An Analysis on Exoplanets and How They Are Affected by Different Factors in Their Star Systems
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2-6-NASA Exoplanet Archive
The NASA Exoplanet Archive Rachel Akeson NASA Exoplanet Science Ins5tute (NExScI) September 29, 2016 NASA Big Data Task Force Overview: Dat a NASA Exoplanet Archive supports both the exoplanet science community and NASA exoplanet missions (Kepler, K2, TESS, WFIRST) • Data • Confirmed exoplanets from the literature • Over 80,000 planetary and stellar parameter values for 3388 exoplanets • Updated weekly • Kepler stellar proper5es, planet candidate, data valida5on and occurrence rate products • MAST is archive for pixel and light curve data • Addi5onal space (CoRoT) and ground-based transit surveys (~20 million light curves) • Transit spectroscopy data • Auto-updated exoplanet plots and movies Big Data Task Force: Exoplanet Archive Overview: Tool s Example: Kepler 14 Time Series Viewer • Interac5ve tables and ploZng for data • Includes light curve normaliza5on • Periodogram calcula5ons • Searches for periodic signals in archive or user-supplied light curves • Transit predic5ons • Uses value from archive to predict future planet transits for observa5on and mission planning • URL-based queries Aliases • Calcula5on of observable proper5es Planet orbital period • Web-based service to collect follow-up observa5ons of planet candidates for Kepler, K2 and TESS (ExoFOP) Stellar ac5vity • Includes user-supplied data, file and notes Big Data Task Force: Exoplanet Archive Data Challenges and Technical Approach (1) • Challenges with Exoplanet Archive are not currently about data volume but about providing CPU resources and data complexity • CPU challenge -
Lecture 3 - Minimum Mass Model of Solar Nebula
Lecture 3 - Minimum mass model of solar nebula o Topics to be covered: o Composition and condensation o Surface density profile o Minimum mass of solar nebula PY4A01 Solar System Science Minimum Mass Solar Nebula (MMSN) o MMSN is not a nebula, but a protoplanetary disc. Protoplanetary disk Nebula o Gives minimum mass of solid material to build the 8 planets. PY4A01 Solar System Science Minimum mass of the solar nebula o Can make approximation of minimum amount of solar nebula material that must have been present to form planets. Know: 1. Current masses, composition, location and radii of the planets. 2. Cosmic elemental abundances. 3. Condensation temperatures of material. o Given % of material that condenses, can calculate minimum mass of original nebula from which the planets formed. • Figure from Page 115 of “Physics & Chemistry of the Solar System” by Lewis o Steps 1-8: metals & rock, steps 9-13: ices PY4A01 Solar System Science Nebula composition o Assume solar/cosmic abundances: Representative Main nebular Fraction of elements Low-T material nebular mass H, He Gas 98.4 % H2, He C, N, O Volatiles (ices) 1.2 % H2O, CH4, NH3 Si, Mg, Fe Refractories 0.3 % (metals, silicates) PY4A01 Solar System Science Minimum mass for terrestrial planets o Mercury:~5.43 g cm-3 => complete condensation of Fe (~0.285% Mnebula). 0.285% Mnebula = 100 % Mmercury => Mnebula = (100/ 0.285) Mmercury = 350 Mmercury o Venus: ~5.24 g cm-3 => condensation from Fe and silicates (~0.37% Mnebula). =>(100% / 0.37% ) Mvenus = 270 Mvenus o Earth/Mars: 0.43% of material condensed at cooler temperatures. -
Exep Science Plan Appendix (SPA) (This Document)
ExEP Science Plan, Rev A JPL D: 1735632 Release Date: February 15, 2019 Page 1 of 61 Created By: David A. Breda Date Program TDEM System Engineer Exoplanet Exploration Program NASA/Jet Propulsion Laboratory California Institute of Technology Dr. Nick Siegler Date Program Chief Technologist Exoplanet Exploration Program NASA/Jet Propulsion Laboratory California Institute of Technology Concurred By: Dr. Gary Blackwood Date Program Manager Exoplanet Exploration Program NASA/Jet Propulsion Laboratory California Institute of Technology EXOPDr.LANET Douglas Hudgins E XPLORATION PROGRAMDate Program Scientist Exoplanet Exploration Program ScienceScience Plan Mission DirectorateAppendix NASA Headquarters Karl Stapelfeldt, Program Chief Scientist Eric