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An Investigation of Aerogravity Assist at Titan and Triton for Capture Into Orbit About Saturn and Neptune 2Nd International Planetary Probe Workshop August 2004, USA
An Investigation of Aerogravity Assist at Titan and Triton for Capture into Orbit About Saturn and Neptune 2nd International Planetary Probe Workshop August 2004, USA Philip Ramsey(1) and James Evans Lyne(2) (1)Department of Mechanical, Aerospace and Biomedical Engineering The University of Tennessee Knoxville, TN 37996 USA [email protected] (2)Department of Mechanical, Aerospace and Biomedical Engineering The University of Tennessee Knoxville, TN 37996 USA [email protected] ABSTRACT proposed that an aerogravity assist maneuver at the moon Titan could be used to capture a probe Previous work by our group has shown that an into orbit about Saturn, using an aeroshell with a aerogravity assist maneuver at the moon Titan with a low to moderate lift-to-drag ratio (0.25 to could be used to capture a spacecraft into a 1.0).1 This approach provides for capture into closed orbit about Saturn if a nominal orbit about the gas giant, while avoiding the atmospheric profile at Titan is assumed. The very high entry speeds and aerothermal heating present study extends that work and examines environment inherent to a trajectory thru the the impact of atmospheric dispersions, variations atmosphere of Saturn itself. in the final target orbit and low density aerodynamics on the aerocapture maneuver. Titan is unique among moons in the solar Accounting for atmospheric dispersions system in that it has an atmosphere considerably substantially reduces the entry corridor width for thicker than Earth’s, with a ground level density a blunt configuration with a lift-to-drag ratio of of about 5.44 kg/m3. -
Planetary Science in the Eyes of Giant Telescopes
Planetary Science in the Eyes of Giant Telescopes Franck Marchis (Carl Sagan Center at the SETI Ins<tute) Feeding the Giants Workshop, Ischia, Italy, August 30 2011, Outline ELTs = Extremely Large Telescopes (E-ELT, TMT, GMT) • Solar System Exploraon – Why Exploring the Solar System with ELTs – Space Mission Programs: Why, Who, Where, When? • Poten<al of the ELTs for Solar System Science – High Angular imaging coupled with spectroscopy in the NIR to explore Io, Titan, and TNOs – Low res UV-NIR spectroscopic combined with All-sky surveys 402 Years of Telescopes Why Planetary Science and the ELTs? • Long heritage of telescopic observaons for the study of the Solar System • Started in 1609 with Galileo Galilei – First publicaon in modern astronomy based on telescope data – Discoveries in the field of Planetary Science • Galilean Moons • Roughness of the Moon surface • Disk appearance of planets & phase of Venus • In 2009, 40% of Keck PR and 25% of Keck AO publicaons are based on Planetary Science results • Strong Public Interest for Planetary Science Toys in Japan Pluto protests 51 Years of Space Missions • First aempts to reach Mars (1960) and Venus (1961) • ~200 solar, lunar and interplanetary missions • More reliable technologies -> more space missions • More accessible technologies -> more countries have access to space (e.g. Japan, China, India,…) • Could the ELTs contribute to Planetary Science in this context? 51 Years of Space Missions (2009) Naonal Geographic 51 Years of Space Missions Inner Solar System NEA 51 Years of Space Missions -
Ice Giants As Exoplanet Analogs K.E
Ice Giants as Exoplanet Analogs K.E. Mandt, O. Mousis, J. Lunine, B. Marty, T. Smith, A. Luspay- Kuti, A. Aguichine @mommascientist Ice Giants as Exoplanet Analogs • Ice Giant mass/radius common among detected exoplanets • Our Ice Giants only explored by single flybys • Major questions remain about formation process, interior structure and composition, energy balance, and interaction with the Sun • Broad international support for a mission to Uranus and/or Neptune What observations of our Ice Giants would help advance Exoplanet characterization efforts? @mommascientist 5 January 2021 2 Big questions about the Ice Giants • Several studies have designed missions to Uranus and/or Neptune • Common Science Goals - How did the Ice Giants form and evolve? - What is the interior structure of the Ice Giants? - How does the planetary dynamo work? - What is the heat balance of the Ice Giants? - What drives atmospheric dynamics? - How did the rings form and evolve? - How did the moons form and evolve? Any mission to the Ice Giants must address system-level goals. The greatest synergy with current exoplanet research is in the origin, evolution, and current state of the planet. 