Ocean Sciences Across the Solar System
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Dustin M. Schroeder
Dustin M. Schroeder Assistant Professor of Geophysics Department of Geophysics, School of Earth, Energy, and Environmental Sciences 397 Panama Mall, Mitchell Building 361, Stanford University, Stanford, CA 94305 [email protected], 440.567.8343 EDUCATION 2014 Jackson School of Geosciences, University of Texas, Austin, TX Doctor of Philosophy (Ph.D.) in Geophysics 2007 Bucknell University, Lewisburg, PA Bachelor of Science in Electrical Engineering (B.S.E.E.), departmental honors, magna cum laude Bachelor of Arts (B.A.) in Physics, magna cum laude, minors in Mathematics and Philosophy PROFESSIONAL EXPERIENCE 2016 – present Assistant Professor of Geophysics, Stanford University 2017 – present Assistant Professor (by courtesy) of Electrical Engineering, Stanford University 2020 – present Center Fellow (by courtesy), Stanford Woods Institute for the Environment 2020 – present Faculty Affiliate, Stanford Institute for Human-Centered Artificial Intelligence 2021 – present Senior Member, Kavli Institute for Particle Astrophysics and Cosmology 2016 – 2020 Faculty Affiliate, Stanford Woods Institute for the Environment 2014 – 2016 Radar Systems Engineer, Jet Propulsion Laboratory, California Institute of Technology 2012 Graduate Researcher, Applied Physics Laboratory, Johns Hopkins University 2008 – 2014 Graduate Researcher, University of Texas Institute for Geophysics 2007 – 2008 Platform Hardware Engineer, Freescale Semiconductor SELECTED AWARDS 2021 Symposium Prize Paper Award, IEEE Geoscience and Remote Sensing Society 2020 Excellence in Teaching Award, Stanford School of Earth, Energy, and Environmental Sciences 2019 Senior Member, Institute of Electrical and Electronics Engineers 2018 CAREER Award, National Science Foundation 2018 LInC Fellow, Woods Institute, Stanford University 2016 Frederick E. Terman Fellow, Stanford University 2015 JPL Team Award, Europa Mission Instrument Proposal 2014 Best Graduate Student Paper, Jackson School of Geosciences 2014 National Science Olympiad Heart of Gold Award for Service to Science Education 2013 Best Ph.D. -
The Hunt for Exomoons with Kepler (Hek)
The Astrophysical Journal, 777:134 (17pp), 2013 November 10 doi:10.1088/0004-637X/777/2/134 C 2013. The American Astronomical Society. All rights reserved. Printed in the U.S.A. THE HUNT FOR EXOMOONS WITH KEPLER (HEK). III. THE FIRST SEARCH FOR AN EXOMOON AROUND A HABITABLE-ZONE PLANET∗ D. M. Kipping1,6, D. Forgan2, J. Hartman3, D. Nesvorny´ 4,G.A.´ Bakos3, A. Schmitt7, and L. Buchhave5 1 Harvard-Smithsonian Center for Astrophysics, Cambridge, MA 02138, USA; [email protected] 2 Scottish Universities Physics Alliance (SUPA), Institute for Astronomy, University of Edinburgh, Blackford Hill, Edinburgh, EH9 3HJ, UK 3 Department of Astrophysical Sciences, Princeton University, Princeton, NJ 05844, USA 4 Department of Space Studies, Southwest Research Institute, Boulder, CO 80302, USA 5 Niels Bohr Institute, Copenhagen University, Denmark Received 2013 June 4; accepted 2013 September 8; published 2013 October 22 ABSTRACT Kepler-22b is the first transiting planet to have been detected in the habitable zone of its host star. At 2.4 R⊕, Kepler-22b is too large to be considered an Earth analog, but should the planet host a moon large enough to maintain an atmosphere, then the Kepler-22 system may yet possess a telluric world. Aside from being within the habitable zone, the target is attractive due to the availability of previously measured precise radial velocities and low intrinsic photometric noise, which has also enabled asteroseismology studies of the star. For these reasons, Kepler-22b was selected as a target-of-opportunity by the “Hunt for Exomoons with Kepler” (HEK) project. In this work, we conduct a photodynamical search for an exomoon around Kepler-22b leveraging the transits, radial velocities, and asteroseismology plus several new tools developed by the HEK project to improve exomoon searches. -
The Evolution of Star Habitable Zones