Mamajek, Deputy Program Chief Scientist Exoplanet Exploration Program JPL CL#19-0790 JPL Document No: 1735632 ExEP Science Plan, Rev A JPL D: 1735632 Release Date: February 15, 2019 Page 2 of 61 Approved by: Dr. Gary Blackwood Date Program Manager, Exoplanet Exploration Program Office NASA/Jet Propulsion Laboratory Dr. Douglas Hudgins Date Program Scientist Exoplanet Exploration Program Science Mission Directorate NASA Headquarters Created by: Dr. Karl Stapelfeldt Chief Program Scientist Exoplanet Exploration Program Office NASA/Jet Propulsion Laboratory California Institute of Technology Dr. Eric Mamajek Deputy Program Chief Scientist Exoplanet Exploration Program Office NASA/Jet Propulsion Laboratory California Institute of Technology This research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration. © 2018 California Institute of Technology. Government sponsorship acknowledged. Exoplanet Exploration Program JPL CL#19-0790 ExEP Science Plan, Rev A JPL D: 1735632 Release Date: February 15, 2019 Page 3 of 61 Table of Contents 1. -
Protoplanetary Disks, Jets, and the Birth of the Stars
Spanish SKA White Book, 2015 Anglada et al. 169 Protoplanetary disks, jets, and the birth of the stars G. Anglada1, M. Tafalla2, C. Carrasco-Gonz´alez3, I. de Gregorio-Monsalvo4, R. Estalella5, N. Hu´elamo6, O.´ Morata7, M. Osorio1, A. Palau3, and J.M. Torrelles8 1 Instituto de Astrof´ısica de Andaluc´ıa,CSIC, E-18008 Granada, Spain 2 Observatorio Astron´omicoNacional-IGN, E-28014 Madrid, Spain 3 Centro de Radioastronom´ıay Astrof´ısica,UNAM, 58090 Morelia, Michoac´an,Mexico 4 Joint ALMA Observatory, Santiago de Chile, Chile 5 Departament d'Astronomia i Meteorologia, Univ. de Barcelona, E-08028 Barcelona, Spain 6 Centro de Astrobiolog´ıa(INTA-CSIC), E-28691 Villanueva de la Ca~nada,Spain 7 Institute of Astronomy and Astrophysics, Academia Sinica, Taipei 106, Taiwan 8 Instituto de Ciencias del Espacio (CSIC)-UB/IEEC, E-08028 Barcelona, Spain Abstract Stars form as a result of the collapse of dense cores of molecular gas and dust, which arise from the fragmentation of interstellar (parsec-scale) molecular clouds. Because of the initial rotation of the core, matter does not fall directly onto the central (proto)star but through a circumstellar accretion disk. Eventually, as a result of the evolution of this disk, a planetary system will be formed. A fraction of the infalling matter is ejected in the polar direction as a collimated jet that removes the excess of mass and angular momentum, and allows the star to reach its final mass. Thus, the star formation process is intimately related to the development of disks and jets. Radio emission from jets is useful to trace accurately the position of the most embedded objects, from massive protostars to proto-brown dwarfs. -
Exoplanet Exploration Collaboration Initiative TP Exoplanets Final Report
EXO Exoplanet Exploration Collaboration Initiative TP Exoplanets Final Report Ca Ca Ca H Ca Fe Fe Fe H Fe Mg Fe Na O2 H O2 The cover shows the transit of an Earth like planet passing in front of a Sun like star. When a planet transits its star in this way, it is possible to see through its thin layer of atmosphere and measure its spectrum. The lines at the bottom of the page show the absorption spectrum of the Earth in front of the Sun, the signature of life as we know it. Seeing our Earth as just one possibly habitable planet among many billions fundamentally changes the perception of our place among the stars. "The 2014 Space Studies Program of the International Space University was hosted by the École de technologie supérieure (ÉTS) and the École des Hautes études commerciales (HEC), Montréal, Québec, Canada." While all care has been taken in the preparation of this report, ISU does not take any responsibility for the accuracy of its content. Electronic copies of the Final Report and the Executive Summary can be downloaded from the ISU Library website at http://isulibrary.isunet.edu/ International Space University Strasbourg Central Campus Parc d’Innovation 1 rue Jean-Dominique Cassini 67400 Illkirch-Graffenstaden Tel +33 (0)3 88 65 54 30 Fax +33 (0)3 88 65 54 47 e-mail: [email protected] website: www.isunet.edu France Unless otherwise credited, figures and images were created by TP Exoplanets. Exoplanets Final Report Page i ACKNOWLEDGEMENTS The International Space University Summer Session Program 2014 and the work on the -
