Solar System Sites That Might Support Life
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Catherinesaunders
The Utility of Robot Sensory Devices in a Collaborative Autonomic Environment Catherine Saunders, Roy Sterritt, George Wilkie School of Computing and Mathematics University of Ulster Northern Ireland [email protected], [email protected], [email protected] Abstract –-This paper proposes an Autonomic architecture that environment and relay meaningful information to each will enable mobile robots to self-manage and collaborate by other. using control loops to monitor their internal state and external environment. The Autonomic Computing MAPE-K control In this paper we discuss the sensor capabilities of the Dr loop is used to design a Robot Autonomic Element and a Robot X80-H platform that will be used for the research. A Mapping Autonomic Element; each can exchange data and collaborate to find an object located within a room. A review of design of the proposed system is included and explained. A the sensor capabilities of the X80-H mobile robot platform is brief literature review of robotic collaborative systems is undertaken with emphasis on how useful each sensor will be to also included. The Research Background section looks at the proposed research. A literature review of other projects why self-managing software systems are needed. that feature robot collaboration is also included. Keywords - autonomic computing; mobile robot; Dr Robot II. ROBOT SENSORY DEVICES X80-H; collaboration; MAPE-K This section gives an overview of the sensors that the Dr Robot X80-H is equipped with. We assess how reliable they are and how useful they will be for our research. We will be I. -
Titan and the Moons of Saturn Telesto Titan
The Icy Moons and the Extended Habitable Zone Europa Interior Models Other Types of Habitable Zones Water requires heat and pressure to remain stable as a liquid Extended Habitable Zones • You do not need sunlight. • You do need liquid water • You do need an energy source. Saturn and its Satellites • Saturn is nearly twice as far from the Sun as Jupiter • Saturn gets ~30% of Jupiter’s sunlight: It is commensurately colder Prometheus • Saturn has 82 known satellites (plus the rings) • 7 major • 27 regular • 4 Trojan • 55 irregular • Others in rings Titan • Titan is nearly as large as Ganymede Titan and the Moons of Saturn Telesto Titan Prometheus Dione Titan Janus Pandora Enceladus Mimas Rhea Pan • . • . Titan The second-largest moon in the Solar System The only moon with a substantial atmosphere 90% N2 + CH4, Ar, C2H6, C3H8, C2H2, HCN, CO2 Equilibrium Temperatures 2 1/4 Recall that TEQ ~ (L*/d ) Planet Distance (au) TEQ (K) Mercury 0.38 400 Venus 0.72 291 Earth 1.00 247 Mars 1.52 200 Jupiter 5.20 108 Saturn 9.53 80 Uranus 19.2 56 Neptune 30.1 45 The Atmosphere of Titan Pressure: 1.5 bars Temperature: 95 K Condensation sequence: • Jovian Moons: H2O ice • Saturnian Moons: NH3, CH4 2NH3 + sunlight è N2 + 3H2 CH4 + sunlight è CH, CH2 Implications of Methane Free CH4 requires replenishment • Liquid methane on the surface? Hazy atmosphere/clouds may suggest methane/ ethane precipitation. The freezing points of CH4 and C2H6 are 91 and 92K, respectively. (Titan has a mean temperature of 95K) (Liquid natural gas anyone?) This atmosphere may resemble the primordial terrestrial atmosphere. -
Page 1 of 18 Michael J. Malaska, Ph. D. Jet Propulsion Laboratory
Michael J. Malaska, Ph. D. Jet Propulsion Laboratory, California Institute of Technology 4800 Oak Grove Dr., MS 183-301 Pasadena, CA 91109-8099 818-354-7652 [email protected] OBJECTIVE Highly creative and enthusiastic individual with a broad background in planetary science, chemistry, and geology with a research program in planetary science at the interface of the sciences of geology, chemistry, and astrobiology with specific skills encompassing field science, laboratory research, and remote sensing. EDUCATION NASA/Jet Propulsion Laboratory, California Institute of Technology, NPP Senior Postdoctoral Fellow, 2012-2015 Mayo Clinic Jacksonville, postdoctoral position in Neurochemistry, 1991-1993. University of