A First Reconnaissance of the Atmospheres of Terrestrial Exoplanets Using Ground-Based Optical Transits and Space-Based UV Spectra
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The Planetary Systems Imager for TMT Astro2020 APC White Paper Optical and Infrared Observations from the Ground Corresponding Author: Michael P
The Planetary Systems Imager for TMT Astro2020 APC White Paper Optical and Infrared Observations from the Ground Corresponding Author: Michael P. Fitzgerald (University of California, Los Angeles; mpfi[email protected]) Co-authors: Diego) Vanessa Bailey (Jet Propulsion Laboratory) Takayuki Kotani (Astrobiology Center/NAOJ) Christoph Baranec (University of Hawaii) David Lafreniere` (Universite´ de Montreal)´ Natasha Batalha (University of California Santa Michael Liu (University of Hawaii) Cruz) Julien Lozi (Subaru) Bjorn¨ Benneke (Universite´ de Montreal)´ Jessica R. Lu (University of California, Berkeley) Charles Beichman (California Institute of Jared Males (University of Arizona) Technology) Mark Marley (NASA Ames Research Center) Timothy Brandt (University of California, Santa Christian Marois (NRC Canada) Barbara) Dimitri Mawet (California Institute of Jeffrey Chilcote (Notre Dame) Technology/JPL) Mark Chun (University of Hawaii) Benjamin Mazin (University of California Santa Ian Crossfield (MIT) Barbara) Thayne Currie (NASA Ames Research Center) Maxwell Millar-Blanchaer (Jet Propulsion Kristina Davis (University of California Santa Laboratory) Barbara) Soumen Mondal (SN Bose National Centre for Richard Dekany (California Institute of Technology) Basic Sciences) Jacques-Robert Delorme (California Institute of Naoshi Murakami (Hokkaido University) Technology) Ruth Murray-Clay (University of California, Santa Ruobing Dong (University of Victoria) Cruz) Rene Doyon (Universite´ de Montreal)´ Norio Narita (Astrobiology Center) Courtney Dressing -
Lurking in the Shadows: Wide-Separation Gas Giants As Tracers of Planet Formation
Lurking in the Shadows: Wide-Separation Gas Giants as Tracers of Planet Formation Thesis by Marta Levesque Bryan In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy CALIFORNIA INSTITUTE OF TECHNOLOGY Pasadena, California 2018 Defended May 1, 2018 ii © 2018 Marta Levesque Bryan ORCID: [0000-0002-6076-5967] All rights reserved iii ACKNOWLEDGEMENTS First and foremost I would like to thank Heather Knutson, who I had the great privilege of working with as my thesis advisor. Her encouragement, guidance, and perspective helped me navigate many a challenging problem, and my conversations with her were a consistent source of positivity and learning throughout my time at Caltech. I leave graduate school a better scientist and person for having her as a role model. Heather fostered a wonderfully positive and supportive environment for her students, giving us the space to explore and grow - I could not have asked for a better advisor or research experience. I would also like to thank Konstantin Batygin for enthusiastic and illuminating discussions that always left me more excited to explore the result at hand. Thank you as well to Dimitri Mawet for providing both expertise and contagious optimism for some of my latest direct imaging endeavors. Thank you to the rest of my thesis committee, namely Geoff Blake, Evan Kirby, and Chuck Steidel for their support, helpful conversations, and insightful questions. I am grateful to have had the opportunity to collaborate with Brendan Bowler. His talk at Caltech my second year of graduate school introduced me to an unexpected population of massive wide-separation planetary-mass companions, and lead to a long-running collaboration from which several of my thesis projects were born. -
