3,308 research outputs found
Modelling the local and global cloud formation on HD 189733b
Context. Observations suggest that exoplanets such as HD 189733b form clouds
in their atmospheres which have a strong feedback onto their thermodynamical
and chemical structure, and overall appearance. Aims. Inspired by mineral cloud
modelling efforts for Brown Dwarf atmospheres, we present the first spatially
varying kinetic cloud model structures for HD 189733b. Methods. We apply a
2-model approach using results from a 3D global radiation-hydrodynamic
simulation of the atmosphere as input for a detailed, kinetic cloud formation
model. Sampling the 3D global atmosphere structure with 1D trajectories allows
us to model the spatially varying cloud structure on HD 189733b. The resulting
cloud properties enable the calculation of the scattering and absorption
properties of the clouds. Results. We present local and global cloud structure
and property maps for HD 189733b. The calculated cloud properties show
variations in composition, size and number density of cloud particles which are
strongest between the dayside and nightside. Cloud particles are mainly
composed of a mix of materials with silicates being the main component. Cloud
properties, and hence the local gas composition, change dramatically where
temperature inversions occur locally. The cloud opacity is dominated by
absorption in the upper atmosphere and scattering at higher pressures in the
model. The calculated 8{\mu}m single scattering Albedo of the cloud particles
are consistent with Spitzer bright regions. The cloud particles scattering
properties suggest that they would sparkle/reflect a midnight blue colour at
optical wavelengths.Comment: Accepted for publication (A&A) - 21/05/2015 (Low Resolution Maps
Did Fomalhaut, HR 8799, and HL Tauri Form Planets via the Gravitational Instability? Placing Limits on the Required Disk Masses
Disk fragmentation resulting from the gravitational instability has been
proposed as an efficient mechanism for forming giant planets. We use the planet
Fomalhaut b, the triple-planetary system HR 8799, and the potential protoplanet
associated with HL Tau to test the viability of this mechanism. We choose the
above systems since they harbor planets with masses and orbital characteristics
favored by the fragmentation mechanism. We do not claim that these planets must
have formed as the result of fragmentation, rather the reverse: if planets can
form from disk fragmentation, then these systems are consistent with what we
should expect to see. We use the orbital characteristics of these recently
discovered planets, along with a new technique to more accurately determine the
disk cooling times, to place both lower and upper limits on the disk surface
density--and thus mass--required to form these objects by disk fragmentation.
Our cooling times are over an order of magnitude shorter than those of Rafikov
(2005),which makes disk fragmentation more feasible for these objects. We find
that the required mass interior to the planet's orbital radius is ~0.1 Msun for
Fomalhaut b, the protoplanet orbiting HL Tau, and the outermost planet of HR
8799. The two inner planets of HR 8799 probably could not have formed in situ
by disk fragmentation.Comment: 5 pages, 1 figure, accepted for publication in ApJ
A comparison of chemistry and dust cloud formation in ultracool dwarf model atmospheres
The atmospheres of substellar objects contain clouds of oxides, iron,
silicates, and other refractory condensates. Water clouds are expected in the
coolest objects. The opacity of these `dust' clouds strongly affects both the
atmospheric temperature-pressure profile and the emergent flux. Thus any
attempt to model the spectra of these atmospheres must incorporate a cloud
model. However the diversity of cloud models in atmospheric simulations is
large and it is not always clear how the underlying physics of the various
models compare. Likewise the observational consequences of different modeling
approaches can be masked by other model differences, making objective
comparisons challenging. In order to clarify the current state of the modeling
approaches, this paper compares five different cloud models in two sets of
tests. Test case 1 tests the dust cloud models for a prescribed L, L--T, and
T-dwarf atmospheric (temperature T, pressure p, convective velocity
vconv)-structures. Test case 2 compares complete model atmosphere results for
given (effective temperature Teff, surface gravity log g). All models agree on
the global cloud structure but differ in opacity-relevant details like grain
size, amount of dust, dust and gas-phase composition. Comparisons of synthetic
photometric fluxes translate into an modelling uncertainty in apparent
magnitudes for our L-dwarf (T-dwarf) test case of 0.25 < \Delta m < 0.875 (0.1
< \Delta m M 1.375) taking into account the 2MASS, the UKIRT WFCAM, the Spitzer
IRAC, and VLT VISIR filters with UKIRT WFCAM being the most challenging for the
models. (abr.)Comment: 22 pages, 17 figures, MNRAS 2008, accepted, (minor grammar/typo
corrections
Comparison of cloud models for Brown Dwarfs
A test case comparison is presented for different dust cloud model approaches
applied in brown dwarfs and giant gas planets. We aim to achieve more
transparency in evaluating the uncertainty inherent to theoretical modelling.
