Terrestrial Planet Finder Coronagraph Science and Technology Definition

Total Page:16

File Type:pdf, Size:1020Kb

Terrestrial Planet Finder Coronagraph Science and Technology Definition JPL Document D-34923 Terrestrial Planet Finder Coronagraph Science and Technology Definition Team (STDT) Report Editors: Marie Levine, Stuart Shaklan and James Kasting (Penn State University) June 12, 2006 National Aeronautics and Space Administration Jet Propulsion Laboratory California Institute of Technology Pasadena, California TPF-C STDT REPORT ii TPF-C STDT REPORT Approvals iii TPF-C STDT REPORT Goals for the Terrestrial Planet Finder Coronagraph Mission The question "are we alone?" has its roots deep in human consciousness, and its answer could revo- lutionize our world view. Starting with Galileo's invention of the telescope 400 years ago, which he used to prove the existence of other worlds, and continuing through a century of astonishing dis- coveries—galaxies, stars, planets, and distant oceans—science has given us a dramatically clearer pic- ture of the universe and our place within it. Today, we finally have tools within reach to seek life be- yond Earth, and to answer this age-old question. The Terrestrial Planet Finder-Coronagraph (TPF-C) mission is a giant step towards that goal. Over the last decade, extrasolar planets have been discovered around nearly 200 nearby stars. Most of these planetary systems are quite different from our own—with Jupiter-sized planets orbiting close to their parent stars—mainly because radial velocity measurements are most sensitive to such planets. New observing techniques, such as coronagraphy and nulling interferometry, are needed to detect smaller, Earth-like planets by their own light and to characterize them as possible harbors for life. Characterization of a terrestrial-sized planet at its most fundamental level means learning about its mass, diameter, temperature, and atmospheric and surface composition. The presence of liquid wa- ter is considered a prerequisite for life, and several gases (O2, O3, CH4, N2O) are considered possible indicators of life. Establishing the presence of any of these compounds in a planet’s atmosphere or on its surface requires spectroscopic measurements of the planet’s emitted and reflected light in both the visible/near-IR and the thermal infrared. The TPF-C mission described in this report is the first of two NASA missions that will obtain these required data. The second is TPF-I/Darwin, a NASA/ESA nulling interferometer that is described elsewhere. In addition to detecting and characterizing Earth-like planets, TPF-C will characterize many Jupiter- like giant planets and circumstellar dust disks. Such planetary system constituents provide clues to the course of planet formation, and may affect the habitability of co-existing terrestrial planets by influencing their bombardment histories. These observations must be carried out in space. Ground-based telescopes cannot do the job, for two reasons. First, ground-based telescopes must observe through the turbulence of the atmosphere. Although some of the resulting blurring can be compensated by adaptive optics, it appears infeasible to see a planet as faint as Earth, even for telescopes as large as 100 m in diameter. Second, Earth’s atmosphere contains significant concentrations of the very biogenic gases that one would wish to measure. Separating out the absorption features of an extrasolar planet’s atmosphere from those of Earth’s atmosphere appears to be an intractable problem, given the small number of photons from the observed planet and the resulting limited spectral resolution. Technology progress necessary for TPF-C has been dramatic in recent years. At least a dozen new types of coronagraphs have been invented that might enable us to see an Earth close to a vastly brighter star. Methods for canceling the halo of starlight scattered within the telescope have also been demonstrated, thereby dramatically relaxing the requirements for optical surface quality. In both areas, laboratory tests are currently getting close to achieving flight-quality performance. The telescope mirror itself needs to be relatively large (8m×3.5m), but it is still within reach of current iv TPF-C STDT REPORT fabrication capabilities. Alternative coronagraph designs described in this report might allow the mission to be accomplished with a smaller mirror. A large visible-wavelength space telescope of the quality needed to detect habitable Earth-sized planets would also have important applications to other areas of astrophysics. In particular, it would profoundly advance the science of extragalactic observations, out to the very edge of the universe. Topics of literally cosmic importance could be addressed, including the expansion rate of the uni- verse, dark energy, dark matter, and the formation of the first stars after the Big Bang. With its planned wide-field camera, TPF-C could conduct many of its deep-space observations in parallel with the search and characterization of Earth-like planets. In addition, the mission would provide dedicated time for separate pointed observations in a program that would be open to the general astronomical