Arxiv:1804.07377V1 [Astro-Ph.SR] 19 Apr 2018
submitted to The Astronomical Journal 20 April 2018 The Solar Neighborhood XLIV: RECONS Discoveries within 10 Parsecs Todd J. Henry1;8, Wei-Chun Jao2;8, Jennifer G. Winters3;8, Sergio B. Dieterich4;8, Charlie T. Finch5;8, Philip A. Ianna1;8, Adric R. Riedel6;8, Michele L. Silverstein2;8, John P. Subasavage7;8, Eliot Halley Vrijmoet2 1RECONS Institute, Chambersburg, PA 17201, USA; [email protected], [email protected] 2Department of Physics and Astronomy, Georgia State University, Atlanta, GA 30302, USA; [email protected], [email protected], [email protected] 3Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA; [email protected] 4Department of Terrestrial Magnetism, Carnegie Institution for Science, Washington, DC 20015, USA; [email protected] 5Astrometry Department, U.S. Naval Observatory, Washington, DC 20392, USA; charlie.fi[email protected] 6Space Telescope Science Institute, Baltimore, MD 21218, USA; [email protected] 7United States Naval Observatory, Flagstaff, AZ 86001, USA; [email protected] ABSTRACT arXiv:1804.07377v1 [astro-ph.SR] 19 Apr 2018 We describe the 44 systems discovered to be within 10 parsecs of the Sun by the RECONS team, primarily via the long-term astrometry program at CTIO that began in 1999. The systems | including 41 with red dwarf primaries, 2 white dwarfs, and 1 brown dwarf | have been found to have trigonometric parallaxes 8Visiting Astronomer, Cerro Tololo Inter-American Observatory. CTIO is operated by AURA, Inc. under contract to the National Science Foundation. { 2 { greater than 100 milliarcseconds (mas), with errors of 0.4{2.4 mas in all but one case. -
100 Closest Stars Designation R.A
100 closest stars Designation R.A. Dec. Mag. Common Name 1 Gliese+Jahreis 551 14h30m –62°40’ 11.09 Proxima Centauri Gliese+Jahreis 559 14h40m –60°50’ 0.01, 1.34 Alpha Centauri A,B 2 Gliese+Jahreis 699 17h58m 4°42’ 9.53 Barnard’s Star 3 Gliese+Jahreis 406 10h56m 7°01’ 13.44 Wolf 359 4 Gliese+Jahreis 411 11h03m 35°58’ 7.47 Lalande 21185 5 Gliese+Jahreis 244 6h45m –16°49’ -1.43, 8.44 Sirius A,B 6 Gliese+Jahreis 65 1h39m –17°57’ 12.54, 12.99 BL Ceti, UV Ceti 7 Gliese+Jahreis 729 18h50m –23°50’ 10.43 Ross 154 8 Gliese+Jahreis 905 23h45m 44°11’ 12.29 Ross 248 9 Gliese+Jahreis 144 3h33m –9°28’ 3.73 Epsilon Eridani 10 Gliese+Jahreis 887 23h06m –35°51’ 7.34 Lacaille 9352 11 Gliese+Jahreis 447 11h48m 0°48’ 11.13 Ross 128 12 Gliese+Jahreis 866 22h39m –15°18’ 13.33, 13.27, 14.03 EZ Aquarii A,B,C 13 Gliese+Jahreis 280 7h39m 5°14’ 10.7 Procyon A,B 14 Gliese+Jahreis 820 21h07m 38°45’ 5.21, 6.03 61 Cygni A,B 15 Gliese+Jahreis 725 18h43m 59°38’ 8.90, 9.69 16 Gliese+Jahreis 15 0h18m 44°01’ 8.08, 11.06 GX Andromedae, GQ Andromedae 17 Gliese+Jahreis 845 22h03m –56°47’ 4.69 Epsilon Indi A,B,C 18 Gliese+Jahreis 1111 8h30m 26°47’ 14.78 DX Cancri 19 Gliese+Jahreis 71 1h44m –15°56’ 3.49 Tau Ceti 20 Gliese+Jahreis 1061 3h36m –44°31’ 13.09 21 Gliese+Jahreis 54.1 1h13m –17°00’ 12.02 YZ Ceti 22 Gliese+Jahreis 273 7h27m 5°14’ 9.86 Luyten’s Star 23 SO 0253+1652 2h53m 16°53’ 15.14 24 SCR 1845-6357 18h45m –63°58’ 17.40J 25 Gliese+Jahreis 191 5h12m –45°01’ 8.84 Kapteyn’s Star 26 Gliese+Jahreis 825 21h17m –38°52’ 6.67 AX Microscopii 27 Gliese+Jahreis 860 22h28m 57°42’ 9.79, -
