A Seminar Named: EARTH 2.0
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The Search for Another Earth – Part II
GENERAL ARTICLE The Search for Another Earth – Part II Sujan Sengupta In the first part, we discussed the various methods for the detection of planets outside the solar system known as the exoplanets. In this part, we will describe various kinds of exoplanets. The habitable planets discovered so far and the present status of our search for a habitable planet similar to the Earth will also be discussed. Sujan Sengupta is an 1. Introduction astrophysicist at Indian Institute of Astrophysics, Bengaluru. He works on the The first confirmed exoplanet around a solar type of star, 51 Pe- detection, characterisation 1 gasi b was discovered in 1995 using the radial velocity method. and habitability of extra-solar Subsequently, a large number of exoplanets were discovered by planets and extra-solar this method, and a few were discovered using transit and gravi- moons. tational lensing methods. Ground-based telescopes were used for these discoveries and the search region was confined to about 300 light-years from the Earth. On December 27, 2006, the European Space Agency launched 1The movement of the star a space telescope called CoRoT (Convection, Rotation and plan- towards the observer due to etary Transits) and on March 6, 2009, NASA launched another the gravitational effect of the space telescope called Kepler2 to hunt for exoplanets. Conse- planet. See Sujan Sengupta, The Search for Another Earth, quently, the search extended to about 3000 light-years. Both Resonance, Vol.21, No.7, these telescopes used the transit method in order to detect exo- pp.641–652, 2016. planets. Although Kepler’s field of view was only 105 square de- grees along the Cygnus arm of the Milky Way Galaxy, it detected a whooping 2326 exoplanets out of a total 3493 discovered till 2Kepler Telescope has a pri- date. -
The Subsurface Habitability of Small, Icy Exomoons J
A&A 636, A50 (2020) Astronomy https://doi.org/10.1051/0004-6361/201937035 & © ESO 2020 Astrophysics The subsurface habitability of small, icy exomoons J. N. K. Y. Tjoa1,?, M. Mueller1,2,3, and F. F. S. van der Tak1,2 1 Kapteyn Astronomical Institute, University of Groningen, Landleven 12, 9747 AD Groningen, The Netherlands e-mail: [email protected] 2 SRON Netherlands Institute for Space Research, Landleven 12, 9747 AD Groningen, The Netherlands 3 Leiden Observatory, Leiden University, Niels Bohrweg 2, 2300 RA Leiden, The Netherlands Received 1 November 2019 / Accepted 8 March 2020 ABSTRACT Context. Assuming our Solar System as typical, exomoons may outnumber exoplanets. If their habitability fraction is similar, they would thus constitute the largest portion of habitable real estate in the Universe. Icy moons in our Solar System, such as Europa and Enceladus, have already been shown to possess liquid water, a prerequisite for life on Earth. Aims. We intend to investigate under what thermal and orbital circumstances small, icy moons may sustain subsurface oceans and thus be “subsurface habitable”. We pay specific attention to tidal heating, which may keep a moon liquid far beyond the conservative habitable zone. Methods. We made use of a phenomenological approach to tidal heating. We computed the orbit averaged flux from both stellar and planetary (both thermal and reflected stellar) illumination. We then calculated subsurface temperatures depending on illumination and thermal conduction to the surface through the ice shell and an insulating layer of regolith. We adopted a conduction only model, ignoring volcanism and ice shell convection as an outlet for internal heat. -
Mars Mars Is the Fourth Terrestrial Planet. It Is Smaller in Size Than
