A&A 406, L33-L37 (2003)
DOI: 10.1051/0004-6361:20030855
M. Della Valle1 - D. Malesani2 - S. Benetti3 - V. Testa4 - M. Hamuy5,1 - L. A. Antonelli4 - G. Chincarini6,7 - G. Cocozza4,8 - S. Covino6 - P. D'Avanzo6 - D. Fugazza9 - G. Ghisellini6 - R. Gilmozzi10 - D. Lazzati11 - E. Mason10 - P. Mazzali12 - L. Stella4
1 - INAF, Osservatorio Astrofisico di Arcetri, largo E. Fermi 5, 50125 Firenze, Italy
2 - International School for Advanced Studies (SISSA/ISAS), via Beirut 2-4, 34016 Trieste, Italy
3 -
INAF, Osservatorio Astronomico di Padova, vicolo dell'Osservatorio 5, 35122 Padova, Italy
4 -
INAF, Osservatorio Astronomico di Roma, via Frascati 33, 00040 Monteporzio Catone (Roma), Italy
5 -
Carnegie Observatories, 813 Santa Barbara Street, Pasadena, California 91101, USA
6 -
INAF, Osservatorio Astronomico di Brera, via E. Bianchi 46, 23807 Merate (Lc), Italy
7 -
University of Milano-Bicocca, Department of Physics, Piazza delle Scienze 3, 20126 Milano, Italy
8 -
University of Roma "Tor Vergata'', Department of Physics, via della Ricerca Scientifica 1, 00133 Roma, Italy
9 -
INAF, Telescopio Nazionale Galileo, Roque de Los Muchachos, PO box 565, 38700 Santa Cruz de La Palma, Spain
10 -
ESO, Alonso de Cordova 3107, Casilla 19001, Vitacura, Santiago, Chile
11 -
Institute of Astrophysics, University of Cambridge, Madingley Road, CB3 0HA Cambridge, UK
12 -
INAF, Osservatorio Astronomico di Trieste, via Tiepolo 11, 34131 Trieste, Italy
Received 25 April 2003 / Accepted 9 June 2003
Abstract
We present photometric and spectroscopic observations of the
gamma-ray burst GRB 021211 obtained during the late stages of its
afterglow. The light curve shows a rebrightening occurring 25 days after the GRB. The analysis of a VLT spectrum obtained during
the bump (27 days after the GRB) reveals a suggestive resemblance with
the spectrum of the prototypical type-Ic SN 1994I, obtained
10 days past maximum light. Particularly we have measured a strong,
broad absorption feature at 3770 Å, which we have identified with Ca II blueshifted by
14 400 km s-1, thus indicating that a
supernova (SN) component is indeed powering the "bump'' in the afterglow
decay. Assuming SN 1994I as a template, the spectroscopic and
photometric data together indicate that the SN and GRB explosions were
at most separated by a few days. Our results suggest that GRBs might be
associated also to standard type-Ic supernovae.
Key words: gamma rays: bursts - supernovae
There is growing evidence that long-duration GRBs (i.e. those lasting
more than 2 s; e.g. Fishman et al. 1994) are associated
with the death of massive stars. The most compelling case for the
existence of a SN-GRB connection is represented by the spatial and
temporal coincidence between GRB 980425 and SN 1998bw (Galama et al. 1998). Very recently, in the spectrum of the nearby (
z =
0.1687) GRB 030329, Stanek et al. (2003) found supernova
features, emerging out of the afterglow spectrum and resembling those of SN 1998bw (Patat et al. 2001). Several other possible SN-GRB
associations have been suggested (e.g. Wang & Wheeler 1998;
Woosley et al. 1998; Germany et al. 2000; Terlevich et al. 1999; Rigon et al. 2003), although none really
compelling due to the poor spatial and temporal coincidences.