community. In summary, TPF-C is one of the most scientifically compelling endeavors that the human race can envision today. The technology needed to accomplish the mission is either available already or well within reach. Pursuing this mission would give NASA a leading role in developing science and tech- nology, and will be inspirational to people everywhere. v TPF-C STDT REPORT A Very Brief History With enlightened foresight, in 1985 NASA organized a Planetary Astronomy Committee, to “pro- vide advice on … initiating the search for and characterization of other planetary systems”. In the same year the Space Science Board of the National Research Council of the National Academy or- ganized the Committee on Planetary and Lunar Exploration to “extend its exploration strategy to planetary systems outside the Solar System”. In 1988 NASA organized a Science Working Group to “formulate a strategy for the discovery and study of other planetary systems”. The first extrasolar planets were discovered only a few years later (1995). Soon thereafter NASA established the first Terrestrial Planet Finder (TPF) Science Working Group, which reported in 1999 that TPF “will revolutionize humanity’s understanding of the origin and evolution of planetary systems”, and produced a schematic design of a thermal-infrared TPF Interferometer (TPF-I) to accomplish that task. In 2000 NASA funded an academic-industry competition to devise additional concepts for finding and characterizing Earth-like planets, resulting in dozens of new ideas, among which the leading one was the TPF Coronagraph (TPF-C). In parallel, in 2000, the second TPF SWG was established to develop an initial Science Requirements Document. In 2005 NASA chartered the Science and Technology Definition Team (STDT) to work with the TPF-C Project scientists and engineers, and deliver a mature Science Requirements Document for TPF-C, a narrative on TPF-C’s potential for general astrophysics observations, a Design Reference Mission, an assessment of design concepts and operational scenarios, recommendations on technol- ogy developments needed, a recommended end-to-end science program, assistance in communicat- ing with the astronomical community, and a report summarizing their work. This is that report. The STDT met in plenary session six times throughout 2005 and early 2006, held scores of tele- phone meetings, and exchanged many hundreds of emails. The STDT built on the foundation of two major studies that had just been completed: the Science Requirements Document of the TPF-C SWG (2004); and the Flight Baseline-1 engineering feasibility study of the TPF-C Project Office at JPL and GSFC (2005). The STDT also incorporated the results of five major competitively-awarded Instrument Concept Studies (2006). In addition, the STDT devoted a very substantial effort to the research and writing of the Science Requirements Document and Design Reference Mission sections of this report. This STDT report contains all of the scientific and engineering material requested in the STDT’s Charter (February 2005), delivered on schedule (June 2006). We plan to publish soon five (5) com- panion Volumes which provide the detailed information behind the STDT Report. The Volumes are: 1) Design Reference Mission Studies, 2) Flight Baseline 1 Design Information and Performance Assessment, 3) Instrument Concept Study Reports, 4) TPF-C Technology Plan and 5) Publications. The STDT wishes it could have delivered even more, however, drastic funding cuts imposed in mid- 2005 and early 2006 precluded the development of two additional parts of the study that had been chartered: a section of advice on the conduct of the end-to-end science program (not provided be- cause the Phase-A start has been delayed indefinitely); and a section on a second iteration of the en- gineering study, Flight Baseline-2 (not provided because the engineering staff was no longer funded). We regret these losses, but we expect that they will be made up in the future. With these caveats, we believe that the present study is more than fully responsive to the STDT’s Charter, and we are pleased to be able to present this study to NASA and the community at large. vi TPF-C STDT REPORT Authors STDT Members J. Roger Angel, University of Arizona Michael E. Brown, California Institute of Technology Robert A. Brown, Space Telescope Science Institute Christopher Burrows, Metajiva Mark Clampin, NASA Goddard Space Flight Center Alan Dressler, Carnegie Observatories Henry C. Ferguson, Space Telescope Science Institute Heidi B. Hammel, Space Science Institute Sara R. Heap, NASA Goddard Space Flight Center Scott D. Horner, Lockheed-Martin Garth D. Illingworth, University of California, Santa Cruz N. Jeremy Kasdin, Princeton University James Kasting, Penn State University (Co-Chair) Mark J. Kuchner, NASA Goddard Space Flight Center Douglas Lin, University of California, Santa Cruz Mark S. Marley, NASA Ames Research Center Victoria Meadows, Spitzer Science Center Martin C. Noecker, Ball Aerospace & Technology Corp. Ben R. Oppenheimer, American Museum of Natural History Sara Seager, Carnegie Institution of Washington Michael Shao, NASA Jet Propulsion Laboratory Karl R.