Terrestrial Planets in High-Mass Disks Without Gas Giants
A&A 557, A42 (2013) Astronomy DOI: 10.1051/0004-6361/201321304 & c ESO 2013 Astrophysics Terrestrial planets in high-mass disks without gas giants G. C. de Elía, O. M. Guilera, and A. Brunini Facultad de Ciencias Astronómicas y Geofísicas, Universidad Nacional de La Plata and Instituto de Astrofísica de La Plata, CCT La Plata-CONICET-UNLP, Paseo del Bosque S/N, 1900 La Plata, Argentina e-mail: [email protected] Received 15 February 2013 / Accepted 24 May 2013 ABSTRACT Context. Observational and theoretical studies suggest that planetary systems consisting only of rocky planets are probably the most common in the Universe. Aims. We study the potential habitability of planets formed in high-mass disks without gas giants around solar-type stars. These systems are interesting because they are likely to harbor super-Earths or Neptune-mass planets on wide orbits, which one should be able to detect with the microlensing technique. Methods. First, a semi-analytical model was used to define the mass of the protoplanetary disks that produce Earth-like planets, super- Earths, or mini-Neptunes, but not gas giants. Using mean values for the parameters that describe a disk and its evolution, we infer that disks with masses lower than 0.15 M are unable to form gas giants. Then, that semi-analytical model was used to describe the evolution of embryos and planetesimals during the gaseous phase for a given disk. Thus, initial conditions were obtained to perform N-body simulations of planetary accretion. We studied disks of 0.1, 0.125, and 0.15 M. -
Volatiles in Protoplanetary Disks
Volatiles in Protoplanetary Disks Thesis by Ke Zhang In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy California Institute of Technology Pasadena, California 2015 (Defended May 15, 2015) ii c 2015 Ke Zhang All Rights Reserved iii Acknowledgements First and foremost, I would like to thank my advisor, Geoffrey Blake, for his patience, guidance, support, and inspiration that made this thesis possible. In retrospect, I am so grateful to have chosen Geoff as my mentor. He is a very special kind of advisor, so rare in the fast-paced world, who can be incredibly patient, waiting for a student to find her passion. But once the student has made up her mind, and starts to ask for resources, opportunities, and attention, he is so supportive and resourceful that the only limitation for the student is herself. It was a great privilege working with Geoff, who is ingeniously creative and vastly knowledgeable. Thank you for all the lessons, support, and, most importantly, for believing in and encouraging me. I'm also thankful for John Carpenter who opened for me the wonderful door of (sub)mm-wave interferometry and gave me a very first opportunity to work with ALMA data. John, you are my role model as a rigorous scientist who understands his field profoundly and is dedicated to getting things right. I would also like to thank Colette Salyk for being such a great mentor and a supportive friend during my years in graduate school. Thanks for taking me to the summit of Mauna Kea and beautiful Charlottesville. -
Origin of Water Ice in the Solar System 309
Lunine: Origin of Water Ice in the Solar System 309 Origin of Water Ice in the Solar System Jonathan I. Lunine Lunar and Planetary Laboratory The origin and early distribution of water ice and more volatile compounds in the outer solar system is considered. The origin of water ice during planetary formation is at least twofold: It condenses beyond a certain distance from the proto-Sun — no more than 5 AU but perhaps as close as 2 AU — and it falls in from the surrounding molecular cloud. Because some of the infalling water ice is not sublimated in the ambient disk, complete mixing between these two sources was not achieved, and at least two populations of icy planetesimals may have been present in the protoplanetary disk. Added