Mars Mars is the fourth terrestrial planet. It is smaller in size than Earth and Venus, but larger than Mercury. Of the planets, Mars is the most hospitable to visiting humans, as it has an atmosphere, though it has no oxygen and is very thin. In the early days of the solar system, Mars has had liquid water on its surface, which is proved by the existence of various minerals that require liquid water to form. The current atmosphere of Mars is too thin and cold for liquid water to exist for long periods of times. Still, there is evidence of terrain shaped by flowing liquids, which are probably temporary flows or floods caused by the melting of ice in the ground. Mars has seasons like the Earth, and ice caps at the poles that grow and shrink over the course of the year. They consist of water ice and CO2 ice, the latter varying more with the seasons. One year on Mars is a bit less than two Earth years. Mars has two moons, Phobos and Deimos. They are very small compared to Mars, and are likely to be asteroids captured by Mars's gravity in the distant past. Giant planets and their moons The outer four planets of the solar system are known as the giant planets, because of their large size (compared to the terrestrial planets). The giant planets of our solar system can be further divided into two categories: gas giants (Jupiter and Saturn) and ice giants (Uranus and Neptune). The gas giants consist mainly of hydrogen (up to 90%) and helium, while the ice giants are mostly "ices" such as water and ammonia, with only some 20% of hydrogen. -
THE ZEN of MAGIC SQUARES, CIRCLES, and STARS Also by Clifford A
THE ZEN OF MAGIC SQUARES, CIRCLES, AND STARS Also by Clifford A. Pickover The Alien IQ Test Black Holes: A Traveler’s Guide Chaos and Fractals Chaos in Wonderland Computers and the Imagination Computers, Pattern, Chaos, and Beauty Cryptorunes Dreaming the Future Fractal Horizons: The Future Use of Fractals Frontiers of Scientific Visualization (with Stuart Tewksbury) Future Health: Computers and Medicine in the 21st Century The Girl Who Gave Birth t o Rabbits Keys t o Infinity The Loom of God Mazes for the Mind: Computers and the Unexpected The Paradox of God and the Science of Omniscience The Pattern Book: Fractals, Art, and Nature The Science of Aliens Spider Legs (with Piers Anthony) Spiral Symmetry (with Istvan Hargittai) The Stars of Heaven Strange Brains and Genius Surfing Through Hyperspace Time: A Traveler’s Guide Visions of the Future Visualizing Biological Information Wonders of Numbers THE ZEN OF MAGIC SQUARES, CIRCLES, AND STARS An Exhibition of Surprising Structures across Dimensions Clifford A. Pickover Princeton University Press Princeton and Oxford Copyright © 2002 by Clifford A. Pickover Published by Princeton University Press, 41 William Street, Princeton, New Jersey 08540 In the United Kingdom: Princeton University Press, 3 Market Place, Woodstock, Oxfordshire OX20 1SY All Rights Reserved Library of Congress Cataloging-in-Publication Data Pickover, Clifford A. The zen of magic squares, circles, and stars : an exhibition of surprising structures across dimensions / Clifford A. Pickover. p. cm Includes bibliographical references and index. ISBN 0-691-07041-5 (acid-free paper) 1. Magic squares. 2. Mathematical recreations. I. Title. QA165.P53 2002 511'.64—dc21 2001027848 British Library Cataloging-in-Publication Data is available This book has been composed in Baskerville BE and Gill Sans. -
Comparative Habitability of Transiting Exoplanets
Draft version October 1, 2015 A Preprint typeset using LTEX style emulateapj v. 04/17/13 COMPARATIVE HABITABILITY OF TRANSITING EXOPLANETS Rory Barnes1,2,3, Victoria S. Meadows1,2, Nicole Evans1,2 Draft version October 1, 2015 ABSTRACT Exoplanet habitability is traditionally assessed by comparing a planet’s semi-major axis to the location of its host star’s “habitable zone,” the shell around a star for which Earth-like planets can possess liquid surface water. The Kepler space telescope has discovered numerous planet candidates near the habitable zone, and many more are expected from missions such as K2, TESS and