July 2021 SAS Newsletter
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Geobiology of the Late Paleoproterozoic Duck Creek Formation, Western Australia
Precambrian Research 179 (2010) 135–149 Contents lists available at ScienceDirect Precambrian Research journal homepage: www.elsevier.com/locate/precamres Geobiology of the late Paleoproterozoic Duck Creek Formation, Western Australia Jonathan P. Wilson a,b,∗, Woodward W. Fischer b, David T. Johnston a, Andrew H. Knoll c, John P. Grotzinger b, Malcolm R. Walter e, Neal J. McNaughton i, Mel Simon d, John Abelson d, Daniel P. Schrag a, Roger Summons f, Abigail Allwood g, Miriam Andres h, Crystal Gammon b, Jessica Garvin j, Sky Rashby b, Maia Schweizer b, Wesley A. Watters f a Department of Earth and Planetary Sciences, Harvard University, USA b Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA c Department of Organismic and Evolutionary Biology, Harvard University, USA d The Agouron Institute, USA e Australian Centre for Astrobiology, University of New South Wales, Australia f Massachusetts Institute of Technology, USA g Jet Propulsion Laboratory, USA h Chevron Corp., USA i Curtin University of Technology, Australia j University of Washington, USA article info abstract Article history: The ca. 1.8 Ga Duck Creek Formation, Western Australia, preserves 1000 m of carbonates and minor Received 25 August 2009 iron formation that accumulated along a late Paleoproterozoic ocean margin. Two upward-deepening Received in revised form 12 February 2010 stratigraphic packages are preserved, each characterized by peritidal precipitates at the base and iron Accepted 15 February 2010 formation and carbonate turbidites in its upper part. Consistent with recent studies of Neoarchean basins, carbon isotope ratios of Duck Creek carbonates show no evidence for a strong isotopic depth gradient, but carbonate minerals in iron formations can be markedly depleted in 13C. -
+ New Horizons
Media Contacts NASA Headquarters Policy/Program Management Dwayne Brown New Horizons Nuclear Safety (202) 358-1726 [email protected] The Johns Hopkins University Mission Management Applied Physics Laboratory Spacecraft Operations Michael Buckley (240) 228-7536 or (443) 778-7536 [email protected] Southwest Research Institute Principal Investigator Institution Maria Martinez (210) 522-3305 [email protected] NASA Kennedy Space Center Launch Operations George Diller (321) 867-2468 [email protected] Lockheed Martin Space Systems Launch Vehicle Julie Andrews (321) 853-1567 [email protected] International Launch Services Launch Vehicle Fran Slimmer (571) 633-7462 [email protected] NEW HORIZONS Table of Contents Media Services Information ................................................................................................ 2 Quick Facts .............................................................................................................................. 3 Pluto at a Glance ...................................................................................................................... 5 Why Pluto and the Kuiper Belt? The Science of New Horizons ............................... 7 NASA’s New Frontiers Program ........................................................................................14 The Spacecraft ........................................................................................................................15 Science Payload ...............................................................................................................16 -
Jet Propulsion Laboratory, Digital Converters
