Extrasolar Planets: from Dust to New Worlds
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Exploring Exoplanet Populations with NASA's Kepler Mission
SPECIAL FEATURE: PERSPECTIVE PERSPECTIVE SPECIAL FEATURE: Exploring exoplanet populations with NASA’s Kepler Mission Natalie M. Batalha1 National Aeronautics and Space Administration Ames Research Center, Moffett Field, 94035 CA Edited by Adam S. Burrows, Princeton University, Princeton, NJ, and accepted by the Editorial Board June 3, 2014 (received for review January 15, 2014) The Kepler Mission is exploring the diversity of planets and planetary systems. Its legacy will be a catalog of discoveries sufficient for computing planet occurrence rates as a function of size, orbital period, star type, and insolation flux.The mission has made significant progress toward achieving that goal. Over 3,500 transiting exoplanets have been identified from the analysis of the first 3 y of data, 100 planets of which are in the habitable zone. The catalog has a high reliability rate (85–90% averaged over the period/radius plane), which is improving as follow-up observations continue. Dynamical (e.g., velocimetry and transit timing) and statistical methods have confirmed and characterized hundreds of planets over a large range of sizes and compositions for both single- and multiple-star systems. Population studies suggest that planets abound in our galaxy and that small planets are particularly frequent. Here, I report on the progress Kepler has made measuring the prevalence of exoplanets orbiting within one astronomical unit of their host stars in support of the National Aeronautics and Space Admin- istration’s long-term goal of finding habitable environments beyond the solar system. planet detection | transit photometry Searching for evidence of life beyond Earth is the Sun would produce an 84-ppm signal Translating Kepler’s discovery catalog into one of the primary goals of science agencies lasting ∼13 h. -
Formation of TRAPPIST-1
EPSC Abstracts Vol. 11, EPSC2017-265, 2017 European Planetary Science Congress 2017 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2017 Formation of TRAPPIST-1 C.W Ormel, B. Liu and D. Schoonenberg University of Amsterdam, The Netherlands ([email protected]) Abstract start to drift by aerodynamical drag. However, this growth+drift occurs in an inside-out fashion, which We present a model for the formation of the recently- does not result in strong particle pileups needed to discovered TRAPPIST-1 planetary system. In our sce- trigger planetesimal formation by, e.g., the streaming nario planets form in the interior regions, by accre- instability [3]. (a) We propose that the H2O iceline (r 0.1 au for TRAPPIST-1) is the place where tion of mm to cm-size particles (pebbles) that drifted ice ≈ the local solids-to-gas ratio can reach 1, either by from the outer disk. This scenario has several ad- ∼ vantages: it connects to the observation that disks are condensation of the vapor [9] or by pileup of ice-free made up of pebbles, it is efficient, it explains why the (silicate) grains [2, 8]. Under these conditions plan- TRAPPIST-1 planets are Earth mass, and it provides etary embryos can form. (b) Due to type I migration, ∼ a rationale for the system’s architecture. embryos cross the iceline and enter the ice-free region. (c) There, silicate pebbles are smaller because of col- lisional fragmentation. Nevertheless, pebble accretion 1. Introduction remains efficient and growth is fast [6]. (d) At approx- TRAPPIST-1 is an M8 main-sequence star located at a imately Earth masses embryos reach their pebble iso- distance of 12 pc. -
Water, Habitability, and Detectability Steve Desch
