (Paper III), but its validity in a broader region of the HR-diagram has not been confirmed until now.
Testing the validity of the theoretical model of stochastic excitation with the help of 3D simulations of the outer layers of stellar models is the main goal of the present paper. For that purpose, we compare the p-mode excitation rates for stars with different temperatures and luminosities as obtained by direct calculations and by the semi-analytical method as outlined below.
Numerical 3D simulations enable one to compute directly the excitation rates of p-modes for stars with various temperatures and luminosities. For instance this was already undertaken for the Sun by Stein & Nordlund (2001) using the numerical approach introduced in Nordlund & Stein (2001). Such calculations will next be called "direct calculations''. They are time-consuming and do not easily allow massive computations of the excitation rates for stars with different temperatures and luminosities. On the other hand, an excitation model offers the advantage of testing separately several properties entering the excitation mechanism which are not well understood or modeled. Furthermore, once it is validated, it can be used for a large set of 1D models of stars.
As it was done for the Sun in Samadi et al. (2003c, hereafter Paper II) and Paper III, 3D simulations can also provide quantities which can be implemented in a formulation for the excitation rate
,
thus avoiding the use of the mixing-length approach with the related free parameters, and assumptions about the turbulent spectra. Such calculations will next be called "semi-analytical calculations''.
We stress however that in any case, we cannot avoid the use of 1D models for computing accurate eigen-frequencies for the whole observed frequency range. In the present paper, the 1D models are constructed to be as consistent as possible with their corresponding 3D simulations, as described in Sect. 3.
This paper is organized as follows: in Sect. 2 we present the methods considered here for computing
,
that is the so-called "direct'' method based on Nordlund & Stein's (2001) approach (Sect. 2.1) and the so-called "semi-analytical'' method based on the approach from Paper I, with modifications as presented in Papers II and III and in the present paper (Sect. 2.2).
Comparisons between direct and semi-analytical calculations of the excitation rates are performed in seven representative cases of solar-like oscillating stars. The seven 3D simulations all have the same number of mesh points. Section 3 describes these simulations and their associated 1D stellar models.
The 3D simulations provide constraints on quantities related to the convective fluctuations,
in particular the eddy time-correlation function,
,
which, as stressed above, plays an important role in the excitation of solar p-modes. The function
is therefore inferred from each simulation and compared with simple analytical function (Sect. 4).
Computations of the excitation rates of their associated p-modes are next undertaken in Sect. 5 using both the direct approach and the semi-analytical approach. In the semi-analytical method, we employ model parameters as derived from the 3D simulations in Sect. 4.
In Sect. 5.2 we derive the expected scaling laws for
,
the maximum in
,
as a function of L/M with both the direct and semi-analytical methods
and compare the results. This allows us to investigate the implications of such power laws for the expected values of
and to compare our results with the seismic observations of solar-like oscillations in Sect. 5.3. We also compare with previous
theoretical results (e.g. Kjeldsen & Bedding 1995; Houdek & Gough 2002).
We finally assess the validity of the present stochastic excitation model and discuss the importance of the choice of the model for
in Sect. 6.
![]() |
(2) |
In Eq. (1) the non-adiabatic Lagrangian pressure fluctuation,
,
is calculated as the following: we first compute the non-adiabatic pressure fluctuations
according to Eq. (A.3) in
Appendix A. We then perform the temporal Fourier transform of
at each depth r to get
.
The mode displacement eigenfunction
and the mode eigenfrequency
are
calculated as explained in Sect. 3. Its vertical derivative,
,
is normalized by the mode energy per unit surface area,
,
and then multiplied by
.
The result is integrated over the simulation depth, squared and divided by
.
We next multiply the result by the area of the simulation box (
)
to obtain
,
the total excitation rates in erg s-1 for the entire star. Indeed the nonadiabatic pressure fluctuations are uncorrelated on large scales, so that average
is inversely
proportional to the area. Multiplication by the area of the stellar simulation gives the excitation rates for the entire star as long as the domain size is sufficiently large to include
several granules.