Jet JUNE Propulsion 2014 Laboratory VOLUME 43 NUMBER 6 JPL 2025 What will JPL be like in 2025? What kind of missions will it be building and flying? How different will the lab be from the JPL of today? Those were the questions on the minds of Executive Council members in early May when they held their annual planning retreat. Over three days they laid out the broad strokes of strategies to make each of the lab’s major program areas robust a decade or more from now. “JPL is currently in good shape, but to remain that way we have to focus on where we are going across the next decade,” JPL Director Charles Elachi said follow- ing the off-site meeting. Among the strategies planned for JPL’s major units, in coming years the Solar System Exploration Director- ate hopes to create missions across a broad spectrum of scales—from flagships to miniature spacecraft. One major focus is to explore the ocean worlds in the outer solar system. The first step for this goal is to continue the development of what is hoped will be the next outer planet mission, Europa Clipper. Thanks to the power of NASA’s new Space Launch System, missions to the outer planets may become more frequent. JPL would also like to execute the first interplanetary mission using a pair of miniature cube- sat spacecraft. The Asteroid Redirect Mission in which JPL has a key role may serve as a model for future Clockwise: 1) Europa Clipper; 2) Mars; 3) Mars Sample Return lander; 4) solar system; 5) Earth satellites; 6) the pulsar planets PSR B1257+12 b, c, and d; 7) spiral closer collaborations with other NASA centers. -
Mars 2020 Mission and NASA’S Mars Exploration Program, Visit: Mars.Nasa.Gov/Mars2020 September 2019 NASA Facts
National Aeronautics and Space Administration Mars 2020 Over the past two decades, missions flown to benefit future robotic and human exploration by NASA’s Mars Exploration Program have of Mars. shown us that Mars was once very different from the cold, dry planet it is today. Evidence Key Objectives discovered by landed and orbital missions point • Explore a geologically diverse landing site to wet conditions billions of years ago. These environments lasted long enough to potentially • Assess ancient habitability support the development of microbial life. • Seek signs of ancient life, particularly in special rocks known to preserve signs of life over time The Mars 2020 rover is designed to better understand the geology of Mars and seek signs of • Gather rock and soil samples that could be ancient life. The mission will collect and store a set returned to Earth by a future NASA mission of rock and soil samples that could be returned to • Demonstrate technology for future robotic and Earth in the future. It will also test new technology human exploration Mission Timeline Key Hardware • Launch in July-August 2020 from Cape The rover will carry seven instruments to conduct Canaveral Air Force Station, Florida unprecedented science and test new technology • Launching on a ULA Atlas 541 procured under on the Red Planet. They are: NASA’s Launch Services Program • Mastcam-Z, an advanced camera system with • Land on Mars on February 18, 2021 at the panoramic and stereoscopic imaging capability site of an ancient river delta in a lake that once with the ability to zoom. The instrument also filled Jezero Crater will determine mineralogy of the Martian surface and assist with rover operations. -
Gao-21-306, Nasa
United States Government Accountability Office Report to Congressional Committees May 2021 NASA Assessments of Major Projects GAO-21-306 May 2021 NASA Assessments of Major Projects Highlights of GAO-21-306, a report to congressional committees Why GAO Did This Study What GAO Found This report provides a snapshot of how The National Aeronautics and Space Administration’s (NASA) portfolio of major well NASA is planning and executing projects in the development stage of the acquisition process continues to its major projects, which are those with experience cost increases and schedule delays. This marks the fifth year in a row costs of over $250 million. NASA plans that cumulative cost and schedule performance deteriorated (see figure). The to invest at least $69 billion in its major cumulative cost growth is currently $9.6 billion, driven by nine projects; however, projects to continue exploring Earth $7.1 billion of this cost growth stems from two projects—the James Webb Space and the solar system. Telescope and the Space Launch System. These two projects account for about Congressional conferees included a half of the cumulative schedule delays. The portfolio also continues to grow, with provision for GAO to prepare status more projects expected to reach development in the next year. reports on selected large-scale NASA programs, projects, and activities. This Cumulative Cost and Schedule Performance for NASA’s Major Projects in Development is GAO’s 13th annual assessment. This report assesses (1) the cost and schedule performance of NASA’s major projects, including the effects of COVID-19; and (2) the development and maturity of technologies and progress in achieving design stability. -
