The long-term monitoring optical light curves of AO 0235+16 in the Johnson's
UBV and Cousins' RI bands are shown in Fig. 1.
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Figure 1: Long-term monitoring light curves of AO 0235+16 in UBVRI; data are from Kinman & Rieke (1975), Rieke et al. (1976), O'Dell et al. (1978a,b), Pica et al. (1980), Impey et al. (1982), Barbieri et al. (1982), Moles et al. (1985), Smith et al. (1987), Sillanpää et al. (1988a), Webb & Smith (1989), Mead et al. (1990), Sitko & Sitko (1991), Sillanpää et al. (1991), Takalo et al. (1992), Xie et al. (1992), Rabbette et al. (1996), Webb et al. (1997), Takalo et al. (1998), Xie et al. (1999), and Ghosh et al. (2000); data plotted after the vertical line are from the present work. |
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Figure 2: Light curves of AO 0235+16 in BVRI bands in the years 1996-2000; all data are from the present work. |
Observatory | Nation | Long. (deg) | Lat. (deg) | Tel. diam. (m) | Filters | Symbola |
MSSSO | Australia | +149.066 | -31.277 | 1.0 | R | filled triangles |
Xinglong | China | +117.575 | +40.393 | 0.6 | R | filled squares |
Vainu Bappu | India | +78.83 | +12.57 | 2.0 | R | asterisks |
Abastumani | Georgia | +42.80 | +41.80 | 0.7 | R | open circles |
Tuorla | Finland | +22.17 | +60.27 | 1.03 | V | |
Roma | Italy | +12.70 | +41.80 | 0.5, 0.7 | BVRI | open triangles |
Perugia | Italy | +12.372 | +43.112 | 0.4 | VRI | open diamonds |
Torino | Italy | +7.775 | +45.038 | 1.05 | BVRI | open squares |
Calar Alto | Spain | -2.546 | +37.224 | 2.2 | R | filled circles |
Teide | Spain | -16.5 | +28.16 | 0.82 | BVRI | crosses |
NOT | Spain | -17.88 | +28.75 | 2.56 | BVRI | asterisks |
Foggy Bottom | USA | -74.25 | +43.24 | 0.4 | R | filled stars |
Climenhaga | Canada | -123.22 | +48.25 | 0.5 | R | filled diamonds |
Although the intense source variability makes a comparison among the
different datasets difficult to perform, a general agreement was found
where the data overlap in time.
Many large-amplitude outbursts are visible from Fig. 1; in the B band the
minimum and maximum magnitudes observed were
(
)
and
(
), respectively. In the R band
the range of magnitudes spanned is from
(
)
to
(
).
An enlargement of the BVRI light curves in the period 1996-2000 is shown in Fig. 2; an inspection of the R-band curve, the best sampled one, reveals three major peaks, one for each of the last three observing seasons.
Details of the 1997-1998 season are visible in Fig. 3,
The peak at
was observed by both the Perugia and the Roma
Observatories, and corresponding peaks were seen also in the BVI bands (see
Figs. 1 and 2). What is quite impressive is the extreme sharpness of the
flare: a brightness increase of
in 4 days (inside a
rise in 27days) was followed by a
decrease in only one day, leading to a
fall in 13 days.
A smoother behaviour characterizes the 1998-1999 observational season (see
Fig. 4):
In the last observing season the temporal coverage was definitely worse than in
the previous two seasons (see Fig. 2); however, a quite interesting feature is
the fall of
in 48 hours occurred in the R band at the beginning of
September 1999 (
-
2451427.657).
The WEBT is an international collaboration among astronomers from all the world with the aim of organizing optical campaigns on blazars of specific interest (Mattox 1999a,b; Villata et al. 2000). These campaigns, lasting from a few days to several weeks, are generally undertaken in concert with observations at other wavelengths, and can be triggered by the discovery of a flaring state of an object, usually in the optical band.
This was indeed the case for the first-light WEBT
campaign: the November 1997 observations of AO 0235+16 were started
after the detection of a considerable brightness increase (about
in a
week) at the end of October 1997 (Webb et al. 1997).
An EGRET target of opportunity observation occurred between November 3 and 11,
1997, but only an upper limit of
above
could be inferred (Hartman, private communication).
Observations by RXTE did not find a high X-ray flux (Webb et al. 2000).
The light curve obtained in the first 11 days of November 1997 is plotted in
Fig. 5.
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Figure 5: Light curve of AO 0235+16 in the Cousins' R band during the first-light WEBT campaign of November 1997; for the explanation of symbols see Table 1. |
In order to avoid spurious variations due to possible systematic effects
among data from different observatories, in the following only flux changes
observed by the same telescope will be considered. A brightness increase of
in two days was detected at the beginning of the campaign and
noticeable flux oscillations were observed all the time. Variations of
0.2-
in 5-7 hours were found in a number of cases; very impressive is
the dimming of half a magnitude in about 5 hours detected in the night
between November 3 and 4. Similar very fast variations have recently been
observed by Romero et al. (2000).
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Figure 7:
The spectral index ![]() |
One item that is interesting to investigate when studying the optical
variability of blazars is whether the flux variations are accompanied by
spectral changes.
In the new data presented in this paper we identified 47 optical spectra
collecting data in at least three filters taken by the same telescope,
with the requirement that the delay from the first frame to the last one is
not greater than 50 min.
We discarded 7 spectra which contained large
errors and analyzed the remaining 40.
A selection of these "well behaved" spectra is
presented in Fig. 6 in the
-
plane,
using different symbols for data taken at different
telescopes. When taking into account that some discrepancies in the spectral
shape can arise from not completely equal photometric systems used in the
various observatories, no significant variations can be recognized when the
flux changes. However, a deeper inspection reveals that the spread
corresponding to the B band is larger than that relative to the I one.
This would suggest that the flux variations are of larger amplitude at the
higher frequencies, as already observed in other blazars.
All 40 "well behaved" optical spectra were then fitted by a classical power
law:
with a
minimizing procedure. The
results are shown in Fig. 7,
where the spectral index
is
plotted as a function of the flux in the R band and
values with
errors greater than 0.25 have been eliminated. One can notice that for high
flux levels
presents an almost constant value of -2.8--2.7,
while it tends to decrease with
decreasing flux, although there is a not negligible spread.
This means that the spectrum basically steepens when the source gets fainter, a
behaviour that is common to blazars.
Copyright ESO 2001