Calculations of excitation rates by the semi-analytical method are based on a model of stochastic excitation. The excitation model we consider is the same as presented in Paper I. In this model of excitation and in contrast to previous models (e.g. Goldreich et al. 1994; Balmforth 1992; Goldreich & Keeley 1977), the driving by turbulent convection is ensured not only by the Reynolds stress tensor but also by the advection of the turbulent fluctuations of entropy by the turbulent movements (the so-called entropy source term).
As in Paper I, we consider only radial p-modes. We do not expect any significant differences for low
degree modes. Indeed, in the region where the excitation takes place, the low
degree modes have the same behavior as the radial modes. Only for very high
degree modes (
)
- which will not be seen in stars other than the Sun - can a significant effect be expected, as is quantitatively confirmed (work in progress).
The excitation rates are computed as in Paper II, except for the change
detailed below. The rate at which a given mode with frequency
is excited
is then calculated with the set of Eqs. (1)-(11) of Paper II.
These equations are based on the excitation model of Paper I, but assume that injection of acoustic energy into the modes is isotropic. However, Eq. (10) of Paper II must be corrected for an analytical error (see Samadi et al. 2005). This yields the following correct expression for Eq. (10) of Paper II:
The method then requires the knowledge of a number of input parameters which are of three different types:
The spatial and time averaged quantities (in 2) and 3) above) are obtained from the 3D simulations in the manner of Paper II. For E(k), however, we use the actual spectrum as calculated from
the 3D simulations and not an analytical fit as was done in Paper II. However as in Paper II, we assume for Es(k) the k-dependency of E(k) (we have checked this assumption for one simulation and found no significant change in
).
For each simulation, we determine
as in Paper III (cf. Sect. 4). Each
is then compared with various analytical forms, among which some were investigated in Paper III. Finally we select the analytical forms which are the closest to the behavior of
and use them, in Sect. 5, to compute
.
Table 1:
Characteristics of the convection 3D simulations:
is the duration of the
relaxed simulations used in the present analysis,
is the pressure scale height at the surface,
the size of the box in the horizontal direction,
the sound speed and
the sound travel time across
.
All the simulations
have a spatial grid of
.
Numerical simulations of surface convection for seven different solar-like stars were performed by Trampedach et al. (1999). These hydrodynamical simulations are characterized by the effective temperature,
and acceleration of gravity, g, as listed in Table 1. The solar simulation with
the same input physics and number of mesh points is included for comparison purposes. The surface gravity is an input parameter, while the effective temperature is adjusted by changing the
entropy of the inflowing gas at the bottom boundary. The simulations have
grid points. All of the models have solar-like chemical composition, with hydrogen abundance X=0.703 and metal abundance Z=0.0145. The simulation time-series all cover at least five periods of the primary p-modes (highest amplitude, one node at the bottom boundary),
and as such should be sufficiently long.
The convection simulations are shallow (only a few percent of the stellar radius) and therefore contain only few modes. To obtain mode eigenfunctions, the simulated domains are augmented by 1D envelope models in the interior by means of the stellar envelope code by Christensen-Dalsgaard & Frandsen (1983a). Convection in the envelope models is based on the mixing-length formalism (Böhm-Vitense 1958).
Trampedach et al. (2006a) fit 1D stellar envelopes to average stratifications of the seven convection simulations by matching temperature
and density at a common pressure point near the bottom of the simulations.
The fitting parameters are the mixing-length parameter,
,
and a
form-factor,
,
in the expression for turbulent pressure:
,
where
is the convective velocities predicted by the mixing-length formulation.
A consistent matching of the simulations and 1D envelopes is
achieved by using the same equation of state (EOS) by
Däppen et al. (1988, also referred to as the MHD EOS, with reference to Mihalas, Hummer, and Däppen)
and opacity distribution functions (ODF) by Kurucz (1992b,a), and also by using
T-
relations derived from the simulations (Trampedach et al. 2006b).
The average stratifications of the 3D simulations, augmented by the fitted 1D envelope models in the interior, were used as the basis for the eigenmode calculations using the adiabatic pulsation code by Christensen-Dalsgaard & Berthomieu (1991). These combinations of averaged 3D simulations and matched 1D envelope models will, from hereon, be referred to as the 1D models.
