 |  |
Astron. Astrophys. 317, 140-163 (1997)
3. Gravitational wave signature
The non-radial motions and the resulting time-dependence and
asphericities of the density stratification due to convection in the
unstable layers both inside the proto-neutron star and in the
neutrino-heated hot-bubble will produce gravitational radiation. Thus,
we have analysed the two- and three-dimensional models discussed in
the previous section and have computed the amount and the signature of
gravitational radiation that can be expected from convection in Type
II supernovae. Moreover, the density and temperature variations in the
neutrino-decoupling region (see Fig. 7) and the fast convective
overturn below the neutrinosphere lead to anisotropies of the neutrino
emission which will also be a source of gravitational waves (Epstein
1978, Turner 1978).
3.1. Formalism
The gravitational wave signal was calculated using a post-Newtonian
approach, where numerically troublesome higher order time derivatives
of the quadrupole moment are transformed into much better tractable
spatial derivatives. In particular, for the gravitational quadrupole
radiation field,
, we used an expression derived independently
by Nakamura & Oohara (1989), and by Blanchet et al. (1990):
![[EQUATION]](img136.gif)
where
is the distance between the observer and the
source,
is the Newtonian gravitational potential,
is the mass-density and
is the velocity. The other quantities have
their usual meaning except for
(with
) which denotes the transverse-traceless (TT)
projection operator onto the plane orthogonal to the outgoing wave
direction
, acting on symmetrical Cartesian tensors
according to
![[EQUATION]](img144.gif)
represents the partial derivative with
respect to the
coordinate. The integrand in Eq. (
4 ) is defined on a compact manifold and is
known to the (2nd order) accuracy level of the numerical algorithm of
the hydro-code. Eq. (
4 ) can be shown to be equivalent to the
standard representation
![[EQUATION]](img147.gif)
where the trace-free part of the mass-quadrupole tensor of the
matter distribution is given by
![[EQUATION]](img148.gif)
It can easily be shown that evaluating the integral of Eq. (
4 ) by an integration scheme (of at least 2nd
order) is by one order of accuracy superior to twice applying
numerical time-differentiation methods to quadrupole data given at
discrete points of time (see Mönchmeyer et al. 1991).
3.1.1. Evaluation in two dimensions
The gravitational radiation field gives direct information about
the second time derivative of the mass-quadrupole tensor (see Eq. (
7 )). In case of axisymmetry the quadrupole
moment, Q, is the only independent component of the quadrupole
tensor. Its relation to the Cartesian components
of the radiative mass-quadrupole tensor is
![[EQUATION]](img150.gif)
As all our simulations were performed in spherical coordinates, it
is natural to represent the (total) radiation field
in terms of the "pure-spin tensor harmonics"
and
with amplitudes
and
in the following way (Thorne 1980):
![[EQUATION]](img156.gif)
For the definitions of
,
,
, and
, see Thorne (1980). In spherical coordinates
the coefficients
and
have especially simple integral
representations over the source. By symmetry, there is only one
nonvanishing quadrupole term in Eq. (
9 ), namely
. Higher-order terms are neglected in the
quadrupole approximation
of the gravitational radiation field
. Transforming Eq. (
4 ) to spherical coordinates and expressing
in terms of unit vectors in the
and
direction, one obtains by comparison of Eq. (
4 ) with the lowest-order term of Eq. (
9 ) for the quadrupole wave amplitude
the expression
![[EQUATION]](img160.gif)
where
, and
.
From the definition of
(Thorne 1980, Eq. (2.39e)) one derives for the
components of
the formula
![[EQUATION]](img164.gif)
The only other nonzero component is
. The total energy radiated in gravitational
waves is then given by the general expression
![[EQUATION]](img166.gif)
The total energy radiated per unit frequency will be denoted by
and was calculated by interpolating the data
for the amplitudes
that are given at non-equidistant times onto
an equidistant temporal grid and using the fast Fourier transform
technique with a rectangular window function.
