“Habitable Extrasolar Planetary Systems, the Case of 55 Cnc”
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Lunar & Planetary Surface Power Management & Distribution
NASA SBIR 2020 Phase I Solicitation Z1.05 Lunar & Planetary Surface Power Management & Distribution Lead Center: GRC Participating Center(s): GSFC, JSC Technology Area: TA3 Space Power and Energy Storage Scope Title Innovative ways to transmit high power for lunar & Mars surface missions Scope Description The Global Exploration Roadmap (January 2018) and the Space Policy Directive (December 2017) detail NASA’s plans for future human-rated space missions. A major factor in this involves establishing bases on the lunar surface and eventually Mars. Surface power for bases is envisioned to be located remotely from the habitat modules and must be efficiently transferred over significant distances. The International Space Station (ISS) has the highest power (100kW), and largest space power distribution system with eight interleaved micro-grids providing power functions similar to a terrestrial power utility. Planetary bases will be similar to the ISS with expectations of multiple power sources, storage, science, and habitation modules, but at higher power levels and with longer distribution networks providing interconnection. In order to enable high power (>100kW) and longer distribution systems on the surface of the moon or Mars, NASA is in need of innovative technologies in the areas of lower mass/higher efficiency power electronic regulators, switchgear, cabling, connectors, wireless sensors, power beaming, power scavenging, and power management control. The technologies of interest would need to operate in extreme temperature environments, including lunar night, and could experience temperature changes from -153C to 123C for lunar applications, and -125C to 80C for Mars bases. In addition to temperature extremes, technologies would need to withstand (have minimal degradation from) lunar dust/regolith, Mars dust storms, and space radiation levels. -
10. Scientific Programme 10.1
10. SCIENTIFIC PROGRAMME 10.1. OVERVIEW (a) Invited Discourses Plenary Hall B 18:00-19:30 ID1 “The Zoo of Galaxies” Karen Masters, University of Portsmouth, UK Monday, 20 August ID2 “Supernovae, the Accelerating Cosmos, and Dark Energy” Brian Schmidt, ANU, Australia Wednesday, 22 August ID3 “The Herschel View of Star Formation” Philippe André, CEA Saclay, France Wednesday, 29 August ID4 “Past, Present and Future of Chinese Astronomy” Cheng Fang, Nanjing University, China Nanjing Thursday, 30 August (b) Plenary Symposium Review Talks Plenary Hall B (B) 8:30-10:00 Or Rooms 309A+B (3) IAUS 288 Astrophysics from Antarctica John Storey (3) Mon. 20 IAUS 289 The Cosmic Distance Scale: Past, Present and Future Wendy Freedman (3) Mon. 27 IAUS 290 Probing General Relativity using Accreting Black Holes Andy Fabian (B) Wed. 22 IAUS 291 Pulsars are Cool – seriously Scott Ransom (3) Thu. 23 Magnetars: neutron stars with magnetic storms Nanda Rea (3) Thu. 23 Probing Gravitation with Pulsars Michael Kremer (3) Thu. 23 IAUS 292 From Gas to Stars over Cosmic Time Mordacai-Mark Mac Low (B) Tue. 21 IAUS 293 The Kepler Mission: NASA’s ExoEarth Census Natalie Batalha (3) Tue. 28 IAUS 294 The Origin and Evolution of Cosmic Magnetism Bryan Gaensler (B) Wed. 29 IAUS 295 Black Holes in Galaxies John Kormendy (B) Thu. 30 (c) Symposia - Week 1 IAUS 288 Astrophysics from Antartica IAUS 290 Accretion on all scales IAUS 291 Neutron Stars and Pulsars IAUS 292 Molecular gas, Dust, and Star Formation in Galaxies (d) Symposia –Week 2 IAUS 289 Advancing the Physics of Cosmic -
Venus: Global Warming Gone Bad Earth & Venus: Sister Planets? Venus Earth