The remaining evidence for the existence of a GRB-SN connection relies
upon the detection of a rebrightening in the afterglow light curves, 20-30 days after the GRB (e.g. Bloom et al. 1999,
2002; Lazzati et al. 2001). These "bumps'' have been
interpreted as signatures of SNe at maximum, emerging out of the
decaying afterglows. However this evidence and, consequently, the
interpretation, are based only on a few photometric measurements in the
afterglow light curves and on the assumption that the evolution of the
underlying SN is similar to SN 1998bw, except for a luminosity
rescaling factor
(see e.g. Price et al. 2003). Alternative explanations, such as
dust echoes (Esin & Blandford 2000), thermal re-emission of the
afterglow light (Waxman & Draine 2000), or thermal radiation
from a preexisting SN remnant (Dermer 2003) are not yet ruled
out. Indirect evidence that at least some long-duration GRBs are
associated with the death of massive stars is provided by the detection
of star-formation features in the host galaxies (e.g. Djorgovski et al. 1998). Emission and absorption features observed in X-ray
spectra (e.g. Piro et al. 2000) are also indicative of large
amounts of metals in the GRB surroundings, which can be provided by SN explosions. Finally, the afterglow spectra of GRB 021004 showed
absorption systems at different velocities, suggesting the presence of
rapidly-moving pre-ejected material surrounding the explosion site
(e.g. Møller et al. 2003).
Start UT | Exp. time | Seeing | R magnitude |
2003 Jan. 9.7* | 63 min | 1.1
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2003 Jan. 15.33 | 15 min | 0.8
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2003 Feb. 28.02 | 75 min | 0.8
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2003 Mar. 9.01 | 50 min | 1.25
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GRB 021211 was detected on 2002 Dec. 12 by the HETE-2 satellite
at 11:18:34 UT (Crew et al. 2002). The -ray fluence was
erg cm-2 in the (7-30) keV band and
erg cm-2 in the
(30-400) keV band (Crew et al. 2003). The GRB was therefore
classified as X-ray rich. Given the redshift z = 1.006 of this event
(Vreeswijk et al. 2002), the inferred (isotropic) energy was
erg, at the low end of the
energy distribution of GRBs (Frail et al. 2001). Owing to the
rapid distribution of coordinates, an optical afterglow was rapidly
discovered by Fox & Price (2002), just 20 min after the GRB
onset, as a pointlike source with magnitude
at
coordinates
,
(J2000; Fox et al. 2003). Moreover, the automatic telescopes RAPTOR (Wozniak et al. 2002), KAIT (Li et al. 2003), and Super-LOTIS (Park
et al. 2002), imaged the error box a few minutes after the
GRB. These observations allowed to monitor the early lightcurve of the
afterglow, which could be described by a broken powerlaw with a
flattening at
min (Li et al. 2003).
The striking feature of the optical afterglow of GRB 021211 was however
its extreme faintness. Compared to other events at similar epochs and
redshifts, this afterglow was dimmer by
3 mag in the
R-band (see e.g. Fox et al. 2003).
This could in principle be due to heavy extinction within the
host. However, Fox et al. (2003) report a broad-band color B-K
= 3.9 (on Dec. 11.6 UT), well within the range of GRB afterglows
(Simon et al. 2001). This indicates that GRB 021211 suffered
negligible extinction. Moreover, this burst was also underluminous in
all observed wavebands: only upper limits were reported in the radio
(Fox et al. 2003; Rol & Strom 2002), submillimeter (Fox
et al. 2003; Hoge et al. 2002), and TeV (McEnery
2002) regions. Unfortunately, no follow-up X-ray observations
were performed.
The intrinsic faintness of the optical afterglow made this event a good
candidate for showing a prominent late-time bump.