3.1.2. Evaluation in three dimensions
If the source is of genuine three-dimensional nature, it is common
to express the gravitational quadrupole radiation field,
, in the following tensorial form (see, e.g.,
Misner et al. 1973)
![[EQUATION]](img168.gif)
with the unit linear-polarization tensors
![[EQUATION]](img169.gif)
and
being the unit polarization vectors in
and
-direction of a spherical coordinate system
and
the tensor product. The amplitudes
and
represent the only two independent modes of
polarization in the TT gauge, and are given by the following
expressions for
![[EQUATION]](img176.gif)
and for
by
![[EQUATION]](img178.gif)
where
![[EQUATION]](img179.gif)
The total energy radiated in form of gravitational waves is then
given by
![[EQUATION]](img180.gif)
with
![[EQUATION]](img181.gif)
3.1.3. Gravitational waves from neutrino emission
In order to estimate the gravitational wave signal associated with
the anisotropic emission of neutrinos, we use Eq. (16) of Epstein
(1978) in the limit of a very distant source,
. In addition, we make use of the approximation
that the gravitational wave signal measured by an observer at time
t is caused only by radiation emitted at time
t' = t - R/c . Hence, we take
, which means that only a neutrino pulse itself
is assumed to cause a gravitational wave signal but memory effects
after the pulse has passed the observer are disregarded. With these
simplifications, one gets for the dimensionless gravitational wave
amplitude
![[EQUATION]](img184.gif)
with
being the angle between the direction towards
the observer and the direction
of the radiation emission, and
denoting the direction dependent neutrino
luminosity, i.e., the energy radiated at time t per unit of
time and per unit of solid angle into direction
. The angular integral over the radiation
source is performed over
and thus over all angles
and
which specify the (beam) direction in the
source coordinate frame
(x',y',z') that we identify with the coordinate frame
used for the hydrodynamical simulations. With the angles
and
defining the radiation direction in the
observer's frame
(x,y,z) (where the observer is located at distance
R along the z -axis) one has
, and the gravitational wave amplitude is given
by
![[EQUATION]](img192.gif)
Replacing
by
in Eq. (
25 ) yields
.
In Eq. (
25 )
and
need to be expressed in terms of the angles
,
,
, and
when
and
define the orientation of the observer's
coordinate system (observer located in z -direction and
y -axis lying in the
x' -
y' -plane) relative to the source coordinate
frame. Choosing
the y - and
y' -axes coincide and the expressions become
rather simple. For
the z -axis and the
z' -axis are identical, too, and the observer is
situated along the system's
z' - (polar) axis. In that case one obtains
![[EQUATION]](img200.gif)
When
is axially symmetrical, the gravitational wave
signal for an observer on the symmetry axis vanishes and
. For
the observer is positioned perpendicular to
the source's
z' -axis in the equatorial plane (z -axis
and
x' -axis coincide) and
becomes
![[EQUATION]](img205.gif)
Equations (
26 ) and (
27 ) can be rewritten as
![[EQUATION]](img206.gif)
with the anisotropy parameter
being defined by
![[EQUATION]](img208.gif)
where
denotes the angle dependent factors appearing
in the integrals of Eqs. (
26 ) and (
27 ), respectively, and
is the total neutrino luminosity,
![[EQUATION]](img211.gif)
Using the dimensionless gravitational wave amplitude of Eq. (
29 ) and taking into account that there is only
one non-zero component of the quadrupole amplitude, Eqs. (
11 ) and (
12 ) allow one to estimate the total energy
E(t) that is associated with the gravitational
waves produced by the anisotropic emission of neutrinos in the
two-dimensional (axially symmetrical) case until time t:
![[EQUATION]](img212.gif)
is a numerical factor of order unity,
typically around 0.5. Employing Eq. (
13 ) and Eqs. (
16 )-(
23 ) and assuming that all amplitudes
contribute roughly equally, one finds that Eq.
(
31 ) also holds for the three-dimensional
situation but with a slightly different value of
.