to this is a third reservoir of water ice planetesimals representing material chemically processed and then condensed in satellite-forming disks around giant planets. Water of hydration in silicates inward of the condensation front might be a sepa- rate source, if the hydration occurred directly from the nebular disk and not later in the parent bodies. The differences among these reservoirs of icy planetesimals ought to be reflected in diverse composition and abundance of trapped or condensed species more volatile than the water ice matrix, although radial mixing may have erased most of the differences. Possible sources of water for Earth are diverse, and include Mars-sized hydrated bodies in the asteroid belt, smaller “asteroidal” bodies, water adsorbed into dry silicate grains in the nebula, and comets. These different sources may be distinguished by their deuterium-to-hydrogen ratio, and by pre- dictions on the relative amounts of water (and isotopic compositional differences) between Earth and Mars. -
Formation and Evolution of Exoplanets
Formation and Evolution of Exoplanets Edited by Rory Barnes Astronomy Department University of Washington Box 351580 Seattle, WA 98195-1850, USA Chapter 1 { Exoplanet Observations, Jacob L. Bean Chapter 2 { Pinpointing Planets in Circumstellar Disks, Alice C. Quillen Chapter 3 { Planet-Planet Interactions, Rory Barnes Chapter 4 { Formation Via Disk Instability, Lucio Mayer Chapter 5 { Core Accretion Model, Olenka Hubickyj Chapter 6 { Formation of Terrestrial Planets, Sean N. Raymond Chapter 7 { Brown Dwarfs, Kevin Luhman Chapter 8 { Exoplanet Chemistry, Katharina Lodders Chapter 9 { Migration and Multiplicity E ects During Giant Planet Formation, Edward W. Thommes Chapter 10 { Planets in Mean Motion Resonance, Wilhelm Kley Chapter 11 { Planet{Planet Gravitational Scattering, Francesco Marzari Chapter 12 { Tides and Exoplanets, Brian Jackson, Rory Barnes & Richard Greenberg Chapter 1 { Exoplanet Observations Jacob L. Bean Institut furAstrophysik Friedrich-Hund-Platz 1 37077 Gottingen Germany The discovery and characterization of planets around other stars has revolutionized our view of planetary system formation and evolution. In this chapter, we summarize the main results from the observational study of exoplanetary systems in the context of how they constrain theory. We focus on the robust ndings that have emerged from examining the orbital, physical, and host star properties of large samples of detected exoplanets. We also describe the limitations and biases of current observational methods and potential overinterpretations of the data that should be avoided. In addition, we discuss compelling individual results that o er views beyond the well explored parameter spaces. Chapter 2 { Pinpointing Planets in Circumstellar Disks Alice C. Quillen Dept. of Physics and Astronomy University of Rochester Rochester, NY 14627 USA Recent observations of circumstellar disks have revealed a variety of interesting morphology: clearings, pu ed up disk edges, gaps, spiral-like features, warps, clumps, and lopsidedness. -
Planet Hunters TESS I: TOI 813, a Subgiant Hosting a Transiting Saturn-Sized Planet on an 84-Day Orbit
MNRAS 000,1{16 (2019) Preprint 15 January 2020 Compiled using MNRAS LATEX style file v3.0 Planet Hunters TESS I: TOI 813, a subgiant hosting a transiting Saturn-sized planet on an 84-day orbit N. L. Eisner ,1? O. Barrag´an,1 S. Aigrain,1 C. Lintott,1 G. Miller,1 N. Zicher,1 T. S. Boyajian,2 C. Brice~no,3 E. M. Bryant,4;5 J. L. Christiansen,6 A. D. Feinstein,7 L. M. Flor-Torres,8 M. Fridlund,9;10 D. Gandolfi,11 J. Gilbert,12 N. Guerrero,13 J. M. Jenkins,6 K. Jones, 1 M. H. Kristiansen,14 A. Vanderburg,15 N. Law,16 A. R. L´opez-S´anchez,17;18 A. W. Mann,16 E. J. Safron,2 M. E. Schwamb,19;20 K. G. Stassun,21;22 H. P. Osborn,23 J. Wang,24 A. Zic,25;26 C. Ziegler,27 F. Barnet,28 S. J. Bean,28 D. M. Bundy,28 Z. Chetnik,28 J. L. Dawson,28 J. Garstone,28 A. G. Stenner,28 M. Huten,28 S. Larish,28 L. D. Melanson28 T. Mitchell,28 C. Moore,28 K. Peltsch,28 D. J. Rogers,28 C. Schuster,28 D. S. Smith,28 D. J. Simister,28 C. Tanner,28 I. Terentev 28 and A. Tsymbal28 Affiliations are listed at the end of the paper. Submitted on 12 September 2019; revised on 19 December 2019; accepted for publication by MNRAS on 8 January 2020. ABSTRACT We report on the discovery and validation of TOI 813 b (TIC 55525572 b), a tran- siting exoplanet identified by citizen scientists in data from NASA's Transiting Exo- planet Survey Satellite (TESS) and the first planet discovered by the Planet Hunters TESS project. -
