Extrasolar Planets I
Total Page:16
File Type:pdf, Size:1020Kb
Load more
										Recommended publications
									
								- 
												  Setting the Stage: Planet Formation and Volatile DeliveryNoname manuscript No. (will be inserted by the editor) Setting the Stage: Planet formation and Volatile Delivery Julia Venturini1 · Maria Paula Ronco2;3 · Octavio Miguel Guilera4;2;3 Received: date / Accepted: date Abstract The diversity in mass and composition of planetary atmospheres stems from the different building blocks present in protoplanetary discs and from the different physical and chemical processes that these experience during the planetary assembly and evolution. This review aims to summarise, in a nutshell, the key concepts and processes operating during planet formation, with a focus on the delivery of volatiles to the inner regions of the planetary system. 1 Protoplanetary discs: the birthplaces of planets Planets are formed as a byproduct of star formation. In star forming regions like the Orion Nebula or the Taurus Molecular Cloud, many discs are observed around young stars (Isella et al, 2009; Andrews et al, 2010, 2018a; Cieza et al, 2019). Discs form around new born stars as a natural consequence of the collapse of the molecular cloud, to conserve angular momentum. As in the interstellar medium, it is generally assumed that they contain typically 1% of their mass in the form of rocky or icy grains, known as dust; and 99% in the form of gas, which is basically H2 and He (see, e.g., Armitage, 2010). However, the dust-to-gas ratios are usually higher in discs (Ansdell et al, 2016). There is strong observational evidence supporting the fact that planets form within those discs (Bae et al, 2017; Dong et al, 2018; Teague et al, 2018; Pérez et al, 2019), which are accordingly called protoplanetary discs.
- 
												  Last Time: Planet FindingLast Time: Planet Finding • Radial velocity method • Parent star’s Doppler shi • Planet minimum mass, orbital period, semi- major axis, orbital eccentricity • UnAl Kepler Mission, was the method with the most planets Last Time: Planet Finding • Transits – eclipse of the parent star: • Planetary radius, orbital period, semi-major axis • Now the most common way to find planets Last Time: Planet Finding • Direct Imaging • Planetary brightness, distance from parent star at that moment • About 10 planets detected Last Time: Planet Finding • Lensing • Planetary mass and, distance from parent star at that moment • You want to look towards the center of the galaxy where there is a high density of stars Last Time: Planet Finding • Astrometry • Tiny changes in star’s posiAon are not yet measurable • Would give you planet’s mass, orbit, and eccentricity One more important thing to add: • Giant planets (which are easiest to detect) are preferenAally found around stars that are abundant in iron – “metallicity” • Iron is the easiest heavy element to measure in a star • Heavy-element rich planetary systems make planets more easily 13.2 The Nature of Extrasolar Planets Our goals for learning: • What have we learned about extrasolar planets? • How do extrasolar planets compare with planets in our solar system? Measurable Properties • Orbital period, distance, and orbital shape • Planet mass, size, and density • Planetary temperature • Composition Orbits of Extrasolar Planets • Nearly all of the detected planets have orbits smaller than Jupiter’s. • This is a selection effect: Planets at greater distances are harder to detect with the Doppler technique. Orbits of Extrasolar Planets • Orbits of some extrasolar planets are much more elongated (have a greater eccentricity) than those in our solar system.
