Planets Galore
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
SETI Is Part of Astrobiology
SETI is Part of Astrobiology Jason T. Wright Department of Astronomy & Physics Center for Exoplanets and Habitable Worlds Penn State University Phone: (814) 863-8470 [email protected] I. SETI is Part of Astrobiology “Traditional SETI is not part of astrobiology” declares the NASA Astrobiology Strategy 2015 document (p. 150). This is incorrect.1 Astrobiology is the study of life in the universe, in particular its “origin, evolution, distribution, and future in the universe.” [emphasis mine] Searches for biosignatures are searches for the results of interactions between life and its environment, and could be sensitive to even primitive life on other worlds. As such, these searches focus on the origin and evolution of life, using past life on Earth as a guide. But some of the most obvious ways in which Earth is inhabited today are its technosignatures such as radio transmissions, alterations of its atmosphere by industrial pollutants, and probes throughout the Solar System. It seems clear that the future of life on Earth includes the development of ever more obvious technosignatures. Indeed, the NASA Astrobiology Strategy 2015 document acknowledges “the possibility” that such technosignatures exist, but erroneously declares them to be “not part of contemporary SETI,” and mentions them only to declare that we should “be aware of the possibility” and to “be sure to include [technosignatures] as a possible kind of interpretation we should consider as we begin to get data on the exoplanets.” In other words, while speculation on the nature of biosignatures and the design of multi-billion dollar missions to find those signatures is consistent with NASA’s vision for astrobiology, speculation on the nature of technosignatures and the design of observations to find them is not. -
Predicting Exoplanet Observability in Time, Contrast, Separation, and Polarization, in Scattered Light
A&A 578, A59 (2015) Astronomy DOI: 10.1051/0004-6361/201424202 & c ESO 2015 Astrophysics Predicting exoplanet observability in time, contrast, separation, and polarization, in scattered light Guillaume Schworer1;2 and Peter G. Tuthill2 1 LESIA, Observatoire de Paris, CNRS/UMR 8109, UPMC, Université Paris Diderot, 5 place J. Janssen, 92195 Meudon, France e-mail: [email protected] 2 Sydney Institute for Astronomy (SIfA), School of Physics, The University of Sydney, NSW 2006, Australia Received 14 May 2014 / Accepted 14 March 2015 ABSTRACT Context. Polarimetry is one of the keys to enhanced direct imaging of exoplanets. Not only does it deliver a differential observable pro- viding extra contrast, but when coupled with spectroscopy, it also reveals valuable information on the exoplanetary atmospheric com- position. Nevertheless, angular separation and contrast ratio to the host-star make for extremely challenging observation. Producing detailed predictions for exactly how the expected signals should appear is of critical importance for the designs and observational strategies of tomorrow’s telescopes. Aims. We aim at accurately determining the magnitudes and evolution of the main observational signatures for imaging an exoplanet: separation, contrast ratio to the host-star and polarization as a function of the orbital geometry and the reflectance parameters of the exoplanet. Methods. These parameters were used to construct a polarized-reflectance model based on the input of orbital parameters and two albedo values. The model is able to calculate a variety of observational predictions for exoplanets at any orbital time. Results. The inter-dependency of the three main observational criteria – angular separation, contrast ratio, polarization – result in a complex time-evolution of the system. -
University of California Santa Cruz