Timescales of the Solar Protoplanetary Disk 233
Russell et al.: Timescales of the Solar Protoplanetary Disk 233 Timescales of the Solar Protoplanetary Disk Sara S. Russell The Natural History Museum Lee Hartmann Harvard-Smithsonian Center for Astrophysics Jeff Cuzzi NASA Ames Research Center Alexander N. Krot Hawai‘i Institute of Geophysics and Planetology Matthieu Gounelle CSNSM–Université Paris XI Stu Weidenschilling Planetary Science Institute We summarize geochemical, astronomical, and theoretical constraints on the lifetime of the protoplanetary disk. Absolute Pb-Pb-isotopic dating of CAIs in CV chondrites (4567.2 ± 0.7 m.y.) and chondrules in CV (4566.7 ± 1 m.y.), CR (4564.7 ± 0.6 m.y.), and CB (4562.7 ± 0.5 m.y.) chondrites, and relative Al-Mg chronology of CAIs and chondrules in primitive chon- drites, suggest that high-temperature nebular processes, such as CAI and chondrule formation, lasted for about 3–5 m.y. Astronomical observations of the disks of low-mass, pre-main-se- quence stars suggest that disk lifetimes are about 3–5 m.y.; there are only few young stellar objects that survive with strong dust emission and gas accretion to ages of 10 m.y. These con- straints are generally consistent with dynamical modeling of solid particles in the protoplanetary disk, if rapid accretion of solids into bodies large enough to resist orbital decay and turbulent diffusion are taken into account. 1. INTRODUCTION chondritic meteorites — chondrules, refractory inclusions [Ca,Al-rich inclusions (CAIs) and amoeboid olivine ag- Both geochemical and astronomical techniques can be gregates (AOAs)], Fe,Ni-metal grains, and fine-grained ma- applied to constrain the age of the solar system and the trices — are largely crystalline, and were formed from chronology of early solar system processes (e.g., Podosek thermal processing of these grains and from condensation and Cassen, 1994). -
Examining Habitability of Kepler Exoplanets Maria Kalambokidis¹
Examining Habitability of Kepler Exoplanets Maria Kalambokidis¹ Department of Astronomy, University of Wisconsin-Madison Abstract Since its launch in 2009, the Kepler spacecraft has confrmed the existence of 3,387 exoplanets with the goal of fnding habitable environments beyond our own. The mechanism capable of stabilizing a planet’s climate is the long-term carbon cycle driven by plate tectonics. We determined the likelihood of plate tectonics for Kepler exoplanets by comparing their interior structures to planets within our solar system. We used the mineral physics toolkit BurnMan to create three models with the same composition as Earth, Mars, and Mercury. We ran 19 exoplanets through the models and calculated their Mantle Radius Fraction (MRF). We found that four exoplanets may be Chthonian, four have Mercury-like MRF values, and two are Earth- like in their MRF values but did not lie within their habitable zone. In the future, as more exoplanet masses are obtained, it is likely that a greater number will appear dynamically similar to the Earth. Introduction Kepler Exoplanets. In the 21st century, the feld of astrobiology has grown tremendously, harnessing the technological and scientifc advancements capable of addressing some of our most fundamental inquiries about life in the universe. Since its launch in 2009, the Kepler spacecraft has utilized transit photometry to explore the diversity of planetary systems beyond our own, confrming the existence of 3,387 exoplanets to date. Many studies have analyzed Kepler’s confrmed exoplanets in an attempt to describe their “Earth-like” properties. Comparisons with the Earth are made considering size (radius) and orbital environment, which is described using the period, semi-major axis, and insolation fux (Batalha 2014).