![[FIGURE]](img18k.gif) | Fig. 18. Quadrupole amplitude
[cm] of various models versus time. The upper left panel shows the amplitude obtained from a two-dimensional simulation of convection inside the proto-neutron star (see Sect. 2.1). The remaining three panels give the amplitudes obtained from two-dimensional simulations of convection in the hot-bubble region. The initial neutrino flux imposed at the inner boundary increases along the model sequence ML2D (top right), LP2D (bottom left), and EP2D (bottom right) from
erg/s to
erg/s (see Janka & Müller 1996), leading to increasingly faster explosions and higher supernova explosion energies (
,
, and
, respectively). The additional thin curve in the lower right panel gives the quadrupole amplitude produced by the convection inside the proto-neutron star alone. It is very small in models ML2D, LP2D, and EP2D because the convectively unstable region inside the proto-neutron star was only partially included in these simulations |
![[FIGURE]](img19k.gif) | Fig. 19. Similar to Fig. 18 but showing the quadrupole amplitude spectra
[kpc/Hz] as a function of the frequency of the emitted gravitational radiation |
![[FIGURE]](img20k.gif) | Fig. 20. Similar to Fig. 18 but showing the spectral energy density
[
Hz] of the quadrupole radiation as a function of the frequency of the emitted gravitational radiation |
![[FIGURE]](img21k.gif) | Fig. 21. Similar to Fig. 18 but showing the energy radiated in form of gravitational waves
[
] as a function of time |
3.2. Two-dimensional results
The results of our gravitational wave analysis for four different
models are displayed in Figs. 18 to 21 which show the quadrupole wave
amplitudes, the quadrupole amplitude spectra, the spectral energy
densities, and the energies radiated in form of gravitational waves,
respectively. One first notices that the signal forms and signal
strengths as well as the spectral distributions of the gravitational
wave energy depend on whether the gravitational radiation is produced
by convection inside the proto-neutron star or by convection in the
hot-bubble region. Generally speaking, in case of convective overturn
processes in the proto-neutron star, the maximum gravitational wave
amplitude is significantly larger (
cm instead of
cm), the spectral energy distribution is
peaked at higher frequencies (at 500 Hz to 1000 Hz instead of at about
100 Hz), and much more energy is radiated in form of gravitational
waves (
instead of
) as compared to multi-dimensional processes
in the hot-bubble region.
In model HB2D, which refers to the two-dimensional simulation of
convection inside the proto-neutron star starting with Hillebrandt's
configuration of a post-bounce stellar core, the strongly unstable
lepton and entropy gradients give rise to large convective velocities
which exceed
cm/s and are hence transonic. As the unstable
layer involves a relatively large amount of mass (
) the angular kinetic energy of the convective
flow is substantial (
erg). Moreover, because of the compact and
quite massive collapsed stellar core (
) in model HB2D the non-radial flow takes
place deep in a strong gravitational potential with convective
elements undershooting the stable layer down to a radius of about 15
km. Consequently, this model produces a relatively strong
gravitational wave signal with a maximum amplitude of
cm (Fig. 18) and a total emitted gravitational
wave energy of
(Fig. 21). Corresponding to the characteristic
overturn timescales of the convective eddies of about 2-10 ms, the
frequency spectrum of the quadrupole amplitude has a broad maximum at
about 100-500 Hz (Fig. 19) and the energy spectrum shows most power
being radiated between 100 and roughly 1000 Hz (Fig. 20).
As discussed in Sect. 2.2, convection inside the proto-neutron star
is much weaker in those of our models which we particularly used to
study convection in the hot-bubble region. There are three reasons for
this. Firstly, only the outer part of the convective zone in the
proto-neutron star is included in the simulations, i.e., only about
of the roughly
that are unstable against convection.
Secondly, the lepton and entropy gradients in Bruenn's initial model
are less unstable than those in Hillebrandt's collapsed stellar core.
Thirdly, due to the smaller core mass of only about
the gravitational potential is weaker in
Bruenn's model and there is less mass in the unstable layer around and
below the neutrinosphere. In the hot-bubble simulations the convective
velocities inside the proto-neutron star are therefore significantly
smaller, only about
cm/s, and, correspondingly, the angular
kinetic energies reach only about
-
erg at a time when the convection inside the
proto-neutron star is fully developed (at
ms, compare Fig. 9 in Janka & Müller
1996). Thus, the resulting gravitational wave signal from the
convective overturn inside the proto-neutron star is very weak in
these models as compared to model HB2D. In fact, in the models where
we followed the neutrino effects in the hot-bubble region, the
gravitational wave emission is strongly dominated by the waves
produced by mass motions in the neutrino-heated layer between
proto-neutron star and supernova shock.
We have analysed three such models, namely models ML2D, LP2D, and
EP2D (equivalent to models T2c, T3c, and T4c, respectively, in Janka
& Müller 1996), whose gravitational wave signature we discuss
in the following. We point out here that the actual gravitational wave
signal of these models will be considerably larger if the whole
convection zone inside the proto-neutron star, which yields only a
minor contribution to the gravitational wave emission in the presented
models, is included in the simulations. Models ML2D, LP2D, and EP2D
are nevertheless useful to investigate especially the characteristics
of the gravitational waves originating from turbulent motions in the
hot-bubble region. We find that the structure of the produced waves
contains detailed information about duration, strength, and pattern of
the accretion and convection processes behind the supernova shock.
