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Chapter Fourteen Men Into Space: the Space Race and Entertainment Television Margaret A. Weitekamp
CHAPTER FOURTEEN MEN INTO SPACE: THE SPACE RACE AND ENTERTAINMENT TELEVISION MARGARET A. WEITEKAMP The origins of the Cold War space race were not only political and technological, but also cultural.1 On American television, the drama, Men into Space (CBS, 1959-60), illustrated one way that entertainment television shaped the United States’ entry into the Cold War space race in the 1950s. By examining the program’s relationship to previous space operas and spaceflight advocacy, a close reading of the 38 episodes reveals how gender roles, the dangers of spaceflight, and the realities of the Moon as a place were depicted. By doing so, this article seeks to build upon and develop the recent scholarly investigations into cultural aspects of the Cold War. The space age began with the launch of the first artificial satellite, Sputnik, by the Soviet Union on October 4, 1957. But the space race that followed was not a foregone conclusion. When examining the United States, scholars have examined all of the factors that led to the space technology competition that emerged.2 Notably, Howard McCurdy has argued in Space and the American Imagination (1997) that proponents of human spaceflight 1 Notably, Asif A. Siddiqi, The Rocket’s Red Glare: Spaceflight and the Soviet Imagination, 1857-1957, Cambridge Centennial of Flight (Cambridge: Cambridge University Press, 2010) offers the first history of the social and cultural contexts of Soviet science and the military rocket program. Alexander C. T. Geppert, ed., Imagining Outer Space: European Astroculture in the Twentieth Century (New York: Palgrave Macmillan, 2012) resulted from a conference examining the intersections of the social, cultural, and political histories of spaceflight in the Western European context. -
Why NASA Consistently Fails at Congress
W&M ScholarWorks Undergraduate Honors Theses Theses, Dissertations, & Master Projects 6-2013 The Wrong Right Stuff: Why NASA Consistently Fails at Congress Andrew Follett College of William and Mary Follow this and additional works at: https://scholarworks.wm.edu/honorstheses Part of the Political Science Commons Recommended Citation Follett, Andrew, "The Wrong Right Stuff: Why NASA Consistently Fails at Congress" (2013). Undergraduate Honors Theses. Paper 584. https://scholarworks.wm.edu/honorstheses/584 This Honors Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Undergraduate Honors Theses by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. The Wrong Right Stuff: Why NASA Consistently Fails at Congress A thesis submitted in partial fulfillment of the requirement for the degree of Bachelors of Arts in Government from The College of William and Mary by Andrew Follett Accepted for . John Gilmour, Director . Sophia Hart . Rowan Lockwood Williamsburg, VA May 3, 2013 1 Table of Contents: Acknowledgements 3 Part 1: Introduction and Background 4 Pre Soviet Collapse: Early American Failures in Space 13 Pre Soviet Collapse: The Successful Mercury, Gemini, and Apollo Programs 17 Pre Soviet Collapse: The Quasi-Successful Shuttle Program 22 Part 2: The Thin Years, Repeated Failure in NASA in the Post-Soviet Era 27 The Failure of the Space Exploration Initiative 28 The Failed Vision for Space Exploration 30 The Success of Unmanned Space Flight 32 Part 3: Why NASA Fails 37 Part 4: Putting this to the Test 87 Part 5: Changing the Method. -
Jjmonl 1603.Pmd