![]() |
Figure 1: Location of the convection simulations in the HR diagram. The symbol sizes vary proportionally to the stellar radii. Evolutionary tracks of stars, with masses as indicated, were calculated on the base of Christensen-Dalsgaard's stellar evolutionary code(Christensen-Dalsgaard 1982; Christensen-Dalsgaard & Frandsen 1983a). |
| Open with DEXTER | |
The positions of the models in the HR diagram are presented in Fig. 1 and their
global parameters are listed in Table 2. Five of the seven models correspond to actual stars, while Star A and Star B are merely sets of atmospheric parameters; their masses and luminosities are therefore assigned somewhat arbitrarily (the L/M-ratios, only depending on
and g, are of course not arbitrary).
Table 2: Fundamental parameters of the 1D-models associated with the 3D simulations of Table 1.
![]() |
Figure 2:
The filled dots represent |
| Open with DEXTER | |
For each simulation,
is computed over the whole wavenumber (k) range covered by the simulations and at different layers within the region where modes are excited.
We present the results at the layer where the excitation is maximum,
i.e., where u0 is maximum, and for two representative wavenumbers:
at which E(k) peaks and
,
where
is the first non-zero wavenumber of the simulations.
Indeed, the amount of acoustic energy going into a given mode is largest
at this layer and at the wavenumber
,
provided that the mode frequency satisfies:
.
Above
,
the efficiency of the excitation
decreases rapidly. Therefore low and intermediate frequency modes
(i.e.,
)
are predominantly excited
at
.
On the other hand, high frequency modes are
predominantly excited by small-scale fluctuations, i.e. at large k.
The exact choice of the representative large wavenumber is quite arbitrary;
however it cannot be too large because of the limited number of mesh points
and in any case, the excitation is negligible above
.
We thus chose the intermediate wavenumber
.
Figure 2 presents
as obtained from the 3D simulations of Procyon,
Cen B and the Sun, at the layer where u0 is maximum and for the wavenumber
.
Although defined as a function of
,
for convenience,
is plotted as a function of
throughout this paper.
Figure 3 displays
for
.
Results for the other simulations are not shown, as the results for Procyon,
Cen B and the Sun correspond to three representative cases.
![]() |
Figure 3:
Same as Fig. 2 for
|
| Open with DEXTER | |
In practice, it is not easy to implement directly in the excitation model the
-variation of
inferred from the 3D simulations. An alternative and convenient way to compute
is to use simple analytical functions for
which are chosen so as to best represent the 3D results. We then compare
computed with the 3D simulations with the following simple analytical forms: the Gaussian form
As shown in Figs. 2 and 3, the Lorentzian
does not reproduce the
-variation of
satisfactorily. This is particularly true for the solar case. This contrast with the results of Paper III where it was found that
reproduces nicely - at the wavenumber where E is maximum -
the
-variation of
inferred from the solar simulation investigated in Paper III.
These differences in the results for the solar case can be explained by the low spatial resolution of the present solar simulation compared with that of Paper III.
Indeed we have compared different solar simulations with different spatial resolution and
found that the
-variation of
converges to that of
as the spatial resolution increases (not shown here). This dependency of
with spatial resolution of the simulation is likely to hold for the non-solar simulations as well. This result then suggests that
is in fact best represented by the Lorentzian form,
.
As a consequence, realistic excitation rates evaluated directly for a
convection simulation should be based on simulations with higher spatial resolution.
However the main goal of the present work is to test the excitation model, which can be done with the present set of simulations. Indeed, we only need to use as inputs for the excitation model the quantities related to the turbulent convection (E(k),
,...) as they are in the simulations, no matter how the real properties of
are.
For the present set of simulations, we compare three analytical forms of
:
Lorentzian, Gaussian and exponential. For large k,
is overall best modeled by a Gaussian (see Fig. 3 for
). For small k (see Fig. 2 for
)
both the exponential and the Gaussian are closer to
than the Lorentzian.
For a given simulation, depending on the frequency, differences between
and the analytical forms are more or less pronounced.
