2020-03-16T18:52:36+00:00Z I I
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
I B R EL ORNIA
i • a _' a SPACE SCIENCES LABORATORY I # # i UNIVERSITY CALIFORNIA i B_R_EL ORNIA : NRT- o62_o r , - o / - . -.- L (NASA. CR OR TMX OR Ai2 NUMBER) |CATRGORY) 4 3 ,.. -. , , "I Space Science_ Lal_oratory W University of California Berkeley, California 94720 0 RADIATION ANOMALIES ON THE LUNAR SURFACE by David Buhl A Technical Report on NASA Grants NsG 101-61 and NsG Z43-6Z Series No. 8, Issue No. 1 Submitted in partial satisfaction of the requirements for the degree of DOCTOR OF PHILOSOPHY Department of Electrical Engineering University of California, Berkeley t January20, 1967 0 8 * 4 r B CONTENTS ABSTRACT ............................. vii ACKNOWLEDGMENTS ....................... _x I • INTRODUCTION ........................... I II. PROPOSAL -- A Study of the Eff;cts of Luna: Cratering on Infrared Observations ............... III. THEORETICAL ANAL _SiS .......... .......... I_ I. Model of a Cra_ered Lunar Surface .............. i8 i. 1 Description nf a model lunar c"ater ............ l_ 1.2 Asstlmp ions made concerning the surface of a crater . ZI i. 3 Consideration of radiation and re radiation in lunar crater 24 1.4 Density nf lunar craters .................. 27 0 Z. Mathematic Aralysis of the Temperature Eistribution ..... _8 2.1 The integral equation for a sl)eric_l crater ........ _8 2.2 Equations describing the temperat;are history of a crater 35 3. Daytime Study of the Moon .................... 42 3.1 The experiments of Pettit and Nicholson ......... 42 3.2 The temperature distribution in an illuminated crater . 44 3.3 The shadow region of a crater ............. 46 3.4 The angular distribution of radiation from a crater . 4q 3.5 _adiation patterns of several craters .......... -
Enceladus's Measured Physical Libration Requires a Global Subsurface Ocean
Enceladus’s measured physical libration requires a global subsurface ocean P. C. Thomas1*, R. Tajeddine1, M. S. Tiscareno1,2, J. A. Burns1,3, J. Joseph1, T. J. Loredo1 , P. Helfenstein1, C. Porco4, 1Cornell Center for Astrophysics and Planetary Science, Cornell University, Ithaca, NY 14853 USA 2Carl Sagan Center for the Study of Life in the Universe, SETI Institute, 189 Bernardo Avenue, Mountain View, CA 94043 3College of Engineering, Cornell University, Ithaca, NY 14853 USA 4Space Science Institute, Boulder, CO 80304, USA *Corresponding author E-mail:[email protected] Several planetary satellites apparently have subsurface seas that are of great interest for, among other reasons, their possible habitability. The geologically diverse Saturnian satellite Enceladus vigorously vents liquid water and vapor from fractures within a south polar depression and thus must have a liquid reservoir or active melting. However, the extent and location of any subsurface liquid region is not directly observable. We use measurements of control points across the surface of Enceladus accumulated over seven years of spacecraft observations to determine the satellite’s precise rotation state, finding a forced physical libration of 0.120 ± 0.014° (2σ). This value is too large to be consistent with Enceladus’s core being rigidly connected to its surface, and thus implies the presence of a global ocean rather than a localized polar sea. The maintenance of a global ocean within Enceladus is problematic according to many thermal models and so may constrain satellite properties or require a surprisingly dissipative Saturn. 1. Introduction Enceladus is a 500-km-diameter satellite of mean density 1609 ± 5 kg-m-3 orbiting Saturn every 1.4 days in a slightly eccentric (e = 0.0047) orbit (Porco et al., 2006). -
Observing the Lunar Libration Zones