California, Berkeley, Ph.D. in Chemistry, 1991. Massachusetts Institute of Technology, S.B. in Chemistry, 1986. RESEARCH SUMMARY My planetary geology research program has focused on the interface of chemical and geological processes on Saturn's moon Titan based on data returned by the Cassini-Huygens spacecraft. These studies examine how liquid hydrocarbon rains and rivers on that world have eroded and dissolved a landscape made of organic materials layered upon rock-hard water ice. My key discoveries include the identification and characterization of labyrinth terrain on Titan, comparison of meandering channels to high-volume rivers on Earth, and the modelling of dissolution processes of Titan surface materials. My current program involves laboratory studies examining the dissolution geology of Titan and the geomorphological mapping of Titan's surface. My 20 year career as an organic chemist in drug discovery was located at the interface of chemistry and biology. This research has discovered new chemical compounds that can interact with enzymes and receptors to control cellular processes and treat diseases. -
The Lakes and Seas of Titan • Explore Related Articles • Search Keywords Alexander G
EA44CH04-Hayes ARI 17 May 2016 14:59 ANNUAL REVIEWS Further Click here to view this article's online features: • Download figures as PPT slides • Navigate linked references • Download citations The Lakes and Seas of Titan • Explore related articles • Search keywords Alexander G. Hayes Department of Astronomy and Cornell Center for Astrophysics and Planetary Science, Cornell University, Ithaca, New York 14853; email: [email protected] Annu. Rev. Earth Planet. Sci. 2016. 44:57–83 Keywords First published online as a Review in Advance on Cassini, Saturn, icy satellites, hydrology, hydrocarbons, climate April 27, 2016 The Annual Review of Earth and Planetary Sciences is Abstract online at earth.annualreviews.org Analogous to Earth’s water cycle, Titan’s methane-based hydrologic cycle This article’s doi: supports standing bodies of liquid and drives processes that result in common 10.1146/annurev-earth-060115-012247 Annu. Rev. Earth Planet. Sci. 2016.44:57-83. Downloaded from annualreviews.org morphologic features including dunes, channels, lakes, and seas. Like lakes Access provided by University of Chicago Libraries on 03/07/17. For personal use only. Copyright c 2016 by Annual Reviews. on Earth and early Mars, Titan’s lakes and seas preserve a record of its All rights reserved climate and surface evolution. Unlike on Earth, the volume of liquid exposed on Titan’s surface is only a small fraction of the atmospheric reservoir. The volume and bulk composition of the seas can constrain the age and nature of atmospheric methane, as well as its interaction with surface reservoirs. Similarly, the morphology of lacustrine basins chronicles the history of the polar landscape over multiple temporal and spatial scales. -
Titan a Moon with an Atmosphere
TITAN A MOON WITH AN ATMOSPHERE Ashley Gilliam Earth 450 – Satellites of Jupiter and Saturn 4/29/13 SATURN HAS > 60 SATELLITES, WHY TITAN? Is the only satellite with a dense atmosphere Has a nitrogen-rich atmosphere resembles Earth’s Is the only world besides Earth with a liquid on its surface • Possible habitable world Based on its size… Titan " a planet in its o# $ght! R = 6371 km R = 2576 km R = 1737 km Ch$%iaan Huy&ns (1629-1695) DISCOVERY OF TITAN Around 1650, Huygens began building telescopes with his brother Constantijn On March 25, 1655 Huygens discovered Titan in an attempt to study Saturn’s rings Named the moon Saturni Luna (“Saturns Moon”) Not properly named until the mid-1800’s THE DISCOVERY OF TITAN’S ATMOSPHERE Not much more was learned about Titan until the early 20th century In 1903, Catalan astronomer José Comas Solà claimed to have observed limb darkening on Titan, which requires the presence of an atmosphere Gerard P. Kuiper (1905-1973) José Comas Solà (1868-1937) This was confirmed by Gerard Kuiper in 1944 Image Credit: Ralph Lorenz Voyager 1 Launched September 5, 1977 M"sions to Titan Pioneer 11 Launched April 6, 1973 Cassini-Huygens Images: NASA Launched October 15, 1997 Pioneer 11 Could not penetrate Titan’s Atmosphere! Image Credit: NASA Vo y a &r 1 Image Credit: NASA Vo y a &r 1 What did we learn about the Atmosphere? • Composition (N2, CH4, & H2) • Variation with latitude (homogeneously mixed) • Temperature profile Mesosphere • Pressure profile Stratosphere Troposphere Image Credit: Fulchignoni, et al., 2005 Image Credit: Conway et al. -
