NAC Planetary Protection Subcommittee, December 8-9, 2015
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USF Board of Trustees ( March 7, 2013)
Agenda item: (to be completed by Board staff) USF Board of Trustees ( March 7, 2013) Issue: Proposed Ph.D. in Integrative Biology ________________________________________________________________ Proposed action: New Degree Program Approval ________________________________________________________________ Background information: This application for a new Ph.D is driven by a recent reorganization of the Department of Biology. The reorganization began in 2006 and was completed in 2009. The reorganization of the Department of Biology, in part, reflected the enormity of the biological sciences, and in part, different research perspectives and directions taken by the faculty in each of the respective areas of biology. Part of the reorganization was to replace the original Ph.D. in Biology with two new doctoral degrees that better serve the needs of the State and our current graduate students by enabling greater focus of the research performed to earn the Ph.D. The well-established and highly productive faculty attracts students to the Tampa Campus from all over the United States as well as from foreign countries. The resources to support the two Ph.D. programs have already been established in the Department of Biology and are sufficient to support the two new degree programs. The reorganization created two new departments; the Department of Cell Biology, Microbiology, and Molecular Biology (CMMB) and the Department of Integrative Biology (IB). This proposal addresses the creation of a new Ph.D., in Integrative Biology offered by the Department of Integrative Biology (CIP Code 26.1399). The name of the Department, Integrative Biology, reflects the belief that the study of biological processes and systems can best be accomplished by the incorporation of numerous integrated approaches Strategic Goal(s) Item Supports: The proposed program directly supports the following: Goal 1 and Goal 2 Workgroup Review: ACE March 7, 2013 Supporting Documentation: See Complete Proposal below Prepared by: Dr. -
Mars Reconnaissance Orbiter
Chapter 6 Mars Reconnaissance Orbiter Jim Taylor, Dennis K. Lee, and Shervin Shambayati 6.1 Mission Overview The Mars Reconnaissance Orbiter (MRO) [1, 2] has a suite of instruments making observations at Mars, and it provides data-relay services for Mars landers and rovers. MRO was launched on August 12, 2005. The orbiter successfully went into orbit around Mars on March 10, 2006 and began reducing its orbit altitude and circularizing the orbit in preparation for the science mission. The orbit changing was accomplished through a process called aerobraking, in preparation for the “science mission” starting in November 2006, followed by the “relay mission” starting in November 2008. MRO participated in the Mars Science Laboratory touchdown and surface mission that began in August 2012 (Chapter 7). MRO communications has operated in three different frequency bands: 1) Most telecom in both directions has been with the Deep Space Network (DSN) at X-band (~8 GHz), and this band will continue to provide operational commanding, telemetry transmission, and radiometric tracking. 2) During cruise, the functional characteristics of a separate Ka-band (~32 GHz) downlink system were verified in preparation for an operational demonstration during orbit operations. After a Ka-band hardware anomaly in cruise, the project has elected not to initiate the originally planned operational demonstration (with yet-to-be used redundant Ka-band hardware). 201 202 Chapter 6 3) A new-generation ultra-high frequency (UHF) (~400 MHz) system was verified with the Mars Exploration Rovers in preparation for the successful relay communications with the Phoenix lander in 2008 and the later Mars Science Laboratory relay operations. -
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. -
General Vertical Files Anderson Reading Room Center for Southwest Research Zimmerman Library
“A” – biographical Abiquiu, NM GUIDE TO THE GENERAL VERTICAL FILES ANDERSON READING ROOM CENTER FOR SOUTHWEST RESEARCH ZIMMERMAN LIBRARY (See UNM Archives Vertical Files http://rmoa.unm.edu/docviewer.php?docId=nmuunmverticalfiles.xml) FOLDER HEADINGS “A” – biographical Alpha folders contain clippings about various misc. individuals, artists, writers, etc, whose names begin with “A.” Alpha folders exist for most letters of the alphabet. Abbey, Edward – author Abeita, Jim – artist – Navajo Abell, Bertha M. – first Anglo born near Albuquerque Abeyta / Abeita – biographical information of people with this surname Abeyta, Tony – painter - Navajo Abiquiu, NM – General – Catholic – Christ in the Desert Monastery – Dam and Reservoir Abo Pass - history. See also Salinas National Monument Abousleman – biographical information