Recommended publications
  • The Discovery of Exoplanets
    L'Univers, S´eminairePoincar´eXX (2015) 113 { 137 S´eminairePoincar´e New Worlds Ahead: The Discovery of Exoplanets Arnaud Cassan Universit´ePierre et Marie Curie Institut d'Astrophysique de Paris 98bis boulevard Arago 75014 Paris, France Abstract. Exoplanets are planets orbiting stars other than the Sun. In 1995, the discovery of the first exoplanet orbiting a solar-type star paved the way to an exoplanet detection rush, which revealed an astonishing diversity of possible worlds. These detections led us to completely renew planet formation and evolu- tion theories. Several detection techniques have revealed a wealth of surprising properties characterizing exoplanets that are not found in our own planetary system. After two decades of exoplanet search, these new worlds are found to be ubiquitous throughout the Milky Way. A positive sign that life has developed elsewhere than on Earth? 1 The Solar system paradigm: the end of certainties Looking at the Solar system, striking facts appear clearly: all seven planets orbit in the same plane (the ecliptic), all have almost circular orbits, the Sun rotation is perpendicular to this plane, and the direction of the Sun rotation is the same as the planets revolution around the Sun. These observations gave birth to the Solar nebula theory, which was proposed by Kant and Laplace more that two hundred years ago, but, although correct, it has been for decades the subject of many debates. In this theory, the Solar system was formed by the collapse of an approximately spheric giant interstellar cloud of gas and dust, which eventually flattened in the plane perpendicular to its initial rotation axis.
    [Show full text]
  • Modeling Super-Earth Atmospheres in Preparation for Upcoming Extremely Large Telescopes
    Modeling Super-Earth Atmospheres In Preparation for Upcoming Extremely Large Telescopes Maggie Thompson1 Jonathan Fortney1, Andy Skemer1, Tyler Robinson2, Theodora Karalidi1, Steph Sallum1 1University of California, Santa Cruz, CA; 2Northern Arizona University, Flagstaff, AZ ExoPAG 19 January 6, 2019 Seattle, Washington Image Credit: NASA Ames/JPL-Caltech/T. Pyle Roadmap Research Goals & Current Atmosphere Modeling Selecting Super-Earths for State of Super-Earth Tool (Past & Present) Follow-Up Observations Detection Preliminary Assessment of Future Observatories for Conclusions & Upcoming Instruments’ Super-Earths Future Work Capabilities for Super-Earths M. Thompson — ExoPAG 19 01/06/19 Research Goals • Extend previous modeling tool to simulate super-Earth planet atmospheres around M, K and G stars • Apply modified code to explore the parameter space of actual and synthetic super-Earths to select most suitable set of confirmed exoplanets for follow-up observations with JWST and next-generation ground-based telescopes • Inform the design of advanced instruments such as the Planetary Systems Imager (PSI), a proposed second-generation instrument for TMT/GMT M. Thompson — ExoPAG 19 01/06/19 Current State of Super-Earth Detections (1) Neptune Mass Range of Interest Earth Data from NASA Exoplanet Archive M. Thompson — ExoPAG 19 01/06/19 Current State of Super-Earth Detections (2) A Approximate Habitable Zone Host Star Spectral Type F G K M Data from NASA Exoplanet Archive M. Thompson — ExoPAG 19 01/06/19 Atmosphere Modeling Tool Evolution of Atmosphere Model • Solar System Planets & Moons ~ 1980’s (e.g., McKay et al. 1989) • Brown Dwarfs ~ 2000’s (e.g., Burrows et al. 2001) • Hot Jupiters & Other Giant Exoplanets ~ 2000’s (e.g., Fortney et al.