Venus: Global warming gone bad Earth & Venus: Sister planets? Venus Earth Mass 5x1024 kg 6x1024 kg a (semi- 0.7 AU 1 AU major axis) What is T at surface ~750 K ~300 K the boiling Temp of water? P at surface ~90 atm ~1 atm atm N2 and H2O CO2 and composition clouds H2SO4 clouds How do we know Venus’s surface temperature? How do we know Venus’s surface temperature? high energy low energy short wavelength long wavelength “bluer” “redder” hot cold How do we know Venus’s surface temperature? the Sun emits light Earth emits light here. T=6000 K here. T=300 K Venus emits light here. T=750 How do we know what the clouds are made of? Spectrum of planet with no atmosphere Amountof light observed above the atmosphere Wavelength of light (in the infrared) How do we know what the clouds are made of? Spectrum of Spectrum of planet with no planet with atmosphere atmosphere Wavelength at which a molecule in the atmosphere absorbs light Amountof light observed above the atmosphere Amountof light observed above the atmosphere Wavelength of light (in the Wavelength of light (in the infrared) infrared) How do we know what the clouds are made of? (Infrared light) How did Venus get so hot? Remember - all gases absorb light at specific wavelengths. “Greenhouse” gases (like carbon dioxide, water and methane) like to absorb in the infrared wavelengths. Planets emit light at infrared wavelengths (same as human bodies). Conclusio n? “Greenhouse” gases don’t lett the heat from the planet escape. -
Why Pluto Is Not a Planet Anymore Or How Astronomical Objects Get Named
3 Why Pluto Is Not a Planet Anymore or How Astronomical Objects Get Named Sethanne Howard USNO retired Abstract Everywhere I go people ask me why Pluto was kicked out of the Solar System. Poor Pluto, 76 years a planet and then summarily dismissed. The answer is not too complicated. It starts with the question how are astronomical objects named or classified; asks who is responsible for this; and ends with international treaties. Ultimately we learn that it makes sense to demote Pluto. Catalogs and Names WHO IS RESPONSIBLE for naming and classifying astronomical objects? The answer varies slightly with the object, and history plays an important part. Let us start with the stars. Most of the bright stars visible to the naked eye were named centuries ago. They generally have kept their old- fashioned names. Betelgeuse is just such an example. It is the eighth brightest star in the northern sky. The star’s name is thought to be derived ,”Yad al-Jauzā' meaning “the Hand of al-Jauzā يد الجوزاء from the Arabic i.e., Orion, with mistransliteration into Medieval Latin leading to the first character y being misread as a b. Betelgeuse is its historical name. The star is also known by its Bayer designation − ∝ Orionis. A Bayeri designation is a stellar designation in which a specific star is identified by a Greek letter followed by the genitive form of its parent constellation’s Latin name. The original list of Bayer designations contained 1,564 stars. The Bayer designation typically assigns the letter alpha to the brightest star in the constellation and moves through the Greek alphabet, with each letter representing the next fainter star. -
Planetary Geology: Goals, Future Directions, and Recommendations
NASA Conference Publication 3005 Planetary Geology: Goals, Future Directions, and Recommendations Proceedings of a workshop held at Arizona State University Tempe, Arizona January 1987 NASA Conference Publication 3005 Planetary Geology: Goals, Future Directions, and Recommendations NASA Office of Space Science and Applications Washington, D. C. Proceedings of a workshop held at Arizona State University Tempe, Arizona January 1987 National Aeronautics and Space Administration Scientific and Technical Information Division Preface This report gives results of a workshop on planetary geology held in January, 1987, at Arizona State University at the request of Dr. David Scott, Discipline Scientist, Planetary Geology and Geophysics, NASA. In addition to reviews by the workshop members, it was reviewed by the Planetary Geology and Geophysics Working Group and incorporated comments from Dr. James Underwood, current Discipline Scientist for the program. R. Greeley, January 1988 TABLE OF CONTENTS Page 1.0 Executive Summary ............................................................................... 1 2.0 Introduction ........................................................................................ 3 3.0 Workshop Conclusions ........................................................................... 5 3.1 Planetary geology studies are in transition from a descriptive phase to prcxess-oriented research .................................................. 5 3.2 Quantitative techniques can be applied to existing data. but there is a need for -
