Eclipse Observations Enabled by NASA's Lunar Reconnaissance
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Advances in the Interpretation and Analysis of Lunar Occultation Light Curves
A&A 538, A56 (2012) Astronomy DOI: 10.1051/0004-6361/201118476 & c ESO 2012 Astrophysics Advances in the interpretation and analysis of lunar occultation light curves A. Richichi1,2 and A. Glindemann2 1 National Astronomical Research Institute of Thailand, 191 Siriphanich Bldg., Huay Kaew Rd., Suthep, Muang, Chiang Mai 50200, Thailand e-mail: [email protected] 2 European Southern Observatory, Karl-Schwarzschild-Str. 2, 85748 Garching bei München, Germany Received 18 November 2011 / Accepted 23 December 2011 ABSTRACT Context. The introduction of fast 2D detectors and the use of very large telescopes have significantly advanced the sensitivity and accuracy of the lunar occultation technique. Recent routine observations at the ESO Very Large Telescope have yielded hundreds of events with results, especially in the area of binary stars, which are often beyond the capabilities of any other techniques. Aims. With the increase in the quality and in the number of the events, subtle features in the light curve patterns have occasionally been detected which challenge the standard analytical definition of the lunar occultation phenomenon as diffraction from an infinite straight edge. We investigate the possible causes for the observed peculiarities. Methods. We have evaluated the available statistics of distortions in occultation light curves observed at the ESO VLT, and compared it to data from other facilities. We have developed an alternative approach to model and interpret lunar occultation light curves, based on 2D diffraction integrals describing the light curves in the presence of an arbitrary lunar limb profile. We distinguish between large limb irregularities requiring the Fresnel diffraction formalism, and small irregularities described by Fraunhofer diffraction. -
University Microfilms, a XEROX Company, Ann Arbor, Michigan
.72-4480 FAJEMIROKUN, Francis Afolabi, 1941- APPLICATION OF NEW OBSERVATIONAL SYSTEMS FOR SELENODETIC CONTROL. The Ohio State University, Ph.D., 1971 Geodesy University Microfilms, A XEROX Company, Ann Arbor, Michigan THIS DISSERTATION HAS BEEN MICROFILMED EXACTLY AS RECEIVED APPLICATION OF NEW OBSERVATIONAL SYSTEMS FOR SELENODETIC CONTROL DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Francis Afolabi Fajemirokun, B. Sc., M. Sc. The Ohio State University 1971 Approved by l/m /• A dviser Department of Geodetic Science PLEASE NOTE: Some Pages have indistinct p rin t. Filmed as received. UNIVERSITY MICROFILMS To Ijigbola, Ibeolayemi and Oladunni ACKNOW LEDGEME NTS The author wishes to express his deep gratitude to the many persons, without whom this work would not have been possible. First and foremost, the author is grateful to the Department of Geodetic Science and themembers of its staff, for the financial support and academic guidance given to him during his studies here. In particular, the author wishes to thank his adviser Professor Ivan I. Mueller, for his encouragement, patience and guidance through the various stages of this work. Professors Urho A. Uotila, Richard H. Rapp and Gerald H. Newsom served on the author’s reading committee, and offered many valuable suggestions to help clarify many points. The author has also enjoyed working with other graduate students in the department, especially with the group at 231 Lord Hall, where there was always an atmosphere of enthusiastic learning and of true friendship. The author is grateful to the various scientists outside the department, with whom he had discussions on the subject of this work, especially to the VLBI group at the Smithsonian Astrophysical Observatory in Cambridge, Ma s sachu s s etts . -
Contributions of a Lunar Geoscience Observer (Lgo) Mission to Fundamental Questions in Lunar Science
CONTRIBUTIONS OF A LUNAR GEOSCIENCE OBSERVER (LGO) MISSION TO FUNDAMENTAL QUESTIONS IN LUNAR SCIENCE by LGO SCIENCE WORKSHOP MEMBERS Contributions Lunar Geoscience Observer Mission Frontispiece: Earth-rise over the lunar highlands. Contributions of a Lunar Geoscience Observer Mission to Fundaments Questions in Lunar Science LGO Science Workshop Members March LGO Science Workshop Members Roger Phillips (Chair), Southern Methodist University Merton Davies, Rand Coworation Michael Drake, University of Arizona Michael Duke, Johnson Space Center Larry Haskin. Washington University James Head, Brown University Eon Mood, University of Arizona Robert Lin, University of California, Berkeley Duane Muhleman, California Institute of Technology Doug Nash (Study Scientist), Jet Propulsion Laboratory Carle Pieters, Brown University Bill Sjogren, Jet Propulsion Laboratory Paul Spudis, U .S. Geological Survey Jeff Taylor, University of New Mexico Jacob Trombka, Goddard Space Flight Center This report was compiled and prepared in the Department of Geological Sciences and the AnthroGraphics Laboratory of Southern Methodist University. Material in this document may be copied without restraint for library, abstract service, educational or personal research purposes. Republication of any portion should be accompanied by the appropriate acknowledgment of this document. For further information, contact: Dr. Roger Phillips Department of Geological Sciences Southern Methodist University Dallas, TX 75275 Executive Summary THE IMPORTANCE OF LUNAR SCIENCE STATUS OF LUNAR SCIENCE DATA AND THEORY The Moon is the keystone in the interlinked knowledge that forms the foundation of our understanding of the silicate Unlike other solar system bodies beyond Earth, the Moon bodies of the solar system. The Moon is remarkable in that it has been intensely studied by telescope, unmanned space- remains the only other planet for which we have samples of crafi and manned missions. -