The discrepancy between
inferred from the 3D simulations and the exponential or the Gaussian forms vary systematically with stellar parameters; decreasing as the convection
gets more forceful, as measured by, e.g., the turbulent- to total-pressure
ratio. Of the three simulations illustrated in Fig. 2, Procyon
has the largest and
Cen B has the smallest
-ratio.
As a whole for the different simulations and scale lengths k, we conclude that
the
-variation of
in the present set of simulations lies between
that of a Gaussian and an exponential. However, neither of them is completely satisfactory. Actually a recent detailed study by Georgobiani et al. (2006, in preparation) tends to show that
cannot systematically be represented at all wavenumbers by a simple form such as a Gaussian, an exponential or a Lorentzian, but rather needs a more generalized power law.
Hence, more sophisticated fits closer to the simulated
-variation of
could have been
considered, but for the sake of simplicity we chose to limit ourselves to the
three forms presented here.
For each simulation, the rates
at which the p-modes of the associated
1D models are excited are computed both directly from the 3D simulations
and with the semi-analytical method (see Sect. 2). In this section, the semi-analytical calculations are based on two analytical forms of
:
a Gaussian and an exponential form as described in Sect. 4. The Lorentzian form as introduced in Sect. 4 is not investigated in the present section. Indeed our purpose here is to test the model of stochastic excitation by using
constraints from the 3D simulations, and a Lorentzian behaviour is never obtained in the present
3D simulations.
![]() |
Figure 4:
Excitation rates, |
| Open with DEXTER | |
The results of the calculations of
using both methods are presented in Fig. 4 for the six most representative simulations. In order to remove the large scattering in the direct
calculations, we perform a running mean over five frequency bins. The results of this averaging are shown by dot-dashed lines. The choice of five frequency bins is somewhat arbitrary. However we notice that between 2 to 10 frequency bins, the maximum and the shape of the spectrum do not significantly change.
Comparisons between direct and semi-analytical calculations using either
or
all show systematic differences: the excitation rates obtained with the direct calculations are systematically lower than those resulting from the semi-analytical method.
These systematic differences are likely due to the too low spatial resolution of the
3D simulations which are used here (see Sect. 5.2 below).
At high frequency, the use of
instead of
results in larger
for all stars. This arises from the fact that
spreads slightly more energy at high frequency than
does (see Fig. 2).
The largest difference between the two types of calculation (direct
versus semi-analytical) is seen in the case of
Procyon. Indeed, the simulation of Procyon shows a pronounced
depression around
mHz. Such a depression is not seen in the semi-analytical calculations. The origin of this depression has not
been clearly identified yet but is perhaps related to some interference
between the turbulence and the acoustic waves
which manifests itself in the pressure fluctuations in the 3D work integral but is
not included in the semi-analytical description.
In order to assess the influence of the spatial resolution of the simulation on our results, we have at our disposal three other solar 3D simulations, with a grid of
,
and
(hereafter S1), and a duration of
42 min, 70 min and 100 min, respectively.
We have computed the p-modes excitation rates according to the direct method for those three simulations. For each of those simulations we have also computed the excitation rates according to the semi-analytical method assuming either a Lorentzian
or a Gaussian
.
![]() |
Figure 5:
Top: as in Fig. 4 for solar simulations only. The solid line corresponds to the semi-analytical calculations based on a Lorentzian |
| Open with DEXTER | |
As shown in Fig. 5 (top), the excitation rates computed according to the direct calculation increase as the spatial resolution of the 3D simulation increases. The excitation rates computed with the 3D simulations with the two highest spatial resolutions reach approximately the same mean amplitude level, indicating that this level of spatial resolution is sufficient for the direct calculations.
We note that as the spatial resolution increases, the semi-analytical calculations using a Lorentzian
decrease by a factor
2 (not shown here). The differences in
the semi-analytical calculations based on the
simulation and the
simulation are found very small, indicating that this level of spatial resolution is sufficient for the semi-analytical calculations too.
Finally, we note that the excitation rates obtained for the
solar simulation (S1) are approximatively two times smaller than excitation rates for the
solar simulation otherwise used throughout this work (S0 hereafter).
This difference is attributed to the fact that the two simulations do not correspond to the same realization. Indeed, as a test, we have extended the duration of the simulation S1 up to 500 min.