UNIVERSITY OF CALIFORNIA SANTA CRUZ BENEATH THE SURFACE OF GIANT PLANETS: EVOLUTION, STRUCTURE, AND COMPOSITION A dissertation submitted in partial satisfaction of the requirements for the degree of DOCTOR OF PHILOSOPHY in ASTRONOMY AND ASTROPHYSICS by Neil L Kelly Miller March 2013 The Dissertation of Neil L Kelly Miller is approved: Jonathan Fortney, Chair Professor D. Lin Professor P. Garaud Professor P. Bodenheimer Tyrus Miller Vice Provost and Dean of Graduate Studies Copyright c by Neil L Kelly Miller 2013 Table of Contents List of Figures v List of Tables xii Abstract xiii Dedication xv Acknowledgments xvi 1 Introduction 1 1.1 TheSolarSystemGiantPlanets . 3 1.2 FromIndividualSystemstoSamples . 4 1.3 Physical Processes in the Evolution of Giant Planets . ........ 8 2 Coupled Thermal and Tidal Evolution of Giant Expolanets 14 2.1 Abstract.................................... 14 2.2 Introduction.................................. 15 2.3 Model:Introduction ............................. 21 2.4 Model:Implementation ........................... 23 2.5 GeneralExamples .............................. 29 2.6 Results..................................... 37 2.6.1 SpecificSystems ........................... 37 2.6.2 SummaryforSuite .......................... 47 ′ 2.6.3 High Qs cases............................. 56 2.7 Discussion&Conclusions . 59 3 Applications of Giant Planet Thermal Evolution Model 74 3.1 Introduction.................................. 74 3.2 CoRoT-2b: Young Planet With Potentially Tidally Inflated Radius . 75 3.3 CoRoT-7b: Potential Evaporative Mass Loss Scenario . ....... 78 3.3.1 EvaporativeMassLossModel. 80 iii 3.3.2 PlanetEvolution ........................... 82 3.4 Kepler11 ................................... 82 3.4.1 Formation and Compositions of Kepler 11 Planets . 82 4 Measuring the Heavy Element Composition of Giant Exoplanets with Lower Irradiation 86 4.1 Abstract.................................... 86 4.2 Introduction.................................. 87 4.3 ModelandMethod............................. -
Lecture-29 (PDF)
Life in the Universe Orin Harris and Greg Anderson Department of Physics & Astronomy Northeastern Illinois University Spring 2021 c 2012-2021 G. Anderson., O. Harris Universe: Past, Present & Future – slide 1 / 95 Overview Dating Rocks Life on Earth How Did Life Arise? Life in the Solar System Life Around Other Stars Interstellar Travel SETI Review c 2012-2021 G. Anderson., O. Harris Universe: Past, Present & Future – slide 2 / 95 Dating Rocks Zircon Dating Sedimentary Grand Canyon Life on Earth How Did Life Arise? Life in the Solar System Life Around Dating Rocks Other Stars Interstellar Travel SETI Review c 2012-2021 G. Anderson., O. Harris Universe: Past, Present & Future – slide 3 / 95 Zircon Dating Zircon, (ZrSiO4), minerals incorporate trace amounts of uranium but reject lead. Naturally occuring uranium: • U-238: 99.27% • U-235: 0.72% Decay chains: • 238U −→ 206Pb, τ =4.47 Gyrs. • 235U −→ 207Pb, τ = 704 Myrs. 1956, Clair Camron Patterson dated the Canyon Diablo meteorite: τ =4.55 Gyrs. c 2012-2021 G. Anderson., O. Harris Universe: Past, Present & Future – slide 4 / 95 Dating Sedimentary Rocks • Relative ages: Deeper layers were deposited earlier • Absolute ages: Decay of radioactive isotopes old (deposited last) oldest (depositedolder first) c 2012-2021 G. Anderson., O. Harris Universe: Past, Present & Future – slide 5 / 95 Grand Canyon: Earth History from 200 million - 2 billion yrs ago. Dating Rocks Life on Earth Earth History Timeline Late Heavy Bombardment Hadean Shark Bay Stromatolites Cyanobacteria Q: Earliest Fossils? Life on Earth O2 History Q: Life on Earth How Did Life Arise? Life in the Solar System Life Around Other Stars Interstellar Travel SETI Review c 2012-2021 G. -
A Flexible Bayesian Framework for Assessing Habitability with Joint Observational and Model Constraints
A Flexible Bayesian Framework for Assessing Habitability with Joint Observational and Model Constraints Amanda R. Truitt1, Patrick A. Young2, Sara I. Walker2, Alexander Spacek1 ABSTRACT The catalog of stellar evolution tracks discussed in our previous work is meant to help characterize exoplanet host-stars of interest for follow-up observations with future missions like JWST. However, the utility of the catalog has been predicated on the assumption that we would precisely know the age of the par- ticular host-star in question; in reality, it is unlikely that we will be able to accurately estimate the age of a given system. Stellar