Impact Craters on Titan: Finalizing Titan's Crater Population
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2105.pdf IMPACT CRATERS ON TITAN: FINALIZING TITAN’S CRATER POPULATION. J. E. Hedgepeth1, C. D. Neish1, E. P. Turtle B. W. Stiles2 1University of Western Ontario Department of Earth Sciences, London, ON ([email protected]), 2Jet Propulsion Laboratory, Pasadena, CA. Introduction: Saturn’s moon Titan is one of the map craters as shapefiles. The craters are meticulously most dynamic bodies in the solar system. It is the only mapped across the surface. This map is compared to the moon with a thick atmosphere, and like Earth’s atmos- most up to date ISS mosaic, updating the crater map phere it has an active hydrological cycle. However, the where necessary. atmosphere of Titan is organic rich and rains methane This finalized catalog of craters on Titan is imported instead of water. As a result, Titan’s surface topography into MATLAB as shapefiles for further analysis. Initial is being modified extensively by many of the same types estimates of crater diameter and center positions are cat- of erosional processes seen on Earth. The methane rain aloged for further work. creates a complex system of river networks, and the Topographic Analysis: Our understanding of im- equatorial regions are covered by seas of organic sand pact cratering controls how we perceive surface changes dunes. on Earth and other worlds. Therefore, constraining cra- The extent of the endogenic and exogenic processes tering processes informs planetary surface evolution. A on Titan is best observed in its impact craters. Impact large catalog of unaltered craters exists on other icy cratering is a fundamental process in planetary geology; worlds that can be compared with those we see on Titan it is a well understood process because of how pervasive [5, 6]. -
Elisa: Astrophysics and Cosmology in the Millihertz Regime Contents
Doing science with eLISA: Astrophysics and cosmology in the millihertz regime Pau Amaro-Seoane1; 13, Sofiane Aoudia1, Stanislav Babak1, Pierre Binétruy2, Emanuele Berti3; 4, Alejandro Bohé5, Chiara Caprini6, Monica Colpi7, Neil J. Cornish8, Karsten Danzmann1, Jean-François Dufaux2, Jonathan Gair9, Oliver Jennrich10, Philippe Jetzer11, Antoine Klein11; 8, Ryan N. Lang12, Alberto Lobo13, Tyson Littenberg14; 15, Sean T. McWilliams16, Gijs Nelemans17; 18; 19, Antoine Petiteau2; 1, Edward K. Porter2, Bernard F. Schutz1, Alberto Sesana1, Robin Stebbins20, Tim Sumner21, Michele Vallisneri22, Stefano Vitale23, Marta Volonteri24; 25, and Henry Ward26 1Max Planck Institut für Gravitationsphysik (Albert-Einstein-Institut), Germany 2APC, Univ. Paris Diderot, CNRS/IN2P3, CEA/Irfu, Obs. de Paris, Sorbonne Paris Cité, France 3Department of Physics and Astronomy, The University of Mississippi, University, MS 38677, USA 4Division of Physics, Mathematics, and Astronomy, California Institute of Technology, Pasadena CA 91125, USA 5UPMC-CNRS, UMR7095, Institut d’Astrophysique de Paris, F-75014, Paris, France 6Institut de Physique Théorique, CEA, IPhT, CNRS, URA 2306, F-91191Gif/Yvette Cedex, France 7University of Milano Bicocca, Milano, I-20100, Italy 8Department of Physics, Montana State University, Bozeman, MT 59717, USA 9Institute of Astronomy, University of Cambridge, Madingley Road, Cambridge, CB3 0HA, UK 10ESA, Keplerlaan 1, 2200 AG Noordwijk, The Netherlands 11Institute of Theoretical Physics University of Zürich, Winterthurerstr. 190, 8057 Zürich Switzerland -
EART163 Planetary Surfaces
