Optical spectral changes are not very evident, but our data suggest a spectrum steepening when the source gets fainter, a feature that has already been recognized for other blazars. This behaviour can be interpreted in terms of radiative losses in the electron population of the emitting jet: when the source is bright, cooling can be balanced or overcome by acceleration processes and the resulting spectrum is flatter; when the flux is low, radiative losses dominate and cause a spectral steepening, since the higher-energy ultra-relativistic electrons emitting synchrotron radiation cool faster than the lower-energy ones. However, also a geometrical interpretation of the kind of that presented in Villata & Raiteri (1999; see also Villata et al. 2000) is possible: if a faint state of the source in a given band occurs when the portion of the curved jet emitting in that band becomes less aligned to the line of sight, then a spectral steepening is expected since the higher-frequency emitting portion of the jet departed first from the line of sight.
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Figure 13:
Discrete Correlation Function (DCF) between the R data and
![]() ![]() |
Discrete autocorrelation function analysis of the optical and radio light curves points out a characteristic time scale for the flux variability of AO 0235+16 of about 11.2 years. However, a deeper insight into the optical and radio light curves aided by DFT analysis and folded light curves reveals that major outbursts occur at roughly half the above time scale, even if one of the events (the 1982 one) appears noticeably delayed.
Indeed, in the best sampled
light curve, there are five large-amplitude outbursts whose
peaks are separated by 2308, 1870, 2007, and 2091 days, giving an
average "period" of 2069
184 days, i.e. 5.7
0.5 years. Taking
into account that the AO 0235+16 redshift is z=0.94, the relation
implies that the period in the source rest frame is
around 2.8 years. Other characteristic frequencies resulting from the DFT
analysis of the radio light curves correspond to periods of 1.8, 2.8, and 3.7years.
In the optical, the sparse sampling makes the analysis of variability time
scales rather difficult. However, discrete autocorrelation function, DFT, and
folded light curves are compatible with a
2069 day periodicity. Such
periodicity would not account for the observed big 1979 optical outburst,
whose radio counterpart was a rather modest flux increase. The optical
autocorrelation analysis puts in evidence also another characteristic time
scale of variability of about 1200 days (3.3 years), which corresponds to the
time separation between the 1975 and 1979 outbursts, while the DFT of the
optical data confirm the 1.8 and 2.8 year periods found in the radio data.
A few previous studies investigated the existence of
periodicities in AO 0235+16: Webb et al. (1988) analyzed the optical
light curve with the Deeming DFT (Deeming 1975), and
derived periods of 2.79, 1.53, and 1.29 years. More recently, Webb et al. (2000) used unequal-interval Fourier transform and CLEAN techniques
and obtained periods of 2.7 and 1.2 years for the optical variations. The
time scales of long-term optical base-level fluctuations have been studied by
Smith & Nair (1995) for three classes of AGNs; they found a best fit
period of 2.9 years for AO 0235+16, attributing a moderate confidence to the
estimate. The Jurkevic technique and the autocorrelation function were adopted
by Fan (2001) for the analysis of the optical light curves,
inferring periods of 1.56,
,
and
years. This last
period is highly compatible with what is derived in the present paper.
Roy et al. (2000) made a cross-correlation analysis between optical
and UMRAO radio data and applied Lomb-Scargle periodograms to the 14.5 and
light curves to infer a
5.8 year periodicity. Their results are
in agreement with what we find in the present paper.
If the major outbursts
in AO 0235+16 really occur every
years, the next one should
peak around February-March 2004,
and a great observational effort should be undertaken since at least summer
2003 to get more information on the details of the flux behaviour in various
bands. Unfortunately, the source is not visible from ground-based optical
observatories during springtime because of solar conjunction.
On the other
hand, another great effort should be addressed to the theoretical
interpretation of such recurrent events, in particular to envisage possible
mechanisms that can "disturb" the period.