We show in how far model results for characteristic dust quantities vary due to
different assumptions. We also demonstrate differences in the spectral energy
distributions resulting from our individual cloud modelling in 1D substellar
atmosphere simulationsComment: 5 pages, Proceeding to "Exoplantes: Detection, Formation, Dynamics",
eds. Ferraz-Mello et
The mineral clouds on HD209 458b and HD189 733b
This is the final version of the article. Available from the publisher via the DOI in this record.3D atmosphere model results are used to comparatively study the kinetic, nonequilibrium
cloud formation in the atmospheres of two example planets guided by
the giant gas planets HD 209 458b and HD 189 733b. Rather independently of hydrodynamic
model differences, our cloud modelling suggests that both planets are covered
in mineral clouds throughout the entire modelling domain. Both planets harbour chemically
complex clouds that are made of mineral particles that have a height-dependent
material composition and size. The remaining gas-phase element abundances strongly
effects the molecular abundances of the atmosphere in the cloud forming regions. Hydrocarbon
and cyanopolyyne molecules can be rather abundant in the inner, dense
part of the atmospheres of HD 189 733b and HD 209 458b. No one value for metallicity
and the C/O ratio can be used to describe an extrasolar planet. Our results concerning
the presence and location of water in relation to the clouds explain some of the
observed differences between the two planets. In HD 189 733b, strong water features
have been reported while such features are less strong for HD 209 458b. By considering
the location of the clouds in the two atmospheres, we see that obscuring clouds exist
high in the atmosphere of HD 209 458b, but much deeper in HD 189 733b. We further
conclude that the (self-imposed) degeneracy of cloud parameters in retrieval methods
can only be lifted if the cloud formation processes are accurately modelled in contrast
to prescribing them by independent parametersWe highlight financial support of the European Community
under the FP7 by the ERC starting grant 257431 and by an
ERC advanced grant 247060. JK acknowledges the Rosen
fellowship from the Brooklyn College New York, US. Some
of the calculations for this paper were performed on the
DIRAC Facility jointly funded by STFC, the Large Facilities
Capital Fund of BIS, and the University of Exeter
A Review of Noncommutative Field Theories
We present a brief review of selected topics in noncommutative field theories
ranging from its revival in string theory, its influence on quantum field
theories, its possible experimental signatures and ending with some
applications in gravity and emergent gravity.Comment: Talk presented at the XIV Mexican School on Particles and Fields,
Morelia, Mexico, November 9-11, 2010; 8 pages. V2 reference adde
A World-Volume Perspective on the Recombination of Intersecting Branes
We study brane recombination for supersymmetric configurations of
intersecting branes in terms of the world-volume field theory. This field
theory contains an impurity, corresponding to the degrees of freedom localized
at the intersection. The Higgs branch, on which the impurity fields condense,
consists of vacua for which the intersection is deformed into a smooth
calibrated manifold. We show this explicitly using a superspace formalism for
which the calibration equations arise naturally from F- and D-flatness.Comment: References adde
The LQG -- String: Loop Quantum Gravity Quantization of String Theory I. Flat Target Space
We combine I. background independent Loop Quantum Gravity (LQG) quantization
techniques, II. the mathematically rigorous framework of Algebraic Quantum
Field Theory (AQFT) and III. the theory of integrable systems resulting in the
invariant Pohlmeyer Charges in order to set up the general representation
theory (superselection theory) for the closed bosonic quantum string on flat
target space. While we do not solve the, expectedly, rich representation theory
completely, we present a, to the best of our knowledge new, non -- trivial
solution to the representation problem. This solution exists 1. for any target
space dimension, 2. for Minkowski signature of the target space, 3. without
tachyons, 4. manifestly ghost -- free (no negative norm states), 5. without
fixing a worldsheet or target space gauge, 6. without (Virasoro) anomalies
(zero central charge), 7. while preserving manifest target space Poincar\'e
invariance and 8. without picking up UV divergences. The existence of this
stable solution is exciting because it raises the hope that among all the
solutions to the representation problem (including fermionic degrees of
freedom) we find stable, phenomenologically acceptable ones in lower
dimensional target spaces, possibly without supersymmetry, that are much
simpler than the solutions that arise via compactification of the standard Fock
representation of the string. Moreover, these new representations could solve
some of the major puzzles of string theory such as the cosmological constant
problem. The solution presented in this paper exploits the flatness of the
target space in several important ways. In a companion paper we treat the more
complicated case of curved target spaces.Comment: 46 p., LaTex2e, no figure
Commutative limit of a renormalizable noncommutative model
Renormalizable models on Moyal space have been obtained by
modifying the commutative propagator. But these models have a divergent "naive"
commutative limit. We explain here how to obtain a coherent such commutative
limit for a recently proposed translation-invariant model. The mechanism relies
on the analysis of the uv/ir mixing in general Feynman graphs.Comment: 11 pages, 3 figures, minor misprints being correcte
Atmospheres from very low-mass stars to extrasolar planets
Within the next few years, several instruments aiming at imaging extrasolar
planets will see first light. In parallel, low mass planets are being searched
around red dwarfs which offer more favorable conditions, both for radial
velocity detection and transit studies, than solar-type stars. We review recent
advancements in modeling the stellar to substellar transition. The revised
solar oxygen abundances and cloud models allow to reproduce the photometric and
spectroscopic properties of this transition to a degree never achieved before,
but problems remain in the important M-L transition characteristic of the
effective temperature range of characterizable exoplanets.Comment: submitted to Memorie della Societa Astronomica Italian
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