![]() |
Figure 1: Light curve of the afterglow of GRB 021211. Filled circles represent data from published or submitted works (Fox et al. 2003; Li et al. 2003; Pandey et al. 2003), open circles are converted from HST measurements (Fruchter et al. 2002), while filled diamonds indicate our data; the arrow shows the epoch of our spectroscopic measurement. The dotted and dot-dashed lines represent the afterglow (see text) and host contribution respectively. The dashed line shows the light curve of SN 1994I reported at z = 1.006 and dereddened with AV = 2 (from Lee et al. 1995). The solid line shows the sum of the three contributions. |
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Figure 2: Rest-frame spectrum of the afterglow of GRB 021211 on 2003 Jan. 8.27 UT, or 27 days after the GRB (thick lines), compared with that of several SNe (thin lines). |
Late-time observations were secured at the ESO VLT-UT4 (Yepun) equipped with the FORS 2 instrument, in the R band, during the period January-March 2003 (see Table 1).
The conversion to absolute flux was obtained by using both standard
calibration and a secondary sequence calibrated, on Feb. 28, with a Landolt
standard field (SA98), to account for the observations
obtained under non-photometric conditions. Aperture photometry was
executed with the packages apphot and photcal within
IRAF, by choosing aperture radii from 0.5
to 3
,
then
correcting to infinity with the values found for the standards and
using the DAOGROW algorithm. The measurements on the various
apertures for the secondary calibrators were found very stable, and we
decided to adopt for the target the innermost aperture magnitude,
corrected for the aperture.
Our results are listed in Table 1 and supersede our
preliminary report (Testa et al. 2003). They have been
complemented with a compilation of observations collected from
literature and plotted in Fig. 1. A rebrightening is clearly
seen, starting 15 days after the burst (Fruchter et al. 2002) and reaching the maximum,
,
during the
first week of January. The contribution of the host galaxy, estimated
from our late-epoch images, is
.
Therefore, the
intrinsic magnitude of the bump was
.
The afterglow contribution is more uncertain. The early-time light curve
presents several fluctuations, and cannot be easily extrapolated to
later epochs. In particular, fitting all data up to 1 day after the GRB with a (convex) broken powerlaw, as used by Li et al. (2003), yields an unacceptable
.
We
suggest two possible alternatives. First, the shape of the lightcurve is
consistent with the presence of two or three rebrightenings underlying a
powerlaw component, similarly to what observed in GRB 021004 (Lazzati
et al. 2002; Nakar et al. 2003). Alternatively, a second
break in the light curve could be present about 10 hours after the GRB. This may be the consequence of the passage of the synchrotron
cooling frequency across the optical band (the jet break is expected to
occur much later for such a low energy event, according to the
correlation of Frail et al. 2001). A fit with a double broken
powerlaw (i.e. with two breaks, see Fig. 1) yields
;
the improvement is highly significant (F-test chance
probability less than 10-6). We note that, whichever extrapolation
is used, the contribution of the afterglow to the flux measured at the
epoch at which our spectrum (the arrow in Fig. 1) was
obtained, is negligible (less then 5% in the most conservative
case). This fact strongly supports that the bump was powered by a
different component other than the afterglow.
We obtained a spectrum of the afterglow + host with FORS 2, on
Jan. 8.27 UT (27 days after the GRB), during the rebrightening phase
shown in Fig. 1. The original spectrum covered the range of
wavelengths
(6000-11 000) Å, although only the interval
(6000-9000) Å afforded an acceptable S/N (3). The resolution
was about 19 Å, and the integration time was
h. The slit
was rotated in such a way to include also the nearby galaxy reported by
Caldwell et al. (2002); this object was well detected and is
clearly separated from our target (the seeing in the 4 exposures was
). The extraction of the spectrum was performed
within the MIDAS and IRAF environments, independently by three of us
(S.B., M.H., and M.D.V.). We clearly detected the emission line at 7472.9 Å already found by Vreeswijk et al.