Moon Minerals a Visual Guide
Moon Minerals a visual guide A.G. Tindle and M. Anand Preliminaries Section 1 Preface Virtual microscope work at the Open University began in 1993 meteorites, Martian meteorites and most recently over 500 virtual and has culminated in the on-line collection of over 1000 microscopes of Apollo samples. samples available via the virtual microscope website (here). Early days were spent using LEGO robots to automate a rotating microscope stage thanks to the efforts of our colleague Peter Whalley (now deceased). This automation speeded up image capture and allowed us to take the thousands of photographs needed to make sizeable (Earth-based) virtual microscope collections. Virtual microscope methods are ideal for bringing rare and often unique samples to a wide audience so we were not surprised when 10 years ago we were approached by the UK Science and Technology Facilities Council who asked us to prepare a virtual collection of the 12 Moon rocks they loaned out to schools and universities. This would turn out to be one of many collections built using extra-terrestrial material. The major part of our extra-terrestrial work is web-based and we The authors - Mahesh Anand (left) and Andy Tindle (middle) with colleague have build collections of Europlanet meteorites, UK and Irish Peter Whalley (right). Thank you Peter for your pioneering contribution to the Virtual Microscope project. We could not have produced this book without your earlier efforts. 2 Moon Minerals is our latest output. We see it as a companion volume to Moon Rocks. Members of staff -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Glossary of Lunar Terminology
Glossary of Lunar Terminology albedo A measure of the reflectivity of the Moon's gabbro A coarse crystalline rock, often found in the visible surface. The Moon's albedo averages 0.07, which lunar highlands, containing plagioclase and pyroxene. means that its surface reflects, on average, 7% of the Anorthositic gabbros contain 65-78% calcium feldspar. light falling on it. gardening The process by which the Moon's surface is anorthosite A coarse-grained rock, largely composed of mixed with deeper layers, mainly as a result of meteor calcium feldspar, common on the Moon. itic bombardment. basalt A type of fine-grained volcanic rock containing ghost crater (ruined crater) The faint outline that remains the minerals pyroxene and plagioclase (calcium of a lunar crater that has been largely erased by some feldspar). Mare basalts are rich in iron and titanium, later action, usually lava flooding. while highland basalts are high in aluminum. glacis A gently sloping bank; an old term for the outer breccia A rock composed of a matrix oflarger, angular slope of a crater's walls. stony fragments and a finer, binding component. graben A sunken area between faults. caldera A type of volcanic crater formed primarily by a highlands The Moon's lighter-colored regions, which sinking of its floor rather than by the ejection of lava. are higher than their surroundings and thus not central peak A mountainous landform at or near the covered by dark lavas. Most highland features are the center of certain lunar craters, possibly formed by an rims or central peaks of impact sites. -
Geokniga-Introduction-Mineral-Exploration.Pdf
Introduction to Mineral Exploration Second Edition Edited by Charles J. Moon, Michael K.G. Whateley & Anthony M. Evans With contributions from William L. Barrett Timothy Bell Anthony M. Evans John Milsom Charles J. Moon Barry C. Scott Michael K.G. Whateley introduction to mineral exploration Introduction to Mineral Exploration Second Edition Edited by Charles J. Moon, Michael K.G. Whateley & Anthony M. Evans With contributions from William L. Barrett Timothy Bell Anthony M. Evans John Milsom Charles J. Moon Barry C. Scott Michael K.G. Whateley Copyright © 2006 by Charles J. Moon, Michael K.G. Whateley, and Anthony M. Evans BLACKWELL PUBLISHING 350 Main Street, Malden, MA 02148-5020, USA 9600 Garsington Road, Oxford OX4 2DQ, UK 550 Swanston Street, Carlton, Victoria 3053, Australia The rights of Charles J. Moon, Michael K.G. Whateley, and Anthony M. Evans to be identified as the Authors of this Work have been asserted in accordance with the UK Copyright, Designs, and Patents Act 1988. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs, and Patents Act 1988, without the prior permission of the publisher. First edition published 1995 by Blackwell Publishing Ltd Second edition published 2006 1 2006 Library of Congress Cataloging-in-Publication Data Introduction to mineral exploration.–2nd ed. / edited by Charles J. Moon, Michael K.G. Whateley & Anthony M. Evans; with contributions from William L. Barrett . [et al.]. p. cm. -
Broward County Hands-On Science Teacher Guide