The Origin of Titan's Atmosphere: Some Recent Advances
The origin of Titan’s atmosphere: some recent advances By Tobias Owen1 & H. B. Niemann2 1University of Hawaii, Institute for Astronomy, 2680 Woodlawn Drive, Honolulu, HI 96822, USA 2Laboratory for Atmospheres, Goddard Space Fight Center, Greenbelt, MD 20771, USA It is possible to make a consistent story for the origin of Titan’s atmosphere starting with the birth of Titan in the Saturn subnebula. If we use comet nuclei as a model, Titan’s nitrogen and methane could easily have been delivered by the ice that makes up ∼50% of its mass. If Titan’s atmospheric hydrogen is derived from that ice, it is possible that Titan and comet nuclei are in fact made of the same protosolar ice. The noble gas abundances are consistent with relative abundances found in the atmospheres of Mars and Earth, the sun, and the meteorites. Keywords: Origin, atmosphere, composition, noble gases, deuterium 1. Introduction In this note, we will assume that Titan originated in Saturn’s subnebula as a result of the accretion of icy planetesimals: particles and larger lumps made of ice and rock. Alibert & Mousis (2007) reached this same point of view using an evolutionary, turbulent model of Saturn’s subnebula. They found that planetesimals made in the solar nebula according to their model led to a huge overabundance of CO on Titan. We obviously have no direct measurements of the composition of these planetes- imals. We can use comets as a guide, always remembering that comets formed in the solar nebula where conditions must have been different from those in Saturn’s subnebula, e.g., much colder. -
Hydrocarbon Lakes on Titan
Icarus 186 (2007) 385–394 www.elsevier.com/locate/icarus Hydrocarbon lakes on Titan Giuseppe Mitri a,∗,AdamP.Showmana, Jonathan I. Lunine a,b, Ralph D. Lorenz a,c a Department of Planetary Sciences and Lunar and Planetary Laboratory, University of Arizona, 1629 E. University Blvd., Tucson, AZ 85721-0092, USA b Istituto di Fisica dello Spazio Interplanetario INAF-IFSI, Via del Fosso del Cavaliere, 00133 Rome, Italy c Now at Space Department, Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723-6099, USA Received 9 March 2006; revised 6 September 2006 Available online 7 November 2006 Abstract The Huygens Probe detected dendritic drainage-like features, methane clouds and a high surface relative humidity (∼50%) on Titan in the vicinity of its landing site [Tomasko, M.G., and 39 colleagues, 2005. Nature 438, 765–778; Niemann, H.B., and 17 colleagues, 2005. Nature 438, 779–784], suggesting sources of methane that replenish this gas against photo- and charged-particle chemical loss on short (10–100) million year timescales [Atreya, S.K., Adams, E.Y., Niemann, H.B., Demick-Montelara, J.E., Owen, T.C., Fulchignoni, M., Ferri, F., Wilson, E.H., 2006. Planet. Space Sci. In press]. On the other hand, Cassini Orbiter remote sensing shows dry and even desert-like landscapes with dunes [Lorenz, R.D., and 39 colleagues, 2006a. Science 312, 724–727], some areas worked by fluvial erosion, but no large-scale bodies of liquid [Elachi, C., and 34 colleagues, 2005. Science 308, 970–974]. Either the atmospheric methane relative humidity is declining in a steady fashion over time, or the sources that maintain the relative humidity are geographically restricted, small, or hidden within the crust itself. -
The Exploration of Titan with an Orbiter and a Lake Probe