(2002). Interpreting this as [O II] 3727 Å in the rest
frame of the host galaxy, this corresponds to a redshift z =
1.006. Following this idea, we could also detect, albeit at lower
significance, emission lines at 9720 Å, 9955 Å, and 10 025 Å, which
we intepret as H
and [O III] 4959 Å and 5007 Å. Our
spectrum, shown in the rest-frame of the GRB (thick lines in
Fig. 2) was smoothed with a boxcar filter (55 Å width)
and cleaned from the emission line [O II]. The spectrum of the
afterglow is characterized by broad low-amplitude undulations blueward
and redward of a broad absorption, the minimum of which is measured at
3770 Å (in the rest frame of the GRB), whereas its blue wing
extends up to
3650 Å. We then compared our spectrum with those
of SNe arranged in different spectroscopic types and obtained at
different epochs (Fig. 2, thin lines). The comparison
includes the type-Ia SN 1991bg (Filippenko et al. 1992; Turatto
et al. 1996), the type-II SN 1999em (Hamuy et al. 2001),
the type-Ib SN 1984L (Harkness et al. 1987), the peculiar
type-Ic SN 1998bw (Galama et al. 1998; Patat et al. 2001), and the type-Ic SN 1994I (Filippenko et al. 1995). Both SN 1999em and SN 1998bw provide a poor match to
the afterglow spectrum. Some similarity can be found with the type-Ia
SN 1991bg and the type-Ib SN 1984L. A more convincing resemblance is
found with the spectrum of the type-Ic SN 1994I, obtained 9 days after
its B-band maximum (Filippenko et al. 1995). The comparison
with SN 1994I (and to some extent also with SN 1991bg and SN 1984L)
strongly supports the identification of the broad absorption with Ca II H+K; the blueshifts corresponding to the minimum of the absorption and
to the edge of the blue wing imply velocities of
km s-1and
km s-1 respectively. In principle the Ca II from the
host galaxy could contaminate our spectrum. However, since the typical
FWHM of absorption (and emission) lines of galaxies is of the order of 10-15 Å (corresponding to less than 1000 km s-1), and the FWHM
of the observed absorption is about 150 Å, one concludes that the Ca II of the host galaxy might affect the observed feature only
marginally, if at all.
![]() |
Figure 3: Comparison of the spectrum of the GRB bump to the ones of SN 1994I taken at different times. Each plot has a different AV, in order to better match our spectrum (we adopted the extinction law by Cardelli et al. 1989). For reference, SN 1994I reached its B-band maximum on 1994 Apr. 9. |
Using SN 1994I as a template, our photometric and spectroscopic data allow us to estimate the time at which the SN exploded, and to compare it with the GRB onset time.
Spectroscopy. In order to further study the spectrum of the SN
associated with the bump, we have used as a reference (see
Fig. 3) the spectral evolution of SN 1994I (Filippenko et al. 1995). To find the best match, different reddenings in the
range
(Richmond et al. 1996) were applied to
each spectrum. The epochs before maximum light (April 9) seem to be
excluded by the morphology of Ca feature, which is broader and located
at shorter wavelengths than in the GRB (the correctness of the
wavelenght axis was checked by measuring the position of the NaD interstellar absorption in each spectrum). Spectra later than Jun. 1 show
a very weak Ca feature and exhibit a poor match with the afterglow
spectrum in the (
3200-3700) Å region. Therefore the match with
the spectra is acceptable over the range
Apr. 9 to
May 31 (
0 to 40 days after SN maximum light).
Since our spectrum was obtained on Jan. 8, we estimate that the maximum
of the SN should have occurred between 2002 Oct. 2 and 2003 Jan. 8 (since
the source was at z = 1). The exact epoch when the SN exploded depends
crucially on the rise time (the time interval from the epoch of the
explosion up to maximum light) of type-Ic SNe. The best documented
cases are SN 1998bw and SN 1999ex. The latter (Stritzinger et al. 2002) reached B-band maximum 18 days after the
explosion, the former after
16 days (Galama et al. 1998). SN 1994I had a faster rise, reaching its maximum (in B) only 12 days after the explosion (Iwamoto et al. 1994). Adopting the latter value, we conclude that the SN exploded between
Sept. 11 and Dec. 15, the later epochs being
favored.