170370 Q2c_ACT_19&20 5/8/07 6:16 PM Page 165 ivit act ies 19&20 TheThe PhasesPhases ofof thethe MoonMoon (Sessions(Sessions II andand II)II) BROWARD COUNTY ELEMENTARY SCIENCE BENCHMARK PLAN Grade 2—Quarter 2 Activities 19 & 20 SC.E.1.1.1 The student knows that the light reflected by the Moon looks a little different every day but looks the same again about every 28 days. SC.H.1.1.1 The student knows that in order to learn, it is important to observe the same things often and compare them. SC.H.1.1.3 The student knows that in doing science, it is often helpful to work with a team and to share findings with others. SC.H.1.1.4 The student knows that people use scientific processes including hypotheses, making inferences, and recording and communicating data when exploring the natural world. SC.H.2.1.1 The student knows that most natural events occur in patterns. ACTIVITY ASSESSMENT OPPORTUNITIES The following suggestions are intended to help identify major concepts covered in the activity that may need extra reinforcement. The goal is to provide opportunities to assess student progress without creating the need for a separate, formal assessment session (or activity) for each of the 40 hands-on activities at this grade level. 1. Session I—Activity 19: Challenge students to explain how the phases of the Moon form a FORcycle. (The MoonPERSONAL starts out as a new Moon, slowly gets bigger until it is a USEfull Moon, then slowly gets smaller until it is a new Moon again. -
Arxiv:2107.09416V1
Draft version July 21, 2021 A Typeset using L TEX twocolumn style in AASTeX631 Estimation of the Eclipse Solar Radius by Flash Spectrum Video Analysis Luca Quaglia,1 John Irwin,2 Konstantinos Emmanouilidis,3 and Alessandro Pessi4 1Sydney, New South Wales, Australia 2Guildford, England, United Kingdom 3Thessaloniki, Greece 4Milan, Italy ABSTRACT The value of the eclipse solar radius during the 2017 August 21st total solar eclipse was estimated to be S⊙ = (959.95±0.05)”at 1 au with no significant dependence on wavelength. The measurement was obtained from the analysis of a video of the eclipse flash spectrum recorded at the southern limit of the umbral shadow path. Our analysis was conducted by extracting light curves from the flash spectrum and comparing them to simulated light curves. Simulations were performed by integrating the limb darkening function (LDF) over the exposed area of photosphere. These numerical integrations relied upon very precise computations of the relative movement of the lunar and solar limbs. Keywords: Solar radius (1488) — Solar eclipses (1489) — Flash spectrum (541) — Light curves (918) — Astronomical simulations (1857) 1. INTRODUCTION rameters is now below the milliarcsecond level while the accuracy of UT1 determination is well below the mil- The value of the solar radius at unit distance S⊙ is one of the fundamental quantities needed to perform very lisecond level. Satellite missions in the last decade have precise eclipse computations. Some of the other required vastly improved the knowledge of the topography of the inputs are: accurate ephemerides for the position of the Moon (Smith et al. 2017) to better than 10 m (corre- centres of mass of the Sun and Moon; accurate models sponding to about 5 mas at the mean geocentric dis- for the orientation of the Earth and Moon; and detailed tance of the Moon), allowing accurate computations of data on the topography of the Moon and Earth. -
INTERAGENCY REPORT: ASTROGEOLOGY 7 ADVANCED SYSTEMS TRAVERSE RESEARCH PROJECT REPORT by G
INTERAGENCY REPORT: ASTROGEOLOGY 7 ADVANCED SYSTEMS TRAVERSE RESEARCH PROJECT REPORT By G. E. Ulrich With a Section on Problems for Geologic Investigations of the Orientale Region of the Moon By R. S. Saunders July 1968 CONTENTS Page Abs tract . ............. 1 Introduct ion . •• # • ••• ••• .' • 2 Physiographic subdivision of the lunar surface 3 Site selection and preliminary traverse research. 8 Lunar topographic data •••••••.•.•••••• 17 Objectives and evaluation of traverse concepts • 20 Recommendations for continued traverse research .••• 26 Problems for geologic investigations of the Orientale region of the Moon, by R. S. Saunders 30 Introduct ion •.•• •••. 30 Physiography 30 Pre-Orbiter observations and i~terpretations 35 Geologic interpretations based on Orbiter photography ••••••••• 38 Conelusions •••• .•••. 54 References 56 ILLUSTRATIONS Figure 1. Map and index to photographs of Orientale basin region ••••.•••••• 4 2. Crater-size frequency distributions of Orientale basin terrain units •••••• 11 3. Orientale basin region showing pre- liminary traverse evaluation areas ••••• 14 4. Effect of photographic exposure on shadow measurements 15 5. Alternate traverse areas for short and intermediate duration missions. North eastern sector of central Orientale basin ................... 24 6. Preliminary photogeologic map of the Orientale basin region. .•• .. .. 32 iii Page Figure 7. Sketch map of Mare Orientale region prepared from Earth-based telescopic photography • 36 8-21. Orbiter IV photographs of Orientale basin region showing-- . 8. Part of wr{nk1e ridge . 41 9. Slump scarps around steptoe and collapse depression . 44 10. Slump scarps along margin of central mare basin outlining collapse depression • • . • 44 11. Possible caldera 45 12. Northeast quadrant of inner ring showing central basin material and mare units 45 13. -
Is It Lunar Or Lunacy?