- 
												  Survival of Satellites During the Migration of a Hot Jupiter: the Influence of TidesEPSC Abstracts Vol. 13, EPSC-DPS2019-1590-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. Survival of satellites during the migration of a Hot Jupiter: the influence of tides Emeline Bolmont (1), Apurva V. Oza (2), Sergi Blanco-Cuaresma (3), Christoph Mordasini (2), Pierre Auclair-Desrotour (2), Adrien Leleu (2) (1) Observatoire de Genève, Université de Genève, 51 Chemin des Maillettes, CH-1290 Sauverny, Switzerland ([email protected]) (2) Physikalisches Institut, Universität Bern, Gesellschaftsstr. 6, 3012, Bern, Switzerland (3) Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA Abstract 2. The model We explore the origin and stability of extrasolar satel- lites orbiting close-in gas giants, by investigating if the Tidal interactions 1 M⊙ satellite can survive the migration of the planet in the 1 MIo protoplanetary disk. To accomplish this objective, we 1 MJup used Posidonius, a N-Body code with an integrated tidal model, which we expanded to account for the migration of the gas giant in a disk. Preliminary re- Inner edge of disk: ain sults suggest the survival of the satellite is rare, which Type 2 migration: !mig would indicate that if such satellites do exist, capture is a more likely process. Figure 1: Schema of the simulation set up: A Io-like satellite orbits around a Jupiter-like planet with a solar- 1. Introduction like host star. Satellites around Hot Jupiters were first thought to be lost by falling onto their planet over Gyr timescales (e.g. [1]). This is due to the low tidal dissipation factor of Jupiter (Q 106, [10]), likely to be caused by the 2.1.
- 
												![Arxiv:1904.05358V1 [Astro-Ph.EP] 10 Apr 2019](https://docslib.b-cdn.net/cover/1935/arxiv-1904-05358v1-astro-ph-ep-10-apr-2019-481935.webp)  Arxiv:1904.05358V1 [Astro-Ph.EP] 10 Apr 2019Draft version April 12, 2019 Typeset using LATEX default style in AASTeX62 The Gemini Planet Imager Exoplanet Survey: Giant Planet and Brown Dwarf Demographics From 10{100 AU Eric L. Nielsen,1 Robert J. De Rosa,1 Bruce Macintosh,1 Jason J. Wang,2, 3, ∗ Jean-Baptiste Ruffio,1 Eugene Chiang,3 Mark S. Marley,4 Didier Saumon,5 Dmitry Savransky,6 S. Mark Ammons,7 Vanessa P. Bailey,8 Travis Barman,9 Celia´ Blain,10 Joanna Bulger,11 Jeffrey Chilcote,1, 12 Tara Cotten,13 Ian Czekala,3, 1, y Rene Doyon,14 Gaspard Duchene^ ,3, 15 Thomas M. Esposito,3 Daniel Fabrycky,16 Michael P. Fitzgerald,17 Katherine B. Follette,18 Jonathan J. Fortney,19 Benjamin L. Gerard,20, 10 Stephen J. Goodsell,21 James R. Graham,3 Alexandra Z. Greenbaum,22 Pascale Hibon,23 Sasha Hinkley,24 Lea A. Hirsch,1 Justin Hom,25 Li-Wei Hung,26 Rebekah Ilene Dawson,27 Patrick Ingraham,28 Paul Kalas,3, 29 Quinn Konopacky,30 James E. Larkin,17 Eve J. Lee,31 Jonathan W. Lin,3 Jer´ ome^ Maire,30 Franck Marchis,29 Christian Marois,10, 20 Stanimir Metchev,32, 33 Maxwell A. Millar-Blanchaer,8, 34 Katie M. Morzinski,35 Rebecca Oppenheimer,36 David Palmer,7 Jennifer Patience,25 Marshall Perrin,37 Lisa Poyneer,7 Laurent Pueyo,37 Roman R. Rafikov,38 Abhijith Rajan,37 Julien Rameau,14 Fredrik T. Rantakyro¨,39 Bin Ren,40 Adam C. Schneider,25 Anand Sivaramakrishnan,37 Inseok Song,13 Remi Soummer,37 Melisa Tallis,1 Sandrine Thomas,28 Kimberly Ward-Duong,25 and Schuyler Wolff41 1Kavli Institute for Particle Astrophysics and Cosmology, Stanford University, Stanford, CA 94305, USA 2Department of Astronomy, California Institute of Technology, Pasadena, CA 91125, USA 3Department of Astronomy, University of California, Berkeley, CA 94720, USA 4NASA Ames Research Center, Mountain View, CA 94035, USA 5Los Alamos National Laboratory, P.O.