The Evolution of Star Habitable Zones Jeffrey J. Wolynski November 17, 2018 Rockledge, FL 32922 Abstract: It was discovered that planets are older, evolving stars. This means the Circumstellar Habitable Zone collapses and/or shrinks into the star itself, thus evolves as the star evolves. Explanation is provided. The habitable zone of a star is the area where liquid water exists or can exist. Since stars cool down and become water worlds as they evolve, combining their hydrogen with the leftover oxygen in large amounts, it is easy to see what happens. The star is too hot in the beginning to form water, or sustain it, but it can heat up other much colder stars allowing them to pool water on their surfaces from a distance. As the star cools and evolves, the distance it can do this diminishes considerably and its habitable zone shrinks. Blue giants have the largest habitable zones, but they quickly contract because they are so young and are evolving rapidly to cooler, less massive states. What this means is that the time variable for the habitable zones of these objects is quite small. The activity of more evolved stars around blue giants should be short-lived, but interesting to say the least. White stars have smaller habitable zones but are still very large. Orange dwarfs have even smaller habitable zones, as well show a noticeable thinning of the zone as opposed to earlier stages. Red dwarfs have very small external habitable zones and the smallest external habitable zone belongs to only the smallest brown dwarfs, which still have a small amount of heat to radiate the surface of another more evolved star. -
JUICE Red Book
ESA/SRE(2014)1 September 2014 JUICE JUpiter ICy moons Explorer Exploring the emergence of habitable worlds around gas giants Definition Study Report European Space Agency 1 This page left intentionally blank 2 Mission Description Jupiter Icy Moons Explorer Key science goals The emergence of habitable worlds around gas giants Characterise Ganymede, Europa and Callisto as planetary objects and potential habitats Explore the Jupiter system as an archetype for gas giants Payload Ten instruments Laser Altimeter Radio Science Experiment Ice Penetrating Radar Visible-Infrared Hyperspectral Imaging Spectrometer Ultraviolet Imaging Spectrograph Imaging System Magnetometer Particle Package Submillimetre Wave Instrument Radio and Plasma Wave Instrument Overall mission profile 06/2022 - Launch by Ariane-5 ECA + EVEE Cruise 01/2030 - Jupiter orbit insertion Jupiter tour Transfer to Callisto (11 months) Europa phase: 2 Europa and 3 Callisto flybys (1 month) Jupiter High Latitude Phase: 9 Callisto flybys (9 months) Transfer to Ganymede (11 months) 09/2032 – Ganymede orbit insertion Ganymede tour Elliptical and high altitude circular phases (5 months) Low altitude (500 km) circular orbit (4 months) 06/2033 – End of nominal mission Spacecraft 3-axis stabilised Power: solar panels: ~900 W HGA: ~3 m, body fixed X and Ka bands Downlink ≥ 1.4 Gbit/day High Δv capability (2700 m/s) Radiation tolerance: 50 krad at equipment level Dry mass: ~1800 kg Ground TM stations ESTRAC network Key mission drivers Radiation tolerance and technology Power budget and solar arrays challenges Mass budget Responsibilities ESA: manufacturing, launch, operations of the spacecraft and data archiving PI Teams: science payload provision, operations, and data analysis 3 Foreword The JUICE (JUpiter ICy moon Explorer) mission, selected by ESA in May 2012 to be the first large mission within the Cosmic Vision Program 2015–2025, will provide the most comprehensive exploration to date of the Jovian system in all its complexity, with particular emphasis on Ganymede as a planetary body and potential habitat. -
2018 Workshop on Autonomy for Future NASA Science Missions