Greenhouse Gases
ClimateClimate onon terrestrialterrestrial planetsplanets H. Rauer Zentrum für Astronomie und Astrophysik, TU Berlin und Institut für Planetenforschung, DLR, Berlin-Adlershof Terrestrial Planets with Atmospheres in our Solar System Venus Earth Mars T = 735 K T = 288 K T = 216 K p = 90 bar p = 1 bar p = 0.007 bar Atmosphere: Atmosphere: Atmosphere: 96% CO2 77% N2 95% CO2 3,5 % N2 21 % O2 2,7 % N2 1 % H2O WhatWhatare aret thehe relevant relevant processesprocesses forfora a stablestablec climate?limate? AA stablestable climate climate needsneeds a a stablestable atmosphere!atmosphere! Three ways to gain a (secondary) atmosphere Ways to loose an atmosphere Could also be a gain Die Fluchtgeschwindigkeit Ep = -GmM/R 2 Ekl= 1/2mv Für Ek<Ep wird das Molekül zurückkehren Für Ek≥Ep wird das Molekül die Atmosphäre verlassen Die kleinst möglichste Geschwindigkeit, die für das Verlassen notwendig ist hat das Molekül für den Fall: Ek+Ep=0 2 1/2mve -GMm/R=0 ve=√(2GM/R) Thermischer Verlust (Jeans Escape) Einzelne Moleküle können von der obersten Schicht der Atmosphäre entweichen, wenn sie genügend Energie besitzen Die Moleküle folgen einer Maxwell-Boltzmann Verteilung: Mittlere quadratische Geschwindigkeit: v=√(2kT/m) Large escape velocities for the giants and ice planets Mars escape velocity is ~½ ve(Earth) - gas giants are massive enough to keep H-He-atmospheres - terrestrial planets atmospheres can have CO2, N2, O2, CH4, H2O, …, but little H and He Additional loss processes are important: Planets with magnetosphere are generally better protected from -
The Earth and Its Atmosphere (Introduction) What, Why, and How???
The Earth and Its Atmosphere (Introduction) What, Why, and How??? What is an Why do planets atmosphere? have atmospheres? What determines the yearly weather cycle? Why is the weather What is the different every year? structure of the Earth’s atmosphere? How was the Earth’s What is the atmosphere formed? Why do we study composition the atmosphere? of the Earth’s atmosphere? What processes determine How different are the daily variations in the the atmospheres of atmosphere? Are they other planets? predictable? What is an atmosphere? • A gaseous envelope surrounding a planet (satellite, comet…). • It is very, very thin compared to the size of the planet Why do planets have atmospheres? Gravity !!! PressurePressure !!!!!! Origin of the Atmosphere (How is an atmosphere formed?) • The early atmosphere of the Earth was very different from the atmosphere today! • Stage I (Primordial Atmosphere): ♦ Acquired by gravitational attraction of volatile gases from the proto planetary nebula of the Sun ♦ Consisted mostly of H2 and He ♦ Small and warm planets (Earth, Mars, Venus, Mercury) lost this atmosphere because the gravity is not strong enough to keep the light hot gases from escaping the planet. ♦ The composition of the atmosphere of the giant planets (Jupiter, Saturn, Uranus and Neptune) today is very close to their primordial atmosphere (why?). The Secondary Atmosphere • Stage II ♦ Outgassing of the terrestrial type planets during the early stages of their geological history. Volcanoes, geysers, cracks, … ♦ Most abundant gasses: H2O, CO2, SO2, H2S, CO ♦ Recall: radon mitigation ♦ On the Earth H2O condensed, formed clouds and rained out to form oceans. ♦ On the Earth most of the abundant gasses then dissolved in the ocean, leaving N2 as the dominant gas. -
