A&A 482, 961-971 (2008)
DOI: 10.1051/0004-6361:20079317
P. Delorme1 - X. Delfosse1 - L. Albert2 - E. Artigau3 - T. Forveille1,4 - C. Reylé5 - F. Allard6 - D. Homeier7 - A. C. Robin5 - C. J. Willott8 - M. C. Liu4,
- T. J. Dupuy4
1 - Laboratoire d'Astrophysique de Grenoble,
Observatoire de Grenoble,
Université Joseph Fourier,
CNRS, UMR 5571
Grenoble,
France
2 -
Canada-France-Hawaii Telescope Corporation,
65-1238 Mamaloha Highway,
Kamuela, HI 96743,
USA
3 -
Gemini Observatory,
Southern Operations Center,
Association of Universities for Research in Astronomy, Inc.,
Casilla 603, La Serena, Chile
4 -
Institute for Astronomy,
2680 Woodlawn Drive, Honolulu,
HI 96822-1839, USA
5 -
Observatoire de Besançon,
Institut UTINAM, University of Franche-Comté,
CNRS-UMR 6213,
BP 1615, 25010 Besançon Cedex, France
6 -
Centre de Recherche Astrophysique de Lyon,
UMR 5574 CNRS, Université de Lyon,
École Normale Supérieure de Lyon,
46 allée d'Italie, 69364 Lyon Cedex 07, France
7 -
Institut für Astrophysik, Georg-August-Universität,
Friedrich-Hund-Platz 1, 37077 Göttingen, Germany
8 -
Physics Department, University of Ottawa,
150 Louis Pasteur, MacDonald Hall, Ottawa, ON K1N 6N5, Canada
Received 21 December 2007 / Accepted 5 March 2008
Abstract
Aims. We report the discovery of CFBDS J005910.90-011401.3 (hereafter CFBDS0059), the coolest brown dwarf identified to date.
Methods. We found CFBDS0059 using i' and z' images from the Canada-France-Hawaii Telescope (CFHT), and present optical and near-infrared photometry, Keck laser-guide-star adaptive optics imaging, and a complete near-infrared spectrum, from 1.0 to 2.2 m.
Results. A side-to-side comparison of the near-infrared spectra of CFBDS0059 and ULAS J003402.77-005206.7 (hereafter ULAS0034), previously the coolest known brown dwarf, indicates that CFBDS0059 is K cooler. We estimate a temperature of
K and gravity of
.
Evolutionary models translate these parameters into an age of 1-5 Gyr and a mass of 15-30
.
We estimate a photometric distance of
13 pc, which puts CFBDS0059 within easy reach of accurate parallax measurements. Its large proper motion suggests membership in the older population of the thin disk. The spectra of both CFBDS0059 and ULAS J0034 show probable absorption by a wide ammonia band on the blue side of the H-band flux peak. If, as we expect, that feature deepens further for still lower effective temperatures, its appearance will become a natural breakpoint for the transition between the T spectral class and the new Y spectral type. Together, CFBDS0059 and ULAS J0034 would then be the first Y0 dwarfs.
Key words: techniques: spectroscopic - surveys - stars: atmospheres - infrared: stars - stars: low-mass, brown dwarfs
Observed stellar and substellar atmospheres cover a continuum of physical
conditions from the hottest stars (100 000 K) to the coolest
known brown dwarfs (previously ULAS J003402.77-005206.7 (hereafter
ULAS0034), >T8
Warren et al. 2007). There
remains however a sizeable temperature gap between the 600-700 K
ULAS0034 and the
100 K giant planets of the Solar System. Many of the
currently known extrasolar planets populate this temperature interval,
characterized by complex atmospheric physics: matter and radiation in these
cold, dense, and turbulent atmospheres couple into a very dynamical mix,
where molecules and dust form and dissipate. Current atmosphere models are
rather uncertain in this unexplored temperature range and they will
significantly benefit from observational constraints.
Two major physical transitions are expected to occur between
700 K
and
400 K and strongly alter the emergent near-infrared
spectra (Burrows et al. 2003): NH3 becomes an abundant
atmospheric constituent and its near-infrared bands become
major spectral features, and water clouds form and deplete
H2O from the gas phase. The corresponding near-infrared
spectral changes are likely to be sufficiently drastic
that the creation of a new spectral type will be warranted
(Kirkpatrick 2000). Kirkpatrick et al. (1999); Kirkpatrick (2000)
reserved the ``Y'' letter for the name of that putative new spectral
type.
To help fill this temperature gap, we conduct the Canada France
Brown Dwarf Survey (CFBDS, Delorme et al. 2008), which uses
MegaCam (Boulade et al. 2003) i' and z' images to select very
cool brown dwarfs (and high redshift quasars) on their very red
i'-z' colour. We present here our coolest
brown dwarf discovery to date, CFBDS J005910.90-011401.3 (hereafter
CFBDS0059), a >T8 dwarf with evidence
of near-infrared NH3 absorption. Section 2 describes
its discovery, and presents our follow-up observations: i', z', Y, J,
H and
photometry and astrometry of CFBDS0059 and (as a reference)
ULAS0034, laser guide star adaptive optics imaging
and a near infrared spectrum of the new brown dwarf.