The full time series has then been divided into subsets of equal
duration of 100 min and p-mode excitation rates have been computed for each subset.
We find that the maximum in the p-modes excitation rates
oscillates from a subset to another about a mean value. The observed
variations are large: the maximum in
can be larger (smaller resp.) by
1.5 (0.5 resp.) times the maximum in the power spectrum obtained by averaging the power spectra of all subsets.
Hence we find that at low spatial resolution, different realizations yield
excitation rates that are scattered about a mean value at each frequency. This dispersion is
likely to be responsible for the factor of two difference between the excitation rate maxima
obtained for the two realizations S0 and S1. This type of dependency of
- with the starting time of the time series and its duration - is expected to be smaller for simulations with resolution higher than
,
because of the larger
number of excitation sources there. This will be studied in a subsequent work.
As seen in Sect 5.2 above,
the characteristics of the simulations influence the semi-analytical
calculations of the mode excitation rates (through the input parameters which
enter the semi-analytical calculations and which are taken
from the 3D simulation). We want to compare the results
of the semi-analytical calculations using
with the semi-analytical calculations using
.
It is
then necessary to insert the 3D inputs in these calculations coming
from simulations with the highest quality, here the highest
available resolution.
Figure 5 (bottom) compares semi-analytical calculations using a Lorentzian
with those using a Gaussian
.
All theses semi-analytical calculations are here based on
the energy spectrum of the simulation with the spatial resolution of
(see Sect. 5.2).
The average level of the excitation rates calculated according to the direct method and with the simulation with the highest spatial resolution is in between the semi-analytical calculations based on Lorentzian
and those based on a Gaussian
,
nevertheless they are in general slightly closer to the semi-analytical calculations based on Lorentzian
.
This result is discussed in Sect. 6.2.1.
Figure 6 shows
,
the maximum in
,
as a function of L/M for the direct and the semi-analytical calculations.
![]() |
Figure 6:
|
| Open with DEXTER | |
The same systematic differences between the direct and the semi-analytical calculations as seen in Fig. 4 are of course observed here. Note that the differences slightly decrease with increasing values of L/M.
We have also computed the excitation rate with the semi-analytical method using
.
The maximum excitation rate as evaluated with
is systematically larger than both the direct calculations and the semi-analytical results based on
or
.
In the solar case,
is found to be closer to the value derived from recent helioseismic data (Baudin et al. 2005) when using a Lorentzian compared to a Gaussian (see also Belkacem et al. 2006b, B06b hereafter). The "observed'' excitation rates are derived from the velocity observations V as follows:
Using the recent helioseismic measurements of V and
by Baudin et al. (2005) and the mode mass computed
here for our solar model at the height h=340 km (cf. Baudin et al. 2005), we find
erg s-1. This value must be compared with those found with
and
,
namely
erg s-1 and
erg s-1 respectively.
Scaling laws: All sets of calculations can be reasonably well fitted with a scaling law of the form
where s is a slope which
depends on the considered set of calculations. Values found for s are summarized in Table 3.
Table 3:
Values found for the slopes s (see Sect. 5.4) and sv (see Sect. 5.5). "Method'' is the method considered for the calculations of
.
For the semi-analytical calculations, we find s=2.6 using
,
s=3.0 using
and s=3.1 for the Gaussian form.
The Lorentzian form results in a power law with a smaller slope than the Gaussian. This can be understood as follows: a Gaussian decreases more rapidly with
than a Lorentzian.
As the ratio L/M of a main sequence star increases, the mode frequencies shift to lower values.
Hence p-modes of stars with large values of L/M receive relatively more acoustic energy
when adopting a Gaussian rather than a Lorentzian
.
It is worthwhile to note that even though the ratio L/M is the ratio of two global stellar quantities, it nevertheless characterizes essentially the stellar surface layers where the mode excitation is located since
.
For the set of direct calculations, some scatter exists
as a consequence of the large statistical fluctuations in
and
a linear regression gives s=3.4. As expected, this value is rather close to that found with the semi-analytical calculations using either
or
.