Observing the Lunar Libration Zones Alexander Vandenbohede 2005 Many Look, Few Observe (Harold Hill, 1991) Table of Contents Introduction 1 1 Libration and libration zones 3 2 Mare Orientale 14 3 South Pole 18 4 Mare Australe 23 5 Mare Marginis and Mare Smithii 26 6 Mare Humboldtianum 29 7 North Pole 33 8 Oceanus Procellarum 37 Appendix I: Observational Circumstances and Equipment 43 Appendix II: Time Stratigraphical Table of the Moon and the Lunar Geological Map 44 Appendix III: Bibliography 46 Introduction – Why Observe the Libration Zones? You might think that, because the Moon always keeps the same hemisphere turned towards the Earth as a consequence of its captured rotation, we always see the same 50% of the lunar surface. Well, this is not true. Because of the complicated motion of the Moon (see chapter 1) we can see a little bit around the east and west limb and over the north and south poles. The result is that we can observe 59% of the lunar surface. This extra 9% of lunar soil is called the libration zones because the motion, a gentle wobbling of the Moon in the Earth’s sky responsible for this, is called libration. In spite of the remainder of the lunar Earth-faced side, observing and even the basic task of identifying formations in the libration zones is not easy. The formations are foreshortened and seen highly edge-on. Obviously, you will need to know when libration favours which part of the lunar limb and how much you can look around the Moon’s limb. -
Physics of the Moon
NASA TECHNICAL NOTE -cNASA TN D-2944 e. / PHYSICS OF THE MOON SELECTED TOPICS CONCERNING LUNAR EXPLORATION Edited by George C. ‘Bucker and Henry E. Siern George C. Marsball Space Flight Center Hzmtsville, A Za: NATIONAL AERONAUTICSAND SPACEADMINISTRATION - WASHINGTON;D. C. TECH LIBRARY KAFB. NM llL5475b NASA TN D-2944 PHYSICS OF THE MOON SELECTED TOPICS CONCERNING LUNAR EXPLORATION Edited by George C. Bucher and Henry E. Stern George C. Marshall Space Flight Center Huntsville, Ala. NATIONAL AERONAUTICS AND SPACE ADMINISTRATION For sole by the Clearinghouse for Federal Scientific and Technical information Springfield, Virginia 22151 - Price 56.00 I - TABLE OF CONTENTS Page SUMMA=. 1 INTRODUCTION. i SECTION I. CHARACTERISTICS OF THE MOON. i . 3 Chapter 1. The Moon’s .History, by Ernst Stuhlinger. 5 Chapter 2. Physical Characteristics of the Lunar Surface, by John Bensko . 39 Chapter 3. The’ Lunar Atmosphere, by Spencer G. Frary . , 55 Chapter 4. Energetic Radiation Environment of the Moon, by Martin 0. Burrell . 65 Chapter 5. The Lunar Thermal Environment , . 9i The Thermal Model of the Moon, by Gerhard B. Heller . 91 p Thermal Properties of the Moon as a Conductor of Heat,byBillyP. Jones.. 121 Infrared Methods of Measuring the Moon’s Temperature, by Charles D. Cochran. 135 SECTION II. EXPLORATION OF THE MOON . .I59 Chapter I. A Lunar Scientific Mission, by Daniel Payne Hale. 161 Chapter 2. Some Suggested Landing Sites for Exploration of the Moon, by Daniel Payne Hale. 177 Chapter 3. Environmental Control for Early Lunar Missions, by ‘Herman P. Gierow and James A. Downey, III . , . .2i I Chapter 4. -
Geophysical Abstracts 186 July-September 1961
Geophysical Abstracts 186 July-September 1961 By JAMES W. CLARKE, DOROTHY B. VITALIANO, VIRGINIA S. NEUSCHEL, and others GEOLOGICAL SURVEY BULLETIN 1146-C Abstracts of current literature pertaining to the physics of the solid earth and to geophysical exploration UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1961 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printtna Office, Washintlton 25, D.C. Price 40 cents (sintUe copy). Subacription price: $1.75 a year; 50 cents additional for foreilln mattin!l. Use of funds for printing this publication has been approved by the Director of the Bureau of the Budget (June 23, 1960). CONTENTS Page Introduction --------------------------------------------------- 351 Extent of coverage ------------------------------------------ 351 List of journals--------------------------------------------- 351 Form of citation-------------------------------------------- 353 Abstracters ------------------------------------------------ 353 Age determinations -------------------------------------------- 353 Cosmogony---------------------------------------------------- 366 Earth currents ------------------------------------------------ 385 Earthquakes and earthquake waves------------------------------- 387 Earth tides and related phenomena------------------------------- 413 Elasticity ----------------------------------------------------- 416 Electrical exploration------------------------------------------ -