    [Show full text]
  • PEAS: the PLANET AS EXOPLANET ANALOG SPECTROGRAPH. E. C. Martin1 and A
    Exoplanets in our Backyard 2020 (LPI Contrib. No. 2195) 3006.pdf PEAS: THE PLANET AS EXOPLANET ANALOG SPECTROGRAPH. E. C. Martin1 and A. J. Skemer1, 1Department of Astronomy & Astrophysics, University of California, Santa Cruz, CA ([email protected]) Introduction: Exoplanets are abundant in our Galaxy • Produce 2D surface maps of Venus, Mars, Jupi- and yet characterizing them remains a technical chal- ter, Saturn, Uranus, Neptune lenGe. Solar System planets provide an opportunity to • Produce fiducial measurements that will be used test the practical limitations of exoplanet observations to plan instruments for future exoplanet mis- with hiGh siGnal-to-noise data, and ancillary data (such sions, such as HabEx/LUVOIR and TMT. as 2D maps and in situ measurements) that we cannot Long term: access for exoplanets. However, data on Solar System • Time-series observations of Solar System plan- planets differ from exoplanets in that Solar System ets to explore variability and weather patterns planets are spatially resolved while exoplanets are all on planets unresolved point-sources. • Comparison to historical data (e.g. [4]) There have been several recent efforts to validate techniques for interpreting exoplanet observations by • Study planetary seismoloGy (oscillation modes) binning images of Solar System planets to a single of Solar System planets pixel: For example, Cowan et al. [1] used images from the EPOXI mission to study Earth’s Globally averaGed PEAS Instrument Design Planetary light collect- properties as it rotated; MayorGa et al. [2] used data ed by the telescope will be split into a spectroGraph from the Cassini spacecraft’s fly-by of Jupiter to ob- system and an imaGinG system for simultaneous obser- serve Globally averaGed reflected liGht phase curves; vations.
    [Show full text]
  • The Exoplanet Revolution
    FEATURES THE EXOPLANET REVOLUTION l Yamila Miguel – Leiden Observatory, Leiden, The Netherlands – DOI: https://doi.org/10.1051/epn/2019506 Hot Jupiters, super-Earths, lava-worlds and the search for life beyond our solar system: the exoplanet revolution started almost 30 years ago and is now taking off. re there other planets like the Earth out discovered the astonishing number of 4000 exoplanets, there? This is probably one of the oldest and counting. Every new discovery shows an amazing questions of humanity. For centuries and diversity that impacts in the perception and understand- Auntil the 90s, we only knew of the existence ing of our own solar system. of 8 planets. But today we live in a privileged time. For the first time in history we know that there are other How to find exoplanets? planets orbiting distant stars. Finding exoplanets is an extremely difficult task. These The first planet orbiting a star similar to the Sun was planets shine mostly due to the reflection of the stellar . Artist’s impression discovered in 1995 -only 24 years ago- and it started light in their atmospheres and their light is incredibly of COROT-7b. a revolution in Astronomy. Today astronomers have weak compared to that of their host stars. For this reason, © ESO/L. Calçada EPN 50/5&6 41 FEATURES THE Exoplanet REVolution observing exoplanets directly is extremely difficult and allows astronomers to calculate the planet’s density, astronomers had to develop indirect techniques that infer important to start assessing planetary compositions the presence of the planet. and diversity. Two of the most successful techniques to discov- er exoplanets are the "Transits" and "Radial Veloci- The Exoplanet Zoo ties" techniques.
    [Show full text]
  • 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.
    [Show full text]
  • Gemini Planet Imager Spectroscopy of the Dusty Substellar Companion HD 206893 B
    The Astronomical Journal, 161:5 (24pp), 2021 January https://doi.org/10.3847/1538-3881/abc263 © 2020. The American Astronomical Society. All rights reserved. Gemini Planet Imager Spectroscopy of the Dusty Substellar Companion HD206893B K. Ward-Duong1,2 , J. Patience2, K. Follette3 , R. J. De Rosa4,5 , J. Rameau6,7 , M. Marley8 , D. Saumon9 , E. L. Nielsen4 , A. Rajan10 , A. Z. Greenbaum11 , J. Lee12, J. J. Wang13,14,40 , I. Czekala4,14,41 , G. Duchêne6,14 , B. Macintosh4 , S. Mark Ammons15 , V. P. Bailey16 , T. Barman17 , J. Bulger18,19 , C. Chen10 , J. Chilcote4,20 , T. Cotten12 , R. Doyon7, T. M. Esposito14 , M. P. Fitzgerald21 , B. L. Gerard22,23 , S. J. Goodsell24 , J. R. Graham14, P. Hibon5 , J. Hom2 , L.-W. Hung25 , P. Ingraham26 , P. Kalas14,27 , Q. Konopacky28 , J. E. Larkin21 , J. Maire28, F. Marchis27 , C. Marois23,29 , S. Metchev30,31 , M. A. Millar-Blanchaer16,42 , R. Oppenheimer32 , D. Palmer15 , M. Perrin10 , L. Poyneer15, L. Pueyo10, F. T. Rantakyrö33 , B. Ren34 , J.-B. Ruffio4 , D. Savransky35 , A. C. Schneider36,37 , A. Sivaramakrishnan10 , I. Song12 , R. Soummer10 , M. Tallis4, S. Thomas26 , J. Kent Wallace16 , S. Wiktorowicz38 , and S. Wolff39 1 Five College Astronomy Department, Amherst College, Amherst, MA 01002, USA; [email protected] 2 School of Earth and Space Exploration, Arizona State University, P.O. Box 871404, Tempe, AZ 85287, USA 3 Physics & Astronomy Department, Amherst College, 21 Merrill Science Drive, Amherst, MA 01002, USA 4 Kavli Institute for Particle Astrophysics and Cosmology, Stanford University, Stanford, CA 94305, USA 5 European Southern Observatory, Alonso de Córdova 3107, Vitacura, Santiago, Chile 6 Univ.