EART163 Planetary Surfaces Francis Nimmo Course Overview • How did the planetary surfaces we see form and evolve? What processes are/were operating? • Techniques to answer these questions: – Images – Modelling/Quantitative analysis – Comparative analysis and analogues • Case studies – examples from this Solar System Course Outline • Week 1 – Introduction, planetary shapes • Week 2 – Strength and rheology • Week 3 – Tectonics • Week 4 – Volcanism and cryovolcanism • Week 5 – Midterm; Impacts • Week 6 – Impacts (cont’d) • Week 7 – Slopes and mass movement • Week 8 – Wind • Week 9 – Water & Ice • Week 10 – Ice cont’d; Recap; Final Recent spacecraft missions (2018-19) ESA landed on a comet (C-G) ~2m JAXA landed on an asteroid (Ryugu) ~10 km CNSA landed on the lunar farside NASA flew by a Kuiper Belt Object (MU69) Logistics • Website: http://www.es.ucsc.edu/~fnimmo/eart163 • Set text – Melosh, Planetary Surface Processes (2011) • Prerequisites – 160; some knowledge of calculus • Grading – based on weekly homeworks (~30%), midterm (~20%), final (~50%). • Homeworks due on Tuesdays • Location/Timing – TuTh 1:30-3:05pm D258 E&MS • Office hours –MoTh 3:05-4:05pm (A219 E&MS) or by appointment (email: [email protected]) • Questions/feedback? - Yes please! Expectations • Homework typically consists of 3 questions • Grad students will have one extra question (harder) • If it’s taking you more than 1 hour per question on average, you’ve got a problem – come and see me • Midterm/finals consist of short (compulsory) and long (pick from a list) questions • In both the midterm and the final you will receive a formula sheet • Showing up and asking questions are usually routes to a good grade • Plagiarism – see website for policy. -
Ceres – VIS-IR Surface Composition Analysis: a Review in Advance of the AD WN Mission Daniela Henckel
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects January 2015 Ceres – VIS-IR Surface Composition Analysis: A Review In Advance Of The AD WN Mission Daniela Henckel Follow this and additional works at: https://commons.und.edu/theses Recommended Citation Henckel, Daniela, "Ceres – VIS-IR Surface Composition Analysis: A Review In Advance Of The AD WN Mission" (2015). Theses and Dissertations. 1783. https://commons.und.edu/theses/1783 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. CERES – VIS-IR SURFACE COMPOSITION ANALYSIS: A REVIEW IN ADVANCE OF THE DAWN MISSION by Daniela Henckel Bachelor of Science, University of Potsdam, 2010 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Science Grand Forks, North Dakota May 2015 This thesis, submitted by Daniela Henckel in partial fulfillment of the requirements for the Degree of Master of Science from the University of North Dakota, has been read by the Faculty Advisory Committee under whom the work has been done and is hereby approved. Dr. Michael J. Gaffey Dr. Ron Fevig Dr. Santosh Seelan Dr. Gabriele Arnold This thesis is being submitted by the appointed advisory committee as having met all of the requirements of the School of Graduate Studies at the University of North Dakota and is hereby approved. -
Planetary Surface Instrument Workshop Report (1995)
PLANETARY SURFACE INSTRUMENTS WORKSHOP Edited by Charles Meyer, Allan H. Treiman, and Theodor Kostiuk Held at Houston, Texas May 12–13, 1995 Sponsored by Lunar and Planetary Institute Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 LPI Technical Report Number 95-05 LPI/TR--95-05 ii Planetary Surface Instruments Workshop Compiled in 1996 by LUNAR AND PLANETARY INSTITUTE The Institute is operated by the Universities Space Research Association under Contract No. NASW-4574 with the National Aeronautics and Space Administration. Material in this volume may be copied without restraint for library, abstract service, education, or personal research purposes; however, republication of any paper or portion thereof requires the written permission of the authors as well as the appropriate acknowledgment of this publication. This report may be cited as Meyer C., Treiman A. H., and Kostiuk T., eds. (1996) Planetary Surface Instruments Workshop. LPI Tech. Rpt. 95- 05, Lunar and Planetary Institute, Houston. 