alactic Observer GJohn J. McCarthy Observatory Volume 9, No. 3 March 2016 GRAIL - On the Trail of the Moon's Missing Mass GRAIL (Gravity Recovery and Interior Laboratory) was a NASA scientific mission in 2011/12 to map the surface of the moon and collect data on gravitational anomalies. The image here is an artist's impres- sion of the twin satellites (Ebb and Flow) orbiting in tandem above a gravitational image of the moon. See inside, page 4 for information on gravitational anomalies (mascons) or visit http://solarsystem. nasa.gov/grail. The John J. McCarthy Observatory Galactic Observer New Milford High School Editorial Committee 388 Danbury Road Managing Editor New Milford, CT 06776 Bill Cloutier Phone/Voice: (860) 210-4117 Production & Design Phone/Fax: (860) 354-1595 www.mccarthyobservatory.org Allan Ostergren Website Development JJMO Staff Marc Polansky It is through their efforts that the McCarthy Observatory Technical Support has established itself as a significant educational and Bob Lambert recreational resource within the western Connecticut Dr. Parker Moreland community. Steve Barone Jim Johnstone Colin Campbell Carly KleinStern Dennis Cartolano Bob Lambert Mike Chiarella Roger Moore Route Jeff Chodak Parker Moreland, PhD Bill Cloutier Allan Ostergren Cecilia Dietrich Marc Polansky Dirk Feather Joe Privitera Randy Fender Monty Robson Randy Finden Don Ross John Gebauer Gene Schilling Elaine Green Katie Shusdock Tina Hartzell Paul Woodell Tom Heydenburg Amy Ziffer In This Issue "OUT THE WINDOW ON YOUR LEFT" ............................... 4 SUNRISE AND SUNSET ...................................................... 13 MARE HUMBOLDTIANIUM AND THE NORTHEAST LIMB ......... 5 JUPITER AND ITS MOONS ................................................. 13 ONE YEAR IN SPACE ....................................................... 6 TRANSIT OF JUPITER'S RED SPOT .................................... -
Constraining the Source Regions of Lunar Meteorites Using Orbital Geochemical Data
Meteoritics & Planetary Science 50, Nr 2, 214–228 (2015) doi: 10.1111/maps.12412 Constraining the source regions of lunar meteorites using orbital geochemical data A. CALZADA-DIAZ1,2*, K. H. JOY3, I. A. CRAWFORD1,2, and T. A. NORDHEIM2,4 1Department of Earth and Planetary Sciences, Birkbeck College, London WC1E 7HX, UK 2Centre for Planetary Sciences UCL/Birkbeck, London WC1E 6BT, UK 3School of Earth, Atmospheric and Environmental Sciences, University of Manchester, Manchester M13 9PL, UK 4Mullard Space Science Laboratory, University College London, Dorking RH5 6NT, UK *Corresponding author. E-mail: [email protected] (Received 30 July 2014; revision accepted 06 November 2014) Abstract–Lunar meteorites provide important new samples of the Moon remote from regions visited by the Apollo and Luna sample return missions. Petrologic and geochemical analysis of these meteorites, combined with orbital remote sensing measurements, have enabled additional discoveries about the composition and age of the lunar surface on a global scale. However, the interpretation of these samples is limited by the fact that we do not know the source region of any individual lunar meteorite. Here, we investigate the link between meteorite and source region on the Moon using the Lunar Prospector gamma ray spectrometer remote sensing data set for the elements Fe, Ti, and Th. The approach has been validated using Apollo and Luna bulk regolith samples, and we have applied it to 48 meteorites excluding paired stones. Our approach is able broadly to differentiate the best compositional matches as potential regions of origin for the various classes of lunar meteorites. Basaltic and intermediate Fe regolith breccia meteorites are found to have the best constrained potential launch sites, with some impact breccias and pristine mare basalts also having reasonably well-defined potential source regions. -