Calwater Field Studies Designed to Quantify the Roles of Atmospheric Rivers and Aerosols in Modulating U.S
CALWATER FIELD STUDIES DESIGNED TO QUANTIFY THE ROLES OF ATMOSPHERIC RIVERS AND AEROSOLS IN MODULATING U.S. WEST COAST PRECIPITATION IN A CHANGING CLIMATE BY F. M. RALPH, K. A. PRATHER, D. CAYAN, J. R. SPAckmAN, P. DEMOTT, M. DETTINGER, C. FAIRALL, R. LEUNG, D. ROSENFELD, S. RUTLEDGE, D. WALISER, A. B. WHITE, J. COrdEIRA, A. MARTIN, J. HELLY, AND J. INTRIERI A group of meteorologists, hydrologists, climate scientists, atmospheric chemists, and oceanographers have created an interdisciplinary research effort to explore the causes of variability of rainfall, flooding and water supply along the U.S. West Coast. alWater is a multiyear program of field cam- air pollution, aerosol chemistry, and climate. The paigns, numerical modeling experiments, and purpose of the CalWater workshop was threefold: 1) to C scientific analysis focused on phenomena that discuss key science gaps and the potential for lever- are key to the water supply and associated extremes aging long-term Hydrometeorology Testbed (HMT) (drought, flood) in the U.S. West Coast region. Table 1 data collection in California (Ralph et al. 2013), 2) to summarizes CalWater’s development timeline. The explore interest in the potential impacts of anthropo- results from CalWater are also relevant in many genic aerosols on California’s water supply, and 3) to other regions around the globe. CalWater began as build on the Suppression of Precipitation (SUPRECIP) a workshop at Scripps Institution of Oceanography experiment from 2005 to 2007 (Rosenfeld et al. 2008b) (SIO) in 2008 that brought -
PIXL Seminar, Nov 2015 Why Micro XRF?
Silicon drift detector response function to hard x-rays (with an introduction on quantitative MicroXRF And the Planetary Instrument for X-ray Lithochemistry) Nicolas Michel-Hart with special thanks to Tim Elam for project guidance Applied Physics Laboratory – University of Washington X-ray Fluorescence and μXRF http://in.niton.com/en/ https://xos.com/technologies/xrf/ https://en.wikipedia.org/wiki/X-ray_fluorescence#/media/File:XRFScan.jpg Elam, PIXL Seminar, Nov 2015 Why Micro XRF? Biosignatures (ooids) hosted in a 2.7 billion-year-old carbonate rock Elam, PIXL Seminar, Nov 2015 Some pixels can be very different Area of element maps Visible light image Recent microbialite from the Death Valley Area Elam, PIXL Seminar, Nov 2015 Mars 2020 Mission • M2020 Science Objectives – Habitability: Characterize the geologic record for astrobiologically relevant environments and geologic diversity – Biosignatures: Search for materials with high biosignature preservation potential – Sample Caching: Obtain a pristine set of geologically diverse samples and cache for future return to Earth – Prepare for Humans: Demonstrate in situ resource utilization technologies and characterize dust size and morphology • Mission life: 1.5 Mars years/1005 Martian days • Flight Instruments delivered by Fall 2018, Launch July 2020, Land February 2021 • Instrument Complement: – Mastcam-Z and Supercam for panoramic/stereo imaging and chemical analysis – MEDA for weather – RIMFAX ground penetrating radar – MOXIE technology experiment to produce Oxygen from CO2 – SHERLOC -
The Detection of Long-Chain Bio-Markers Using Atomic Force Microscopy