5 January 2021 3 Giant Planet Formation and Evolution • What was the composition of the solid building blocks? • Did the Protosolar Nebula (PSN) composition vary with distance from the Sun? • What contributed to the noble gas isotope mixtures? Heavy elements trace building block formation, PSN composition, planet formation, and planet evolution @mommascientist Image credit: NASA/STScI -
Arxiv:2012.11628V3 [Astro-Ph.EP] 26 Jan 2021
manuscript submitted to JGR: Planets The Fundamental Connections Between the Solar System and Exoplanetary Science Stephen R. Kane1, Giada N. Arney2, Paul K. Byrne3, Paul A. Dalba1∗, Steven J. Desch4, Jonti Horner5, Noam R. Izenberg6, Kathleen E. Mandt6, Victoria S. Meadows7, Lynnae C. Quick8 1Department of Earth and Planetary Sciences, University of California, Riverside, CA 92521, USA 2Planetary Systems Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA 3Planetary Research Group, Department of Marine, Earth, and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA 4School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287, USA 5Centre for Astrophysics, University of Southern Queensland, Toowoomba, QLD 4350, Australia 6Johns Hopkins University Applied Physics Laboratory, Laurel, MD 20723, USA 7Department of Astronomy, University of Washington, Seattle, WA 98195, USA 8Planetary Geology, Geophysics and Geochemistry Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA Key Points: • Exoplanetary science is rapidly expanding towards characterization of atmospheres and interiors. • Planetary science has similarly undergone rapid expansion of understanding plan- etary processes and evolution. • Effective studies of exoplanets require models and in-situ data derived from plan- etary science observations and exploration. arXiv:2012.11628v4 [astro-ph.EP] 8 Aug 2021 ∗NSF Astronomy and Astrophysics Postdoctoral Fellow Corresponding author: Stephen R. Kane, [email protected] {1{ manuscript submitted to JGR: Planets Abstract Over the past several decades, thousands of planets have been discovered outside of our Solar System. These planets exhibit enormous diversity, and their large numbers provide a statistical opportunity to place our Solar System within the broader context of planetary structure, atmospheres, architectures, formation, and evolution. -
A New View of Haze Formation and Energy Balance in Triton's Cold And
EPSC Abstracts Vol. 13, EPSC-DPS2019-332-1, 2019 EPSC-DPS Joint Meeting 2019 c Author(s) 2019. CC Attribution 4.0 license. A New View of Haze Formation and Energy Balance in Triton’s Cold and Hazy Atmosphere Xi Zhang (1), Kazumasa Ohno (2), Darrell Strobel (3), Ryo Tazaki (4), and Satoshi Okuzumi (2) (1) University of California Santa Cruz, Santa Cruz, USA ([email protected]), (2) Tokyo Institute of Technology, Tokyo, Japan, (3) Johns Hopkins University, Baltimore, USA, (4) Tohoku University, Sendai, Japan Abstract missing coolant is needed to understand the energy balance in Triton’s lower atmosphere. This research on Neptune’s moon Triton consists of two parts. To start we built the first microphysical 2. Methods model of Triton haze formation including fractal aggregation of monomers and condensation of We have built the first bin-scheme microphysical supersaturated hydrocarbons and nitriles. Our model model for Triton’s haze and cloud formation. Our can explain the UV occultation and visible scattering model simulates the evolution of size distributions in observations from Voyager 2 spacecraft during the a one-dimensional framework with sedimentation, Neptune flyby. With our model we find that haze coagulation, condensation and vertical eddy mixing. particles play a dominant role in the energy balance We consider that the haze particles are initially in the lower atmosphere of Triton, which was composed of fractal aggregates—non-spherical neglected in previous studies. Future ice giant particles comprised of many many spherical missions with a Triton lander should be able to monomers—similar in previous studies on Titan and measure the infrared fluxes from the near-surface Pluto (e.g., Cabane et al. -