PLATO. These candidates often require significant follow-up observations for validation, so prioritizing planets for habitability from transit data has become an important aspect of the search for life in the universe. We propose a method to compare transiting planets for their potential to support life based on transit data, stellar properties and previously reported limits on planetary emitted flux. For a planet in radiative equilibrium, the emitted flux increases with eccentricity, but decreases with albedo. As these parameters are often unconstrained, there is an “eccentricity-albedo degeneracy” for the habitability of transiting exoplanets. Our method mitigates this degeneracy, includes a penalty for large-radius planets, uses terrestrial mass-radius relationships, and, when available, constraints on eccentricity to compute a number we call the “habitability index for transiting exoplanets” that represents the relative probability that an exoplanet could support liquid surface water. We calculate it for Kepler Objects of Interest and find that planets that receive between 60–90% of the Earth’s incident radiation, assuming circular orbits, are most likely to be habitable. -
Dynamical Evolution and Bombardment of the Early Solar System: a Few Highlights from the Last 50 Years
50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 1545.pdf DYNAMICAL EVOLUTION AND BOMBARDMENT OF THE EARLY SOLAR SYSTEM: A FEW HIGHLIGHTS FROM THE LAST 50 YEARS. W. F. Bottke1 1Southwest Research Institute and NASA’s SSERVI-ISET Team, Boulder, CO ([email protected]). Introduction. Over the last several decades, there orbital migration of Jupiter and Saturn in a gas disk, has been a transformation in our theoretical under- Jupiter could have migrated inward all the way to ~1.5 standing of early Solar System evolution. Historically, AU from the Sun. At that point Jupiter and Saturn it was thought that the planets and small bodies formed could have become trapped in their mutual 2:3 reso- near their current locations. Starting in the 1980’s with nance and would have begun to move outward. pioneering work by Ward, Lin, and Papaloizou, (for The Grand Tack model studied the gravitational planet–gas disk interactions) in the late 1970s and Fer- scattering of asteroids by Jupiter and Saturn during nandez and Ip (for planet–planetesimal disk interac- their inward, then outward migration. This model not tions) in the early 1980s, however, it has now become only reproduces the mass and mixture of spectral types clear that the structure of the Solar System most likely in the asteroid belt, but also truncates the planetesimal changed as the planets grew and migrated [e.g., 1, 2]. disk from which the terrestrial planets form, as in Han- Evidence for giant planet migration can be found in sen’s work. This allowed them to form a low-mass the orbital structures of the Kuiper belt, Trojans, irreg- Mars. -
Transmitting Signals Over Interstellar Distances: Three Approaches
Transmitting signals over interstellar distances: Three approaches compared in the context of the Drake equation Luc ARNOLD, Aix Marseille Université, CNRS, OHP (Observatoire de Haute Provence), Institut Pythéeas, UMS 3470, 04870 Saint-Michel-l’Observatoire, France Correspondance: Luc ARNOLD, CNRS - Observatoire de Haute Provence, 04870 Saint- Michel-l’Observatoire, France. Email: [email protected] Running title: Transmitting signals over interstellar distances and the Drake equation Abstract: I compare three methods for transmitting signals over interstellar distances: radio transmitters, lasers and artificial transits. The quantitative comparison is based on physical quantities depending on energy cost and transmitting time L, the last parameter in the Drake equation. With our assumptions, radio transmitters are the most energy-effective, while macro-engineered planetary-sized objects producing artificial transits seem effective on the long term to transmit an attention-getting signal for a time that might be much longer than the lifetime of the civilization that produced the artifact. Keywords: SETI – optical SETI – Dysonian SETI – artificial transits – Drake equation - interstellar communication Accepted for publication in the International Journal of Astrobiology. 