NOTE: This document was prepared by a team that participated in the 2018 Workshop on Autonomy for Future NASA Science Missions. It is for informational purposes to inform discussions regarding the use of autonomy in notional science missions and does not specify Agency plans or directives. 2018 Workshop on Autonomy for Future NASA Science Missions: Ocean Worlds Design Reference Mission Reports Table of Contents Introduction .................................................................................................................................... 2 The Ocean Worlds Design Reference Mission Report .................................................................... 3 Ocean Worlds Design Reference Mission Report Summary ........................................................ 20 1 NOTE: This document was prepared by a team that participated in the 2018 Workshop on Autonomy for Future NASA Science Missions. It is for informational purposes to inform discussions regarding the use of autonomy in notional science missions and does not specify Agency plans or directives. Introduction Autonomy is changing our world; commercial enterprises and academic institutions are developing and deploying drones, robots, self-driving vehicles and other autonomous capabilities to great effect here on Earth. Autonomous technologies will also play a critical and enabling role in future NASA science missions, and the Agency requires a specific strategy to leverage these advances and infuse them into its missions. To address this need, NASA sponsored the -
Revolution Changed the Climate
Revolution changed the climate In the first in a series of four articles about climate change and agriculture in New Zealand, Dr Harry Clark of the New Zealand Agricultural Greenhouse Gas Research Centre lifts the lid on the origins and science of climate change, explaining how human activities are dramatically increasing concentrations of greenhouse gases and triggering major environmental changes. ABOUT 250 years ago a revolution began in Europe that would drastically alter the lives and lifestyles of millions, eventually billions, of people worldwide. Clever industrialists discovered that by extracting and burning fossil fuels like coal and oil they could power machines capable of producing goods and food on an unprecedented scale. Soon they discovered the same fuels could drive vehicles of previously unimaginable might, carrying their goods to market faster and in larger quantities than ever before. Fortunes were made. The population exploded. Forests made way for towns, roads and railways and farms to feed the hungry masses. Little did those pioneering industrialists know their revolution would reverberate in a very different way, centuries later. The unconstrained burning of fossil fuels and rapid deforestation that characterise the industrial era have significantly disrupted the cycles of elements like carbon, nitrogen and phosphorus, which are found naturally in the earth and atmosphere. Atmospheric concentrations of some of these elements in their gaseous form – named greenhouse gases or ‘GHGs’ – have increased rapidly, causing the atmosphere to warm up and our climate to change. Average and extreme temperatures around the planet are rising, resulting in reduced snow cover, melting glaciers, extended growing seasons and shifting rainfall patterns. -
Alien Maps of an Ocean-Bearing World
Alien Maps of an Ocean-Bearing World The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Cowan, Nicolas B., Eric Agol, Victoria S. Meadows, Tyler Robinson, Timothy A. Livengood, Drake Deming, Carey M. Lisse, et al. 2009. Alien maps of an ocean-bearing world. Astrophysical Journal 700(2): 915-923. Published Version doi: 10.1088/0004-637X/700/2/915 Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:4341699 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Open Access Policy Articles, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#OAP Accepted for publication in ApJ A Preprint typeset using LTEX style emulateapj v. 10/09/06 ALIEN MAPS OF AN OCEAN-BEARING WORLD Nicolas B. Cowan1, Eric Agol, Victoria S. Meadows2, Tyler Robinson2, Astronomy Department and Astrobiology Program, University of Washington, Box 351580, Seattle, WA 98195 Timothy A. Livengood3, Drake Deming2, NASA Goddard Space Flight Center, Greenbelt, MD 20771 Carey M. Lisse, Johns Hopkins University Applied Physics Laboratory, SD/SRE, MP3-E167, 11100 Johns Hopkins Road, Laurel, MD 20723 Michael F. A’Hearn, Dennis D. Wellnitz, Department of Astronomy, University of Maryland, College Park MD 20742 Sara Seager, Department of Earth, Atmospheric, and Planetary Sciences, Dept of Physics, Massachusetts Institute of Technology, 77 Massachusetts Ave. 54-1626, MA 02139 David Charbonneau, Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138 and the EPOXI Team Accepted for publication in ApJ ABSTRACT When Earth-mass extrasolar planets first become detectable, one challenge will be to determine which of these worlds harbor liquid water, a widely used criterion for habitability. -