Science Concept 5: Lunar Volcanism Provides a Window Into the Thermal and Compositional Evolution of the Moon
Science Concept 5: Lunar Volcanism Provides a Window into the Thermal and Compositional Evolution of the Moon Science Concept 5: Lunar volcanism provides a window into the thermal and compositional evolution of the Moon Science Goals: a. Determine the origin and variability of lunar basalts. b. Determine the age of the youngest and oldest mare basalts. c. Determine the compositional range and extent of lunar pyroclastic deposits. d. Determine the flux of lunar volcanism and its evolution through space and time. INTRODUCTION Features of Lunar Volcanism The most prominent volcanic features on the lunar surface are the low albedo mare regions, which cover approximately 17% of the lunar surface (Fig. 5.1). Mare regions are generally considered to be made up of flood basalts, which are the product of highly voluminous basaltic volcanism. On the Moon, such flood basalts typically fill topographically-low impact basins up to 2000 m below the global mean elevation (Wilhelms, 1987). The mare regions are asymmetrically distributed on the lunar surface and cover about 33% of the nearside and only ~3% of the far-side (Wilhelms, 1987). Other volcanic surface features include pyroclastic deposits, domes, and rilles. These features occur on a much smaller scale than the mare flood basalts, but are no less important in understanding lunar volcanism and the internal evolution of the Moon. Table 5.1 outlines different types of volcanic features and their interpreted formational processes. TABLE 5.1 Lunar Volcanic Features Volcanic Feature Interpreted Process -
Issue 36, June 2008
June2008 June2008 In This Issue: 7 Supernova Birth Seen in Real Time Alicia Soderberg & Edo Berger 23 Arp299 With LGS AO Damien Gratadour & Jean-René Roy 46 Aspen Instrument Update Joseph Jensen On the Cover: NGC 2770, home to Supernova 2008D (see story starting on page 7 Engaging Our Host of this issue, and image 52 above showing location Communities of supernova). Image Stephen J. O’Meara, Janice Harvey, was obtained with the Gemini Multi-Object & Maria Antonieta García Spectrograph (GMOS) on Gemini North. 2 Gemini Observatory www.gemini.edu GeminiFocus Director’s Message 4 Doug Simons 11 Intermediate-Mass Black Hole in Gemini South at moonset, April 2008 Omega Centauri Eva Noyola Collisions of 15 Planetary Embryos Earthquake Readiness Joseph Rhee 49 Workshop Michael Sheehan 19 Taking the Measure of a Black Hole 58 Polly Roth Andrea Prestwich Staff Profile Peter Michaud 28 To Coldly Go Where No Brown Dwarf 62 Rodrigo Carrasco Has Gone Before Staff Profile Étienne Artigau & Philippe Delorme David Tytell Recent 31 66 Photo Journal Science Highlights North & South Jean-René Roy & R. Scott Fisher Photographs by Gemini Staff: • Étienne Artigau NICI Update • Kirk Pu‘uohau-Pummill 37 Tom Hayward GNIRS Update 39 Joseph Jensen & Scot Kleinman FLAMINGOS-2 Update Managing Editor, Peter Michaud 42 Stephen Eikenberry Science Editor, R. Scott Fisher MCAO System Status Associate Editor, Carolyn Collins Petersen 44 Maxime Boccas & François Rigaut Designer, Kirk Pu‘uohau-Pummill 3 Gemini Observatory www.gemini.edu June2008 by Doug Simons Director, Gemini Observatory Director’s Message Figure 1. any organizations (Gemini Observatory 100 The year-end task included) have extremely dedicated and hard- completion statistics 90 working staff members striving to achieve a across the entire M 80 0-49% Done observatory are worthwhile goal. -
Apollo Over the Moon: a View from Orbit (Nasa Sp-362)