When these dynamical processes have direct influence on the neutrino
emission, e.g., when matter accreted onto the neutron star produces
additional neutrino emission, we notice correlations of the neutrino
luminosity with the gravitational wave amplitude and luminosity.
Moreover, our models suggest that strength and duration of turbulent
processes around the proto-neutron star are correlated with the size
and temporal decay of the neutrino fluxes from the proto-neutron star
and with the explosion energy of the supernova. For this reason we
expect, and indeed observe, characteristic differences of the
gravitational wave signature of models with different explosion
dynamics and different explosion parameters.
In model ML2D the temporal modulations of the gravitational wave
signal and the neutrino losses from the hot-bubble region show clear
correlations (compare the upper right panel in Fig. 18 with Fig. 18 in
Janka & Müller 1996). Neutrino emission and gravitational
wave emission from the turbulent layers around the proto-neutron star
in this model are produced by downflows of cold material from the
postshock region. These narrow downflows reach very high velocities of
more than twice the speed of sound and are abruptly decelerated at a
radius of about 80 km (see Figs. 15 and 16 in Janka & Müller
1996). The peaks and characteristic features in the neutrino emission
are associated with the dissipation of kinetic energy of the gas in
the surroundings of the proto-neutron star. The aspherical, dynamical
gas motions also act as source of gravitational waves. The large
variations of the gravitational wave amplitude around
-140 ms (Fig. 18) are directly correlated with
spikes in the lepton number loss/gain rate and the energy loss/gain
rate of the stellar gas at the same epoch (Fig. 18 in Janka &
Müller 1996). Similarly, the variation of the gravitational wave
amplitude between 150 ms and 200 ms is mirrored by a correlated
activity in the lepton and energy loss/gain rates. Actually, one can
observe a slight time-lag of the neutrino emission. This shift can be
explained by the fact that the gravitational wave emission traces the
dynamical infall of the downflows, whereas the neutrino emission peaks
at the moment when the infalling gas reaches highest temperatures and
densities, i.e., typically at the moment when it is decelerated and
strongly compressed near the proto-neutron star. The characteristic
timescale of gas motions and convective overturn in the hot-bubble
region is of the order of several ten to about 100 ms. The frequency
spectrum of the quadrupole amplitude therefore peaks at frequencies of
about 10 to roughly 100 Hz (Fig. 19), and the energy spectrum has a
maximum between 50 and 200 Hz with significant power in the frequency
range from 10 to 400 Hz (Fig. 20).
The gravitational wave signal of model LP2D is characterized by the
low-frequency emission from the aspherical expansion of postshock
material and by the superimposed high-frequency modes that are
produced by small-scale convective processes in the neutrino heated
hot-bubble region. The prolate, large-scale deformation of the
supernova shock leads to a time-dependent mass quadrupole moment that
varies within a typical time of about 100 ms. While the effect of the
expansion of supernova shock and ejecta becomes prominent in the
gravitational wave signature at times later than about 100 ms after
the start of the simulation, the overturn of neutrino-heated material
determines the wave amplitude during the first 100 ms where signal
variations on timescales of 10-20 ms are visible. The gravitational
wave amplitude reaches a maximum value of
cm (Fig. 18) and has typical frequencies
between about 10 and 100 Hz (Fig. 19). The energy spectrum peaks at
about 50-70 Hz ((Fig. 20) and the total energy radiated in
gravitational waves is
which is almost a factor of 20 smaller than in
model ML2D where it is
within a similar time of 200-300 ms after
supernova shock formation. While the major part of the gravitational
wave emission of model ML2D is produced by anisotropic, dynamical
downflows of matter from the postshock region to the proto-neutron
star, roughly half of the gravitational wave energy of model LP2D
results from overturn motions of neutrino-heated gas and the other
half from the large-scale expansion.