Neptune Polar Orbiter with Probes*
NEPTUNE POLAR ORBITER WITH PROBES* 2nd INTERNATIONAL PLANETARY PROBE WORKSHOP, AUGUST 2004, USA Bernard Bienstock(1), David Atkinson(2), Kevin Baines(3), Paul Mahaffy(4), Paul Steffes(5), Sushil Atreya(6), Alan Stern(7), Michael Wright(8), Harvey Willenberg(9), David Smith(10), Robert Frampton(11), Steve Sichi(12), Leora Peltz(13), James Masciarelli(14), Jeffrey Van Cleve(15) (1)Boeing Satellite Systems, MC W-S50-X382, P.O. Box 92919, Los Angeles, CA 90009-2919, [email protected] (2)University of Idaho, PO Box 441023, Moscow, ID 83844-1023, [email protected] (3)JPL, 4800 Oak Grove Blvd., Pasadena, CA 91109-8099, [email protected] (4)NASA Goddard Space Flight Center, Greenbelt, MD 20771, [email protected] (5)Georgia Institute of Technology, 320 Parian Run, Duluth, GA 30097-2417, [email protected] (6)University of Michigan, Space Research Building, 2455 Haward St., Ann Arbor, MI 48109-2143, [email protected] (7)Southwest Research Institute, Department of Space Studies, 1050 Walnut St., Suite 400, Boulder, CO 80302, [email protected] (8)NASA Ames Research Center, Moffett Field, CA 94035-1000, [email protected] (9)4723 Slalom Run SE, Owens Cross Roads, AL 35763, [email protected] (10) Boeing NASA Systems, MC H013-A318, 5301 Bolsa Ave., Huntington Beach, CA 92647-2099, [email protected] (11)Boeing NASA Systems, MC H012-C349, 5301 Bolsa Ave., Huntington Beach, CA 92647-2099 [email protected] (12)Boeing Satellite Systems, MC W-S50-X382, P.O. Box 92919, Los Angeles, CA 90009-2919, [email protected] (13) )Boeing NASA Systems, MC H013-C320, 5301 Bolsa Ave., Huntington Beach, CA 92647-2099, [email protected] (14)Ball Aerospace & Technologies Corp., P.O. -
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland)
Abstracts of Extreme Solar Systems 4 (Reykjavik, Iceland) American Astronomical Society August, 2019 100 — New Discoveries scope (JWST), as well as other large ground-based and space-based telescopes coming online in the next 100.01 — Review of TESS’s First Year Survey and two decades. Future Plans The status of the TESS mission as it completes its first year of survey operations in July 2019 will bere- George Ricker1 viewed. The opportunities enabled by TESS’s unique 1 Kavli Institute, MIT (Cambridge, Massachusetts, United States) lunar-resonant orbit for an extended mission lasting more than a decade will also be presented. Successfully launched in April 2018, NASA’s Tran- siting Exoplanet Survey Satellite (TESS) is well on its way to discovering thousands of exoplanets in orbit 100.02 — The Gemini Planet Imager Exoplanet Sur- around the brightest stars in the sky. During its ini- vey: Giant Planet and Brown Dwarf Demographics tial two-year survey mission, TESS will monitor more from 10-100 AU than 200,000 bright stars in the solar neighborhood at Eric Nielsen1; Robert De Rosa1; Bruce Macintosh1; a two minute cadence for drops in brightness caused Jason Wang2; Jean-Baptiste Ruffio1; Eugene Chiang3; by planetary transits. This first-ever spaceborne all- Mark Marley4; Didier Saumon5; Dmitry Savransky6; sky transit survey is identifying planets ranging in Daniel Fabrycky7; Quinn Konopacky8; Jennifer size from Earth-sized to gas giants, orbiting a wide Patience9; Vanessa Bailey10 variety of host stars, from cool M dwarfs to hot O/B 1 KIPAC, Stanford University (Stanford, California, United States) giants. 2 Jet Propulsion Laboratory, California Institute of Technology TESS stars are typically 30–100 times brighter than (Pasadena, California, United States) those surveyed by the Kepler satellite; thus, TESS 3 Astronomy, California Institute of Technology (Pasadena, Califor- planets are proving far easier to characterize with nia, United States) follow-up observations than those from prior mis- 4 Astronomy, U.C. -
The Atmospheres of Pluto and Triton: Investigations with ALMA. M.A. Gurwell1, E