    [Show full text]
  • Biosignatures Search in Habitable Planets
    galaxies Review Biosignatures Search in Habitable Planets Riccardo Claudi 1,* and Eleonora Alei 1,2 1 INAF-Astronomical Observatory of Padova, Vicolo Osservatorio, 5, 35122 Padova, Italy 2 Physics and Astronomy Department, Padova University, 35131 Padova, Italy * Correspondence: [email protected] Received: 2 August 2019; Accepted: 25 September 2019; Published: 29 September 2019 Abstract: The search for life has had a new enthusiastic restart in the last two decades thanks to the large number of new worlds discovered. The about 4100 exoplanets found so far, show a large diversity of planets, from hot giants to rocky planets orbiting small and cold stars. Most of them are very different from those of the Solar System and one of the striking case is that of the super-Earths, rocky planets with masses ranging between 1 and 10 M⊕ with dimensions up to twice those of Earth. In the right environment, these planets could be the cradle of alien life that could modify the chemical composition of their atmospheres. So, the search for life signatures requires as the first step the knowledge of planet atmospheres, the main objective of future exoplanetary space explorations. Indeed, the quest for the determination of the chemical composition of those planetary atmospheres rises also more general interest than that given by the mere directory of the atmospheric compounds. It opens out to the more general speculation on what such detection might tell us about the presence of life on those planets. As, for now, we have only one example of life in the universe, we are bound to study terrestrial organisms to assess possibilities of life on other planets and guide our search for possible extinct or extant life on other planetary bodies.
    [Show full text]
  • 1 Director's Message
    1 Director’s Message Markus Kissler-Patig 3 Weighing the Black Hole in M101 ULX-1 Stephen Justham and Jifeng Liu 8 World’s Most Powerful Planet Finder Turns its Eye to the Sky: First Light with the Gemini Planet Imager Bruce Macintosh and Peter Michaud 12 Science Highlights Nancy A. Levenson 15 Operations Corner: Update and 2013 Review Andy Adamson 20 Instrumentation Development: Update and 2013 Review Scot Kleinman ON THE COVER: GeminiFocus January 2014 The cover of this issue GeminiFocus is a quarterly publication of Gemini Observatory features first light images from the Gemini 670 N. A‘ohoku Place, Hilo, Hawai‘i 96720 USA Planet Imager that Phone: (808) 974-2500 Fax: (808) 974-2589 were released at the Online viewing address: January 2014 meeting www.gemini.edu/geminifocus of the American Managing Editor: Peter Michaud Astronomical Society Science Editor: Nancy A. Levenson held in Washington, D.C. Associate Editor: Stephen James O’Meara See the press release Designer: Eve Furchgott / Blue Heron Multimedia that accompanied the images starting on Any opinions, findings, and conclusions or recommendations page 8 of this issue. expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation. Markus Kissler-Patig Director’s Message 2013: A Successful Year for Gemini! As 2013 comes to an end, we can look back at 12 very successful months for Gemini despite strong budget constraints. Indeed, 2013 was the first stage of our three-year transition to a reduced opera- tions budget, and it was marked by a roughly 20 percent cut in contributions from Gemini’s partner countries.
    [Show full text]
  • 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.