1 1. Introduction One of the most effective methods to discover exoplanets is the so-called transit method: When a planet transits in front of its star, it blocks a small fraction of the stellar light, producing a small decrease of the observed stellar flux. The depth of the transit light curve is proportional to planet cross-section. Assuming the shape of the transiting object is spherical, which is a reasonable model for a planet, then the object cross-section is just proportional to the planet radius squared. -
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. -
PLANETARY CANDIDATES OBSERVED by Kepler. VIII. a FULLY AUTOMATED CATALOG with MEASURED COMPLETENESS and RELIABILITY BASED on DATA RELEASE 25
Draft version October 13, 2017 Typeset using LATEX twocolumn style in AASTeX61 PLANETARY CANDIDATES OBSERVED BY Kepler. VIII. A FULLY AUTOMATED CATALOG WITH MEASURED COMPLETENESS AND RELIABILITY BASED ON DATA RELEASE 25 Susan E. Thompson,1, 2, 3, ∗ Jeffrey L. Coughlin,2, 1 Kelsey Hoffman,1 Fergal Mullally,1, 2, 4 Jessie L. Christiansen,5 Christopher J. Burke,2, 1, 6 Steve Bryson,2 Natalie Batalha,2 Michael R. Haas,2, y Joseph Catanzarite,1, 2 Jason F. Rowe,7 Geert Barentsen,8 Douglas A. Caldwell,1, 2 Bruce D. Clarke,1, 2 Jon M. Jenkins,2 Jie Li,1 David W. Latham,9 Jack J. Lissauer,2 Savita Mathur,10 Robert L. Morris,1, 2 Shawn E. Seader,11 Jeffrey C. Smith,1, 2 Todd C. Klaus,2 Joseph D. Twicken,1, 2 Jeffrey E. Van Cleve,1 Bill Wohler,1, 2 Rachel Akeson,5 David R. Ciardi,5 William D. Cochran,12 Christopher E. Henze,2 Steve B. Howell,2 Daniel Huber,13, 14, 1, 15 Andrej Prša,16 Solange V. Ramírez,5 Timothy D. Morton,17 Thomas Barclay,18 Jennifer R. Campbell,2, 19 William J. Chaplin,20, 15 David Charbonneau,9 Jørgen Christensen-Dalsgaard,15 Jessie L. Dotson,2 Laurance Doyle,21, 1 Edward W. Dunham,22 Andrea K. Dupree,9 Eric B. Ford,23, 24, 25, 26 John C. Geary,9 Forrest R. Girouard,27, 2 Howard Isaacson,28 Hans Kjeldsen,15 Elisa V. Quintana,18 Darin Ragozzine,29 Avi Shporer,30 Victor Silva Aguirre,15 Jason H. Steffen,31 Martin Still,8 Peter Tenenbaum,1, 2 William F. -
Recipe for a Habitable Planet
Recipe for a Habitable Planet Aomawa Shields Clare Boothe Luce Associate Professor Shields Center for Exoplanet Climate and Interdisciplinary Education (SCECIE) University of California, Irvine ASU School of Earth and Space Exploration (SESE) December 2, 2020 A moment to pause… Leading effectively during COVID-19 • Employees Need Trust and Compassion: Be Present, Even When You're Distant • Employees Need Stability: Prioritize Wellbeing Amid Disruption • Employees Need Hope: Anchor to Your "True North" From “3 strategies for leading effectively during COVID-19” (https://www.gallup.com/workplace/306503/strategies-leading-effectively-amid-covid.aspx) Hobbies: reading movies, shows knitting mixed media/collage violin tea yoga good restaurants spa days the beach hiking smelling flowers hanging with family BINGO Ill. Niklas Elmehed. Ill. Niklas Elmehed. © Nobel Media. © Nobel Media. RadialVelocity (m/s) Nobel Prize in Physics 2019 Mayor & Queloz 1995 https://exoplanets.nasa.gov/ As of December 2, 2020 Aomawa Shields Recipe for a Habitable World Credit: NASA NNASA’sASA’s KKeplerepler MMissionission TESS Transiting Exoplanet Survey Satellite Credit: NASA-JPL/Caltech Proxima Centauri b Credit: ESO/M. Kornmesser LHS 1140b Credit: ESO TOI 700d Credit: NASA TESS planets in the Earth-sized regime Credit: NASA’s Goddard Space Flight Center Which ones do we follow up on? 20 The Habitable Zone (Kasting et al. 1993, Kopparapu et al. 2013) ) Runaway greenhouse Maximum CO2 greenhouse Stellar Mass (M Mass Stellar Distance from Star (AU) Snowball Earth Many factors can affect planetary habitability Aomawa Shields Recipe for a Habitable World Liquid water Aomawa Shields Recipe for a Habitable World Isotopic Birth Tides Orbit Abundance Environ. -