of people with this surname Afghanistan War – NM – See also Iraq War Abousleman – biographical information of people with this surname Abrams, Jonathan – art collector Abreu, Margaret Silva – author: Hispanic, folklore, foods Abruzzo, Ben – balloonist. See also Ballooning, Albuquerque Balloon Fiesta Acequias – ditches (canoas, ground wáter, surface wáter, puming, water rights (See also Land Grants; Rio Grande Valley; Water; and Santa Fe - Acequia Madre) Acequias – Albuquerque, map 2005-2006 – ditch system in city Acequias – Colorado (San Luis) Ackerman, Mae N. – Masonic leader Acoma Pueblo - Sky City. See also Indian gaming. See also Pueblos – General; and Onate, Juan de Acuff, Mark – newspaper editor – NM Independent and -
Mars, the Nearest Habitable World – a Comprehensive Program for Future Mars Exploration
Mars, the Nearest Habitable World – A Comprehensive Program for Future Mars Exploration Report by the NASA Mars Architecture Strategy Working Group (MASWG) November 2020 Front Cover: Artist Concepts Top (Artist concepts, left to right): Early Mars1; Molecules in Space2; Astronaut and Rover on Mars1; Exo-Planet System1. Bottom: Pillinger Point, Endeavour Crater, as imaged by the Opportunity rover1. Credits: 1NASA; 2Discovery Magazine Citation: Mars Architecture Strategy Working Group (MASWG), Jakosky, B. M., et al. (2020). Mars, the Nearest Habitable World—A Comprehensive Program for Future Mars Exploration. MASWG Members • Bruce Jakosky, University of Colorado (chair) • Richard Zurek, Mars Program Office, JPL (co-chair) • Shane Byrne, University of Arizona • Wendy Calvin, University of Nevada, Reno • Shannon Curry, University of California, Berkeley • Bethany Ehlmann, California Institute of Technology • Jennifer Eigenbrode, NASA/Goddard Space Flight Center • Tori Hoehler, NASA/Ames Research Center • Briony Horgan, Purdue University • Scott Hubbard, Stanford University • Tom McCollom, University of Colorado • John Mustard, Brown University • Nathaniel Putzig, Planetary Science Institute • Michelle Rucker, NASA/JSC • Michael Wolff, Space Science Institute • Robin Wordsworth, Harvard University Ex Officio • Michael Meyer, NASA Headquarters ii Mars, the Nearest Habitable World October 2020 MASWG Table of Contents Mars, the Nearest Habitable World – A Comprehensive Program for Future Mars Exploration Table of Contents EXECUTIVE SUMMARY .......................................................................................................................... -
Martian Crater Morphology
ANALYSIS OF THE DEPTH-DIAMETER RELATIONSHIP OF MARTIAN CRATERS A Capstone Experience Thesis Presented by Jared Howenstine Completion Date: May 2006 Approved By: Professor M. Darby Dyar, Astronomy Professor Christopher Condit, Geology Professor Judith Young, Astronomy Abstract Title: Analysis of the Depth-Diameter Relationship of Martian Craters Author: Jared Howenstine, Astronomy Approved By: Judith Young, Astronomy Approved By: M. Darby Dyar, Astronomy Approved By: Christopher Condit, Geology CE Type: Departmental Honors Project Using a gridded version of maritan topography with the computer program Gridview, this project studied the depth-diameter relationship of martian impact craters. The work encompasses 361 profiles of impacts with diameters larger than 15 kilometers and is a continuation of work that was started at the Lunar and Planetary Institute in Houston, Texas under the guidance of Dr. Walter S. Keifer. Using the most ‘pristine,’ or deepest craters in the data a depth-diameter relationship was determined: d = 0.610D 0.327 , where d is the depth of the crater and D is the diameter of the crater, both in kilometers. This relationship can then be used to estimate the theoretical depth of any impact radius, and therefore can be used to estimate the pristine shape of the crater. With a depth-diameter ratio for a particular crater, the measured depth can then be compared to this theoretical value and an estimate of the amount of material within the crater, or fill, can then be calculated. The data includes 140 named impact craters, 3 basins, and 218 other impacts. The named data encompasses all named impact structures of greater than 100 kilometers in diameter. -
Session 2 Classifying Living Things