Is It Lunar or Lunacy? Summary Learn all about the moon, its phases and even how to make a model. Materials One 4" foam ball to represent Earth One foam ball to represent moon (1/4 size of the Earth) Twelve wooden Skewers pointed on each end Black paint Red paint or red permanent marker Heavy foam board measuring 26" X 26" between 3/4" to an inch" in thickness Hula hoop Protractor Straw String Two small washers - Galileo - Moon Phase Chart - The Rising and Setting of the Sun Table - The Rising and Setting of the Moon Table - Instructions for Making Moon Model Additional Resources Books - Earth, Moon, and Sun--Earth Science Delta Science Module , Teacher's Guide. ISBN# 0-87504-166-3 - Earth, Moon, and Stars -- LHS GEMS, Teacher's Guide ISBN# 0-912511-18-4 - The Moon Book , by Gail Gibbons - Galileo , by Leonard Everett Fisher ISBN# 0-02-735235-8 - The Universe at Your Fingertips--An Astronomy Activity and Resource Notebook Project ASTRO Astronomical Society of the Pacific (415) 337 - 1100 ISBN# 1-886733-00-7 Videos - How and Why--The Moon and the Universe , Volume 4. 1-888-661d-8104 www.mediakids.com Background for Teachers When Buzz Aldrin first stepped on the lunar surface and looked around at the alien landscape, he exclaimed: "Magnificent desolation!" It was a perfect description of the stark, inhospitable lunar surface which has no atmosphere or water. Standing on the Moon's surface, the astronauts saw a barren vista of rocks, boulders and fine dust. In the distance, rounded hills and mountains reaching toward an utterly black sky, whether it was day or night. -
From the Editor Chair's Report by Bernie Venasse Volume 24
Volume 24, Number 6 April 2017 From The Chair’s Report by Bernie Venasse Editor Hamilton Amateur Astronomers General Meeting for April 7th 2017. With the arrival of Note that this occurs on the FIRST Friday of the month…… April, winter skies and Our scheduled speaker this month is Dr. Pauline Barmby, visiting us from weather give way to Western University in London, Ontario. Her presentation will focus on the past, the Spring constel- present, and future of big data in astronomy. lations and Spring “Big data” is the hot new thing in finance, health care, advertising and weather …and more. But as one of the first observational sciences, astronomy has been dealing hopefully clearer with big data for thousands of years. New and imminent facilities for capturing skies! and storing astronomical observations will lead to what some call the “tsunami of data” in astronomy. Techniques like machine learning and citizen science Happy Reading! are needed to get the most science out of these enormous datasets. You will learn how big our big data in astronomy really is, and about some of the Bob Christmas, Editor discoveries that it has enabled. Pauline Barmby is an associate professor in Western’s Department of editor ‘AT’ Physics & Astronomy and associate dean (graduate and postdoctoral studies) amateurastronomy.org in Western’s Faculty of Science. She received her BSc in Physics and Astronomy (Continued on page 2) IN THIS ISSUE: § NASA’s Space Place § Snippets from April Fools’ Day § § Cartoon Corner March 2017 General Meeting Summary § § The Sky This Month 2017 Calendar of Events § § Upcoming McCallion Planetarium Shows Treasurer’s Report § § Easter and Astronomy Upcoming Events Contact Information Hamilton Amateur Astronomers Event Horizon April 2017 Page 1 Chair’s Report (continued) H.A.A.’s Loaner Scope Program from UBC (1995) and her PhD in Astronomy We at the HAA are proud of our from Harvard University (2001).