Section 3 discusses the kinematics and the dynamical population
membership of CFBDS0059. Section 4 compares the
spectrum of CFBDS0059 with those of Gl570D (T7.5), 2MASS J0415-09 (T8) and ULAS0034, and in the light of synthetic spectra
uses that comparison to determine its effective temperature, gravity
and metallicity. We also examine in that section the new spectral
features which appear below 700 K, in particular an NH3 band,
and discuss new spectral indices for spectral classification beyond T8. Finally, Sect. 5 summarizes our findings and sketches
our near-future plans.
Field ultracold brown dwarfs are intrinsically very faint, and
as a result they can only be identified in sensitive wide-field
imaging surveys. They are most easily
detected in the near infrared, and one could thus
naively expect them to be most easily identified in that wavelength
range. Brown dwarf spectra however very much differ from a black body, and
their considerable structure from deep absorption lines and bands
produces broad-band pure near-infrared colours that loop back
to the blue. At modest signal to noise ratios, those colours
are not very distinctive. Brown dwarfs are therefore more easily
recognized by including at least one photometric band under 1 m.
At those shorter wavelengths their spectra have extremely steep
spectral slopes, and the resulting very red i'-z' and z'-J
colours easily stand out.
As discussed in detail in Delorme et al. (2008), the CFBDS survey brown dwarf identification is a two-step process:
We first identified CFBDS0059 as a brown dwarf candidate when comparing a
360 s RCS2 z' exposure from 2005 December 27 with a 500 s CFBDS
i' exposure from 2006 August 31. CFBDS0059 is undetected in the
i' image to
(
), in spite of a strong
z' detection (
). The RCS2 survey obtains
contemporaneous g', r' and z' images, and we checked the g'
and r' exposures for a counterpart. These images, which
were obtained within 50 min of the z' observation,
show no object at the position of CFBDS0059. This essentially
excludes that the z' detection was due to a variable or slowly
moving object with neutral colours. The
(
)
lower limit was thus secure, and made CFBDS0059 a
very strong candidate for follow-up.
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Figure 1:
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Table 1:
Wide band
and
CFHT photometry
measured with Megacam, MKO-system Y, J, H, and
measured
with WIRCam and associated colours.
For comparison we include previous Y, J, H, and
K photometry of ULAS0034.
Our initial J-band imaging consists of five 20-s dithered
exposures with the SOFI near-infrared camera on the ESO NTT
telescope at La Silla on 2006 November 12. As discussed
below, the photometric system of that instrument is non-standard.
We used a modified
version of the jitter utility within the ESO Eclipse package
(Devillard 1997) to subtract the background and coadd the five
exposures. We extracted photometry from the resulting image using
PSF fitting within Source Extractor (Bertin & Arnouts (1996) and Bertin &
Delorme, in preparation) and obtain
.
The resulting
colour confirmed CFBDS0059 as a strong
very late-T dwarf candidate and we triggered H-band spectroscopic
observations with NIRI (Hodapp et al. 2003) at Gemini-North.
Those were obtained in queue mode on 2007 July 30 and immediately
confirmed the very cool nature of CFBDS0059. We then requested J and K-band spectroscopy with the same instrument, which
was obtained on 2007 September 1.
All spectra were obtained through a 0.7
-wide slit, which
produces a resolving power of
.
The object is dithered along the slit. The H-band spectrum is the sum
of 16 300-s integrations,
while the Y+J and K band spectra each are the sum of 9 300-s integrations.
Consecutive image pairs are pair subtracted, flat fielded using a
median combined spectral flat and corrected for both spectral and
spatial distortions. Spectra are extracted using a positive and a
negative extraction box matched to the trace profile. A first wavelength
calibration was obtained with argon lamp arc spectra taken at the end of
the sequence, and the wavelength scale was then fine tuned to match the
atmospheric OH-lines. Individual spectra extracted from image pairs
were then normalized and median combined into final spectra. Per-pixel S/N of 25, 40 and 5 where achieved on the J, H and K-band peaks
respectively.
For all 3 wavelength settings the A0 star HIP10512 was observed
immediately after the science observations to calibrate the
instrumental spectral response and the telluric transmission.
The J filter of the SOFI camera on the NTT has a quite non-standard
bandpass, for which the large colour corrections that result from
the strong structrure in T dwarf spectra (e.g. Stephens & Leggett 2004)
have not been fully characterized. To compare the
spectral energy distribution (SEDs) of CFBDS0059 and ULAS0034
(Warren et al. 2007) we therefore prefered to obtain additional
near-infrared wide-band photometry with WIRCam (Puget et al. 2004)
on CFHT, which uses standard Mauna Kea Observatory infrared filters
(Simons & Tokunaga 2002; Tokunaga & Vacca 2005; Tokunaga et al. 2002, MKOsystem). The observations
(2007 August 1st and 5th) used
dithering patterns of 60 arcsec amplitude for total (respectively
individual) exposure times of 300 (60), 150 (30), 300 (15) and 720 (20) seconds
for the Y, J, H and
bands. The skies were photometric and
the seeing varied between 0.8 and 1.0
.