The Evolving Universe and the Origin of Life
Pekka Teerikorpi · Mauri Valtonen · Kirsi Lehto · Harry Lehto · Gene Byrd · Arthur Chernin The Evolving Universe and the Origin of Life The Search for Our Cosmic Roots Second Edition The Evolving Universe and the Origin of Life Pekka Teerikorpi • Mauri Valtonen • Kirsi Lehto • Harry Lehto • Gene Byrd • Arthur Chernin The Evolving Universe and the Origin of Life The Search for Our Cosmic Roots Second Edition 123 Pekka Teerikorpi Mauri Valtonen Department of Physics and Astronomy Department of Physics and Astronomy University of Turku University of Turku Turku, Finland Turku, Finland Kirsi Lehto Harry Lehto Department of Biology Department of Physics and Astronomy University of Turku University of Turku Turku, Finland Turku, Finland Gene Byrd Arthur Chernin Department of Physics and Astronomy Sternberg Astronomical Institute The University of Alabama Moscow University Tuscaloosa, AL, USA Moscow, Russia ISBN 978-3-030-17920-5 ISBN 978-3-030-17921-2 (eBook) https://doi.org/10.1007/978-3-030-17921-2 1st edition: © 2009 Springer Science+Business Media, LLC 2nd edition: © Springer Nature Switzerland AG 2019 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. -
Westminsterresearch the Astrobiology Primer V2.0 Domagal-Goldman, S.D., Wright, K.E., Adamala, K., De La Rubia Leigh, A., Bond
WestminsterResearch http://www.westminster.ac.uk/westminsterresearch The Astrobiology Primer v2.0 Domagal-Goldman, S.D., Wright, K.E., Adamala, K., de la Rubia Leigh, A., Bond, J., Dartnell, L., Goldman, A.D., Lynch, K., Naud, M.-E., Paulino-Lima, I.G., Kelsi, S., Walter-Antonio, M., Abrevaya, X.C., Anderson, R., Arney, G., Atri, D., Azúa-Bustos, A., Bowman, J.S., Brazelton, W.J., Brennecka, G.A., Carns, R., Chopra, A., Colangelo-Lillis, J., Crockett, C.J., DeMarines, J., Frank, E.A., Frantz, C., de la Fuente, E., Galante, D., Glass, J., Gleeson, D., Glein, C.R., Goldblatt, C., Horak, R., Horodyskyj, L., Kaçar, B., Kereszturi, A., Knowles, E., Mayeur, P., McGlynn, S., Miguel, Y., Montgomery, M., Neish, C., Noack, L., Rugheimer, S., Stüeken, E.E., Tamez-Hidalgo, P., Walker, S.I. and Wong, T. This is a copy of the final version of an article published in Astrobiology. August 2016, 16(8): 561-653. doi:10.1089/ast.2015.1460. It is available from the publisher at: https://doi.org/10.1089/ast.2015.1460 © Shawn D. Domagal-Goldman and Katherine E. Wright, et al., 2016; Published by Mary Ann Liebert, Inc. This Open Access article is distributed under the terms of the Creative Commons Attribution Noncommercial License (http://creativecommons.org/licenses/by- nc/4.0/) which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited. The WestminsterResearch online digital archive at the University of Westminster aims to make the research output of the University available to a wider audience. -
Monday, November 13, 2017 WHAT DOES IT MEAN to BE HABITABLE? 8:15 A.M. MHRGC Salons ABCD 8:15 A.M. Jang-Condell H. * Welcome C
Monday, November 13, 2017 WHAT DOES IT MEAN TO BE HABITABLE? 8:15 a.m. MHRGC Salons ABCD 8:15 a.m. Jang-Condell H. * Welcome Chair: Stephen Kane 8:30 a.m. Forget F. * Turbet M. Selsis F. Leconte J. Definition and Characterization of the Habitable Zone [#4057] We review the concept of habitable zone (HZ), why it is useful, and how to characterize it. The HZ could be nicknamed the “Hunting Zone” because its primary objective is now to help astronomers plan observations. This has interesting consequences. 9:00 a.m. Rushby A. J. Johnson M. Mills B. J. W. Watson A. J. Claire M. W. Long Term Planetary Habitability and the Carbonate-Silicate Cycle [#4026] We develop a coupled carbonate-silicate and stellar evolution model to investigate the effect of planet size on the operation of the long-term carbon cycle, and determine that larger planets are generally warmer for a given incident flux. 9:20 a.m. Dong C. F. * Huang Z. G. Jin M. Lingam M. Ma Y. J. Toth G. van der Holst B. Airapetian V. Cohen O. Gombosi T. Are “Habitable” Exoplanets Really Habitable? A Perspective from Atmospheric Loss [#4021] We will discuss the impact of exoplanetary space weather on the climate and habitability, which offers fresh insights concerning the habitability of exoplanets, especially those orbiting M-dwarfs, such as Proxima b and the TRAPPIST-1 system. 