age is relatively straight- forward to calculate for stellar clusters, but it is difficult to accurately measure the age of an individual star to high precision. Unfortunately, this is the kind of information we should consider as we attempt to constrain the long-term habit- ability potential of a given planetary system of interest. This is ultimately why we must rely on predictions of accurate stellar evolution models, as well a con- sideration of what we can observably measure (stellar mass, composition, orbital radius of an exoplanet) in order to create a statistical framework wherein we can identify the best candidate systems for follow-up characterization. In this paper we discuss a statistical approach to constrain long-term planetary habitability by evaluating the likelihood that at a given time of observation, a star would have a planet in the 2 Gy continuously habitable zone (CHZ2). Additionally, we will discuss how we can use existing observational data (i.e. -
Transit Timing Analysis of the Hot Jupiters WASP-43B and WASP-46B and the Super Earth Gj1214b
Transit timing analysis of the hot Jupiters WASP-43b and WASP-46b and the super Earth GJ1214b Mathias Polfliet Promotors: Michaël Gillon, Maarten Baes 1 Abstract Transit timing analysis is proving to be a promising method to detect new planetary partners in systems which already have known transiting planets, particularly in the orbital resonances of the system. In these resonances we might be able to detect Earth-mass objects well below the current detection and even theoretical (due to stellar variability) thresholds of the radial velocity method. We present four new transits for WASP-46b, four new transits for WASP-43b and eight new transits for GJ1214b observed with the robotic telescope TRAPPIST located at ESO La Silla Observatory, Chile. Modelling the data was done using several Markov Chain Monte Carlo (MCMC) simulations of the new transits with old data and a collection of transit timings for GJ1214b from published papers. For the hot Jupiters this lead to a general increase in accuracy for the physical parameters of the system (for the mass and period we found: 2.034±0.052 MJup and 0.81347460±0.00000048 days and 2.03±0.13 MJup and 1.4303723±0.0000011 days for WASP-43b and WASP-46b respectively). For GJ1214b this was not the case given the limited photometric precision of TRAPPIST. The additional timings however allowed us to constrain the period to 1.580404695±0.000000084 days and the RMS of the TTVs to 16 seconds. We investigated given systems for Transit Timing Variations (TTVs) and variations in the other transit parameters and found no significant (3sv) deviations. -
Optical SETI: the All-Sky Survey
Professor van der Veen Project Scientist, UCSB Department of Physics, Experimental Cosmology Group class 4 [email protected] frequencies/wavelengths that get through the atmosphere The Planetary Society http://www.planetary.org/blogs/jason-davis/2017/20171025-seti-anybody-out-there.html THE ATMOSPHERE'S EFFECT ON ELECTROMAGNETIC RADIATION Earth's atmosphere prevents large chunks of the electromagnetic spectrum from reaching the ground, providing a natural limit on where ground-based observatories can search for SETI signals. Searching for technology that we have, or are close to having: Continuous radio searches Pulsed radio searches Targeted radio searches All-sky surveys Optical: Continuous laser and near IR searches Pulsed laser searches a hypothetical laser beacon watch now: https://www.youtube.com/watch?time_continue=41&v=zuvyhxORhkI Theoretical physicist Freeman Dyson’s “First Law of SETI Investigations:” Every search for alien civilizations should be planned to give interesting results even when no aliens are discovered. Interview with Carl Sagan from 1978: Start at 6:16 https://www.youtube.com/watch?v=g- Q8aZoWqF0&feature=youtu.be Anomalous signal recorded by Big Ear Telescope at Ohio State University. Big Ear was a flat, aluminum dish three football fields wide, with reflectors at both ends. Signal was at 1,420 MHz, the hydrogen 21 cm ‘spin flip’ line. http://www.bigear.org/Wow30th/wow30th.htm May 15, 2015 A Russian observatory reports a strong signal from a Sun-like star. Possibly from advanced alien civilization. The RATAN-600 radio telescope in Zelenchukskaya, at the northern foot of the Caucasus Mountains location: star HD 164595 G-type star (like our Sun) 94.35 ly away, visually located in constellation Hercules 1 planet that orbits it every 40 days unusual radio signal detected – 11 GHz (2.7 cm) claim: Signal from a Type II Kardashev civilization Only one observation Not confirmed by other telescopes Russian Academy of Sciences later retracted the claim that it was an ETI signal, stating the signal came from a military satellite. -