- 
												  Correlations Between the Stellar, Planetary, and Debris Components of Exoplanet Systems Observed by Herschel⋆A&A 565, A15 (2014) Astronomy DOI: 10.1051/0004-6361/201323058 & c ESO 2014 Astrophysics Correlations between the stellar, planetary, and debris components of exoplanet systems observed by Herschel J. P. Marshall1,2, A. Moro-Martín3,4, C. Eiroa1, G. Kennedy5,A.Mora6, B. Sibthorpe7, J.-F. Lestrade8, J. Maldonado1,9, J. Sanz-Forcada10,M.C.Wyatt5,B.Matthews11,12,J.Horner2,13,14, B. Montesinos10,G.Bryden15, C. del Burgo16,J.S.Greaves17,R.J.Ivison18,19, G. Meeus1, G. Olofsson20, G. L. Pilbratt21, and G. J. White22,23 (Affiliations can be found after the references) Received 15 November 2013 / Accepted 6 March 2014 ABSTRACT Context. Stars form surrounded by gas- and dust-rich protoplanetary discs. Generally, these discs dissipate over a few (3–10) Myr, leaving a faint tenuous debris disc composed of second-generation dust produced by the attrition of larger bodies formed in the protoplanetary disc. Giant planets detected in radial velocity and transit surveys of main-sequence stars also form within the protoplanetary disc, whilst super-Earths now detectable may form once the gas has dissipated. Our own solar system, with its eight planets and two debris belts, is a prime example of an end state of this process. Aims. The Herschel DEBRIS, DUNES, and GT programmes observed 37 exoplanet host stars within 25 pc at 70, 100, and 160 μm with the sensitiv- ity to detect far-infrared excess emission at flux density levels only an order of magnitude greater than that of the solar system’s Edgeworth-Kuiper belt. Here we present an analysis of that sample, using it to more accurately determine the (possible) level of dust emission from these exoplanet host stars and thereafter determine the links between the various components of these exoplanetary systems through statistical analysis.
- 
												![Arxiv:2012.11628V3 [Astro-Ph.EP] 26 Jan 2021](https://docslib.b-cdn.net/cover/5762/arxiv-2012-11628v3-astro-ph-ep-26-jan-2021-535762.webp)  Arxiv:2012.11628V3 [Astro-Ph.EP] 26 Jan 2021manuscript submitted to JGR: Planets The Fundamental Connections Between the Solar System and Exoplanetary Science Stephen R. Kane1, Giada N. Arney2, Paul K. Byrne3, Paul A. Dalba1∗, Steven J. Desch4, Jonti Horner5, Noam R. Izenberg6, Kathleen E. Mandt6, Victoria S. Meadows7, Lynnae C. Quick8 1Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA 2Planetary Systems Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA 3Planetary Research Group, Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA 4School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA 5Centre for Astrophysics, University of Southern Queensland, Toowoomba, QLD 4350, Australia 6Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA 7Department of Astronomy, University of Washington, Seattle, WA 98195, USA 8Planetary Geology, Geophysics and Geochemistry Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA Key Points: • Exoplanetary science is rapidly expanding towards characterization of atmospheres and interiors. • Planetary science has similarly undergone rapid expansion of understanding plan- etary processes and evolution. • Effective studies of exoplanets require models and in-situ data derived from plan- etary science observations and exploration. arXiv:2012.11628v4 [astro-ph.EP] 8 Aug 2021 ∗NSF Astronomy and Astrophysics Postdoctoral Fellow Corresponding author: Stephen R. Kane, [email protected] {1{ manuscript submitted to JGR: Planets Abstract Over the past several decades, thousands of planets have been discovered outside of our Solar System. These planets exhibit enormous diversity, and their large numbers provide a statistical opportunity to place our Solar System within the broader context of planetary structure, atmospheres, architectures, formation, and evolution.
- 
												  Exploring Exoplanet Populations with NASA's Kepler MissionSPECIAL 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.