Table 1 summarizes the magnitudes of CFBDS0059 and
ULAS0034 in all available bands. The WIRCam photometry
of ULAS0034 agrees with the Warren et al. (2007) measurements
within better than 1
for H band and within 1.5
for J.
The Warren et al. (2007) K-band measurement used a
K filter, while our WIRCam measurement uses the narrower
and bluer
filter. The 0.15 mag difference between these two
observations is approximately consistent with the
Stephens & Leggett (2004) prediction for the effect of these
different filter bandpasses at late-T spectral types.
Similarly, the better short-wavelength quantum efficiency
of the WIRCam detector can qualitatively explain the
0.2 mag (2
)
discrepancy between our
Y photometry and the Warren et al. (2007) WFCam measurement.
The near-IR colours of the two brown dwarfs are similar, except
which is
0.5 mag bluer for CFBDS0059 than for
ULAS0034. We will interpret the implications of this low
flux when
we examine the near-infrared spectrum.
CFBDS0059 and ULAS0034 are serendipitously just 6.3 degrees apart
on the sky, and at similar photometric distances from Earth since
they have similar spectral types and apparent magnitudes, and we
initially entertained the idea that they might, perhaps, be part of
a common moving group.
The proper motion of CFBDS0059 however, measured between our 2005
Megacam z' and 2007 WIRCam images, and uncorrected for its
parallactic motion, is
/yr,
/yr (Table 2).
ULAS0034 on the other hand moves by
/yr and
/yr (Warren et al. 2007).
The two proper motions are thus sufficiently different that the two
brown dwarfs are clearly unrelated. We checked for main sequence
common proper motion companions to CFBDS0059, which would have
provided welcome age and metallicity constraints (e.g. Scholz et al. 2003)
but did not find any match within a 10 arcmin radius.
Table 2: Astrometry of CFBDS0059 (Epoch: August 5th, 2007).
We obtained a series of dithered images, offsetting the telescope by a
few arcseconds, with a total integration time of 1080 s. We
used the filter, which has a central wavelength of
1.592
m and a width of 0.126
m. This filter is
positioned near the H-band flux peak emitted by late-T dwarfs.
The images were reduced in a standard fashion. We constructed flat
fields from the differences of images of the telescope dome interior
with and without continuum lamp illumination. Then we created a
master sky frame from the median average of the bias-subtracted,
flat-fielded images and subtracted it from the individual images.
Images were registered and stacked to form a final mosaic, with a
full-width at half-maximum of 0.09
and a Strehl ratio of 0.05.
No companions were clearly detected in a
region centred on CFBDS0059.
We determined upper limits from the direct imaging by first smoothing
the final mosaic with an analytical representation of the PSF's radial
profile, modeled as the sum of multiple gaussians. We then measured
the standard deviation in concentric annuli centred on the science
target, normalized by the peak flux of the targets, and adopted 10
as the flux ratio limits for any companions. These limits
were verified with implantation of fake companions into the image
using translated and scaled versions of the science target.
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Figure 2: Adaptive Optic detections limits as a function of the separation from CFBDS0059. Dashed lines show the equivalent mass and temperature for a given contrast. The first value assumes an age of 1 Gyr and the second an age of 5 Gyr. |
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Figure 2 presents the final upper limits on any companions. We
employed the ``COND'' models of Baraffe et al. (2003) to convert
the limits into companion masses, for assumed ages of 1 and 5 Gyr and
a photometric distance estimate of 13 pc. We assumed any cooler
companions would have similar
colours to
CFBDS0059.
We estimate a spectrophotometric distance for CFBDS0059 by adopting
,
based on an approximate T9/Y0 spectral type (discussed below)
and on an extrapolation of the MJ versus spectral type relation of
Knapp et al. (2004) beyond T8 (2MASSJ0415-0935, hereafter 2M0415).
This extrapolation is consistent with the Chabrier et al. (2000) models
which predict
between brown dwarfs of
K and 625 K (like 2M0415 and CFBDS0059).
The resulting
pc has significant systematic uncertainties,
because spectral typing beyond T8 is just being defined, and especially
because the linear 1 mag/subtype decline seen at earlier
subtypes may not continue beyond T8. The adaptive optics
observations exclude any companion of similar luminosity beyond 1.2 AU,
but CFBDS0059 could still of course be a tighter binary. Its small
distance fortunately puts CFBDS0059 within easy reach of
modern parallax measurements.
We use the Besancon stellar population model (Robin et al. 2003) to generate synthetic stars between 10 pc and 20 pc for the thin (dots) and thick (star symbol) disk populations at the galactic position of CFBDS0059. Figure 3 shows their proper motions together with those of CFBDS0059 and ULAS0034. The contour lines show the probability that an object with a given proper motion belongs to the thin disk rather than the thick disk (halo membership probabilities are negligible). CFBDS0059, at its probable distance, is well within the 95% probability thin disk membership region, and ULAS0034 is within the 99% probability region. In spite of its somewhat high proper motion for an object beyond 10 pc, CFBDS0059 therefore most likely belongs to the thin disk. The mean age of the simulated stars in the region of the proper motion diagram occupied by CFBDS0059 is 4 Gyr, suggesting that it is an older member of the thin disk. That age is consistent with the 1 to 5 Gyr range derived below from comparison to COND evolutionary models (Baraffe et al. 2003). As any kinematic age for an individual star, this determination has large error bars, but it suggests that CFBDS0059 might be older than ULAS0034.
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Figure 3: Thin disk probability membership contours in proper motion space from the Besancon stellar population model. The contours are generated for synthetic stars with distances between 10 and 20 pc, belonging to the thin disk (small dots) and the thick disk (small stars, with the density of the latter increased by a factor of 10 for display purposes). Less than one halo star would appear on the plot. Based on their measured proper motion, the likelihood that CFBDS0059 (large open square) and ULAS0034 (large open triangle) belongs to the thin disk are 95% and >99%. |
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Figures 4 and 5 present our
spectrum of CFBDS0059, together with those of ULAS0034
(Warren et al. 2007, >T8), 2M0415
(Burgasser et al. 2003, T8) and Gl570D (Burgasser et al. 2000, T7.5),
which successively were the coolest known brown dwarfs.
Thanks to their earlier discovery, 2M0415 and
Gl570D have the best characterized atmospheric parameters
(Saumon et al. 2007,2006), and they provide the most solid baseline
for a differential study. The Warren et al. (2007) spectrum of
ULAS0034, kindly communicated by Leggett, was obtained
with GNIRS on Gemini South and its
= 500
resolution matches that of our NIRI spectrum of CFBDS0059.
We downloaded the Burgasser et al. (2002,2003) OSIRIS spectra
of the two other brown dwarfs from the Ultracool Dwarf
Catalog
,
and degraded their original spectral resolution of
to match that of the
GNIRS and NIRI spectra. Stronger telluric absorption from
the lower altitude telescopes explains the wider blanked
regions in the corresponding spectra, but doesn't measurably
affect any comparison: as illustrated by CFBDS0059, late-T dwarfs
have essentially negligible flux wherever telluric H2O absorption
matters. Because the OSIRIS spectra do not cover the Y band, we complement them by lower resolution spectra from
Geballe et al. (2001) and Knapp et al. (2004) for
.
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Figure 4:
0.9-2.3 ![]() ![]() |
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Figure 5:
Y, J and H-bands
spectra of the four cool brown dwarfs. The green vertical lines in the
1.15-1.35 ![]() ![]() |
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Atmospheric parameters of ultracool dwarfs are ideally determined
from a combination of near and mid-IR information
(e.g. Saumon et al. 2007,2006), but low resolution near-infrared
spectra alone provide a useful proxy when mid-IR photometry and
spectra are not (yet) available (e.g. Leggett et al. 2007; Burgasser et al. 2006a).
Burgasser et al. (2006a) used a grid of solar metallicity cool brown dwarfs
to calibrate two spectral ratios, H2O-J and K/H, which respectively
measure the strength of H2O absorption at 1.15
m and
the flux ratio between the K and H peaks, to
and
.
Warren et al. (2007) however found that H2O-J essentially
saturates below
= 750 K, and therefore chose not to use this
spectral index for spectral types later than T8.
They demonstrate on the other hand that the combination
of the K/J index with the width of J-band peak, parametrised by
their WJ index, becomes a good
and
diagnostic
at
K, and remains useful significantly
below 750 K. We adopt their method.
Table 3 lists our measurement of these two indices
for CFBDS0059, and Fig. 6 compares them with the
Warren et al. (2007) measurements for 2M0415, HD3651B, Gl570D and
ULAS0034. To derive
and
from the indices
we use model indices from solar-abundance BT-settl atmospheric
models (Warren et al. 2007; Allard et al. 2003; Allard et al. 2008, in prep.).
The model with NH3 at chemical equilibrium abundance
clearly produces too much absorption in the blue side of the H-band,
confirming the finding of Saumon et al. (2007,2006) that
non-equilibrium processes keep the NH3 partial pressure well below
its equilibrium value. We then use models that keep the abundances of
NH3 and N2 at a fixed value in all parts of the atmosphere where the
reaction timescale exceeds the mixing
timescale, which typically occurs at the 600-800 K temperature level.
These ``quenched'' models agree much better with the observed band shape.
As a first
order correction for the remaining imperfections
of the theoretical spectra, the model indices are shifted into
agreement with the measurements of 2M0415 at the
(
K;
and [M/H] = 0) determined for
that brown dwarf by Saumon et al. (2007). The
K and
resulting from this calibration for Gl570D are
consistent with the
-820 K and
-5.25
derived by Saumon et al. (2006) from a complete spectral analysis.
For HD3651B (T7.5, Luhman et al. 2007),
-890 K and
-5.3 resulting from this calibration are roughly
consistent with the
-840 K and
-5.5
derived by Liu et al. (2007).
CFBDS0059 and ULAS0034 have very similar WJ indices,
but the new brown dwarf has a significatively smaller K/J index.
Visual comparison of the two spectra (Fig. 4)
confirms that CFBDS0059 does have a weaker K-band
peak than any of the 3 comparison cool brown dwarfs. As widely
discussed in the recent literature (e.g. Liu et al. 2007, Fig. 3 in
Burgasser et al. 2006a, or Fig. 3 in Leggett et al. 2007),
for a fixed metallicity a weaker K-band peak is evidence of
either a lower temperature or a higher gravity. The WJindex lifts this degeneracy: it indicates, again assuming
identical chemical compositions for the two brown dwarfs,
that CFBDS0059 is cooler by K and has a
higher
than ULAS0034.
As also discussed by Warren et al. (2007), the above uncertainties
only reflect the random errors in the spectral indices. They are
appropriate when comparing two very similar objects, like CFBDS0059
and ULAS0034, since systematic errors then cancel out. They must
on the other hand be increased to compute absolute effective
temperatures and gravity: one then needs to account for the
uncertainties on the 2M0415 parameters which anchor the
Fig. 6 grid (
K and
;
Saumon et al. 2007), and for the uncertainties in the atmospheric
models which may distort the grid between its anchor point
(
K;
and [M/H] = 0) and the
600 K
region of interest here. We conservatively adopt
K and
.
This 2-parameter analysis obviously cannot determine all three
main atmospheric parameters (
,
and metallicity).
As discussed by Warren et al. (2007), it actually determines the temperature
with no ambiguity but leaves a combination of
and
undetermined, and they demonstrated that in the WJ versus J/K plot
metallicity is degenerate with surface gravity, with
.
CFBDS0059 is thus definitely
cooler than ULAS0034, but from WJ versus J/K diagram it
can have either higher surface gravity or lower metallicity.
This degeneracy affects the full JHK-band spectrum, where any metallicity
vs. gravity difference is at most very subtle. It is however lifted by the
shape of the Y-band peak (Figs. 3 of Burgasser et al. 2006a or
Leggett et al. 2007), since lower metallicity shifts the Y-band flux
density peak of submetallic brown dwarfs significantly blueward.
Figure 5 shows no such shift, and the two objects
therefore have similar metallicities.
Table 3: Measured spectral classification indices for CFBDS0059 and ULAS 0034.
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Figure 6:
WJ versus J/K indices. The grid represents
indices measured on solar metallicity BT-settl model
spectra, shifted into agreement of the
(
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Figure 7 overlays the observed CFBDS0059 spectrum with the
synthetic spectrum for the closest point of the solar metallicity
atmospheric model grid. Except on the red side of the H-band,
model and observations agree well, boosting our confidence
in the derived atmospheric parameters.
The main remaining predictive shortcoming of the models is their overestimated
absorption on the red side of the H-band peak. The principal
opacity source in this region is the methane band centred at
,
for which comprehensive theoretical predictions
are available, but only for transitions from the vibrational
ground state (as will be discussed in detail in Homeier et al.,
in preparation). To make up for the missing absorption from higher
bands, which constitutes a significant fraction of the opacity at brown
dwarf temperatures, a constant empirical correction factor
was used. This correction must in turn lead to some overestimate
of the CH4 absorption as we reach the lower end of the T dwarf
temperature range. Another possible source of errors are uncertainties
in the models' temperature profile. The BT-Settl models
self-consistently describe gravitational settling, convective turbulence,
advection, condensation, coalescence and coagulation of condensates
to predict the formation and vertical extent of cloud layers
(Allard et al. 2003; Helling et al. 2007). In late T dwarfs these clouds are
predicted to reside deep in the optically thick part
of the atmosphere. Their opacity is thus not directly visible
in the spectrum, but it may still
impact the thermal structure, and thus the relative abundance especially of
temperature-sensitive species like CH4.
Another (less serious) disagreement between the models and the observed
spectra occurs in the Y band. The models overestimate the flux on
the blue side of the Y-peak, and they imperfectly reproduce the
general shape of the peak. As discussed below, the opacities in that
band are dominated by pressure-broadened wings of the 0.77
K I line on the blue side and CH4 on the red side.
For Baraffe et al. (2003) evolutionary models, the
-670 K and
-5.05
determined above translate into an age of 1-5 Gyr and a
mass of 15
(for 1 Gyr) to 30
(for 5 Gyr).
The kinematics of CFBDS0059 suggests that it belongs to
an older population, and therefore slightly favour a higher
mass and older age.
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Figure 7:
Overlay of the CFBDS0059 spectrum with the solar metallicity
(
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Direct comparison of the four spectra can be used to shed light on incipient new features and atmospheric chemistry. Features which are seen in both CFBDS0059 and ULAS0034 are likely to be real even when their significance is modest in each object, and those which are absent or weaker in the two hotter brown dwarfs, can reasonably be assigned to low temperature molecules. Conversely, features which disapear in the two cooler objects trace higher temperature species.
As discussed above, the Y-band spectra of CFBDS0059 and ULAS0034
do not differ much. Given the strong sensitivity of that band to [M/H] that implies that the two objects have similar chemical
compositions. The shape of the Y-band peaks of these two coolest
brown dwarfs on the other hand differ from that of 2M0415 and Gl570,
with the CFBDS0059 and ULAS0034 peaks extending further into the blue.
The dominant absorbers in the blue wings of the Y-band peak is
the pressure-broadened wing of the 0.77 m K I line (e.g. Burgasser et al. 2006a), which must weaken as K I depletes from the gas
phase under
K. As anticipated by
Leggett et al. (2007), the slope of the blue side of the Y-band
peak therefore shows good potential as an effective temperature
diagnostics beyond spectral type T8.
The strength of the J-band K I doublet is a good gravity estimator in
ultracool dwarfs (e.g. Knapp et al. 2004), because an increased
pressure at a fixed temperature favors KCl over K (Lodders 1999)
and consequently weakens atomic potassium features. At
-800 K the the J-band K I doublets remain
weakly visible and useful as a gravity proxy (Fig. 7 of Knapp et al. (2004)).
At
K on the other hand, the K I doublets have
completely vanished at the resolution of the current spectra
(Fig. 5), even at the probably lower gravity of
ULAS0034. Potassium is thus mostly converted to KCl (or perhaps
other compounds) in the relevant photospheric layers.
The strongest new feature is wide absorption on the blue side of the
H-band, at
.
It is conspicuous
in CFBDS0059 and well detected in ULAS0034, and with hindsight
is weakly visible in the 2M0415 spectrum
(Fig. 5). It is however clearly stronger
at
K. To visually emphasize this broad
feature, we bin the spectra to
and overlay the four
H-band spectra (Fig. 8, left panel). Absorption
sets in at
and becomes deeper for
.
These wavelengths overlap
with strong H2O and NH3 bands. Either molecule
could a priori be responsible for the absorption.
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Figure 8:
Left: H-band spectrum of the four cool brown dwarfs binned
to
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Those molecules unfortunately
have imperfect opacity data, and the NH3 laboratory line lists in
particular are incomplete below m. Computed ammonia
opacities are therefore strictly lower limits. Leggett et al. (2007)
compare synthetic spectra computed with and
without NH3 opacity, using the Irwin et al. (1999) line list for
m, and find that ammonia absorption in cold brown
dwarfs strongly depletes the blue wing of the H band (their
Fig. 10). Similarly, Fig. 9 of Saumon et al. (2000) plots synthetic H-band
spectra with and without NH3 opacity, and find differences in two
wavelength ranges: the NH3-rich model is significantly more absorbed
for
m and it has weaker but significant absorption
in the
range.
Figure 8 right panel plots two BT-Settl
models for (
K;
), without any
near-infrared NH3 opacity, and with NH3 opacity for that
molecule at its chemical equilibrium abundance. As discussed
above the BT-Settl models do not reproduce the observed
H-peak shape very well, and a quantitative comparison is thus
difficult. The comparison of the two models nonetheless confirms
the Saumon et al. (2000) conclusion that ammonia produces strong
absorption below
m and weaker residual out to
1.595
m. These model predictions qualitatively match the behaviour seen
in Fig. 8, left panel.
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Figure 9: Flux ratio between CFBDS0059 and Gl570D (black), together with the laboratory room temperature transmission spectrum of NH3 (Irwin et al. 1999) (red, top panel) and the 600 K H2O transmission spectrum computed from the HITRAN molecular database (red, bottom panel). The grey bands mark the parts of the spectrum affected by strong (dark grey) or moderate (light grey) CH4 absorption. |
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Figure 10: Flux ratio between ULAS0034 and Gl 570D (black). The overlays repeat those of Fig. 9. |
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To emphasize the changes in brown dwarfs spectra when their
effective temperature decreases from 800 to
600 K, we
plot in Fig. 9 the ratio of the spectra of CFBDS0059 and
Gl570D. The signal to noise ratio of the resulting K-band spectrum
is too low for detailed analysis, and we therefore focus on the Y, J and
H flux peaks. To avoid confusion from changes in
the temperature-sensitive methane bands, we also mostly ignore
the parts of the spectrum affected by CH4 absorption bands, hatched
in dark and light grey for respectively stronger and weaker
bands. Figure 10 shows the equivalent plot for ULAS0034,
which is very similar.
The H-band spectrum ratio prominently shows the new absorption band,
which outside the CH4 band closely matches the 300 K NH3
transmission spectrum of Irwin et al. (1999). Both spectra are
strongly absorbed between 1.49 and 1.52 m and rebound
from 1.52 to 1.57
m. Water absorption, by contrast, is a
poor match to the features of spectrum ratio. The strongest
water absorption (as computed from the HITRAN molecular
database for a 600 K temperature) occurs below 1.49
m,
at significantly bluer wavelengths than the CFBDS0059
absorption feature.
Some weaker but still significant bands of the Irwin et al. (1999)
laboratory ammonia spectrum occur in the J band. Those again match
features of the CFBDS0059/Gl570D flux ratio, but that agreement is much
less conclusive: water and ammonia absorptions overlap on the red side
J-band peak, and CH4 absorption affects the blue side of the
peak. A 1.25-1.27 m feature is seen on both flux
ratios and on the ammonia transmission, and could be
due to ammonia since it is clear of any strong H2O absorption band. The slight wavelength shift between
the laboratory and observed features however leaves
that association uncertain.
Detailed synthetic spectra based on fully reliable opacities will
be needed to decide whether NH3 absorption matters in the
J band at the effective temperature of CFBDS0059.
The main pattern in the Y-band is a blue slope, which reflects
the weaker pressure-broadened K I wing in the cooler brown dwarf.
The weak 1.03
m NH3 band is not seen.
Ammonia is easily detected in mid-infrared SPITZER spectra
for all spectral types cooler than T2 (Cushing et al. 2006; Roellig et al. 2004),
though significantly weaker than initially expected because mixing from
lower atmospheric levels
reduces its abundance in the high atmosphere below the local equilibrium
value (Saumon et al. 2006).
Weak near-infrared absorption by ammonia has been tentatively
detected by Saumon et al. (2000) in the T7p dwarfs Gl 229B, but
CFBDS0059 and ULAS0034 provide the first incontrovertible
evidence of a strong near-infrared NH3 band in brown
dwarf spectra.
This conclusion contrasts with Warren et al. (2007) finding
possible but inconclusive evidence of ammonia in ULAS0034.
The main difference between the two analyses is that
Warren et al. (2007) focused on a higher resolution search,
at a necessarily lower signal to noise ratio, for individual
NH3 lines between 1.5 and 1.58 m.
We instead looked for the global signature of the absorption
band, which only becomes obvious when looking at the full
H-band spectrum.
Table 3 lists for CFBDS0059 the spectral indices used by the spectral classification scheme of Burgasser et al. (2006b), which refines the previous schemes of Geballe et al. (2002) and Burgasser et al. (2002). These indices would imply a T8 classification, identical to that of 2M0415. As discussed above however, the near-infrared spectrum of CFBDS0059 demonstrates that it is over 100 K cooler than 2M0415 and shows clearly different spectral features. Based on the new indices we present later, CFBDS0059 should be assigned a later spectral type. The almost identical Burgasser et al. (2006b) indices of the two brown dwarfs instead reflect those indices measuring H2O and CH4 absorption bands which saturate and lose their effective temperature sensitivity at the T8 spectral type of 2M0415. Beyond T8 the Burgasser et al. (2006b) classification scheme therefore needs to be extended, with new spectral indicators that do not saturate until significantly later spectral types.
Fully defining this extension is beyond the scope of the present paper,
since two known objects beyond T8 are not enough to explore spectral
variability, but one can nonetheless start exploring. Since the main
new feature is NH3 absorption in the blue wings of the H-band
peak, we define a new NH3-H index as
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(1) |
Table 4: NH3-H indices for the five brown dwarfs discussed in this paper.
Over the limited effective temperature range spanned by Gl570D, HD3651B, 2M0415, ULAS0034 and CFBDS0059, and as far as one can infer from just 5 examples, the NH3-H and WJ indices correlate strongly (Fig. 11). The numerator of WJ is centred at wavelengths where both ammonia (Fig. 10 of Leggett et al. 2007) and CH4 have significant opacity, and future modeling work should be able to establish whether the two indices probe the same molecule or not. Since the near-infrared spectra of ULAS0034 and CFBDS0059 differ significantly more from that of the T8 2M0415 than the latter differs from the T7.5 Gl570D (as quantitatively demonstrated by Fig. 11), it is natural to assign a full spectral subtype to the interval between the two coolest brown dwarfs and 2M0415. By that reasoning, and if ULAS0034 and CFBDS0059 are considered as T dwarfs, their spectral type should be T9, or perhaps slightly later.
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Figure 11:
NH3-H index versus WJ index. The error bars represent
the 1![]() |
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The T spectral class however is quite unlikely to remain the last
spectral type, since for sufficiently low effective temperatures
atmospheric models predict major changes in visible and
near-infrared brown dwarf spectra: NH3 bands are predicted
to appear in, and eventually to dominate, the near-infrared
spectrum, the strong pressure-broadened optical lines of Na I
and K I are predicted to disappear as those atomic species get
incorporated into molecules and solids, and water clouds
are predicted to form and to largely deplete water from the gas
phase (Kirkpatrick 2005; Burrows et al. 2003).
Since spectral classification, for mostly practical reasons, is
traditionally based on optical and near-infrared spectra,
such a major transition will justify the introduction of
a new spectral type, for which the Y letter has long been
reserved (Kirkpatrick et al. 1999; Kirkpatrick 2000). If the
m NH3 band
keeps deepening as the effective temperature decreases further,
and eventually becomes a major spectral feature,
its appearance at
K will become a natural
transition between the T and Y spectral classes. ULAS0034
and CFBDS0059 would then be the first Y dwarfs, and the prototypes
for Y0 brown dwarfs, rather than T9. That decision will to some
extent remain a matter of convention, but it must in any case wait
until larger numbers of similarly cool brown dwarfs can
document spectral trends in finer detail, and preferably
over a wider effective temperature range.
We have reported the discovery of CFBDS0059, a very cool brown
dwarf, discovered in the CFBDS survey (Delorme et al. 2008).
Its effective temperature is K cooler than that of
ULAS0034, most likely making it the coolest brown dwarf known at the present
time. High spatial resolution imaging establishes than CFBDS0059
has no similarly bright companion beyond 0.09
,
and no companion
with a contrast under 3.5 mag beyond 0.3
(respectively 1.2 and 3.9 AU at the 13 pc photometric distance). Its kinematics
suggest, with significant error bars, a
4 Gyr age at which
CFBDS0059 would be a
30
brown dwarf. The atmospheric
parameters of CFBDS0059 however are compatible with any age from
5 Gyr down to 1 Gyr, for which its mass would be
15
.
A trigonometric parallax measurement together with mid-infrared
photometry and spectroscopy with SPITZER will significantly
refine its physical parameters, as demonstrated by
Saumon et al. (2007) for slightly warmer brown dwarfs.
We assign absorption in the blue wing of the H-band peaks of both ULAS 0034 and CFBDS 0059 to an NH3 band. If that assignment is confirmed, and if, as we expect, the band deepens at still lower effective temperatures, its development would naturally define the scale of the proposed Y spectral class. ULAS 0034 and CFBDS 0059 would then become the prototypes of the Y0 sub-class.
The CFBDS survey has to date identified two brown dwarfs later than T8, CFBDS0059 and ULAS0034 (which we identified independently of Warren et al. 2007; Delorme et al. 2008) in the analysis of approximately 40% of its final 1000 square degree coverage. We therefore expect to find another few similarly cool objects, and hopefully one significantly cooler one.
CFBDS0059 and ULAS0034 provide a peek into the atmospheric physics for
conditions that start approaching those in giant planets, and the
future discoveries that can be expected from CFBDS, ULAS, and
Pan-STARRS will further close the remaining gap. They also
bring into a sharper light the remaining imperfections of
the atmopsheric models, and emphasize in particular the
importance of more complete opacity data. Our analysis
relies on a room temperature absorption NH3 spectrum,
but higher excitation bands than can be excited at 300 K
must matter in
= 600 K brown dwarfs. The eventual
identification of ammonia absorption in the J band will
also need complete opacity information for H2O
and CH4 and full spectral synthesis, since the bands of
the three molecules overlap in that spectral range.
The spectral indices that define the T dwarf spectral class saturate below 700 K, which means that new ones will be needed at lower effective temperatures. We introduce one here, NH3-H, which measures the likely NH3 absorption in the H band. Together with the WJ index of Warren et al. (2007) and the slope of the blue side of the Y-band peak (Leggett et al. 2007), it will hopefully define a good effective temperature sequence. Metallicity and gravity diagnostics are less immediately apparent, but will need to be identified as well.
Acknowledgements
We are grateful to our referee, Sandy Leggett, for her very detailed report and numerous suggestions which significantly improved this paper. We would like to thank the observers and queue coordinators who carried out our service observations at CFHT (programs 05BC05, 06AC20, 07BD97) and Gemini-North (GN-2007A-Q-201, GN-2007B-Q-3). We also thanks the NTT and Keck Observatory support astronomers for their help during the observations which led to these results. We thank S. Leggett and S Warren for providing their spectrum of ULAS0034 in a convenient numerical format, and Sandy Leggett for communicating spectra of 2M0415 and Gl 570D and the room temperature absorption spectrum of NH3. We would also like to thank David Ehrenreich for providing us the computed 600 K water absorption. Financial support from the ``Programme National de Physique Stellaire'' (PNPS) of CNRS/INSU, France, is gratefully acknowledged. MCL acknowledges support for this work from NSF grant AST-0507833 and an Alfred P. Sloan Research Fellowship.