Lunar Differential Flux Scans at 22 Microns
RICE UNIVERSITY LUNAR DIFFERENTIAL FLUX SCANS AT 22 MICRONS by Wendell W. Mendell A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE Thesis Director's Signature: l Bouston, Texas /august, 1971 LUNAR DIFFERENTIAL FLUX SCANS AT 22 MICRONS by Wendell W. Mendell ABSTRACT The nighttime lunar surface has been scanned at a variety of phases both before and after new Moon. A differential chopping technique was used which records the flux difference between adjacent resolution elements along a scan. In principle the differential scan can be integrated to provide the flux distribution, but slow drifts in the sensor null level frustrated this procedure. However, some cold limb temperatures have been calculated using the planet Jupiter for calibration. The measurements were made with a resolution element of 27 arc seconds on the 28-inch telescope at the University of Arizona. Scan positions were determined by noting features on the illuminated portion of the Moon through a bore-sighted guide telescope. Positional accuracies are within two reso¬ lution elements. The technique is particularly sensitive to the detection of nighttime anomalies, and more than 150 of these have been identified. Prior to new Moon is seen large scale thermal structure, corresponding to a previously unknown nonlinear cooling property of the lunar highlands. The nonlinear behavior consistently disappears 3.5 to 4 days after sunset. The effect could be due to the large scale roughness of the highlands or to a significant rock population with a mean size on the order of 10 cm. TABLE OF CONTENTS Page I. -
L-G-0000007469-0035722768.Pdf
Lunar Orbiter Photographic Atlas of the Near Side of the Moon Charles J. Byrne Lunar Orbiter Photographic Atlas of the Near Side of the Moon Charles J. Byrne Image Again Middletown, NJ USA Cover illustration: Earth-based photograph of the full Moon from the “Consolidated Lunar Atlas” on the Website of the Lunar and Planetary Institute. British Library Cataloging-in-Publication Data Byrne, Charles J., 1935– Lunar Orbiter photographic atlas of the near side of the Moon 1. Lunar Orbiter (Artificial satellite) 2. Moon–Maps 3. Moon–Photographs from space I. Title 523.3 0223 ISBN 1852338865 Library of Congress Cataloging-in-Publication Data Byrne, Charles J., 1935– Lunar Orbiter photographic atlas of the near side of the Moon : with 619 figures / Charles J. Byrne. p. cm. Includes bibliographical references and index. ISBN 1-85233-886-5 (acid-free paper) 1. Moon–Maps. 2. Moon–Photographs from space. 3. Moon–Remote-sensing images. 4. Lunar Orbiter (Artificial satellite) I. Title. G1000.3.B9 2005 523.3 022 3–dc22 2004045006 Additional material to this book can be downloaded from http://extras.springer.com. ISBN 1-85233-886-5 Printed on acid-free paper. © 2005 Springer-Verlag London Limited Apart from any fair dealing for the purposes of research or private study, or criticism, or review, as permitted under the Copyright, Designs and Patents Act 1988, this publication may only be repro- duced, stored or transmitted, in any form or by any means, with the prior permission in writing of the publishers, or in the case of reprographic reproduction in accordance with the terms of licenses issued by the Copyright Licensing Agency. -
Results for Anomalous Polar Craters from the LRO Mini-RF Imaging Radar P
JOURNAL OF GEOPHYSICAL RESEARCH: PLANETS, VOL. 118, 1–14, doi:10.1002/jgre.20156, 2013 Evidence for water ice on the moon: Results for anomalous polar craters from the LRO Mini-RF imaging radar P. D. Spudis,1 D. B. J. Bussey,2 S. M. Baloga,3 J. T. S. Cahill,2 L. S. Glaze,4 G. W. Patterson,2 R. K. Raney,2 T. W. Thompson,5 B. J. Thomson,6 and E. A. Ustinov 5 Received 6 December 2012; revised 28 August 2013; accepted 9 September 2013. [1] The Mini-RF radar instrument on the Lunar Reconnaissance Orbiter spacecraft mapped both lunar poles in two different RF wavelengths (complete mapping at 12.6 cm S-band and partial mapping at 4.2 cm X-band) in two look directions, removing much of the ambiguity of previous Earth- and spacecraft-based radar mapping of the Moon’s polar regions. The poles