Astrophysics Division Astrophysics Douglas Hudgins Program Scientist, Exoplanet Exploration Program Key NASA/SMD Science Themes
National Aeronautics and Space Administration NASA and the Search for Life on Planets around Other Stars A presentation to the National Academies Committee on Exoplanet Science Strategy 6 March 2018 Paul Hertz Director, Astrophysics Division Astrophysics Douglas Hudgins Program Scientist, Exoplanet Exploration Program Key NASA/SMD Science Themes Protect and Improve Life on Earth Search for Life Elsewhere Discover the Secrets of the Universe 2 Talk summary 3 NASA’s Exoplanet Exploration Program Space Missions and Mission Studies Public Communications Kepler, WFIRST Decadal Studies K2 Starshade Coronagraph Supporting Research & Technology Key Sustaining Research NASA Exoplanet Science Institute Technology Development Coronagraph Masks Large Binocular Keck Single Aperture Telescope Interferometer Imaging and RV High-Contrast Deployable Archives, Tools, Sagan Fellowships, Imaging Starshades Professional Engagement NN-EXPLORE https://exoplanets.nasa.gov 4 Foundational Documents for the NASA’s Astrophysics Division 5 NASA’s cross-divisional Search for Life Elsewhere ASTROPHYSICS • Exoplanet detection and Planetary SCIENCE/ characterization ASTROBIOLOGY • Stellar characterization • Comparative planetology • Mission data analysis • Planetary atmospheres Hubble, Spitzer, Kepler, • Assessment of observable TESS, JWST, WFIRST, biosignatures etc. • Habitability EARTH SCIENCES • GCM • Planets as systems PLANETARY SCIENCE RESEARCH HELIOPHYSICS • Exoplanet characterization • Stellar characterization • Protoplanetary disks • Stellar winds • Planet formation • Detection of planetary • Comparative planetology magnetospheres 6 Exoplanet Exploration at NASA 2007 - present 7 The Spitzer Space Telescope For the last decade, the Spitzer Space Telescope has used both spectroscopic and photometric measurements in the mid-IR to probe exoplanets and exoplanetary systems. • Spitzer follow up observations of known transiting systems have revealed additional, new planets and helped refine measurements of the size and orbital dynamics of known planets as small as the Earth. -
“Formas Primitivas” De Ideias Oopulares
A FORMA DAS IDEIAS A Câmara Estenopeica Como Método de Destilação de “Formas Primitivas” de Ideias Populares (Expressões Idiomáticas) Salomé Filipa Pereira Arieira Tese de Doutoramento Directora Mª Sol Alonso Romera Facultad de Bellas Artes de Pontevedra Departamento de Dibujo Setembro 2015 Aos meus dois amores: ao meu marido Tony Oliveira e ao meu filho Gaspar, pelo amor infinito e indescritível com que recheiam os meus dias. Aos meus pais Odete e Filipe, pela coragem exemplar e pelo apoio que me transmitem sempre, desde o meu primeiro momento no mundo. À Diretora desta Tese, Sol Alonso, pela disponibilidade total que demonstrou ao longo destes anos para me guiar e acompanhar, e pela amizade e sabedoria com que desde sempre me presenteou. À Direção da Escola Artística de Soares dos Reis por todo o apoio dado ao longo destes últimos anos. Ao Miguel Paiva, à Luisa Fragoso e ao Leonardo Mira, por toda a colaboração e apoio prestados. Ao Miguel Borges (Cigano) pela disponibilidade demonstrada na cedência dos espaços que serviram de palco a várias imagens estenopeicas do projeto prático desta investigação. À Lurdes Arieira e à Claudia Tomás pelo empréstimo de alguns dos elementos fotografados (máquina de picar AGRADECIMENTOS carne e fichas de póquer). À Joana Castelo e ao David, pela gentileza que tiveram na digitalização dos negativos do projeto prático. À Sara e ao André (Blues Photography) pelo cuidado nas impressões fotográficas do projeto prático (versão impressa). À Eduarda Coelho, por me ter salvo no momento da análise sintática das Expressões Idiomáticas. À Maria Peña, cuja amizade se estende desde o início do Curso de Doutoramento, superanto barreiras físicas e temporais. -