Water, Habitability, and Detectability Steve Desch PI, “Exoplanetary Ecosystems” NExSS team School of Earth and Space Exploration, Arizona State University with Ariel Anbar, Tessa Fisher, Steven Glaser, Hilairy Hartnett, Stephen Kane, Susanne Neuer, Cayman Unterborn, Sara Walker, Misha Zolotov Astrobiology Science Strategy NAS Committee, Beckmann Center, Irvine, CA (remotely), January 17, 2018 How to look for life on (Earth-like) exoplanets: find oxygen in their atmospheres How Earth-like must an exoplanet be for this to work? Seager et al. (2013) How to look for life on (Earth-like) exoplanets: find oxygen in their atmospheres Oxygen on Earth overwhelmingly produced by photosynthesizing life, which taps Sun’s energy and yields large disequilibrium signature. Caveats: Earth had life for billions of years without O2 in its atmosphere. First photosynthesis to evolve on Earth was anoxygenic. Many ‘false positives’ recognized because O2 has abiotic sources, esp. photolysis (Luger & Barnes 2014; Harman et al. 2015; Meadows 2017). These caveats seem like exceptions to the ‘rule’ that ‘oxygen = life’. How non-Earth-like can an exoplanet be (especially with respect to water content) before oxygen is no longer a biosignature? Part 1: How much water can terrestrial planets form with? Part 2: Are Aqua Planets or Water Worlds habitable? Can we detect life on them? Part 3: How should we look for life on exoplanets? Part 1: How much water can terrestrial planets form with? Theory says: up to hundreds of oceans’ worth of water Trappist-1 system suggests hundreds of oceans, especially around M stars Many (most?) planets may be Aqua Planets or Water Worlds How much water can terrestrial planets form with? Earth- “snow line” Standard Sun distance models of distance accretion suggest abundant water. -
The Angular Momentum of Condensations Within Elephant Trunks
A&A 503, 477–482 (2009) Astronomy DOI: 10.1051/0004-6361/200912238 & c ESO 2009 Astrophysics The angular momentum of condensations within elephant trunks V. L ora 1,A.C.Raga2, and A. Esquivel2 1 Instituto de Astronomía, Universidad Nacional Autónoma de México, Ap. 70-468, 04510, D.F México 2 Instituto de Ciencias Nucleares, Universidad Nacional Autónoma de México, Ap. 70-543, 04510, D.F México e-mail: [email protected] Received 31 March 2009 / Accepted 22 May 2009 ABSTRACT Aims. The radiation from newly born stars photoevaporates their parental neutral cloud, leading to the formation of dense clumps that will eventually form stars. Methods. We present 3D simulations of the interaction of a neutral cloud with an external ionising radiation field, and compute the angular momenta of these collapsing clumps. Results. The angular momenta of these collapsing clumps show that they have preferential orientations mostly perpendicular to the direction of the incident ionising photon field. Therefore, the axes of the jet systems that will be eventually ejected (from the star+accretion disk systems that will form) will be oriented approximately perpendicular to the direction to the photoionising source. Key words. ISM: kinematics and dynamics – ISM: clouds – ISM: HII regions – stars: formation 1. Introduction of elephant trunks is quite small, their alignment approximately perpendicular to the direction to the ionising photon source The radiation from newly born stars photoionises and erodes the might be indicative of a systematic alignment. This alignment parental cloud, producing structures such as the so-called ele- implies that the angular momenta of the low mass star+disk sys- phant trunks. -
A Spitzer Survey of Protoplanetary Disk Dust in the Young Serpens Cloud: How Do Dust Characteristics Evolve with Time?