Pluto System After New Horizons 2019 (LPI Contrib. No. 2133) 7060.pdf The Atmospheres of Pluto and Triton: Investigations with ALMA. M.A. Gurwell1, E. Lellouch2, B.J. Butler3, R. Moreno4, A. Moullet5, D.F. Strobel6, and P. Lavvas7. 1Center for Astrophysics | Harvard & Smithsonian (Cam- bridge, MA 02138 USA; [email protected]), 2LESIA, Observatoire de Paris (92195 Meudon, France; em- [email protected]), 3National Radio Astronomy Observatory (Socorro, NM 87801 USA; bbut- [email protected]), 4LESIA, Observatoire de Paris (92195 Meudon, France; [email protected]), 5SOFIA Sci- ence Center, NASA Ames Research Center (Moffett Field, CA 94035 USA; [email protected]), 6Departments of Earth & Planetary Sciences and Physics & Astronomy, Johns Hopkins University (Baltimore, MD 21218 USA; [email protected]), 7GSMA, Université Reims Champagne-Ardenne (51687 Reims Cedex 2, France; panayotis.lav- [email protected]) Introduction: Pluto and Triton hold unique clues hyperfine structure of HCN; see Fig. 1), providing a for understanding the composition and evolution of the strong confirmation of the presence of CO, and the outer solar system, and are recognized as benchmarks first observation of HCN in Pluto's atmosphere. The for studies of the Kuiper Belt. They are two of the larg- results are detailed in [5] and summarized here. The est known and most easily observed KBO members CO and HCN lines probed Pluto's atmosphere up to (from Earth, but with caveats), and they are similar in ∼450 km and ∼900 km altitude, respectively. The CO many ways; for one example, they both possess thin mole fraction was 515 ± 40 ppm for a 12 µbar surface (10 microbar class), N2-dominated atmospheres. -
Neptune Science with Argo – a Voyage Through the Outer Solar System
Neptune Science with Argo – A Voyage through the Outer Solar System C. J. Hansen (JPL), A. S. Aljabri (JPL), D. Banfield (Cornell), E. B. Bierhaus (LMA), M. Brown (CIT), J. E. Colwell (UCF), M. Dougherty (Imperial College, UK), A. R. Hendrix (JPL), A. Ingersoll (CIT), K. Khurana (UCLA), D. Landau (JPL), A. McEwen (UAz), D. A. Paige (UCLA), C. Paranicas (APL), C. M. Satter (JPL), B. Schmidt (UCLA), M. Showalter (ARC), L. J. Spilker (JPL), T. Spilker (JPL), J. Stansberry (UAz), N. Strange (JPL), M. Tiscareno (Cornell) Some earlier co-authors have recused themselves due to Decadal Survey panel obligations Primary author contact: Candice Hansen, 626-438-5640, Jet Propulsion Laboratory, 4800 Oak Grove Dr., Pasadena, CA 91109, [email protected] This white paper describes the Neptune science to be achieved by Argo (Neptune’s rings, Triton, and the Kuiper Belt Object science objectives are described in separate white papers, authored by L. Spilker, C. Hansen and J. Stansberry, resp.) 27 August 2009 Argo is an innovative pragmatic concept for a New Frontiers 4 mission to significantly expand our knowledge of the outer Solar System. It exploits an upcoming launch window that permits a close Triton encounter during a flyby through the Neptune system, and then continues on to a scientifically-selected Kuiper Belt Object. The mission will yield significant advances in our understanding of evolutionary processes of small bodies in the outer Solar System, in addition to providing an opportunity for historic advances in ice-giant system science. By carefully focusing scientific goals and optimizing the payload, Argo can provide paradigm-shifting science within the New Frontiers cost envelope. -
Formation of Telluric Planets and the Origin of Terrestrial Water
BIO Web of Conferences 2, 01003 (2014) DOI: 10.1051/bioconf/20140201003 C Owned by the authors, published by EDP Sciences, 2014 Formation of telluric planets and the origin of terrestrial water Sean Raymond1;a 1Laboratoire d’Astrophysique de Bordeaux, UMR 5804 Abstract. Simulations of planet formation have failed to reproduce Mars’ small mass (compared with Earth) for 20 years. Here I will present a solution to the Mars problem that invokes large-scale migration of Jupiter and Saturn while they were still embedded in the gaseous protoplanetary disk. Jupiter first migrated inward, then "tacked" and migrated back outward when Saturn caught up to it and became trapped in resonance. If this tack occurred when Jupiter was at 1.5 AU then the inner disk of rocky planetesimals and em- bryos is truncated and the masses and orbits of all four terrestrial planet are quantitatively reproduced. As the giant planets migrate back outward they re-populate the asteroid belt from two different source populations, matching the structure of the current belt. C-type material is also scattered inward to the terrestrial planet-forming zone, delivering about the right amount of water to Earth on 10-50 Myr timescales. 1 Introduction 2 The formation of terrestrial planets As described in the Introduction, the final stages of terrestrial planet formation take place in the presence of any giant planets that may have formed. In addition, it is during this phase that bodies are large enough that during gravitational close encounters they can obtain large eccentricities. Thus, the feeding zones of the terrestrial planets are determined during their final accretion. -