Many models have been proposed to explain the 12 year period inferred from the optical light curve of another well-known BL Lac
object, i.e. OJ 287; most of them foresee the existence of a binary black
hole system (Sillanpää et al. 1988b; Lehto & Valtonen
1996; Villata et al. 1998; Valtaoja et al. 2000;
Abraham 2000). It would be interesting
to see whether those models can be adapted to explain the quasi-periodic
variability observed in AO 0235+16.
As for the cross-correlation between the optical and radio data, the analysis
of the light curves is constrained by the sometimes very sparse optical
sampling. However, in general we can say that
a radio flux increase always corresponds to each major optical flare;
the vice versa is likely true. Such correlation would suggest that the
same mechanism is responsible for the optical and radio variations.
However, two different
behaviours seem to be present: optical and radio fluxes are seen sometimes to
reach their maximum values at the same time, while in some cases the higher
frequencies lead the lower ones. This would mean that two different mechanisms
are presumably at work in the long-term variability.
Outbursts occurring simultaneously in all bands may suggest that the
synchrotron emission from the radio to the optical band is produced by the same
population of relativistic electrons in the same region. But they may also
favour the microlensing scenario, which was already suggested for explaining
the variability of AO 0235+16 (Stickel et al. 1988; Takalo et al. 1998; Webb et al. 2000; but see Kayser 1988 for a
critical discussion). The presence of several foreground objects in the field
of the source supports this scenario. One item against this hypothesis is that
during the strong flux increase detected in both the optical and radio bands
in 1997, the X-ray and -ray fluxes were not seen in a high state.
On the other hand, the fact that in the radio and optical domains the variations observed at the higher frequencies lead those at the lower ones makes one think to an inhomogeneous jet, where a disturbance travelling downstream enhances first the emission at the higher frequencies and then the emission at the lower ones. An alternative view is given by geometrical models such as the previously mentioned helical model by Villata & Raiteri (1999), if we imagine that the portion of the jet emitting the higher-energy radiation gets closer to the line of sight before that producing the lower-energy flux, as already noted for the spectral changes.
A different interpretation is required to explain the noticeable intraday
variability shown by AO 0235+16 in both the optical and radio bands.
Indeed, on short time scales, the flux behaviour can be very different with
respect to that exhibited on long time scales. Kraus et al. (1999)
observed an "unusual" radio event in October 1992, in which the
maximum
preceded the maxima at 3.6 and
,
and the variation amplitude was larger at
the lower frequencies. They applied a number of models, both of intrinsic and
of extrinsic nature, and concluded that, in any case, the size of the emitting
region must be very small, implying a Doppler factor of order 100. Such a
high value was subsequently confirmed by Frey et al. (2000) by
analyzing VSOP observations of AO 0235+16.
We found several episodes of very fast intraday variability in the radio light
curves; in some cases we are in the presence of single points that appear to
deviate from the longer trends shown by the data, but there are cases in which
the variation is confirmed by more than one point. Calculation of the
brightness temperature for the fastest variability events (
)
in the
light curve (containing data
generally of higher signal-to-noise ratio with respect to the lower
frequencies ones) led to values by far exceeding the Compton limit, implying
Doppler factors in the range 30-70. Indeed, such results must be taken with
caution, since a much better sampling is needed in order to derive reliable
Doppler factors from the radio intraday variability.
In conclusion, all the items pointed out by the present work (such as the 5.7 year periodicity, delayed flux variations at lower frequencies, high Doppler factors) would need a further observational effort in the next years, in order to fix them to more precise results.
Acknowledgements
We gratefully acknowledge useful suggestions by the referee, Dr. K. Ghosh. We thank R. C. Hartman for communicating us the result of the EGRET VP 6311 on AO 0235+16. This research has made use of:
- the NASA/IPAC Extragalactic Database (NED), which is operated by the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration;
- data from the University of Michigan Radio Astronomy Observatory, which is supported by the National Science Foundation and by funds from the University of Michigan.
Copyright ESO 2001