Planetary and Space Science ∎ (∎∎∎∎) ∎∎∎–∎∎∎ Contents lists available at ScienceDirect Planetary and Space Science journal homepage: www.elsevier.com/locate/pss The exploration of Titan with an orbiter and a lake probe Giuseppe Mitri a,n, Athena Coustenis b, Gilbert Fanchini c, Alex G. Hayes d, Luciano Iess e, Krishan Khurana f, Jean-Pierre Lebreton g, Rosaly M. Lopes h, Ralph D. Lorenz i, Rachele Meriggiola e, Maria Luisa Moriconi j, Roberto Orosei k, Christophe Sotin h, Ellen Stofan l, Gabriel Tobie a,m, Tetsuya Tokano n, Federico Tosi o a Université de Nantes, LPGNantes, UMR 6112, 2 rue de la Houssinière, F-44322 Nantes, France b Laboratoire d’Etudes Spatiales et d’Instrumentation en Astrophysique (LESIA), Observatoire de Paris, CNRS, UPMC University Paris 06, University Paris-Diderot, Meudon, France c Smart Structures Solutions S.r.l., Rome, Italy d Center for Radiophysics and Space Research, Cornell University, Ithaca, NY 14853, United States e Dipartimento di Ingegneria Meccanica e Aerospaziale, Università La Sapienza, 00184 Rome, Italy f Institute of Geophysics and Planetary Physics, Department of Earth and Space Sciences, Los Angeles, CA, United States g LPC2E-CNRS & LESIA-Obs., Paris, France h Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States i Johns Hopkins University, Applied Physics Laboratory, Laurel, MD, United States j Istituto di Scienze dell‘Atmosfera e del Clima (ISAC), Consiglio Nazionale delle Ricerche (CNR), Rome, Italy k Istituto di Radioastronomia (IRA), Istituto Nazionale -
AVIATR—Aerial Vehicle for In-Situ and Airborne Titan Reconnaissance a Titan Airplane Mission Concept
Exp Astron DOI 10.1007/s10686-011-9275-9 ORIGINAL ARTICLE AVIATR—Aerial Vehicle for In-situ and Airborne Titan Reconnaissance A Titan airplane mission concept Jason W. Barnes · Lawrence Lemke · Rick Foch · Christopher P. McKay · Ross A. Beyer · Jani Radebaugh · David H. Atkinson · Ralph D. Lorenz · Stéphane Le Mouélic · Sebastien Rodriguez · Jay Gundlach · Francesco Giannini · Sean Bain · F. Michael Flasar · Terry Hurford · Carrie M. Anderson · Jon Merrison · Máté Ádámkovics · Simon A. Kattenhorn · Jonathan Mitchell · Devon M. Burr · Anthony Colaprete · Emily Schaller · A. James Friedson · Kenneth S. Edgett · Angioletta Coradini · Alberto Adriani · Kunio M. Sayanagi · Michael J. Malaska · David Morabito · Kim Reh Received: 22 June 2011 / Accepted: 10 November 2011 © The Author(s) 2011. This article is published with open access at Springerlink.com J. W. Barnes (B) · D. H. Atkinson · S. A. Kattenhorn University of Idaho, Moscow, ID 83844-0903, USA e-mail: [email protected] L. Lemke · C. P. McKay · R. A. Beyer · A. Colaprete NASA Ames Research Center, Moffett Field, CA, USA R. Foch · Sean Bain Naval Research Laboratory, Washington, DC, USA R. A. Beyer Carl Sagan Center at the SETI Institute, Mountain View, CA, USA J. Radebaugh Brigham Young University, Provo, UT, USA R. D. Lorenz Johns Hopkins University Applied Physics Laboratory, Silver Spring, MD, USA S. Le Mouélic Laboratoire de Planétologie et Géodynamique, CNRS, UMR6112, Université de Nantes, Nantes, France S. Rodriguez Université de Paris Diderot, Paris, France Exp Astron Abstract We describe a mission concept for a stand-alone Titan airplane mission: Aerial Vehicle for In-situ and Airborne Titan Reconnaissance (AVI- ATR). With independent delivery and direct-to-Earth communications, AVI- ATR could contribute to Titan science either alone or as part of a sustained Titan Exploration Program. -
Atmospheric Planetary Probes And
SPECIAL ISSUE PAPER 1 Atmospheric planetary probes and balloons in the solar system A Coustenis1∗, D Atkinson2, T Balint3, P Beauchamp3, S Atreya4, J-P Lebreton5, J Lunine6, D Matson3,CErd5,KReh3, T R Spilker3, J Elliott3, J Hall3, and N Strange3 1LESIA, Observatoire de Paris-Meudon, Meudon Cedex, France 2Department Electrical & Computer Engineering, University of Idaho, Moscow, ID, USA 3Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA 4University of Michigan, Ann Arbor, MI, USA 5ESA/ESTEC, AG Noordwijk, The Netherlands 6Dipartment di Fisica, University degli Studi di Roma, Rome, Italy The manuscript was received on 28 January 2010 and was accepted after revision for publication on 5 November 2010. DOI: 10.1177/09544100JAERO802 Abstract: A primary motivation for in situ probe and balloon missions in the solar system is to progressively constrain models of its origin and