The theoretical oscillation velocity amplitudes V can be computed
according to Eq. (9) The calculation requires the knowledge of the excitation rates,
,
damping rates,
,
and mode mass,
.
Although it is possible - in principle - to compute the convective dampings from the 3D simulations (Nordlund & Stein 2001),
it is a difficult task which is under progress. However, using for instance Gough's Mixing-Length Theory (1976,1977, G'MLT hereafter), it is possible to compute
and
for different stellar models of given L,M and deduce
,
the maximum of the mode amplitudes, as a function of L/M at the cost of some inconsistencies.
In Samadi et al. (2001), calculations of the damping rates
based on G'MLT were performed
for stellar models with different values of L and M. Although these stellar models are not the same as those considered here, it is still possible, for a crude estimate, to determine the dependency of
with L/M.
Hence we proceed as follows: for each stellar model computed in Samadi et al. (2001), we derive the values of
and
at the frequency
at which the maximum amplitude is expected. From the stars for which solar-like oscillations have been detected, Bedding & Kjeldsen (2003) have shown that this frequency is proportional to the cut-off frequency. Hence we determine
where
is the cut-off frequency of a given model
and the symbol
refers to solar quantities (
mHz and
mHz). We then obtain (
)
as a function of L and M.
On the other hand, in Sect. 5.4, we have established
as a function of L and M. Then, according to Eq. (9), we can determine
for the different power laws of
.
We are interested here in the slope (i.e. variation with L/M) of
and
not its absolute magnitude, therefore we scale the theoretical and observed
with a same normalization value which is taken as the solar value
cm s-1 as determined recently by Baudin et al. (2005).
We find that
increases as
(L/M)sv with different values for svdepending on the assumptions for
.
The values of sv are summarized in Table 3 and illustrated in Fig. 7. We find
with
and
with
.
![]() |
Figure 7:
Same as Fig. 6 for
|
| Open with DEXTER | |
These scaling laws must be compared with
observations of a few stars for which solar-like oscillations have been detected in Doppler velocity. The observed
are taken from Table 1 of HG02, except for
Boo,
Her A,
Vir, HD 49933 and
Ara, for which we use the
quoted by Carrier et al. (2003), Martic et al. (2001), Martic et al. (2004), Mosser et al. (2005) and Bouchy et al. (2005) respectively and
Oph and
Ser quoted by Barban et al. (2004).
Figure 7 shows that the observations also indicate a monotonic logarithmic increase of
with L/M despite a large dispersion which may at least partly arise from different origins of the data sets. For the observations we find a "slope''
.
This is close to the theoretical slope obtained when adopting
and definitely lower than the slopes obtained when adopting
or adopted by HG02.
One goal of the present work has been to validate the model of stochastic excitation presented in Paper I. The result of this test is summarized in Sect. 6.1.
A second goal has been to study the properties of the turbulent eddy time-correlation,
,
and the importance for the calculation of the excitation rates,
,
of the adopted form of
.
Section 6.2 deals with this subject.
In order to check the validity of the excitation model, seven 3D simulations of stars, including the Sun, have been considered.
For each simulation, we calculated the p-mode excitation rates,
,
using two methods: the semi-analytical excitation model
(cf. Sect. 2.2) that we are testing,
and a direct calculation as detailed in
Sect. 2.
In the latter method, the work performed by the pressure fluctuations
on the p-modes is calculated directly from the 3D simulations.
In the semi-analytical method,
is computed according to the excitation model of Paper I. The calculation uses,
as input, information from the 3D simulations as for instance
the eddy time-correlation (
)
and the kinetic energy spectra (E(k)).
However although
has been computed for each simulation, in practice for simplifying the
problem of implementation as well as for comparison purpose with Paper III,
we chose to represent the
variation of
with simple analytical functions.
It is found that the
-variation of
in the present simulations lies
loosely between that of an exponential and a Gaussian. We then perform the validation test of the excitation model using those two forms of
.
We find that using either
or
in the semi-analytical calculations of
results in systematically higher excitation
rates than those obtained with direct 3D calculations. These systematic differences are attributed to the low spatial resolution of our present set of simulations. Indeed we have shown here that using solar simulations with different spatial resolutions, the resulting excitation rates increase
with increasing spatial resolution.