The Astrophysical Journal, 714:778–798, 2010 May 1 doi:10.1088/0004-637X/714/1/778 C 2010. The American Astronomical Society. All rights reserved. Printed in the U.S.A. A SPITZER SURVEY OF PROTOPLANETARY DISK DUST IN THE YOUNG SERPENS CLOUD: HOW DO DUST CHARACTERISTICS EVOLVE WITH TIME? Isa Oliveira1,2, Klaus M. Pontoppidan2, Bruno Mer´ın3, Ewine F. van Dishoeck1,4, Fred Lahuis1,5, Vincent C. Geers6, Jes K. Jørgensen7, Johan Olofsson8, Jean-Charles Augereau8, and Joanna M. Brown4 1 Leiden Observatory, Leiden University, P.O. Box 9513, 2300 RA Leiden, The Netherlands; [email protected] 2 California Institute of Technology, Division for Geological and Planetary Sciences, MS 150-21, Pasadena, CA 91125, USA 3 Herschel Science Center, European Space Agency (ESA), P.O. Box 78, 28691 Villanueva de la Canada˜ (Madrid), Spain 4 Max-Planck Institut fur¨ Extraterrestrische Physik, Giessenbachstrasse 1, 85748 Garching, Germany 5 SRON Netherlands Institute for Space Research, P.O. Box 800, 9700 AV Groningen, The Netherlands 6 University of Toronto, 50 St. George St., Toronto, ON M5R 2W9, Canada 7 Centre for Star and Planet Formation, Natural History Museum of Denmark, University of Copenhagen, Øster Voldgade 5-7, DK-1350 Copenhagen, Denmark 8 Laboratoire d’Astrophysique de Grenoble, Universite´ Joseph Fourier, CNRS, UMR 5571, Grenoble, France Received 2009 December 28; accepted 2010 March 16; published 2010 April 14 ABSTRACT We present Spitzer InfraRed Spectrograph (IRS) mid-infrared (5–35 μm) spectra of a complete flux-limited sample (3mJyat8μm) of young stellar object (YSO) candidates selected on the basis of their infrared colors in the Serpens Molecular Cloud. -
The Potential to Form Planets in the Orion Nebula ! Rita Mann Plaskett Fellow NRC-Herzberg
The Potential to Form Planets in the Orion Nebula ! Rita Mann Plaskett Fellow NRC-Herzberg ! James Di Francesco, Sean Andrews, Jonathan Williams, Doug Johnstone, John Bally, Meredith Hughes, Luca Ricci, Brenda Matthews Protoplanetary Disks in the Orion Nebula Most stars form in rich clusters Our Solar System formed in a massive star forming environment. To understand planet formation, we need to study disk properties in massive star forming regions! HST images of protostars in Orion Orion Nebula Cluster Trapezium Cluster • Thousands of protostars • Ages ~ 1-2 Myr • Distance ~ 400 pc 1 • θ Ori C, 40M¤, O6 SpT Orion Nebula Cluster Massive Stars • Hostile environment • Many low mass stars near ϑ1C have teardrop shaped morphologies Low Mass Stars PROPLYDS: PROtoPLanetarY DiskS Photoevaporating Proplyds -7 VLA mass-loss rate of 10 M¤/yr Churchwell et al. (1987) Mdisk < 0.1 M¤ Evaporation Timescales < 1 Myr Material removed too quickly! C.R. O’Dell Is planet formation inhibited in rich clusters? Disk Masses in Orion: Previous Attempts Millimeter Wavelength Interferometers (clustered disks) BIMA OVRO PdBI Mundy et al. (1995) Bally et al. (1998) Lada (1999) λ = 3.5 mm λ = 1.3 mm λ = 1.3 mm low sensitivity no detections never published Mdisk ≲ 15 MJUP Radio-Submillimeter SED -0.1 2-4 Ffree-free ~ ν + Fdust ~ ν λ = 1 cm Radio-Submillimeter SED -0.1 2-4 Ffree-free ~ ν + Fdust ~ ν λ = 1 cm 1 mm Radio-Submillimeter SED -0.1 2-4 Ffree-free ~ ν + Fdust ~ ν λ = 1 cm 1 mm Higher frequency observations: more sensitive to dust emission! Interferometry with -
Formation of the Solar System (Chapter 8)
Formation of the Solar System (Chapter 8) Based on Chapter 8 • This material will be useful for understanding Chapters 9, 10, 11, 12, 13, and 14 on “Formation of the solar system”, “Planetary geology”, “Planetary atmospheres”, “Jovian planet systems”, “Remnants of ice and rock”, “Extrasolar planets” and “The Sun: Our Star” • Chapters 2, 3, 4, and 7 on “The orbits of the planets”, “Why does Earth go around the Sun?”, “Momentum, energy, and matter”, and “Our planetary system” will be useful for understanding this chapter Goals for Learning • Where did the solar system come from? • How did planetesimals form? • How did planets form? Patterns in the Solar System • Patterns of motion (orbits and rotations) • Two types of planets: Small, rocky inner planets and large, gas outer planets • Many small asteroids and comets whose orbits and compositions are similar • Exceptions to these patterns, such as Earth’s large moon and Uranus’s sideways tilt Help from Other Stars • Use observations of the formation of other stars to improve our theory for the formation of our solar system • Use this theory to make predictions about the formation of other planetary systems Nebular Theory of Solar System Formation • A cloud of gas, the “solar nebula”, collapses inwards under its own weight • Cloud heats up, spins faster, gets flatter (disk) as a central star forms • Gas cools and some materials condense as solid particles that collide, stick together, and grow larger Where does a cloud of gas come from? • Big Bang -> Hydrogen and Helium • First stars use this -