In model EP2D the explosion happens faster (due to higher core
neutrino fluxes) and the convective overturn in the neutrino-heated
region is correspondingly shorter. The contribution of the large-scale
deformation and expansion of the postshock region to the gravitational
wave signal therefore clearly dominates the wave amplitude after about
100 ms (Fig. 18). On a timescale of hundreds of milliseconds the wave
amplitude exhibits the slow variation associated with the change of
the mass quadrupole moment due to the global dynamical evolution of
the explosion. However, it shows only little substructure of higher
frequencies because the rapid expansion of model EP2D limits the
duration of the phase of convective overturn in the hot-bubble region
to about 100 ms. This can be verified in the quadrupole amplitude
spectrum (Fig. 19) which confirms the clear dominance of low-frequency
modes (around 1-10 Hz) and essentially no pronounced features at
higher frequencies. The corresponding energy spectrum (Fig. 20) is
very flat and spans the range of frequencies between about 1 Hz and
roughly 100 Hz. Even stronger than in case of model LP2D, the global,
asymmetrical expansion of model EP2D on a timescale of several 100 ms
is reflected in the fact that significant, or even most, power is in a
fundamental, low-frequency signal of a few Hz. Model EP2D emits about
of gravitational wave energy which is about
50% less than model LP2D. In the lower right panels of Figs. 18-21 the
thin solid lines correspond to the gravitational wave signal that
originates from the incompletely represented (see above) convective
region inside the proto-neutron star for model EP2D. A comparison of
the thin and thick lines, the latter representing the total signal,
shows that most of the emission is produced by the convection in the
hot-bubble region. Only at early times after bounce (
ms, which is when the convective overturn in
the neutrino-heated region is not yet fully developed) do convective
motions around and inside the neutrinosphere contribute significantly
to the total gravitational wave emission (see Fig. 18) at frequencies
above 50 Hz (Figs. 19 and 20) and with an integrated energy of about
. At later times the signal of convection in
the proto-neutron star is minor and the results shown for models ML2D,
LP2D, and EP2D in Figs. 18-21 do indeed primarily originate from the
mass motions in the hot-bubble region and from the explosive expansion
of the supernova.
Comparing the three models we see that with increasing neutrino
flux (imposed as an inner boundary condition) and hence with
increasing explosion energy the convective activity in the hot-bubble
region changes from violent, long-lasting convective overturn
associated with accretion processes (model ML2D) to rapid expansion
and relatively slowly changing large-scale deformation (model LP2D)
which eventually dominate the overall asymmetry and the quadrupole
moment of the exploding star (model EP2D). This change of the
characteristics of non-radial motions in the hot-bubble and postshock
regions is directly reflected in the dominant frequencies of the
gravitational wave signal, which drop from about 200 Hz (model ML2D)
down to less than 10 Hz (model EP2D). Thus, a measurement of the
frequency of the wave signal provides important insights into the
explosion dynamics. Moreover, since the signal produced by the
convection inside the proto-neutron star is typically of much higher
frequency (500-1000 Hz), such a measurement would also allow to
discriminate the contributions from both convection zones.
Unfortunately, the calculated maximum dimensionless amplitudes
(Eq. (
11 )) are too small to be detected for a
supernova outside our own Galaxy, because they lie in the range
for a source at a distance of 10 kpc.
![[FIGURE]](img22k.gif) | Fig. 22. The four panels show the time evolution of the density fluctuations on a sphere with a radius of 65 km located in the middle of the convective layer inside the proto-neutron star. The snapshots are taken at 9.0 ms (top left), 12.2 ms (top right), 13.6 ms (bottom left), and 16.6 ms (bottom right) after the start of the 3D simulation. The ratio of maximum density to minimum density is 1.11, 2.09, 2.32, and 1.72, respectively. In each panel the white frame marks the 60 by 60 degree sector in which the simulation was performed. Note that the fluctuations are homogeneously distributed over the sphere at all times and that the size of the structures increases with time |
![[FIGURE]](img23k.gif) | Fig. 23. The gravitational wave signal of convective instabilities inside the proto-neutron star according to the three-dimensional model HB3D. The upper left panel shows the quadrupole waveforms of the two independent signal amplitudes
and
at the pole (
,
; solid and dotted lines) and at the equator (
,
; dashed and dashed-dotted lines), respectively. The upper right panel shows the frequency spectra of the polar amplitudes
(solid curve) and
(dotted curve), the lower left panel the energy radiated in form of gravitational waves,
[
], as a function of time, and the lower right panel displays the corresponding spectral energy density |
3.3. Three-dimensional results
The analysis of the three-dimensional model caused some problems
because our simulation volume involved only a 60 by 60 degree sector
of a full sphere. Simply extending the data from the computational
volume to the whole sphere by making use of the periodic boundary
conditions imposed in angular direction during the simulation did not
make sense because a spherical potential was used in the simulation
and because the resulting configuration was highly symmetrical in
angular direction. The computed sector fits into the full sphere
exactly three times in
-direction and six times in
-direction which gives rise to a 60, 120, and
180 degree rotational symmetry around the z -axis.