    [Show full text]
  • Exoplanet Meteorology: Characterizing the Atmospheres Of
    Exoplanet Meteorology: Characterizing the Atmospheres of Directly Imaged Sub-Stellar Objects by Abhijith Rajan A Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy Approved April 2017 by the Graduate Supervisory Committee: Jennifer Patience, Co-Chair Patrick Young, Co-Chair Paul Scowen Nathaniel Butler Evgenya Shkolnik ARIZONA STATE UNIVERSITY May 2017 ©2017 Abhijith Rajan All Rights Reserved ABSTRACT The field of exoplanet science has matured over the past two decades with over 3500 confirmed exoplanets. However, many fundamental questions regarding the composition, and formation mechanism remain unanswered. Atmospheres are a window into the properties of a planet, and spectroscopic studies can help resolve many of these questions. For the first part of my dissertation, I participated in two studies of the atmospheres of brown dwarfs to search for weather variations. To understand the evolution of weather on brown dwarfs we conducted a multi- epoch study monitoring four cool brown dwarfs to search for photometric variability. These cool brown dwarfs are predicted to have salt and sulfide clouds condensing in their upper atmosphere and we detected one high amplitude variable. Combining observations for all T5 and later brown dwarfs we note a possible correlation between variability and cloud opacity. For the second half of my thesis, I focused on characterizing the atmospheres of directly imaged exoplanets. In the first study Hubble Space Telescope data on HR8799, in wavelengths unobservable from the ground, provide constraints on the presence of clouds in the outer planets. Next, I present research done in collaboration with the Gemini Planet Imager Exoplanet Survey (GPIES) team including an exploration of the instrument contrast against environmental parameters, and an examination of the environment of the planet in the HD 106906 system.
    [Show full text]
  • The Intrinsic Shape of Galaxy Bulges 3
    The intrinsic shape of galaxy bulges J. M´endez-Abreu Abstract The knowledge of the intrinsic three-dimensional (3D) structure of galaxy components provides crucial information about the physical processes driving their formationand evolution.In this paper I discuss the main developments and results in the quest to better understand the 3D shape of galaxy bulges. I start by establishing the basic geometrical description of the problem. Our understanding of the intrinsic shape of elliptical galaxies and galaxy discs is then presented in a historical context, in order to place the role that the 3D structure of bulges play in the broader picture of galaxy evolution. Our current view on the 3D shape of the Milky Way bulge and future prospects in the field are also depicted. 1 Introduction and overview Galaxies are three-dimensional (3D) structures moving under the dictates of gravity in a 3D Universe. From our position on the Earth, astronomers have only the op- portunity to observe their properties projected onto a two-dimensional (2D) plane, usually called the plane of the sky. Since we can neither circumnavigate galaxies nor wait until they spin around, our knowledge of the intrinsic shape of galaxies is still limited, relying on sensible, but sometimes not accurate, physical and geometrical hypotheses. Despite the obvious difficulties inherent to measure the intrinsic 3D shape of galaxies, it is doubtless that it keeps an invaluable piece of information about their formation and evolution. In fact, astronomers have acknowledged this since galaxies arXiv:1502.00265v2 [astro-ph.GA] 31 Aug 2015 were established to be island universes and the topic has produced an outstanding amount of literature during the last century.
    [Show full text]
  • Dark Matter and Background Light
    Dark Matter and Background Light J.M. Overduin Gravity Probe B, Hansen Experimental Physics Laboratory, Stanford University, Stanford, California, U.S.A. 94305-4085 and P.S. Wesson Department of Physics, University of Waterloo, Ontario, Canada N2L 3G1 Abstract Progress in observational cosmology over the past five years has established that the Universe is dominated dynamically by dark matter and dark energy. Both these new and apparently independent forms of matter-energy have properties that are inconsistent with anything in the existing standard model of particle physics, and it appears that the latter must be extended. We review what is known about dark matter and energy from their impact on the light of the night sky. Most of the candidates that have been proposed so far are not perfectly black, but decay into or otherwise interact with photons in characteristic ways that can be accurately modelled and compared with observational data. We show how experimental limits on the intensity of cosmic background radiation in the microwave, infrared, optical, arXiv:astro-ph/0407207v1 10 Jul 2004 ultraviolet, x-ray and γ-ray bands put strong limits on decaying vacuum energy, light axions, neutrinos, unstable weakly-interacting massive particles (WIMPs) and objects like black holes. Our conclusion is that the dark matter is most likely to be WIMPs if conventional cosmology holds; or higher-dimensional sources if spacetime needs to be extended. Key words: Cosmology, Background radiation, Dark matter, Black holes, Higher-dimensional field theory PACS: 98.80.-k, 98.70.Vc, 95.35.+d, 04.70.Dy, 04.50.+h Email addresses: [email protected] (J.M.
    [Show full text]