9:40 a.m. Fisher T. M. * Walker S. I. Desch S. J. Hartnett H. E. Glaser S. Limitations of Primary Productivity on “Aqua Planets:” Implications for Detectability [#4109] While ocean-covered planets have been considered a strong candidate for the search for life, the lack of surface weathering may lead to phosphorus scarcity and low primary productivity, making aqua planet biospheres difficult to detect. -
Exploration of Mars by the European Space Agency 1
Exploration of Mars by the European Space Agency Alejandro Cardesín ESA Science Operations Mars Express, ExoMars 2016 IAC Winter School, November 20161 Credit: MEX/HRSC History of Missions to Mars Mars Exploration nowadays… 2000‐2010 2011 2013/14 2016 2018 2020 future … Mars Express MAVEN (ESA) TGO Future ESA (ESA- Studies… RUSSIA) Odyssey MRO Mars Phobos- Sample Grunt Return? (RUSSIA) MOM Schiaparelli ExoMars 2020 Phoenix (ESA-RUSSIA) Opportunity MSL Curiosity Mars Insight 2020 Spirit The data/information contained herein has been reviewed and approved for release by JPL Export Administration on the basis that this document contains no export‐controlled information. Mars Express 2003-2016 … First European Mission to orbit another Planet! First mission of the “Rosetta family” Up and running since 2003 Credit: MEX/HRSC First European Mission to orbit another Planet First European attempt to land on another Planet Original mission concept Credit: MEX/HRSC December 2003: Mars Express Lander Release and Orbit Insertion Collission trajectory Bye bye Beagle 2! Last picture Lander after release, release taken by VMC camera Insertion 19/12/2003 8:33 trajectory Credit: MEX/HRSC Beagle 2 was found in January 2015 ! Only 6km away from landing site OK Open petals indicate soft landing OK Antenna remained covered Lessons learned: comms at all time! Credit: MEX/HRSC Mars Express: so many missions at once Mars Mission Phobos Mission Relay Mission Credit: MEX/HRSC Mars Express science investigations Martian Moons: Phobos & Deimos: Ionosphere, surface, -
Estimated Attenuation Rates Using GPR and TDR in Volcanic Depos
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE Electromagnetic signal penetration in a planetary soil 10.1002/2016JE005192 simulant: Estimated attenuation rates using GPR Key Points: and TDR in volcanic deposits on Mount Etna • GPR methodologies for evaluating the loss tangent of volcanic sediments S. E. Lauro1 , E. Mattei1 , B. Cosciotti1 , F. Di Paolo1 , S. A. Arcone2, M. Viccaro3,4 , • Characterization of electrical 1 properties of a planetary soil simulant and E. Pettinelli • Comparison between GPR and TDR 1 2 measurements Dipartimento di Matematica e Fisica, Università degli Studi Roma TRE, Rome, Italy, US Army ERDC-CRREL, Hanover, New Hampshire, USA, 3Dipartimento di Scienze Biologiche Geologiche e Ambientali, Università degli Studi di Catania, Catania, Italy, 4Osservatorio Etneo, Istituto Nazionale di Geofisica e Vulcanologia, Catania, Italy Correspondence to: S. E. Lauro, Abstract Ground-penetrating radar (GPR) is a well-established geophysical terrestrial exploration method [email protected] and has recently become one of the most promising for planetary subsurface exploration. Several future landing vehicles like EXOMARS, 2020 NASA ROVER, and Chang’e-4, to mention a few, will host GPR. A GPR Citation: survey has been conducted on volcanic deposits on Mount Etna (Italy), considered a good analogue for Lauro, S. E., E. Mattei, B. Cosciotti, F. Di Paolo, S. A. Arcone, M. Viccaro, and Martian and Lunar volcanic terrains, to test a novel methodology for subsoil dielectric properties estimation. E. Pettinelli (2017), Electromagnetic The stratigraphy of the volcanic deposits was investigated using 500 MHz and 1 GHz antennas in two different signal penetration in a planetary soil configurations: transverse electric and transverse magnetic.