50 Years of Existence of the European Southern Observatory (ESO) 30 Years of Swiss Membership with the ESO
Federal Department for Economic Affairs, Education and Research EAER State Secretariat for Education, Research and Innovation SERI 50 years of existence of the European Southern Observatory (ESO) 30 years of Swiss membership with the ESO The European Southern Observatory (ESO) was founded in Paris on 5 October 1962. Exactly half a century later, on 5 October 2012, Switzerland organised a com- memoration ceremony at the University of Bern to mark ESO’s 50 years of existence and 30 years of Swiss membership with the ESO. This article provides a brief summary of the history and milestones of Swiss member- ship with the ESO as well as an overview of the most important achievements and challenges. Switzerland’s route to ESO membership Nearly twenty years after the ESO was founded, the time was ripe for Switzerland to apply for membership with the ESO. The driving forces on the academic side included the Universi- ty of Geneva and the University of Basel, which wanted to gain access to the most advanced astronomical research available. In 1980, the Federal Council submitted its Dispatch on Swiss membership with the ESO to the Federal Assembly. In 1981, the Federal Assembly adopted a federal decree endorsing Swiss membership with the ESO. In 1982, the Swiss Confederation filed the official documents for ESO membership in Paris. In 1982, Switzerland paid the initial membership fee and, in 1983, the first year’s member- ship contributions. High points of Swiss participation In 1987, the Federal Council issued a federal decree on Swiss participation in the ESO’s Very Large Telescope (VLT) to be built at the Paranal Observatory in the Chilean Atacama Desert. -
Exoplanet.Eu Catalog Page 1 # Name Mass Star Name
exoplanet.eu_catalog # name mass star_name star_distance star_mass OGLE-2016-BLG-1469L b 13.6 OGLE-2016-BLG-1469L 4500.0 0.048 11 Com b 19.4 11 Com 110.6 2.7 11 Oph b 21 11 Oph 145.0 0.0162 11 UMi b 10.5 11 UMi 119.5 1.8 14 And b 5.33 14 And 76.4 2.2 14 Her b 4.64 14 Her 18.1 0.9 16 Cyg B b 1.68 16 Cyg B 21.4 1.01 18 Del b 10.3 18 Del 73.1 2.3 1RXS 1609 b 14 1RXS1609 145.0 0.73 1SWASP J1407 b 20 1SWASP J1407 133.0 0.9 24 Sex b 1.99 24 Sex 74.8 1.54 24 Sex c 0.86 24 Sex 74.8 1.54 2M 0103-55 (AB) b 13 2M 0103-55 (AB) 47.2 0.4 2M 0122-24 b 20 2M 0122-24 36.0 0.4 2M 0219-39 b 13.9 2M 0219-39 39.4 0.11 2M 0441+23 b 7.5 2M 0441+23 140.0 0.02 2M 0746+20 b 30 2M 0746+20 12.2 0.12 2M 1207-39 24 2M 1207-39 52.4 0.025 2M 1207-39 b 4 2M 1207-39 52.4 0.025 2M 1938+46 b 1.9 2M 1938+46 0.6 2M 2140+16 b 20 2M 2140+16 25.0 0.08 2M 2206-20 b 30 2M 2206-20 26.7 0.13 2M 2236+4751 b 12.5 2M 2236+4751 63.0 0.6 2M J2126-81 b 13.3 TYC 9486-927-1 24.8 0.4 2MASS J11193254 AB 3.7 2MASS J11193254 AB 2MASS J1450-7841 A 40 2MASS J1450-7841 A 75.0 0.04 2MASS J1450-7841 B 40 2MASS J1450-7841 B 75.0 0.04 2MASS J2250+2325 b 30 2MASS J2250+2325 41.5 30 Ari B b 9.88 30 Ari B 39.4 1.22 38 Vir b 4.51 38 Vir 1.18 4 Uma b 7.1 4 Uma 78.5 1.234 42 Dra b 3.88 42 Dra 97.3 0.98 47 Uma b 2.53 47 Uma 14.0 1.03 47 Uma c 0.54 47 Uma 14.0 1.03 47 Uma d 1.64 47 Uma 14.0 1.03 51 Eri b 9.1 51 Eri 29.4 1.75 51 Peg b 0.47 51 Peg 14.7 1.11 55 Cnc b 0.84 55 Cnc 12.3 0.905 55 Cnc c 0.1784 55 Cnc 12.3 0.905 55 Cnc d 3.86 55 Cnc 12.3 0.905 55 Cnc e 0.02547 55 Cnc 12.3 0.905 55 Cnc f 0.1479 55 -