In order to compute the gravitational radiation we instead
proceeded as follows. First we divided the simulated sector into 36
subsectors of 10 by 10 degree each. Then these 36 subsectors were
randomly distributed over the full sphere. This process is justified,
because the angular distribution of the dynamical variables varies on
scales smaller than or, at least, not much larger than 10 degrees (see
Sect. 2.1.2 and Fig. 12). However, one has to take into account that
in
-direction the linear extent of the subsectors
decreases like
when approaching the poles at
and
. We therefore mapped one 10 by 10 degree
subsector as constructed in the simulated
degree wedge over several pole-near subsectors
such that the length scales of the structures were approximately
conserved. This mapping procedure of the data was repeated for all
radial shells and for all times while keeping the association of
subsectors of the computational cone with
their randomly chosen mapping locations on the sphere fixed.
The resulting angular distribution is displayed in Fig. 22 showing
the density on a sphere of radius 65 km (which is right inside the
convective layer in the proto-neutron star) at different moments of
the evolution. Fig. 22 shows that the structures are indeed small
enough and the mapping process is random enough to produce
statistically homogeneous angular distributions. The result is so
perfect that if we omitted the white solid line that marks the
boundary of the computed sector, it would be impossible to locate the
wedge of the simulation by eye inspection.
Fig. 22 further shows that the angular scale of the fluctuations is
time-dependent and grows steadily with time from the onset of the
instability at about 9 ms (upper left panel in Fig. 22). The level of
the fluctuations reaches a maximum at about 13.6 ms (lower left panel
in Fig. 22), when the ratio of maximum to minimum density is 2.32 at
65 km. Within the next 3 ms the ratio drops to a value of 1.72 (lower
right panel in Fig. 22) which reflects the increasing homogenization
of the mixing layer.
From the density distribution on the full sphere as constructed by
the mapping procedure we computed the corresponding three-dimensional
gravitational potential taking into account the central point mass
(see Sect. 2.1). The three-dimensional Poisson solver employed in the
calculation of the potential is an extension of the two-dimensional
solver of Müller & Steinmetz (1995) and was provided by
Zwerger (personal communication). Using the computed three-dimensional
gravitational potential and the mapped density and velocity
distributions, we were able to derive the gravitational wave signature
of model HB3D from Eqs. (
13 -
23 ).
According to Fig. 23 model HB3D, which is the three-dimensional
analogue of model HB2D, emits significantly less energy in form of
gravitational waves. There are several reasons for that. Firstly, the
convective elements are smaller, only about half of the typical size
found in two dimensions (
), and the mass motions are therefore less
coherent and do not cause the strong large-scale deformations seen in
2D. Secondly, the rising and sinking convective elements move with
smaller velocities in three spatial dimensions,
, which leads to reduced over- and
undershooting (only about 0.8 instead of 1.2 pressure scale heights,
see Sect. 2.1) and is another reason for the weaker large-scale
deformation of the outer layers of the proto-neutron star in the 3D
model HB3D. While model HB2D emits a gravitational wave energy of
, model HB3D radiates an energy of only
during the same time interval of 32 ms
(compare Figs. 18 and 23). The quadrupole amplitudes of both
polarizations (
and
) are also shown in Fig. 23 for an observer at
the pole and at the equator, respectively. The maximum absolute values
of the amplitudes never exceed 4 cm which is about a factor of 100
smaller than in the two-dimensional model HB2D (see Fig. 18). This
corresponds to a maximum dimensionless gravitational wave amplitude
(Eq. (
13 )) of
for a source at distance 10 kpc, about a
factor of 15 smaller than in HB2D. A comparison of Figs. 19 and 20
with Fig. 23 (upper and lower right panels, respectively) reveals that
the frequency spectrum of the quadrupole amplitude and the spectral
energy density show more relative power, respectively are more peaked,
towards lower frequencies in case of model HB3D. In HB3D the spectral
maxima are around 100-200 Hz and the spectra drop rapidly towards
higher frequencies, whereas the amplitude spectrum of HB2D has a broad
region of highest power between 100 and 700 Hz (Fig. 18) and the
spectral energy density of HB2D peaks between about 200 and 600 Hz.