chl APOLLO OVER THE MOON: A VIEW FROM ORBIT (NASA SP-362) Chapter 1 - Introduction Harold Masursky, Farouk El-Baz, Frederick J. Doyle, and Leon J. Kosofsky [For a high resolution picture- click here] Objectives [1] Photography of the lunar surface was considered an important goal of the Apollo program by the National Aeronautics and Space Administration. The important objectives of Apollo photography were (1) to gather data pertaining to the topography and specific landmarks along the approach paths to the early Apollo landing sites; (2) to obtain high-resolution photographs of the landing sites and surrounding areas to plan lunar surface exploration, and to provide a basis for extrapolating the concentrated observations at the landing sites to nearby areas; and (3) to obtain photographs suitable for regional studies of the lunar geologic environment and the processes that act upon it. Through study of the photographs and all other arrays of information gathered by the Apollo and earlier lunar programs, we may develop an understanding of the evolution of the lunar crust. In this introductory chapter we describe how the Apollo photographic systems were selected and used; how the photographic mission plans were formulated and conducted; how part of the great mass of data is being analyzed and published; and, finally, we describe some of the scientific results. Historically most lunar atlases have used photointerpretive techniques to discuss the possible origins of the Moon's crust and its surface features. The ideas presented in this volume also rely on photointerpretation. However, many ideas are substantiated or expanded by information obtained from the huge arrays of supporting data gathered by Earth-based and orbital sensors, from experiments deployed on the lunar surface, and from studies made of the returned samples. -
Astronomy. Louisiana Arts and Science Center, Baton Rouge Report Number Dfsc -66- 1332 -1 Pub Date Edrs Price Hf -$0.50 Hc -$4.40 108P
REPORT RESUMES t! ED 018 385 88 SE 004 443 ASTRONOMY. LOUISIANA ARTS AND SCIENCE CENTER, BATON ROUGE REPORT NUMBER DFSC -66- 1332 -1 PUB DATE EDRS PRICE HF -$0.50 HC -$4.40 108P. DESCRIPTORS- *ASTRONOMY, *ANNOTATED BIBLIOGRAPHIES, *CURRICULUM, *ELEMENTARY SCHOOL SCIENCE, *PHYSICAL SCIENCES, *SECONDARY SCHOOL SCIENCE, AUDIOVISUAL AIDS, BIBLIOGRAPHIES, CURRICULUM DEVELOPMENT, STUDENT PROJECTS, SCIENCE ACTIVITIES, TEACHING GUIDES, TEACHING TECHNIQUES, SCIENCE UNITS, LOUISIANA ARTS AND SCIENCE CENTER, BATON ROUGE, LOUISIANA, WORLD BOOK ENCYCLOPEDIA, THIS TEACHER'S GUIDE FOR A UNIT ON ASTRONOMY ESTABLISHES (1) UNDERSTANDINGS AND. ATTITUDES, (2) SKILLS, AND (3) CONCEPTS TO BE GAINED IN THE STUDY) THE OVERVIEW EXPLAINS THE ORGANIZATION AND OBJECTIVES OF THE UNIT. TOPICAL DIVISIONS ARE (1) THE EARTH,(2) THE NOON,(3) THE SUN,(4) THE SOLAR SYSTEM,(5) THE STARS, (6) THE UNIVERSE, AND(7) SPACE EXPLORATION. A VOCABULARY LIST, BIBLIOGRAPHY, TESTS, CHARTS, AND A LIST OF STUDENT ACTIVITIES COMPRISE THE MATERIAL. MOST OF THE FACTUAL PRESENTATION IS IN QUESTION AND ANSWER FORM. THE ANNOTATED BIBLIOGRAPHY IS CODED TO INDICATE THREE LEVELS OF DIFFICULTY. THE CONCLUDING SECTION LISTS DEMONSTRATIONS, FILMS, AND FILMSTRIPS. (DH) ........_ ) ; ,. , ; ; '4;4' sat, f,e, 1 . 4 , . 'T A :r...; ; t; .,,,. .1 " * :41 .. A . U SDEPARTMENT Of MALIK EDUCATION & WELFARE OFFICE Of EDUCATION THIS DOCUMENT HAS BEEN REPRODUCED EXACTLY AS RECEIVED FROM THE PERSON OR ORGANIZATION ORIGINATING 11 POINTS OF VIEW OR OPINIONS STATED DO NOT NECESSARILY REPRESENT OFFICIAL OFFICE OF EDUCATION POSITION OR POLICY ASTRONOMY LOUISIANA ARTS AND SCIENCE CENTER a Es --.11. ASTRONOMY Objectives for Astronomy Unit iG I A. Understandings and attitudes 1. To understand and appreciate the smallness of the Earth and the vastness of the universe. -