Mini-Magnetospheres and Moon-Magnetosphere Interactions: Overview Moon-Magnetosphere Interactions
manuscript submitted to Space Physics and Aeronomy: Magnetospheres Mini-magnetospheres and Moon-magnetosphere interactions: Overview Moon-magnetosphere Interactions Joachim Saur 1Institut f¨urGeophysik und Meteorologie, Universit¨atzu K¨oln,Cologne, Germany Key Points: • Review of moon-magnetosphere interaction (MMI) in the solar system • MMI is generally sub-Alfv´enicand generates Alfv´enwings with auroral footprints on planets • Observations of MMI can reveal atmospheres, plumes, ionospheres, subsurface oceans, and dynamos arXiv:1908.06446v1 [astro-ph.EP] 18 Aug 2019 Corresponding author: Joachim Saur, [email protected] {1{ manuscript submitted to Space Physics and Aeronomy: Magnetospheres Abstract "Moon-magnetosphere interaction" stands for the interaction of magnetospheric plasma with an orbiting moon. Observations and modeling of moon-magnetosphere interaction is a highly interesting area of space physics because it helps to better understand the ba- sic physics of plasma flows in the universe and it provides geophysical information about the interior of the moons. Moon-magnetosphere interaction is caused by the flow of mag- netospheric plasma relative to the orbital motions of the moons. The relative velocity is usually slower than the Alfv´envelocity of the plasma around the moons. Thus the in- teraction generally forms Alfv´enwings instead of bow shocks in front of the moons. The local interaction, i.e., the interaction within several moon radii, is controlled by prop- erties of the atmospheres, ionospheres, surfaces, nearby dust-populations, the interiors of the moons as well as the properties of the magnetospheric plasma around the moons. The far-field interaction, i.e., the interaction further away than a few moon radii, is dom- inated by the magnetospheric plasma and the fields, but it still carries information about the properties of the moons. -
Solar System Interiors, Atmospheres, and Surfaces Investigations Via Radio Links: Goals for the Next Decade
White Paper for the Planetary Science and Astrobiology Decadal Survey 2023-2032 The National Academies of Sciences, Engineering, and Medicine Solar System Interiors, Atmospheres, and Surfaces Investigations via Radio Links: Goals for the Next Decade SW Asmar1 ([email protected], 818-354-6288), RA Preston1, P Vergados1, DH Atkinson1, T Andert2, H Ando3, CO Ao1, JW Armstrong1, N Ashby4, J-P Barriot5, PM Beauchamp1, DJ Bell1, PL Bender6, M Di Benedetto7, BG Bills1, MK Bird8, TM Bocanegra-Bahamon1, GK Botteon1, S Bruinsma9, DR Buccino1, KL Cahoy10, P Cappuccio7, RK Choudhary11, V Dehant12, C Dumoulin13, D Durante7, CD Edwards1, HM Elliott1, TA Ely1, AI Ermakov14, F Ferri15, FM Flasar16, RG French17, A Genova7, SJ Goossens16,18, B Häusler2, R Helled19, DP Hinson20, MD Hofstadter1, L Iess7, T Imamura21, AP Jongeling1, Ö Karatekin12, Y Kaspi22, MM Kobayashi1, A Komjathy1, AS Konopliv1, ER Kursinski23, TJW Lazio1, S Le Maistre12, FG Lemoine16, RJ Lillis14, IR Linscott24, AJ Mannucci1, EA Marouf25, J-C Marty9, SE Matousek1, K Matsumoto26, EM Mazarico16, V Notaro7, M Parisi1, RS Park1, M Pätzold8, GG Peytaví2, MP Pugh1, NO Rennó27, P Rosenblatt13, D Serra28, RA Simpson20,24, DE Smith10, PG Steffes29, BD Tapley30, S Tellmann8, P Tortora31, SG Turyshev1, T Van Hoolst12, AK Verma32, MM Watkins1, W Williamson1, MA Wieczorek33, P Withers34, M Yseboodt12, N Yu1, M Zannoni31, MT Zuber10 1: Jet Propulsion Laboratory, California Institute of Technology 18. University of Maryland 2: Universität der Bundeswehr München, Germany 19. Universität Zürich, Switzerland 3. Kyoto Sangyo University, Japan 20. SETI Institute 4. National Institute of Standards & Technology 21. The University of Tokyo, Japan 5.