We have next investigated the dependence of
with L/M(See Fig. 6),
where L and M are the stellar luminosity and mass respectively.
As in previous works based on a purely theoretical approach (e.g. Samadi et al. 2003a),
we find that
scales approximatively as (L/M)s where s is
the slope of the scaling law: we find s=3.4 with the direct
calculations and s=3.2 and s=3.1 with the semi-analytical
calculations using
and
respectively. This indicates a general agreement between the
scaling properties of both types of calculations, which validates to some extent the adopted excitation model across the domain of the HR diagram studied here.
For the sake of simplicity, only simple analytical
forms for
have been investigated here.
We expect that the use of more sophisticated forms for
would reduce the dispersion between the analytical and direct calculations,
but would not affect the conclusions of the present paper.
The slope s of the scaling law for
,
is found to
depend significantly on the adopted analytical form for
.
The semi-analytical calculations using the Lorentzian form
for
results in a significantly smaller slope s than those based on the
Gaussian or the exponential or from direct calculations (see Table 3).
Except for the Sun, independent and accurate enough constraints on both the
mode damping rates and the mode excitation rates are not yet
available. We are then left to perform comparison between predicted and
observed mode amplitudes. Unfortunately, obtaining tight constraints
on
using comparison between predicted and observed mode amplitudes
is hampered by large uncertainties in the theoretical estimates of the damping rates.
It is therefore currently difficult to derive the excitation rates
for the few stars for which solar-like oscillations have been detected (see Samadi et al. 2004).
The future space mission COROT (Baglin & The Corot Team 1998) will provide high-quality data on seismic
observations. Indeed the COROT mission will be the first mission that will provide
both high precision mode amplitudes and line-widths for stars other than the Sun.
It will then be possible to use the observed damping rates and to
derive the excitation rate
free of the uncertainties associated with a theoretical computation of damping rates. In particular, it will be possible to determine
as a function of L and M from the observed stars. Such observations will provide valuable constraints for our models for
.
We can, nevertheless, already give some arguments below in favor of the Lorentzian being the correct description for
.
In the 3D simulations studied here, including that of the Sun,
the inferred
dependency of
is far from a Lorentzian, in contrast
to that found with the solar 3D simulation investigated in Paper III.
However, by investigating solar simulations with different resolutions,
we find that, as the spatial resolution increases,
tends towards
a Lorentzian
-dependency. This explanation is likely to stand for non-solar simulations too,
but has not yet been confirmed (work in progress).
Furthermore, as shown in Fig. 5, bottom, the direct calculations obtained with the simulation with the highest spatial resolution available is slightly closer to the semi-analytical calculations using the Lorentzian form than those using the Gaussian one.
Independently of the resolution (if large enough of course), a
Lorentzian
predicts larger values for
than a Gaussian or an exponential do.
In particular in the solar case, the semi-analytical calculation using
results in a
closer to the
helioseismic constraints derived by Baudin et al. (2005)
compared to using
or
.
This latter result is in agreement with that of Paper III.
Part of the remaining discrepancies with the helioseismic constraints are attributed to the adopted closure model according to Belkacem et al. (2006b, B06b hereafter). Indeed, theoretical models of stochastic excitation adopt the quasi-normal approximation (QNA). As shown in B06b, the skew introduced by the QNA result in a under-estimation of the solar p mode excitation rates. When the so-called closure model with plumes proposed by Belkacem et al. (2006a) is adopted, new semi-theoretical calculations fit rather well the recent helioseismic constraints derived by Baudin et al. (2005, see B06b).
Consequences of the predicted power laws for
have also been crudely investigated here for the expected value of
,
the maximum value of the mode velocity (Fig. 7). Calculations of
from
require the knowledge of the mode damping rates,
,
which cannot be fully determined from the simulations. We are then led to use theoretical calculations of the damping rates. We consider here those performed by Samadi et al. (2001) which are based on Gough's (1976,1977) non-local and time-dependent formulation of convection. From those values of
and the different power laws for
expected values of
are obtained.
We find, as in Houdek & Gough (2002, HG02), that
scales as
(L/M)sv.