University of Groningen Evaluating Galactic Habitability Using High
University of Groningen Evaluating galactic habitability using high-resolution cosmological simulations of galaxy formation Forgan, Duncan; Dayal, Pratika; Cockell, Charles; Libeskind, Noam Published in: International Journal of Astrobiology DOI: 10.1017/S1473550415000518 IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Final author's version (accepted by publisher, after peer review) Publication date: 2017 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Forgan, D., Dayal, P., Cockell, C., & Libeskind, N. (2017). Evaluating galactic habitability using high- resolution cosmological simulations of galaxy formation. International Journal of Astrobiology, 16(1), 60–73. https://doi.org/10.1017/S1473550415000518 Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). The publication may also be distributed here under the terms of Article 25fa of the Dutch Copyright Act, indicated by the “Taverne” license. More information can be found on the University of Groningen website: https://www.rug.nl/library/open-access/self-archiving-pure/taverne- amendment. Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. -
Why Should We Care About TRAPPIST-1?
PUBLISHED: 27 MARCH 2017 | VOLUME: 1 | ARTICLE NUMBER: 0104 news & views EXOPLANETS Why should we care about TRAPPIST-1? The discovery of a system of six (possibly system we’ve found with terrestrial planets seven) terrestrial planets around the tightly packed together and in resonance. TRAPPIST-1 star, announced in a paper Their orbits are also all co-planar, as the by Michaël Gillon and collaborators image shows, and luckily for us this orbital (Nature 542, 456–460; 2017) attracted a plane passes through the line of sight great deal of attention from researchers between us and TRAPPIST-1: all these as well as the general public. Reactions planets are ‘transiting’. This is much more ranged from the enthusiastic — already than a simple technical detail, as it allows us hypothesizing a string of inhabited to characterize all their atmospheres — an planets — to those who felt that it essential step to understand their climate didn’t add anything substantial to our and propensity for habitability. current knowledge of exoplanets and Finally and maybe most importantly, was ultimately not worth the hype. The these planets are distributed over all of cover of the Nature issue hosting the the three zones related to different phases paper (pictured), made by Robert Hurt, (IPAC) HURT NASA/JPL-CALTECH/ROBERT of water, as cleverly represented by the a visualization scientist at Caltech, is a illustration. However, this information, fine piece of artwork, but it also helps us They can thus be called ‘terrestrial’ without linked to the concept of habitable or in assessing the actual relevance of the any qualms about terminology. -
One-Armed Oscillations in Be Star Discs
A&A 456, 1097–1104 (2006) Astronomy DOI: 10.1051/0004-6361:20065407 & c ESO 2006 Astrophysics One-armed oscillations in Be star discs J. C. B. Papaloizou1 andG.J.Savonije2 1 Department of Applied Mathematics and Theoretical Physics, Centre for Mathematical Sciences, Wilberforce Road, Cambridge CB3 0WA, UK 2 Astronomical Institute “Anton Pannekoek”, University of Amsterdam, Kruislaan 403, 1098 SJ Amsterdam, The Netherlands e-mail: [email protected] Received 11 April 2006 / Accepted 20 June 2006 ABSTRACT Aims. In this paper we study the effect of the quadrupole-term in the gravitational potential of a rotationally deformed central Be star on one armed density waves in the circumstellar disc. The aim is to explain the observed long-term violet over red (V/R) intensity variations of the double peaked Balmer emission-lines, not only in cool Be star systems, but also in the hot systems like γ Cas. Methods. We have carried