An Examination of Mare Age Based On
An Examination of Mare Age Based On Cratering Density The Chenango Forks Lunar Research Team: Sharon Hartzell, Jackson Haskell, Benjamin Daniels, Sarah Maximowicz, and Sarah Andrus Objective Cooled basaltic lava flows, known as maria, cover approximately sixteen percent of the lunar surface. The determination of absolute and relative ages of maria is an important question in lunar research, because it provides insight into the geologic history of the lunar environment. Many samples returned from the Apollo and Luna missions have been absolutely dated using radiogenic techniques. However, not all samples returned from the moon have been radiogenically dated. Furthermore, returned samples represent only a small portion of each visited mare. One of the major challenges facing lunar researches is the fact that most maria are still unvisited. The lack of complete data from visited maria in combination with the absence of data from unvisited maria has compelled lunar researchers to rely on remote techniques for relative dating. The overriding goal of our research was to develop and utilize a method for analyzing the ages of the twenty‐three lunar maria. Approach •Areas of the twenty‐three lunar maria were analyzed in three distinct investigations. Investigation 1: Total crater count to determine cratering densities, and comparison of densities to absolute age Investigation 2: Analysis of crater weathering in relation to age Investigation 3: Analysis of crater size in relation to age •A relative age map was created to display the distribution of the maria on the moon’s surface. The •Analysis of age dist ributions within individual mari a revealed several interesting trends: Investigation 1 map itself was obtained from Google Moon, and the maria were highlighted based on the scale Method displayed below. -
Applications of Solar Wind Particle Impact Simulations at Lunar Magnetic Anomalies to the Study of Lunar Swirls
47th Lunar and Planetary Science Conference (2016) 2648.pdf APPLICATIONS OF SOLAR WIND PARTICLE IMPACT SIMULATIONS AT LUNAR MAGNETIC ANOMALIES TO THE STUDY OF LUNAR SWIRLS. C. J. Tai Udovicic1, G. Y. Kramer2, and E. M. Harnett3, 1Dept of Earth Sciences, University of Toronto, 22 Russell St, Toronto, ON, Canada, ([email protected]), 2Lunar and Planetary Institute, 3600 Bay Area Bvld, Houston, TX, ([email protected]), 3University of Washington, Earth and Space Sciences, Seattle, WA ([email protected]). Introduction: Lunar swirls are high albedo features highlands often appear to have swirl-like anomalies due that exhibit low spectral maturity. They have been to their complicated topography. To mitigate this, we identified at various sites on the Moon, and all coincide generated a slope map from the WAC GLD100 (SLP), with a lunar magnetic anomaly (magnomaly) [1], which we overlayed with the WAC 643 nm normalized although not all magnomalies have an identifiable swirl. reflectance image to distinguish high albedo swirls from The leading hypothesis for lunar swirl origin is high albedo slopes. Even so, after one pass of the region, presented in [2] as magnetic field standoff of the solar only about half of the swirls could be detected with this wind which causes uneven space weathering at the swirl method alone. The remaining half were found after surface. This hypothesis fails to explain why lunar using particle simulations as a guide. swirls are observed at some but not all of the magnetic Solar wind particle tracking simulations: We anomalies present on the Moon. To investigate the solar used the 2D solar wind particle tracking simulation wind standoff hypothesis further and to improve swirl presented in [2]. -