- 
												  The Search for Exomoons and the Characterization of Exoplanet AtmospheresCorso di Laurea Specialistica in Astronomia e Astrofisica The search for exomoons and the characterization of exoplanet atmospheres Relatore interno : dott. Alessandro Melchiorri Relatore esterno : dott.ssa Giovanna Tinetti Candidato: Giammarco Campanella Anno Accademico 2008/2009 The search for exomoons and the characterization of exoplanet atmospheres Giammarco Campanella Dipartimento di Fisica Università degli studi di Roma “La Sapienza” Associate at Department of Physics & Astronomy University College London A thesis submitted for the MSc Degree in Astronomy and Astrophysics September 4th, 2009 Università degli Studi di Roma ―La Sapienza‖ Abstract THE SEARCH FOR EXOMOONS AND THE CHARACTERIZATION OF EXOPLANET ATMOSPHERES by Giammarco Campanella Since planets were first discovered outside our own Solar System in 1992 (around a pulsar) and in 1995 (around a main sequence star), extrasolar planet studies have become one of the most dynamic research fields in astronomy. Our knowledge of extrasolar planets has grown exponentially, from our understanding of their formation and evolution to the development of different methods to detect them. Now that more than 370 exoplanets have been discovered, focus has moved from finding planets to characterise these alien worlds. As well as detecting the atmospheres of these exoplanets, part of the characterisation process undoubtedly involves the search for extrasolar moons. The structure of the thesis is as follows. In Chapter 1 an historical background is provided and some general aspects about ongoing situation in the research field of extrasolar planets are shown. In Chapter 2, various detection techniques such as radial velocity, microlensing, astrometry, circumstellar disks, pulsar timing and magnetospheric emission are described. A special emphasis is given to the transit photometry technique and to the two already operational transit space missions, CoRoT and Kepler.
- 
												  Can Brown Dwarfs Survive on Close Orbits Around Convective Stars? CA&A 589, A55 (2016) Astronomy DOI: 10.1051/0004-6361/201527100 & c ESO 2016 Astrophysics Can brown dwarfs survive on close orbits around convective stars? C. Damiani1 and R. F. Díaz2 1 Université Paris-Sud, CNRS, Institut d’Astrophysique Spatiale, UMR8617, 91405 Orsay Cedex, France e-mail: [email protected] 2 Observatoire astronomique de l’Université de Genève, 51 ch. des Maillettes, 1290 Versoix, Switzerland e-mail: [email protected] Received 1 August 2015 / Accepted 23 February 2016 ABSTRACT Context. The mass range of brown dwarfs extends across the planetary domain to stellar objects. There is a relative paucity of brown dwarfs companions around FGKM-type stars compared to exoplanets for orbital periods of less than a few years, but most of the short-period brown dwarf companions that are fully characterised by transits and radial velocities are found around F-type stars. Aims. We examine the hypothesis that brown dwarf companions could not survive on close orbit around stars with important convec- tive envelopes because the tides and angular momentum loss, the result of magnetic braking, would lead to a rapid orbital decay with the companion being quickly engulfed. Methods. We use a classical Skumanich-type braking law and constant time-lag tidal theory to assess the characteristic timescale for orbital decay for the brown dwarf mass range as a function of the host properties. Results. We find that F-type stars may host massive companions for a significantly longer time than G-type stars for a given orbital period, which may explain the paucity of G-type hosts for brown dwarfs with an orbital period less than five days.
- 
												  Dynamical Evolution of Planetary SystemsDynamical Evolution of Planetary Systems Alessandro Morbidelli Abstract Planetary systems can evolve dynamically even after the full growth of the planets themselves. There is actually circumstantial evidence that most plane- tary systems become unstable after the disappearance of gas from the protoplanetary disk. These instabilities can be due to the original system being too crowded and too closely packed or to external perturbations such as tides, planetesimal scattering, or torques from distant stellar companions. The Solar System was not exceptional in this sense. In its inner part, a crowded system of planetary embryos became un- stable, leading to a series of mutual impacts that built the terrestrial planets on a timescale of ∼ 100My. In its outer part, the giant planets became temporarily unsta- ble and their orbital configuration expanded under the effect of mutual encounters. A planet might have been ejected in this phase. Thus, the orbital distributions of planetary systems that we observe today, both solar and extrasolar ones, can be dif- ferent from the those emerging from the formation process and it is important to consider possible long-term evolutionary effects to connect the two. Introduction This chapter concerns the dynamical evolution of planetary systems after the re- moval of gas from the proto-planetary disk. Most massive planets are expected to form within the lifetime of the gas component of protoplanetary disks (see chapters by D’Angelo and Lissauer for the giant planets and by Schlichting for Super-Earths) and, while they form, they are expected to evolve dynamically due to gravitational interactions with the gas (see chapter by Nelson on planet migration).