115 pp. This report is distributed by ORDER DEPARTMENT Lunar and Planetary Institute 3600 Bay Area Boulevard Houston TX 77058-1113 Mail order requestors will be invoiced for the cost of shipping and handling. Cover: MIMOS-II, a miniaturized Mössbauer instrument with two detector channels, developed for use in space missions with very limited power resources like the Small Stations of the Russian Mars ’96 Mission. LPI Technical Report 95-05 iii Introduction The next steps in the exploration of the solar system will include robotic missions to the surfaces of planets, moons, asteroids, and comets. For the greatest possible returns from these missions, their scientific rationales must be closely coordinated with development of appropriate instrumentation and with the constraints of mission and program planning. -
第 28 届国际天文学联合会大会 Programme Book
IAU XXVIII GENERAL ASSEMBLY 20-31 AUGUST, 2012 第 28 届国际天文学联合会大会 PROGRAMME BOOK 1 Table of Contents Welcome to IAU Beijing General Assembly XXVIII ........................... 4 Welcome to Beijing, welcome to China! ................................................ 6 1.IAU EXECUTIVE COMMITTEE, HOST ORGANISATIONS, PARTNERS, SPONSORS AND EXHIBITORS ................................ 8 1.1. IAU EXECUTIVE COMMITTEE ..................................................................8 1.2. IAU SECRETARIAT .........................................................................................8 1.3. HOST ORGANISATIONS ................................................................................8 1.4. NATIONAL ADVISORY COMMITTEE ........................................................9 1.5. NATIONAL ORGANISING COMMITTEE ..................................................9 1.6. LOCAL ORGANISING COMMITTEE .......................................................10 1.7. ORGANISATION SUPPORT ........................................................................ 11 1.8. PARTNERS, SPONSORS AND EXHIBITORS ........................................... 11 2.IAU XXVIII GENERAL ASSEMBLY INFORMATION ............... 14 2.1. LOCAL ORGANISING COMMITTEE OFFICE .......................................14 2.2. IAU SECRETARIAT .......................................................................................14 2.3. REGISTRATION DESK – OPENING HOURS ...........................................14 2.4. ON SITE REGISTRATION FEES AND PAYMENTS ................................14 -
Planetary Surface Processes
Planetary Surface Processes Nathan Bridges Applied Physics Laboratory (and former JPLer and ongoing coworker with many at JPL and Caltech) rippled sand in Gale Crater MSL landing ellipse HiRISE image ESP_023957_1755 Properties of Bodies with Major Atmospheres Venus Earth Mars Titan Solar distance (AU) 0.72 1 1.7 10.1 Orbital period (d) 224 365 687 10,759 (Sun) 16 (Saturn) Rotation period ‐243 d 24 h 24h 37m 16 d Axial tilt (°) 177.4 23.4 25.2 0 Diameter (km) 12,104 12,742 6779 5152 Surface gravity (m s‐2) 8.9 9.8 3.7 1.4 Surface temperature (K) 737 184‐330 130‐308 94 Surface pressure (bars) 92 1 0.6 1.5 Typical surface basalt water; basalt water ice; composition silicates hydrocarbons (liquid, ices, tholins) Atmospheric composition 96.5% CO2 78.1% N2 96.0% CO2 95.0% N2 (lower troposphere) 3.5% N2 21.0% O2 1.9% Ar 4.9% CH4 0.9% Ar 1.9% N2 0.1% O2 0.1% CO Surface Processes of Bodies with Major Atmospheres Venus Earth Mars Titan Aeolian √√√√ Fluvial X √ minor √ Glacial/periglacial X √√ ? Impact √√√√ Mass wasting √√√√ Seasonal X √√ √ Tectonics √√√? Volcanism √√√√ Climate Change ? √ maybe ? Apology for these objects that are not covered I can’t talk about everything, nor do I know everything etc. Earth largely passed over because we know a lot more and it is not in scope with this talk Io and Enceladus are mentioned later for volcanics Dust and Dust Aggregates Comparison of Terrestrial and Martian Dust Transport and Size [Bridges and Muhs, 2012; Muhs and Bettis, 2003] Dust Lifting and Storms (mostly Earth and Mars) Known: The approximate mechanisms conditions, locations, and times of year when local, regional, and (in the case of Mars) global storms occur Unknown: Precise prediction of storms more than a few days in advance and location centers to a few km or less Solution: Rapid repeat data collection: ‐ images ‐ surface and atmospheric temp.