SEEDS – Direct Imaging Survey for Exoplanets and Disks
SEEDS – Direct Imaging Survey for Exoplanets and Disks K. G. Helminiak 1,2, M. Kuzuhara3,4, T. Kudo3, M. Tamura3,5, T. Usuda1, J. Hashimoto6, T. Matsuo7, M. W. McElwain8, M. Momose9, T. Tsukagoshi9, and the SEEDS/HiCIAO team 1Subaru Telescope, National Astronomical Observatory of Japan, 650 North Aohoku Place, Hilo, HI 96720, USA 2Nicolaus Copernicus Astronomical Center, Department of Astrophysics, ul. Rabia´nska 8, 87-100 Toru´n,Poland 3National Astronomical Observatory Japan (NAOJ), Osawa 2-21-1, Mitaka, Tokyo 181-8588, Japan 4Department of Earth and Planetary Science, Tokyo Institute of Technology, 2-12-1 Ookayama, Meguro-ku, Tokyo 181-8588, Japan 5School of Science, The University of Tokyo, Hongo 7-3-1, Bunkyo, Tokyo 113-0033, Japan 6Department of Physics and Astronomy, The University of Oklahoma, 440 West Brooks Street, Norman, OK 73019, USA 7Department of Astronomy, Kyoto University, Kitashirakawa-Oiwake-cho, Sakyo-ku, Kyoto, Kyoto 606-8502, Japan 8Exoplanets and Stellar Astrophysics Laboratory, Code 667, Goddard Space Flight Center, Greenbelt, MD 20771, USA 9College of Science, Ibaraki University, Bunkyo 2-1-1, Mito 310-8512, Japan Abstract. Exoplanets on wide orbits (r & 10 AU) can be revealed by high-contrast direct imaging, which is efficient for their detailed detections and characterizations compared with indirect techniques. The SEEDS campaign, using the 8.2-m Subaru Telescope, is one of the most extensive campaigns to search for wide-orbit exoplanets via direct imaging. Since 2009 to date, the campaign has surveyed exoplanets around stellar targets selected from the solar neighborhood, moving groups, open clusters, and star- 750 SEEDS–DirectImagingSurveyforExoplanetsandDisks forming regions. -
Nasa Technical Memorandum Tm-88427 Formation Of
https://ntrs.nasa.gov/search.jsp?R=19860016441 2020-03-20T14:24:06+00:00Z NASA TECHNICAL MEMORANDUM TM-88427 FORMATION OF THE CENTRAL UPLIFT IN METEORIC CRATERS Jvanov, B.A.; Bazilevskiy, A.T.; Sazonova, L.V. Translation of "Ob obrazovanii tsentralnogo podnyatiya v meteoritnykh kraterakh," in "Meteoritika, Akademiya nauk SSSR" No. 40, 1982, pp. 67-81 , f(NASA-TM-88427) FORMATION OF THE CENTBAL N86-25913 DfLIFT IN flETIOEIC CEATEBS {Hatioiial Aeronautics and Space administration) 33 p HC A03/MP A01 CSCX 08G Unclas G3/46 43587 NATIONAL AERONAUTICS AND SPACE ADMINISTRATION WASHINGTON, D.C. 20546 MAY, 1986 FORMATION OF THE CENTRAL UPLIFT IN METEORIC CRATERS V.A. Ivanov INTRODUCTION. /671 Central peaks or central uplifts in meteoric craters are a necessary element in the structure of craters in a certain size range, e.g. craters with a diameter of 25-200 km on the Moon and 4-70 (?) km on Earth. Smaller craters have a simple cup shape; larger craters are complex multiringed structures. The transition from simple cup-shaped craters to craters with central uplifts is associated with a decrease in relative crater depth, which brings into question the depth of excavation during formation of craters with complex structure. A change in crater structure indicates a change in the mechanics of crater formation and requires caution when one attempts to extrapolate to natural occurrences the set of data accumulated during study of this process using experimental explosions and hypervelocity impacts under laboratory conditions. The purpose of this article is to discuss and, if possible, evaluate the relationship of various processes which accompany crater formation; to attempt to identify those which can be related to the natural appearance of central uplifts in impact craters on a certain scale.