evolution. Specifically, understanding the origin and evolution of multiple planetary atmospheres within our solar system would provide a basis for comparative studies that lead to a better understanding of the origin and evolution of our Q1 own solar system as well as extra-solar planetary systems. Hereafter, the authors discuss in situ exploration science drivers, mission architectures, and technologies associated with probes at Venus, the giant planets and Titan. Q2 Keywords: 1 INTRODUCTION provide significant design challenge, thus translating to high mission complexity, risk, and cost. Since the beginning of the space age in 1957, the This article focuses on the exploration of planetary United States, European countries, and the Soviet bodies with sizable atmospheres, using entry probes Union have sent dozens of spacecraft, including and aerial mobility systems, namely balloons. -
Detection of Chemical Species in Titan's Atmosphere Using High
UNIVERSIDADE DE LISBOA FACULDADE DE CIÊNCIAS DEPARTAMENTO FÍSICA Detection of Chemical Species in Titan’s Atmosphere using High-Resolution Spectroscopy José Luís Fernandes Ribeiro Mestrado em Física Especialização em Astrofísica e Cosmologia Dissertação orientada por: Doutor Pedro Machado 2019 Acknowledgments This master’s thesis would not be possible without the support of my parents, Maria de F´atimaPereira Fernandes Ribeiro and Lu´ısCarlos Pereira Ribeiro, who I would like to thank for believing in me, encouraging me and allowing me to embark on this journey of knowledge and discovery. They made the person that I am today. I would like to thank all my friends and colleagues who accompanied me all these years for the great moments and new experiences that happened trough these years of university. They contributed a lot to my life and for that I am truly grateful. I just hope that I contributed to theirs as well. I also would like to thank John Pritchard from ESO Operations Support for helping me getting the EsoReflex UVES pipeline working on my computer, without him we would probably wouldn’t have the Titan spectra reduced by now. And I also like to thank Doctor Santiago P´erez-Hoyos for his availability to teach our planetary sciences group how to use the NEMESIS Radiative Transfer model and Doctor Th´er`ese Encrenaz for providing the ISO Saturn and Jupiter data. I would like to give a special thank you to Jo˜aoDias and Constan¸caFreire, for their support and help during this work. Lastly, and surely not the least, I would like to thank my supervisor Pedro Machado for showing me how to be a scientist and how to do scientific work. -
Regional Geomorphology and History of Titan's Xanadu Province
Icarus 211 (2011) 672–685 Contents lists available at ScienceDirect Icarus journal homepage: www.elsevier.com/locate/icarus Regional geomorphology and history of Titan’s Xanadu province J. Radebaugh a,, R.D. Lorenz b, S.D. Wall c, R.L. Kirk d, C.A. Wood e, J.I. Lunine f, E.R. Stofan g, R.M.C. Lopes c, P. Valora a, T.G. Farr c, A. Hayes h, B. Stiles c, G. Mitri c, H. Zebker i, M. Janssen c, L. Wye i, A. LeGall c, K.L. Mitchell c, F. Paganelli g, R.D. West c, E.L. Schaller j, The Cassini Radar Team a Department of Geological Sciences, Brigham Young University, S-389 ESC Provo, UT 84602, United States b Johns Hopkins Applied Physics Laboratory, Laurel, MD 20723, United States c Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, United States d US Geological Survey, Branch of Astrogeology, Flagstaff, AZ 86001, United States e Wheeling Jesuit University, Wheeling, WV 26003, United States f Department of Physics, University of Rome ‘‘Tor Vergata”, Rome 00133, Italy g Proxemy Research, P.O. Box 338, Rectortown, VA 20140, USA h Department of Geological Sciences, California Institute of Technology, Pasadena, CA 91125, USA i Department of Electrical Engineering, Stanford University, 350 Serra Mall, Stanford, CA 94305, USA j Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA article info abstract Article history: Titan’s enigmatic Xanadu province has been seen in some detail with instruments from the Cassini space- Received 20 March 2009 craft.