applied sciences Article The Detection of Long-Chain Bio-Markers Using Atomic Force Microscopy Mark S. Anderson Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., Pasadena, CA 91109, USA; [email protected]; Tel.: +1-818-354-3278 Received: 15 February 2019; Accepted: 22 March 2019; Published: 27 March 2019 Abstract: The detection of long-chain biomolecules on mineral surfaces is presented using an atomic force microscope (AFM). This is achieved by using the AFM’s ability to manipulate molecules and measure forces at the pico-newton scale. We show that a highly characteristic force-distance signal is produced when the AFM tip is used to detach long-chain molecules from a surface. This AFM force spectroscopy method is demonstrated on bio-films, spores, fossils and mineral surfaces. The method works with AFM imaging and correlated tip enhanced infrared spectroscopy. The use of AFM force spectroscopy to detect this class of long chain bio-markers has applications in paleontology, life detection and planetary science. Keywords: long-chain bio-markers 2; AFM 3; tip enhanced spectroscopy 1. Introduction Scanning probe microscopes are fundamental tools in microscopy and nanotechnology. The most widely utilized of the probe microscopes is the atomic force microscope (AFM) that was first described in 1986 by Binnig, Gerber and Quate [1]. With an AFM, a tip mounted on a micro-fabricated cantilever is scanned over the surface and the interaction between the tip and the substrate is detected by monitoring the deflection of the cantilever [2]. These microscopes are remarkable for their ability to image individual atoms or molecules. -
NASA Announces Mars 2020 Rover Payload to Explore the Red Planet As Never Before - 2020 Mission Plans
mars.jpl.nasa.gov NASA Announces Mars 2020 Rover Payload to Explore the Red Planet as Never Before - 2020 Mission Plans 5 min read• original Payload for NASA's Mars 2020 Rover This diagram shows the science instruments for NASA's Mars 2020 rover mission. Credit: NASA Planning for NASA's 2020 Mars rover envisions a basic structure that capitalizes on the design and engineering work done for the NASA rover Curiosity, which landed on Mars in 2012, but with new science instruments selected through competition for accomplishing different science objectives. Credit: NASA/JPL-Caltech The next rover NASA will send to Mars in 2020 will carry seven carefully-selected instruments to conduct unprecedented science and exploration technology investigations on the Red Planet. NASA announced the selected Mars 2020 rover instruments Thursday at the agency's headquarters in Washington. Managers made the selections out of 58 proposals received in January from researchers and engineers worldwide. Proposals received were twice the usual number submitted for instrument competitions in the recent past. This is an indicator of the extraordinary interest by the science community in the exploration of the Mars. The selected proposals have a total value of approximately $130 million for development of the instruments. The Mars 2020 mission will be based on the design of the highly successful Mars Science Laboratory rover, Curiosity, which landed almost two years ago, and currently is operating on Mars. The new rover will carry more sophisticated, upgraded hardware and new instruments to conduct geological assessments of the rover's landing site, determine the potential habitability of the environment, and directly search for signs of ancient Martian life. -
DAVINCI: Deep Atmosphere Venus Investigation of Noble Gases, Chemistry, and Imaging Lori S
DAVINCI: Deep Atmosphere Venus Investigation of Noble gases, Chemistry, and Imaging Lori S. Glaze, James B. Garvin, Brent Robertson, Natasha M. Johnson, Michael J. Amato, Jessica Thompson, Colby Goodloe, Dave Everett and the DAVINCI Team NASA Goddard Space Flight Center, Code 690 8800 Greenbelt Road Greenbelt, MD 20771 301-614-6466 Lori.S.Glaze@ nasa.gov Abstract—DAVINCI is one of five Discovery-class missions questions as framed by the NRC Planetary Decadal Survey selected by NASA in October 2015 for Phase A studies. and VEXAG, without the need to repeat them in future New Launching in November 2021 and arriving at Venus in June of Frontiers or other Venus missions. 