are typical highland terrain, showing expected values of radar cross section (albedo) and circular polarization ratio (CPR). Most fresh craters display high values of CPR in and outside the crater rim; the pattern of these CPR distributions is consistent with high levels of wavelength-scale surface roughness associated with the presence of block fields, impact melt flows, and fallback breccia. A different class of polar crater exhibits high CPR only in their interiors, interiors that are both permanently dark and very cold (less than 100 K). Application of scattering models developed previously suggests that these anomalously high-CPR deposits exhibit behavior consistent with the presence of water ice. -
AN EXAMINATION of CRATERS in the ORIENTALE BASIN Jackson Haskell, Dallas Moffitt, Benjamin Daniels, Taylor Powers, Rebecca Ollerenshaw
AN EXAMINATION OF CRATERS IN THE ORIENTALE BASIN Jackson Haskell, Dallas Moffitt, Benjamin Daniels, Taylor Powers, Rebecca Ollerenshaw The new resource of the LROC images has allowed the possibility of new research throughout the lunar field, particularly on the far side of the moon where images had been previously unreliable due to low quality. Using these new images, we chose a data pool that had been previously data poor and was expanded by the LROC mission. The Orientale basin offered an ideal location to investigate craters with remarkable features or characteristics. With the new imagery, we intended to further scientific knowledge by investigating an area that had been previously unavailable and uninvestigated. Riccioli Hartwig Observations Observation It is a crater without a central peak Between the “parent” crater and Hartwig that also exhibits extensive A, there is great difference in weathering weathering. This is shown by the due to crater impacts. excessive faulting and has a high crater Hypothesis density. Additionally it is filled with There is a discrepancy in age as seen in the non‐impact generated basalt. difference in crater density and texture. It Hypothesis is highly unlikely that Hartwig A is In order to exhibit this kind of localized contemporaneous with its supposed basaltic filling in an area where one “parent” crater, let alone its secondary. It would expect to find a central peak in a is far more likely that an impactor crater of this size, it is hypothesized completely independent of the Hartwig that a second, unrelated impactor event came later, and only happened to could have caused a crater, coincide geographically, causing it to be overlapping and destroying Riccioli’s misnamed. -
AAP (Apollo Applications Program)
Index AAP (Apollo Applications Program), 118, 255; exposure, 323, 418n.21; relative, 134, 163-65,173-77,239,266, 17,47,86,90-93,99-IOO,334·See 403nn·34,35 also Crater ages; Crater counts; Abbey, George, 279 Geochronology; Maria; Stratigraphic Abelson, Philip, 379n.60, 381-82n.19 sequences Abulfeda chain, 286 Agglutinates, 342 ACIC (Air Force Chart and Information Agnew, Spiro, 240, 4I4n.14 Center), 37, 42, 43, 52, 56, J09, 156, Air force, 31,32,33. See also ACIC; AFCRL 167, 374-75n.16, 428-29n.24. Seealso Albedo, 2, 70-71, 342-43, 402-3n.32; as LAC age indicator, 88, 91-93, 285, 334, Adams,]ohn, 178, 405n.7, 426n.49 342; of blocks, 147; of craters, 147, Ad Hoc Apollo Site Evaluation 342; mare-terra contrast in, 2, 36, 342; Committee, 284, 3 I I of maria and plains, 87-88, 334-35; of Adler, Isidore, 261, 393n.I6 Moon, 206; of rays, 91, 92-93,342; of Aeon, defined, 5, 369-70n.7 slopes, 91, 92-93,147,342 Aeronutronic Division (cameras and Albritton, Claude, 13,39 capsules), 82, 96, 387n.9 Aldrin, Buzz, 78,122-23, 188; as Apollo AES (Apollo Extension System), I 16-18 II LMP, 182, 188, 199-206,208,222; AFCRL (Air Force Cambridge Research other assignments, 130, 182, 184 Laboratories), 26, 33, 68, 88 Allen, Harvey Julian, 48 Agena (rocket), 150-51 AlIen,]oseph, 264, 268, 271, 273, 274, Ages, 5, 345; absolute, 47-48, 208-21 I, 275,277,278 255-56,280-82,329,334-35, AlIenby, Richard, 114, 405n.13 41 In.28, 4I7n.17; absolute versus Alpha-particle spectrometer (orbital), relative, 5, 28, 100,3°7,334; bedrock 261 versus soil, 2 I I, 245, 345; Alpha