Photometry. In Fig. 1 we have superimposed to the light
curve of the afterglow decay the light curve of SN 1994I (Lee et al. 1995), reported at z = 1.006 and
dereddened by AV = 2 mag (Richmond et al. 1996). The
K-correction has been computed from U-band data, considering that,
at z = 1.006, the U-band roughly corresponds to the observed
R-band. The plot (solid line) shows that the luminosity at maximum of
SN 1994I (
assuming AV = 2; see Table 10 of
Richmond et al. 1996) agrees very well with that of the bump
(
).
In the figure, a null time delay between the GRB and the SN explosion
was used. Letting this delay free to vary did not significantly improve
the fit (F-test chance probability of 36%); the best fit time delay
is
comoving days.
Evidently the photometric observations provide a tighter constraint on the SN-GRB delay. However the uncertainties above are only statistical, while systematics are more difficult to evaluate, especially in consideration of the paucity of observation of type-Ic SNe in their rising phase. Yet, the combination of our photometric and spectroscopic data provide evidence that the SN and the GRB explosions occurred within days from one another, at the most.
The detection of a broad (
Å) absorption feature, in
the spectrum of the "bump'', which we have identified with the Ca II H+K doublet (blueshifted by
15 000 km s-1) suggests that the
rebrightening of the GRB 021211 afterglow was powered by a SN. Assuming
for this SN a spectroscopic and photometric behavior similar to that of SN 1994I, our data indicate that the SN and GRB explosion may have
occurred almost simultaneuosly, or at most separated by a few days. The
temporal coincidence between the SN and GRB 021211 holds for "short''
rise times, of the order of 10-12 days (as observed for SN 1994I;
Iwamoto et al. 1994).
On the other hand, if a longer rise time (16-20 days, such as that
observed in SN 1998bw or SN 1999ex) were used, the conclusion would be
that the SN went off several days before GRB 021211.
It is interesting to note that SN 1994I, the spectrum of which provides the best match to that observed in GRB 021211, is a typical type-Ic event rather than an exceptional 1998bw-like object, as the one proposed for association with GRB 980425 and GRB 030329 (Galama et al. 1998; Stanek et al. 2003). If the SN associated with GRB 021211 indeed shared the properties of SN 1994I, this would open the interesting possibility that GRBs may be associated with standard type-Ic SNe, and not only with the more powerful events known as "hypernovae''. This fact may have interesting consequences on the rate of GRB events. One caveat is that the recently studied SN 2002ap (Mazzali et al. 2002) shared some of the properties of hypernovae (e.g. a high expansion velocity), but was not significantly brighter than standard type-Ic SNe. Even if its pre-maximum spectra showed significantly broader lines than our case, this difference vanished after maximum, such that it may not be easy to distinguish between the two types of SNe. However, SN 2002ap had a broader light curve, and it was too faint in the U-band (Yoshii et al. 2003). It remains however not firmly estabilished whether GRB 021211 was associated with a standard type-Ic SN or with a "low-energy hypernova'' similar to SN 2002ap. We last note that even if GRBs are indeed mainly associated with standard type-Ic SNe, the discovery of overluminous type-Ic events (like SN 1998bw) associated with GRBs is observationally favored, since the SN component can emerge and be observed at early times, when the transient is more frequently monitored.
Acknowledgements
We thank Alexei Filippenko and Nando Patat for giving us the spectra of SN 1994I and SN 1998bw respectively, and the ESO directorate for accepting our DDT proposal. Mario Vietri, Peter Höflich and Lucia Ballo are acknowledged for useful discussion. We also thank the anonymous referee for her/his comments, which have improved the presentation of the data. We also appreciate the work of the observing staff at Paranal. We thank the Italian Collaboration for Optical Bursts (CIBO) for showing us preliminary photometric data.