Erosion of an Exoplanetary Atmosphere Caused by Stellar Winds J
A&A 630, A52 (2019) https://doi.org/10.1051/0004-6361/201935543 Astronomy & © ESO 2019 Astrophysics Erosion of an exoplanetary atmosphere caused by stellar winds J. M. Rodríguez-Mozos1 and A. Moya2,3 1 University of Granada (UGR), Department of Theoretical Physics and Cosmology, 18071 Granada, Spain 2 School of Physics and Astronomy, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK e-mail: [email protected]; [email protected] 3 Stellar Astrophysics Centre, Department of Physics and Astronomy, Aarhus University, Ny Munkegade 120, 8000 Aarhus C, Denmark Received 26 March 2019 / Accepted 8 August 2019 ABSTRACT Aims. We present a formalism for a first-order estimation of the magnetosphere radius of exoplanets orbiting stars in the range from 0.08 to 1.3 M . With this radius, we estimate the atmospheric surface that is not protected from stellar winds. We have analyzed this unprotected surface for the most extreme environment for exoplanets: GKM-type and very low-mass stars at the two limits of the habitable zone. The estimated unprotected surface makes it possible to define a likelihood for an exoplanet to retain its atmosphere. This function can be incorporated into the new habitability index SEPHI. Methods. Using different formulations in the literature in addition to stellar and exoplanet physical characteristics, we estimated the stellar magnetic induction, the main characteristics of the stellar wind, and the different star-planet interaction regions (sub- and super- Alfvénic, sub- and supersonic). With this information, we can estimate the radius of the exoplanet magnetopause and thus the exoplanet unprotected surface. -
Early Mars As a Key to Understanding Planetary Habitability
Early Mars as a Key to Understanding Planetary Habitability Bethany Ehlmann Professor of Planetary Science, Geological & Planetary Sciences Research Scientist, Jet Propulsion Laboratory California Institute of Technology July 13, 2017 | Midterm Review Planetary Decadal Survey Outline: Early Mars as a Key to Understanding Planetary Habitability • What we have learned and what we can learn about early Mars [15 min] • Suggested exploration plans [5 min] • Questions/Discussion [10 min] Key Discoveries in Mars Science since 2010 *Publication date of last Mars references in V&V • Extent and diversity of potential ancient habitats (lakes, rivers, aquifers, hydrothermal systems, soil formation) • Mafic, Ultramafic, and Felsic igneous rocks • Modern liquid water • Recent Ice Ages and Episodicity of Climates above the Triple Point of Water • Modern active methane, likely with local sources • Modern active surface processes • Modern atmospheric loss rates See also MEPAG report to V&V Decadal Midterm (May 4, 2017): https://mepag.jpl.nasa.gov/meeting/2017-07/MEPAG_Johnson_MTDS_v04.pdf Key Discoveries in Mars Science since 2010 *Publication date of last Mars references in V&V • Extent and diversity of potential ancient habitats (lakes, Ancient rivers, aquifers, hydrothermal systems, soil formation) • Mafic, Ultramafic, and Felsic igneous rocks • Modern liquid water • Recent Ice Ages and Episodicity of Climates above the Triple Point of Water [see also Byrne talk, next] • Modern active methane, likely with local sources • Modern active surface processes • Modern atmospheric loss rates [see Jakosky talk, next] Modern See also MEPAG report to V&V Decadal Midterm (May 4, 2017): https://mepag.jpl.nasa.gov/meeting/2017-07/MEPAG_Johnson_MTDS_v04.pdf Key Finding since V&V: Modern Mars is active (methane, geomorphology, ice, water) Bridges et al., 2011; 2012 Mass wasting of the N.