2023, DAVINCI would be the first U.S. entry probe to target Venus’ atmosphere in 45 years. DAVINCI is designed to study The three major DAVINCI science objectives are: the chemical and isotopic composition of a complete cross- section of Venus’ atmosphere at a level of detail that has not • Atmospheric origin and evolution: Understand the been possible on earlier missions and to image the surface at origin of the Venus atmosphere, how it has evolved, optical wavelengths and process-relevant scales. and how and why it is different from the atmospheres of Earth and Mars. TABLE OF CONTENTS • Atmospheric composition and surface interaction: Understand the history of water on Venus and the 1. INTRODUCTION ....................................................... 1 chemical processes at work in the lower atmosphere. 2. MISSION DESIGN ..................................................... 2 • Surface properties: Provide insights into tectonic, 3. PAYLOAD ................................................................. 2 volcanic, and weathering history of a typical tessera 4. SUMMARY ................................................................ 3 (highlands) terrain. -
Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): Status and Relevance for Numerical Weather Prediction, Atmospheric Pollution and Climate Research
GAW Report No. 226 WWRP 2016-1 WCRP Report No. 9/2016 Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): status and relevance for numerical weather prediction, atmospheric pollution and climate research (Geneva, Switzerland, 23-25 February 2015) WEATHER CLIMATE WATER CLIMATE WEATHER WMO-No. 1172 GAW Report No. 226 WWRP 2016-1 WCRP Report No. 9/2016 Coupled Chemistry-Meteorology/ Climate Modelling (CCMM): status and relevance for numerical weather prediction, atmospheric pollution and climate research (Geneva, Switzerland, 23-25 February 2015) WMO-No. 1172 2016 WMO-No. 1172 © World Meteorological Organization, 2016 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chairperson, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 84 03 P.O. Box 2300 Fax: +41 (0) 22 730 80 40 CH-1211 Geneva 2, Switzerland E-mail: [email protected] ISBN 978-92-63-11172-2 NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of itsfrontiers or boundaries. The mention of specific companies or products does not imply that they are endorsed or recommended by WMO in preference to others of a similar nature which are not mentioned or advertised. -
The Supercam Instrument Suite on the NASA Mars 2020 Rover: Body Unit and Combined System Tests
Space Sci Rev (2021) 217:4 https://doi.org/10.1007/s11214-020-00777-5 The SuperCam Instrument Suite on the NASA Mars 2020 Rover: Body Unit and Combined System Tests RogerC.Wiens1 · Sylvestre Maurice2 · Scott H. Robinson1 · Anthony E. Nelson1 · Philippe Cais3 · Pernelle Bernardi4 · Raymond T. Newell1 · Sam Clegg1 · Shiv K. Sharma5 · Steven Storms1 · Jonathan Deming1 · Darrel Beckman1 · Ann M. Ollila1 · Olivier Gasnault2 · Ryan B. Anderson6 · Yves André7 · S. Michael Angel8 · Gorka Arana9 · Elizabeth Auden1 · Pierre Beck10 · Joseph Becker1 · Karim Benzerara11 · Sylvain Bernard11 · Olivier Beyssac11 · Louis Borges1 · Bruno Bousquet12 · Kerry Boyd1 · Michael Caffrey1 · Jeffrey Carlson13 · Kepa Castro9 · Jorden Celis1 · Baptiste Chide2,14 · Kevin Clark13 · Edward Cloutis15 · Elizabeth C. Cordoba13 · Agnes Cousin2 · Magdalena Dale1 · Lauren Deflores13 · Dorothea Delapp1 · Muriel Deleuze7 · Matthew Dirmyer1 · Christophe Donny7 · Gilles Dromart16 · M. George Duran1 · Miles Egan5 · Joan Ervin13 · Cecile Fabre17 · Amaury Fau11 · Woodward Fischer18 · Olivier Forni2 · Thierry Fouchet4 · Reuben Fresquez1 · Jens Frydenvang19 · Denine Gasway1 · Ivair Gontijo13 · John Grotzinger18 · Xavier Jacob20 · Sophie Jacquinod4 · Jeffrey R. Johnson21 · Roberta A. Klisiewicz1 · James Lake1 · Nina Lanza1 · Javier Laserna22 · Jeremie Lasue2 · Stéphane Le Mouélic23 · Carey Legett IV1 · Richard Leveille24 · Eric Lewin10 · Guillermo Lopez-Reyes25 · Ralph Lorenz21 · Eric Lorigny7 · Steven P. Love1 · Briana Lucero1 · Juan Manuel Madariaga9 · Morten Madsen19 · Soren Madsen13