This difference of the wave frequencies is a result of the smaller
convective velocities and the correspondingly longer overturn
timescales and less violent convection in the three-dimensional
situation.
3.4. Gravitational waves from anisotropic neutrino emission
The gravitational wave emission associated with the anisotropic
radiation of neutrinos can only be estimated for the presented models
because no multi-dimensional neutrino transport was used in the
simulations, in fact some of the models were computed without
including neutrino effects at all.
In order to estimate the anisotropy parameter
defined in Eq. (
29 ) we used the following procedure. Assuming
that the neutrino flux can be approximated by black-body emission and
thus scales with the fourth power of the temperature T and with
the area
of the emitting surface region, we employed
to evaluate Eq. (
29 ). Here
denotes a mass-weighted radial average of
in the neutrinospheric layer that is
considered to encompass densities of
to
. The mean
is evaluated by adding up the mass-weighted
contributions of all grid cells along a specified radial beam
direction
. Repeating this for all angular directions and
for all given time levels of a model yields the needed input
into Eq. (
29 ).
Evaluating the two-dimensional model HB2D we find that the
anisotropic neutrino emission associated with the convective processes
inside the proto-neutron star leads to an equatorial anisotropy
parameter of
(Eq. (
29 ) with the angular factor of Eq. (
27 )) at a time when the convective overturn is
fully developed (
ms after the start of the simulation). We
obtain numerical values that are rather close to those of the relative
quadrupole moment of
. A test integration, moreover, was in
agreement with the analytical result for the axially symmetrical case,
namely that the corresponding polar anisotropy parameter
(Eq. (
29 ) with the angular factor of Eq. (
26 )) is negligibly small. Using the
temperature distribution from the three-dimensional simulation HB3D we
get
for
ms, again fairly similar to what is obtained
from the quadrupole formula.
The anisotropy parameters
therefore turn out to be roughly a factor of
10 smaller in the 3D case than in the 2D situation. Correspondingly,
when going from 2D to 3D, the gravitational radiation field
(Eq. (
28 )) becomes about one order of magnitude
smaller and the gravitational wave energy
(Eq. (
31 )) approximately two orders of magnitude, if
the neutrino luminosities of both cases are similar. Assuming constant
luminosity
and anisotropy
for an emission time
, one gets
![[EQUATION]](img285.gif)
and
![[EQUATION]](img286.gif)
For
erg/s and a typical emission time of one
second - which assumes that convective overturn and anisotropic
neutrino emission continue during most of the time when the
gravitational binding energy of the proto-neutron star (a few
erg) is lost by neutrino emission - one finds
to be of the order of several 100 cm, i.e.,
for a source at a distance of 10 kpc. The
gravitational wave energy is
. For the three-dimensional case these numbers
are
and
.
The gravitational wave signal from anisotropic mass motions due to
convection inside the proto-neutron star was found (Sects. 3.2 and
3.3) to be
and
for model HB2D and
and
for the three-dimensional model HB3D. A
comparison shows that the gravitational wave amplitude associated with
the neutrino emission is somewhat larger than the wave amplitude due
to convective motions. In two dimensions the neutrino gravitational
wave amplitude is about 5 times larger, in three dimensions the factor
can become even 10. The total energy radiated in gravitational waves,
however, is dominated by the contributions from the mass quadrupole
moment. Neutrino gravitational waves account only for a minor fraction
(for a few per cent at most) of the total gravitational wave energy in
two-dimensional models, while in 3D they contribute up to several 10%
of the gravitational wave energy.
Like the gravitational waves from convective motions inside the
newly formed neutron star, the neutrino gravitational waves are
predominantly emitted in the frequency band between several 10 Hz and
a few 100 Hz because of the common origin and thus similar timescales
of the anisotropic processes. In case of the neutrino gravitational
waves there is also a superimposed low-frequency component (
Hz to a few Hz) caused by the long-time
variation of the neutrino emission from the cooling neutron star on a
timescale of about one second.
© European Southern Observatory (ESO) 1997
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