out semi-analytic and numerical studies of low-frequency one armed global oscillations in near Keplerian discs around Be stars. In these we have investigated surface density profiles for the circumstellar disc which have inner narrow low surface density or gap regions, just interior to global maxima close to the rapidly rotating star, as well as the mode inner boundary conditions. Results. Our results indicate that it is not necessary to invoke extra forces such as caused by line absorption from the stellar flux in order to explain the long-term V/R variations in the discs around massive Be stars. When there exists a narrow gap between the star and its circumstellar disc, with the result that the radial velocity perturbation is non-zero at the inner disc boundary, we find oscillation (and V/R) periods in the observed range for plausible magnitudes for the rotational quadrupole term. -
Detection of Nitrogen Gas in the Β Pictoris Circumstellar Disc P
Manuscript version: Published Version The version presented in WRAP is the published version (Version of Record). Persistent WRAP URL: http://wrap.warwick.ac.uk/110773 How to cite: The repository item page linked to above, will contain details on accessing citation guidance from the publisher. Copyright and reuse: The Warwick Research Archive Portal (WRAP) makes this work by researchers of the University of Warwick available open access under the following conditions. Copyright © and all moral rights to the version of the paper presented here belong to the individual author(s) and/or other copyright owners. To the extent reasonable and practicable the material made available in WRAP has been checked for eligibility before being made available. Copies of full items can be used for personal research or study, educational, or not-for-profit purposes without prior permission or charge. Provided that the authors, title and full bibliographic details are credited, a hyperlink and/or URL is given for the original metadata page and the content is not changed in any way. Publisher’s statement: Please refer to the repository item page, publisher’s statement section, for further information. For more information, please contact the WRAP Team at: [email protected] warwick.ac.uk/lib-publications A&A 621, A121 (2019) Astronomy https://doi.org/10.1051/0004-6361/201834346 & © ESO 2019 Astrophysics Detection of nitrogen gas in the β Pictoris circumstellar disc P. A. Wilson1,2,3,4,5, R. Kerr6, A. Lecavelier des Etangs4,5, V. Bourrier4,5,7, A. Vidal-Madjar4,5, F. Kiefer4,5, and I. -
Gas Accretion by Giant Planets : a Study with 3D Inviscid Hydrodynamical Simulations
EPSC Abstracts Vol. 8, EPSC2013-363, 2013 European Planetary Science Congress 2013 EEuropeaPn PlanetarSy Science CCongress c Author(s) 2013 Gas Accretion by Giant Planets : a study with 3D inviscid hydrodynamical simulations J. Szulágyi (1), A. Morbidelli (1), A. Crida (1) and F. Masset (2) (1) University of Nice-Sophia Antipolis, CNRS, Observatoire de la Côte d’Azur, Laboratoire Lagrange, France ([email protected]) (2) Institute of Physical Sciences, Universidad Nacional Autónoma de México Abstract If this were true, there should be a dichotomy in the mass distribution of planets : planets should be either We investigate the properties of the circumplanetary smaller than 30 Earth masses (those that did not ∼ disc (CPD) of a Jupiter-mass planet with a three- reach the phase of runaway gas accretion) or of mul- dimensional hydrodynamical nested grid code. We tiple Jupiter-masses (those that entered and completed perform isothermal simulations of a large radial por- the fast runaway gas accretion). Planets in between tion of the circumstellar disc and, with the help of a these two mass categories should be extremely rare, system of 8 nested grids, we zoom into the planet’s conversely to what is observed [4]. vicinity. Since giant planets are thought to form in a A very likely possibility, however, is that the cir- dead zone, we do not use any prescribed viscosity in cumplanetary disc acts as a regulator of the rate of gas the fluid-dynamics equations. accretion onto the planet. In particular, if the circum- We discuss in details the geometry of the circum- planetary disc (CPD) has a very low viscosity [8], then planetary disc, and especially focus on the role of the the transport of angular momentum through this disc polar inflow.