Calculations by HG02 result in
.
Our semi-analytical calculations of
based on a Gaussian
result in a slightly smaller slope (
).
On the other hand, using a Lorentzian
results in a slope
which is closer to that derived from the few stars for which oscillation
amplitudes have been measured.
From this result, we conclude that the problem of the over-estimation of
the amplitudes of the solar-like oscillating stars more luminous than the Sun is
related to the choice of the model for
.
Indeed, previous theoretical calculations by Houdek et al. (1999) are based on the assumption of a Gaussian
.
As shown here, the Gaussian assumption results in a larger slope svthan the Lorentzian
.
This is the reason why Houdek et al. (1999) over-estimate
for
.
On the other hand, if one assumes
,
a scaling factor is no longer required
to reproduce
for the solar p-modes. Moreover, as a consequence of the smaller slope, sv, resulting from a Lorentzian
,
the predicted amplitudes for other stars match the observations better.
This result further indicates that a Lorentzian is the better choice for
,
as was also concluded in Paper III.
Departures of the theoretical curve from the observed points in Fig. 7 can be attributed to several causes which remain to be investigated:
Another issue concerns the relative contribution of the turbulent pressure. The excitation of solar-like oscillations is generally attributed to the turbulent pressure (i.e. Reynolds stress) and the entropy fluctuations (i.e. non-adiabatic gas pressure fluctuations) and occurs in the super-adiabatic region where those two terms are the largest. In Paper III, it was found that the two driving sources are of the same order of magnitude, in contradiction with the results by Stein & Nordlund (2001) who found - based on their 3D numerical simulations of convection - that the turbulent pressure is the dominant contribution to the excitation. The discrepancy is removed here as we used a corrected version of the formulation of the contribution of the Reynolds stress of Paper I (see Eq. (3)), leading to a larger contribution from the Reynolds stress.
For the Sun, assuming
(
resp.), we now find that
the Reynolds stress contribution is 5 times (3 times resp.) larger
than that due to the entropy fluctuations (non-adiabatic gas-pressure fluctuations).
Hence, the Reynolds stress is indeed the dominant source of excitation
in agreement with the results of Stein & Nordlund (2001). The best agreement with the latter results is obtained with a Lorentzian
.
However, we find that the relative contribution from Reynolds stresses decreases rapidly with (L/M). For instance, in the simulation of Procyon, the Reynolds stress represents only
30% of the total excitation rate.
From that, we conclude that the excitation by entropy fluctuations cannot be neglected, especially for stars more luminous than the Sun.
Acknowledgements
R.S.'s work has been supported by Société de Secours des Amis des Sciences (Paris, France) and by Fundacão para a Ciência e a Tecnologia (Portugal) under grant SFRH/BPD/11663/2002. R.F.S. is supported by NASA grants NAG 5 12450 and NNG04GB92G and by NSF grant AST0205500. We thank the referee, Mathias Steffen, for his judicious suggestions which helped improve this manuscript.
The adiabatic variation of the gas pressure does not contribute to the
work over an oscillation period as it is in phase with the volume (or density) variation.
In practice, however, it is beneficial for
the accuracy of the computation of excitation to
subtract the adiabatic part of the gas pressure fluctuation, since it
reduces the coherent part. That part gives zero contribution only in
the limit of infinite time, or for an exact integer number
of periods. However, in practice, it gives rise to a random (or noisy)
contribution. Indeed, as we deal with a lot of different modes
it is hard to find a time-interval which is an integer
number of periods of each and all of the modes at the same time.
The Lagrangian variations of gas pressure,
must satisfy
![]() |
(A.2) |
However, what we want to subtract off from
is that part of the pressure variation that is due to adiabatic compression and expansion due to the particular radial
wave modes (i.e. the low amplitude perturbation of
on top of the possibly large variations horizontally of
that
is an average of).
To find the nonadiabatic pressure fluctuations,
we start with calculations of horizontal averages of the primary quantities,
,
,
and
.
We convert these averages
to the pseudo-Lagrangian frame of reference, in which the net mass flux vanishes.
We then compute fluctuations of the resulting quantities
with respect to time, i.e., subtract their time averages: