203 research outputs found
Spectral Variability from the Patchy Atmospheres of T and Y Dwarfs
Brown dwarfs of a variety of spectral types have been observed to be
photometrically variable. Previous studies have focused on objects at the L/T
transition, where the iron and silicate clouds in L dwarfs break up or
dissipate. However, objects outside of this transitional effective temperature
regime also exhibit variability. Here, we present models for mid-late T dwarfs
and Y dwarfs. We present models that include patchy salt and sulfide clouds as
well as water clouds for the Y dwarfs. We find that for objects over 375 K,
patchy cloud opacity would generate the largest amplitude variability within
near-infrared spectral windows. For objects under 375 K, water clouds also
become important and generate larger amplitude variability in the mid-infrared.
We also present models in which we perturb the temperature structure at
different pressure levels of the atmosphere to simulate hot spots. These models
show the most variability in the absorption features between spectral windows.
The variability is strongest at wavelengths that probe pressure levels at which
the heating is the strongest. The most illustrative types of observations for
understanding the physical processes underlying brown dwarf variability are
simultaneous, multi-wavelength observations that probe both inside and outside
of molecular absorption features.Comment: 6 pages, 5 figures, Accepted for publication in ApJ Letter
Photolytic Hazes in the Atmosphere of 51 Eri b
We use a 1D model to address photochemistry and possible haze formation in
the irradiated warm Jupiter, 51 Eridani b. The intended focus was to be carbon,
but sulfur photochemistry turns out to be important. The case for organic
photochemical hazes is intriguing but falls short of being compelling. If
organic hazes form, they are likeliest to do so if vertical mixing in 51 Eri b
is weaker than in Jupiter, and they would be found below the altitudes where
methane and water are photolyzed. The more novel result is that photochemistry
turns HS into elemental sulfur, here treated as S. In the cooler
models, S is predicted to condense in optically thick clouds of solid
sulfur particles, whilst in the warmer models S remains a vapor along with
several other sulfur allotropes that are both visually striking and potentially
observable. For 51 Eri b, the division between models with and without
condensed sulfur is at an effective temperature of 700 K, which is within error
its actual effective temperature; the local temperature where sulfur condenses
is between 280 and 320 K. The sulfur photochemistry we have discussed is quite
general and ought to be found in a wide variety of worlds over a broad
temperature range, both colder and hotter than the 650-750 K range studied
here, and we show that products of sulfur photochemistry will be nearly as
abundant on planets where the UV irradiation is orders of magnitude weaker than
it is on 51 Eri b.Comment: 24 pages including 11 figures and a tabl
Detecting Water In the atmosphere of HR 8799 c with L-band High Dispersion Spectroscopy Aided By Adaptive Optics
High dispersion spectroscopy of brown dwarfs and exoplanets enables exciting
science cases, e.g., mapping surface inhomogeneity and measuring spin rate.
Here, we present band observations of HR 8799 c using Keck NIRSPEC
(R=15,000) in adaptive optics (AO) mode (NIRSPAO). We search for molecular
species (HO and CH) in the atmosphere of HR 8799 c with a template
matching method, which involves cross correlation between reduced spectrum and
a template spectrum. We detect HO but not CH, which suggests
disequilibrium chemistry in the atmosphere of HR 8799 c, and this is consistent
with previous findings. We conduct planet signal injection simulations to
estimate the sensitivity of our AO-aided high dispersion spectroscopy
observations. We conclude that contrast can be reached in band.
The sensitivity is mainly limited by the accuracy of line list used in modeling
spectra and detector noise. The latter will be alleviated by the NIRSPEC
upgrade.Comment: 14 pages, 5 figures, 5 tables, accepted for publication on AJ,
references update
A Comparison of Near-Infrared Photometry and Spectra for Y Dwarfs with a New Generation of Cool Cloudy Models
We present YJHK photometry, or a subset, for the six Y dwarfs discovered in
WISE data by Cushing et al.. The data were obtained using NIRI on the Gemini
North telescope. We also present a far-red spectrum obtained using GMOS-North
for WISEPC J205628.90+145953.3. We compare the data to Morley et al. (2012)
models, which include cloud decks of sulfide and chloride condensates. We find
that the models with these previously neglected clouds can reproduce the energy
distributions of T9 to Y0 dwarfs quite well, other than near 5um where the
models are too bright. This is thought to be because the models do not include
departures from chemical equilibrium caused by vertical mixing, which would
enhance the abundance of CO, decreasing the flux at 5um. Vertical mixing also
decreases the abundance of NH_3, which would otherwise have strong absorption
features at 1.03um and 1.52um that are not seen in the Y0 WISEPC
J205628.90+145953.3. We find that the five Y0 to Y0.5 dwarfs have 300 < T_eff K
< 450, 4.0 < log g < 4.5 and f_sed ~ 3. These temperatures and gravities imply
a mass range of 5 - 15 M_Jupiter and ages around 5 Gyr. We suggest that WISEP
J182831.08+265037.8 is a binary system, as this better explains its luminosity
and color. We find that the data can be made consistent with observed trends,
and generally consistent with the models, if the system is composed of a T_eff
= 325 K and log g ~ 4.0
secondary, corresponding to masses of 10 and 7 M_Jupiter and an age around 2
Gyr. If our deconvolution is correct, then the T_eff = 300 K cloud-free model
fluxes at K and W2 are too faint by 0.5 - 1.0 magnitudes. We will address this
discrepancy in our next generation of models, which will incorporate water
clouds and mixing.Comment: 39 pages, 10 Figures, 8 Tables. Accepted by ApJ. This revision
replaces Figures 9 and 10 with B & W versions, corrects figure captions for
color online only, corrects references. Text is unchanged. Tables 3, 4 and 8
are available at http://www.gemini.edu/staff/sleggett, other model data are
available at http://www.ucolick.org/~cmorley/cmorley/Data.htm
Water Clouds in Y Dwarfs and Exoplanets
The formation of clouds affects brown dwarf and planetary atmospheres of
nearly all effective temperatures. Iron and silicate condense in L dwarf
atmospheres and dissipate at the L/T transition. Minor species such as sulfides
and salts condense in mid-late T dwarfs. For brown dwarfs below Teff=450 K,
water condenses in the upper atmosphere to form ice clouds. Currently over a
dozen objects in this temperature range have been discovered, and few previous
theoretical studies have addressed the effect of water clouds on brown dwarf or
exoplanetary spectra. Here we present a new grid of models that include the
effect of water cloud opacity. We find that they become optically thick in
objects below Teff=350-375 K. Unlike refractory cloud materials, water ice
particles are significantly non-gray absorbers; they predominantly scatter at
optical wavelengths through J band and absorb in the infrared with prominent
features, the strongest of which is at 2.8 microns. H2O, NH3, CH4, and H2 CIA
are dominant opacity sources; less abundant species such as may also be
detectable, including the alkalis, H2S, and PH3. PH3, which has been detected
in Jupiter, is expected to have a strong signature in the mid-infrared at 4.3
microns in Y dwarfs around Teff=450 K; if disequilibrium chemistry increases
the abundance of PH3, it may be detectable over a wider effective temperature
range than models predict. We show results incorporating disequilibrium
nitrogen and carbon chemistry and predict signatures of low gravity in
planetary- mass objects. Lastly, we make predictions for the observability of Y
dwarfs and planets with existing and future instruments including the James
Webb Space Telescope and Gemini Planet Imager.Comment: 23 pages, 20 figures, Revised for Ap
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