Astron. Astrophys. 319, 515-524 (1997)
3. Power spectra
The root mean square residuals technique used in this section for
the estimation of red noise power density and associated random walk
noise strengths is discussed in detail by Cordes (1980) and Deeter
(1984). The applications made by Baykal et al., (1993a, b) are the
examples of its use in characterizing random walk processes.
For the case of th-order red noise (or
r th-time integral of white noise time series) with strength
, the mean squared residual for data spanning an
interval T is proportional to . The
proportionality factor (or normalization coefficient) depends on the
degree m of the polynomial removed prior to computing the mean
square residual; this factor can be obtained by determining the
expected mean square residual for unit strength red noise
( ) over a unit interval
( ), either by Monte-Carlo methods (Cordes 1980)
or by mathematical evaluation (Deeter 1984). The mean square residual,
after removing a polynomial of degree m over an interval of
length T, is then given by
![[EQUATION]](img25.gif)
where is the proportionality factor which
has been derived from a unit-strength noise process. Our preliminary
analysis showed that the angular velocity residuals can be
characterized by first order red noise (or random walk). This noise
process is adopted in computing the normalization coefficients. The
normalization coefficient is computed by Monte Carlo simulation,
sampling the simulated data as the real data set was sampled (Cordes
1980). Because most of the BATSE data are approximately equally spaced
at 1 day intervals, the normalization coefficient differs by no more
than 15 from the theoretical prediction for
equally spaced data (assuming a sampling interval of one day) as given
in Table 1 and 2 of Deeter 1984.
As a next step, time scales are sampled at nearly octave spacings
for the power density estimators (Deeter 1984). To do this the entire
length of the data is taken as the longest time-scale. Then the
intervals are halved successively to get down to the shortest
practical time scale. Intervals with insufficent data points are
discarded. The mean squared residuals for the remaining intervals are
calculated and converted into the noise strengths
( ) using Eq. 1. The contributions of the
measurement errors have been computed by converting the estimated
variances of angular velocities into noise strengths and by employing
the identical procedure above.
Estimated noise strengths on each time scale are combined into a
single power density estimate ( , where f
is the frequency, Rice (1954); Boynton (1981)) by averaging, and are
represented by a frequency equal to the inverse of the time scale. In
order to estimate the power density error bars, the effective number
of degrees of freedom, for each estimate is determined by generating
its statistical distribution by using Monte Carlo simulations of a
first order red noise process, sampled in the same way as our angular
velocity data (Blackman & Tukey 1958; Deeter & Boynton 1982).
Then the power density error bars are computed for a given effective
number of degrees of freedom by computing the power density values
corresponding to the and
points of the distribution; these are
equivalent to confidence level for a Gaussian
(Blackman & Tukey 1958). In Fig. 3, we display the resulting
power density estimates (or noise strengths) of the angular
acceleration fluctuations.
![[FIGURE]](img34.gif) |
Fig. 3. Power spectrum of angular accelerations (or noise strengths, see the text). The asterisks denote the measurement errors.
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In the analysis, we have found the crossover frequency between the
errors and noise strengths around days). We
have fitted a straight line to the 8 lower octave power density
estimates and found which is consistent with
white noise in the angular accelerations
( ) with the mean power density (or noise
strength) rad2 /sec3.
In order to crudely estimate the step size of the fluctuations
and the rate R of torque events we make
use of the autocorrelation of angular acceleration
) time series. We took the numerical time
derivative of the angular velocity ( ) time
series at time scales corresponding to the cross over frequency (see
Fig. 7b) and represented the autocorrelation function in
Fig. 4. Autocorrelation function of white noise time series can
be expressed as (Jenkins & Watts 1968),
![[EQUATION]](img45.gif)
where is the white noise variance at zero
time lag . As seen from Fig. 4, actually
the autcorrelation function shows correlation for time lags
( ) up to 8-19 days.
![[FIGURE]](img43.gif) |
Fig. 4. Autocorrelation function of angular accelerations time series.
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The step size of the fluctuation during this time scale can be
estimated
. By using the values
rad2 /sec4 and , from the
autocorrelation function and the random walk noise strength estimate
from the power spectrum we estimated the rate of torque events as
![[EQUATION]](img51.gif)
This implies a torque event occurs within
days and lasts days. These events appear as a
delta function (or unresolved events) if we are studying the long time
scale fluctuations and make the power spectra of
flat at low frequency (or long time scales
days). But at high frequencies (or short time
scales days), it is quite natural to see
decrease in power density estimates. If we express the white noise
time series as a sum of Gaussians , with a small
finite variance , then we would expect the power
spectrum to have the form
. Therefore at frequencies
one should see a decrease in the power spectra
at order of . This is qualitatively seen in our
low resolution power spectra (see Fig. 3).
© European Southern Observatory (ESO) 1997
Online publication: July 3, 1998
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