Session 2 Classifying Living Things Our Earth hosts an astonishing diversity of life forms. We can find plants, animals, and other types of organisms in almost every habitat that we encounter. In Session 1, characteristics shared by all life forms were introduced as features that unify the living world. Session 2 focuses on how life’s diversity arises from variation on these same unifying features. A closer look at cells, in particular, introduces fundamental differences among life forms that have become one basis for biological classification. The Video How do we answer the question: What is it? Just what makes a plant a plant, or an animal an animal? Sally Goetz Shuler, representing Science and Technology for Children (STC), highlights questions like these as she introduces us to activities in the Organisms unit. The children in the Science Studio give us insight into how second and third graders define plants and animals, as well as their awareness of other life forms. Stephanie Selznick’s first graders in Dorchester, Massachusetts use Venn diagrams to determine how plants and animals are alike and different. Their early ideas are based on observations of class terrariums and aquariums, where they’ve observed these life forms over time. Dr. Paul Williams returns to share what’s going on in Bottle Biology—an ongoing Web site-based activity designed to apply session topics and to serve as a K–6 resource as well. We hear from Dr. Colleen Cavanaugh as she takes us to the deepest parts of the ocean to introduce us to her favorite group of living things—life forms that aren’t classified as plants or animals. -
Evolutionary Argument Against Naturalism?” International Journal for Philosophy of Religion 69.3 (2010): 193–204
1 On Plantinga on Belief in Naturalism1 Troy Cross Introduction Naturalism, according to Alvin Plantinga, is the thesis “that there is no such person as God or anything at all like God” (2011b, 435; see also, 2002a, 1; 2011a, vix), and one could be forgiven for thinking that what Plantinga calls his “Evolutionary Argument Against Naturalism”, or “EAAN”, which he has refined and defended for over two decades, is an argument against that thesis (1991, 1993, 2002a, 2002b, 2011a, 2011b). But that would be a mistake. The conclusion of the EAAN is not about the truth of naturalism but about the rationality of believing naturalism to be true: it is that one cannot rationally and reflectively believe that contemporary evolutionary theory is correct about our origins while also believing that neither God nor anything like God exists.2 The difference between truth and rational belief is important here. Consider Moore’s paradoxical sentence: “I don’t believe it’s raining but as a matter of fact it is” (Moore, 209). Nothing prevents that sentence, or others like it, from being true. If you 1 For instructive conversations on this topic I am indebted to John Bang, George Bealer, Mark Bedau, Eliyah Cohen, Bryan Cross, Augie Faller, Emma Handte, Elad Gilo, Nick Gigliotti, John Hare, Jordan Horowitz, Paul Hovda, Alexander Pruss, Margaret Scharle, Derek Schiller, Mackenzie Sullivan, and Carol Voeller. I also wish to thank audiences at Reed College and the University of Nebraska Omaha where I presented early versions of some of this material. Anthony Nguyen gave me many helpful comments on a draft. -
VERITAS – a Discovery-Class Venus Surface Geology and Geophysics Mission Anthony Freeman, Suzanne E
VERITAS – a Discovery-class Venus surface geology and geophysics mission Anthony Freeman, Suzanne E. Joern Helbert Erwan Mazarico Smrekar, Scott Hensley, Mark German Aerospace Center (DLR) NASA Goddard Space Flight Center Wallace, Christophe Sotin, Murray Institutefor Planetary Research Planetary Geodynamics Lab Darrach, Peter Xaypraseuth Rutherfordstrasse 2, 8800 Greenbelt Rd. Jet Propulsion Laboratory, 12489 Berlin, Germany Greenbelt, MD 20771 California Institute of Technology +49-30-67055-319, 301 614-6504, 4800 Oak Grove Dr. [email protected] [email protected] Pasadena, CA 91109 818-354-1887 [email protected] Abstract— Our understanding of solar system evolution is spacecraft adapted for the environment at Venus, and to follow limited by a great unanswered question: How Earthlike is the old adage – keep it simple. The mission has only two Venus? We know that these “twin” planets formed with instruments, and VISAR for example has only one mode of similar bulk composition and size. Yet the evolutionary path operation. The VEM instrument is a simple pushbroom imager Venus followed has diverged from Earth’s, in losing its surface with no moving parts. Gravity science is carried out using the water and becoming hotter than Mercury. What led to this? spacecraft’s fixed-antenna telecom system. No new The answer has profound implications for how terrestrial technologies are used. Onboard processing of the radar data planets become habitable and the potential for life in the using a COTS space-qualified processor reduces data volume universe. to levels commensurate with downlink rates for other NASA planetary orbiters, so no heroics are required to get the data Prior Venus missions discovered that its surface (like Earth’s) back. -
Lockheed Martin to Help NASA Uncover Mysteries of Venus with VERITAS and DAVINCI+ Spacecraft