- 
												  Ground-Based Secondary Eclipse Detection of the Very-Hot Jupiter OGLE-TR-56BA&A 493, L31–L34 (2009) Astronomy DOI: 10.1051/0004-6361:200811268 & c ESO 2009 Astrophysics Letter to the Editor Ground-based secondary eclipse detection of the very-hot Jupiter OGLE-TR-56b D. K. Sing1 and M. López-Morales2, 1 Institut d’Astrophysique de Paris, CNRS/UPMC, 98bis boulevard Arago, 75014 Paris, France e-mail: [email protected] 2 Carnegie Institution of Washington, Dept. of Terrestrial Magnetism, 5241 Broad Branch Road NW, Washington, DC 20015, USA e-mail: [email protected] Received 31 October 2008 / Accepted 21 November 2008 ABSTRACT We report on the detection of the secondary eclipse of the very-hot Jupiter OGLE-TR-56b from combined z-band time series pho- tometry obtained with the VLT and Magellan telescopes. We measure a flux decrement of 0.0363 ± 0.0091% from the combined +127 Magellan and VLT datasets, which indicates a blackbody brightness temperature of 2718−107 K, a very low albedo, and a small in- cident radiation redistribution factor, indicating a lack of strong winds in the planet’s atmosphere. The measured secondary depth is consistent with thermal emission, but our precision is not sufficient to distinguish between a black-body emitting planet, or emission as predicted by models with strong optical absorbers such as TiO/VO. This is the first time that thermal emission from an extrasolar planet is detected at optical wavelengths and with ground-based telescopes. Key words. binaries: eclipsing – planetary systems – stars: individual: OGLE-TR-56 – techniques: photometric 1. Introduction Here we present the results of the follow-up observations to test that prediction.
- 
												  Brown Dwarf Desert Evolved Systems Atmospheres AndIrradiated brown dwarfs - hot Jupiter analogues? Sarah L Casewell1* STFC Ernest Rutherford Research Fellow 1. University of Leicester, Department of Physics and Astronomy, Leicester, UK *email: [email protected] As brown dwarfs have atmospheres similar to those we see in Jupiter and in hot Jupiter exoplanets, irradiated brown dwarfs have been described as “filling the fourth corner of parameter space between the solar system planets, hot Jupiter exoplanets and isolated brown dwarfs”. Irradiated brown dwarfs are however, rare. There are only about 22 known around main sequence stars, and even fewer that have survived the evolution of their host star to form close, post-common envelope systems where the brown dwarf orbits a white dwarf. These systems are however, extremely useful. The white dwarf emits more at shorter wavelengths, where the brown dwarf is brightest in the infrared, meaning it is possible to directly observe the brown dwarf – something that is extremely challenging for the main sequence star-brown dwarf systems. BROWN DWARF DESERT ATMOSPHERES AND IRRADIATION Despite there being a plethora of Hot Jupiters known, there are very few The brown dwarfs in these systems are highly irradiated leading to emission brown dwarfs discovered in similar orbits, a phenomenon known as the lines being seen from hydrogen, Ca I, Na I, K I, Ti I and Fe in the systems with brown dwarf desert. This is thought to be caused by the difference in white dwarfs hotter than 13000 K. The hottest primaries show fewer emission formation mechanisms, planets forming via core accretion around stars, lines due to dissociation, but large day- night temperature differences of ~500 but brown dwarfs forming via gravitational instabilty .