Astrobiology and the Search for Life Beyond Earth in the Next Decade
Astrobiology and the Search for Life Beyond Earth in the Next Decade Statement of Dr. Andrew Siemion Berkeley SETI Research Center, University of California, Berkeley ASTRON − Netherlands Institute for Radio Astronomy, Dwingeloo, Netherlands Radboud University, Nijmegen, Netherlands to the Committee on Science, Space and Technology United States House of Representatives 114th United States Congress September 29, 2015 Chairman Smith, Ranking Member Johnson and Members of the Committee, thank you for the opportunity to testify today. Overview Nearly 14 billion years ago, our universe was born from a swirling quantum soup, in a spectacular and dynamic event known as the \big bang." After several hundred million years, the first stars lit up the cosmos, and many hundreds of millions of years later, the remnants of countless stellar explosions coalesced into the first planetary systems. Somehow, through a process still not understood, the laws of physics guiding the unfolding of our universe gave rise to self-replicating organisms − life. Yet more perplexing, this life eventually evolved a capacity to know its universe, to study it, and to question its own existence. Did this happen many times? If it did, how? If it didn't, why? SETI (Search for ExtraTerrestrial Intelligence) experiments seek to determine the dis- tribution of advanced life in the universe through detecting the presence of technology, usually by searching for electromagnetic emission from communication technology, but also by searching for evidence of large scale energy usage or interstellar propulsion. Technology is thus used as a proxy for intelligence − if an advanced technology exists, so to does the ad- vanced life that created it. -
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. -
Snowball Earth: a Thin-Ice Solution with Flowing Sea Glaciers’’ by David Pollard and James F
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, C09016, doi:10.1029/2005JC003411, 2006 Click Here for Full Article Comment on ‘‘Snowball Earth: A thin-ice solution with flowing sea glaciers’’ by David Pollard and James F. Kasting Stephen G. Warren1,2 and Richard E. Brandt1 Received 22 November 2005; revised 22 May 2006; accepted 9 June 2006; published 14 September 2006. Citation: Warren, S. G., and R. E. Brandt (2006), Comment on ‘‘Snowball Earth: A thin-ice solution with flowing sea glaciers’’ by David Pollard and James F. Kasting, J. Geophys. Res., 111, C09016, doi:10.1029/2005JC003411. 1. Introduction 2. Choices of Model Variables That Favor [1] Pollard and Kasting [2005] (hereinafter referred to as Thin Ice PK) have coupled an energy-balance climate model to an 2.1. Albedo of Cold Glacier Ice ice-shelf flow model, to investigate the Snowball Earth [2] As sea glaciers flowed equatorward into the tropical episodes of the Neoproterozoic, 600–800 million years region of net sublimation, their surface snow and subsurface ago, when the ocean apparently froze all the way to the firn would sublimate away, exposing bare glacier ice to equator [Hoffman and Schrag, 2002]. PK’s particular con- the atmosphere and solar radiation. This ice would be cern was to investigate the possibility that over a wide freshwater (meteoric) ice, which originated from compres- equatorial band where sublimation exceeded snowfall, the sion of snow, so it would contain numerous bubbles, giving bare ice may have been thin enough to permit transmission a high albedo. The albedo of cold (nonmelting) glacier ice of sunlight to the water below, providing an extensive exposed by sublimation (Antarctic ‘‘blue ice’’) has been refugium for the photosynthetic eukaryotes that survived measured as 0.55–0.65 in four experiments in the Atlantic the Snowball events.