Lockheed Martin to Help NASA Uncover Mysteries of Venus with VERITAS and DAVINCI+ Spacecraft June 2, 2021 Lockheed Martin has a major role in NASA's long-anticipated return to Venus DENVER, June 2, 2021 /PRNewswire/ -- To learn more about how terrestrial planets evolve over time, NASA selected the VERITAS and DAVINCI+ missions for its Discovery Program, both bound for Venus. Lockheed Martin will design, build and operate both spacecraft. The missions will launch in 2026 and 2030 respectively, and will combine to study Venus' dense atmosphere, topography and geologic processes in great depth. Both missions will aim to discover how Venus – which may have been the first potentially habitable planet in our solar system – became inhospitable to life. They represent NASA's return to Earth's sister planet after more than three decades. "We're very grateful for this opportunity to work with NASA and the missions' principal investigators to fully understand how rocky planets evolved and what it means for our planet, Earth," said Lisa Callahan, vice president and general manager of Lockheed Martin's Commercial Civil Space business. "Our team who designed these two spacecraft to study Venus in unprecedented detail – and yield answers to its greatest mysteries – is beyond excited!" The operations and science for DAVINCI+ – which stands for Deep Atmosphere Venus Investigation of Noble Gases, Chemistry and Imaging Plus – will be managed by NASA's Goddard Space Flight Center in Greenbelt, Maryland. VERITAS – which stands for Venus Emissivity, Radio Science, InSAR, Topography & Spectroscopy – will have its science and operations managed by NASA's Jet Propulsion Laboratory in Southern California. -
MDRS Final Summary Report – Crew 78 Vincent Beaudry, Kathryn Denning, Judah Epstein, Dirk Geeroms, Balwant Rai, Grier Wilt
MDRS final summary report – Crew 78 Vincent Beaudry, Kathryn Denning, Judah Epstein, Dirk Geeroms, Balwant Rai, Grier Wilt Introduction If interplanetary colonization is to be possible, humanity needs to learn as much as possible about how to rise to the challenges involved. One way to achieve this is, of course, through simulations. Our crew, the 78th in the Mars Desert Research Station simulation, was intensively international, composed of 2 Canadians (Kathryn Denning, Vincent Beaudry), 2 Americans (Judah Epstein, Grier Wilt), one Belgian (Dirk Geeroms) and one Indian (Balwant Rai). None of us had met before, and joining together to overcome language barriers and explore cultural differences provided us with an intense intercultural experience, surely akin to those which will be a part of future space exploration. As a group, we: developed our own knowledge of the challenges of space exploration; contributed to some ongoing MDRS research into extremophiles, environmental impact, and plant growth; furthered our individual projects in human physiology, long-distance teaching, and anthropology; acted as subjects for outside human factors researchers; and worked together to make life at the Hab go smoothly, including making some improvements to the Hab and to the EVA equipment. The Group Our crew was comprised of 6 individuals, with the following specialties: Vincent Beaudry was the commander, Judah Epstein the engineer and executive officer, Balwant Rai the scientist and health and security officer, Grier Wilt our biologist, Dirk Geeroms the teacher and astronomer, and Kathryn Denning our anthropologist and journalist. Although we all had our respective roles within this two weeks journey, we all enjoyed very much taking part in each others experiences and in the everyday tasks. -
Ancient Geodynamics and Global-Scale Hydrology on Mars
R EPORTS 15. ccs represents the CO2 concentration at the chloro- component and calculate eq from a weighting of plast surface, which is the limit of CA activity and is 75:25 C4 grasses:trees to allow for the presence of thus assumed to represent the site of CO2-H2Oin trees in savanna-type habitats. Group 9 (C3 grassland leaves. ccs is typically a midway value between those and agriculture) we assume comprises 25:50:25 for in the liquid-air interfaces and the sites of CO2 trees:C3 grasses:C4 grasses; the C3 and C4 grasses assimilation inside leaves (14). include some C3 herbs and C4 grass species as crops. 16. Supplementary data are available on Science Online 31. G. Hoffmann et al., in preparation. at www.sciencemag.org/cgi/content/full/291/5513/ 32. J. R. Ehleringer, T. E. Cerling, B. R. Helliker, Oecologia 2584/DC1. 112, 285 (1997). 17. M. D. Hatch, J. N. Burnell, Plant Physiol. 93, 825 33. G. J. Collatz, J. A. Berry, J. S. Clark, Oecologia 114, 441 (1990). (1998). 18. E. Utsoniyama, S. Muto, Physiol. Plant. 88, 413 34. J. Lloyd, G. D. Farquhar, Oecologia 99, 201 (1994). (1993). 35. M. Trolier, J. W. C. White, J. R. Lawrence, W. S. 19. A. Makino et al., Plant Physiol. 100, 1737 (1992) Broecker, J. Geophys. Res. 101, 25897 (1996). 20. G. A. Mills, H. C. Urey, J. Am. Chem. Soc. 62, 1019 36. R. A. Houghton, Tellus 51B, 298 (1999). (1940). 37. R. H. Waring, W. H. Schlesinger, Forest Ecosystems 21. J. S.