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Rare Astronomical Sights and Sounds
Jonathan Powell Rare Astronomical Sights and Sounds The Patrick Moore The Patrick Moore Practical Astronomy Series More information about this series at http://www.springer.com/series/3192 Rare Astronomical Sights and Sounds Jonathan Powell Jonathan Powell Ebbw Vale, United Kingdom ISSN 1431-9756 ISSN 2197-6562 (electronic) The Patrick Moore Practical Astronomy Series ISBN 978-3-319-97700-3 ISBN 978-3-319-97701-0 (eBook) https://doi.org/10.1007/978-3-319-97701-0 Library of Congress Control Number: 2018953700 © Springer Nature Switzerland AG 2018 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. The publisher, the authors, and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. -
Lunar Laser Ranging: the Millimeter Challenge
REVIEW ARTICLE Lunar Laser Ranging: The Millimeter Challenge T. W. Murphy, Jr. Center for Astrophysics and Space Sciences, University of California, San Diego, 9500 Gilman Drive, La Jolla, CA 92093-0424, USA E-mail: [email protected] Abstract. Lunar laser ranging has provided many of the best tests of gravitation since the first Apollo astronauts landed on the Moon. The march to higher precision continues to this day, now entering the millimeter regime, and promising continued improvement in scientific results. This review introduces key aspects of the technique, details the motivations, observables, and results for a variety of science objectives, summarizes the current state of the art, highlights new developments in the field, describes the modeling challenges, and looks to the future of the enterprise. PACS numbers: 95.30.Sf, 04.80.-y, 04.80.Cc, 91.4g.Bg arXiv:1309.6294v1 [gr-qc] 24 Sep 2013 CONTENTS 2 Contents 1 The LLR concept 3 1.1 Current Science Results . 4 1.2 A Quantitative Introduction . 5 1.3 Reflectors and Divergence-Imposed Requirements . 5 1.4 Fundamental Measurement and World Lines . 10 2 Science from LLR 12 2.1 Relativity and Gravity . 12 2.1.1 Equivalence Principle . 13 2.1.2 Time-rate-of-change of G ....................... 14 2.1.3 Gravitomagnetism, Geodetic Precession, and other PPN Tests . 14 2.1.4 Inverse Square Law, Extra Dimensions, and other Frontiers . 16 2.2 Lunar and Earth Physics . 16 2.2.1 The Lunar Interior . 16 2.2.2 Earth Orientation, Precession, and Coordinate Frames . 18 3 LLR Capability across Time 20 3.1 Brief LLR History . -
Moon-Earth-Sun: the Oldest Three-Body Problem
Moon-Earth-Sun: The oldest three-body problem Martin C. Gutzwiller IBM Research Center, Yorktown Heights, New York 10598 The daily motion of the Moon through the sky has many unusual features that a careful observer can discover without the help of instruments. The three different frequencies for the three degrees of freedom have been known very accurately for 3000 years, and the geometric explanation of the Greek astronomers was basically correct. Whereas Kepler’s laws are sufficient for describing the motion of the planets around the Sun, even the most obvious facts about the lunar motion cannot be understood without the gravitational attraction of both the Earth and the Sun. Newton discussed this problem at great length, and with mixed success; it was the only testing ground for his Universal Gravitation. This background for today’s many-body theory is discussed in some detail because all the guiding principles for our understanding can be traced to the earliest developments of astronomy. They are the oldest results of scientific inquiry, and they were the first ones to be confirmed by the great physicist-mathematicians of the 18th century. By a variety of methods, Laplace was able to claim complete agreement of celestial mechanics with the astronomical observations. Lagrange initiated a new trend wherein the mathematical problems of mechanics could all be solved by the same uniform process; canonical transformations eventually won the field. They were used for the first time on a large scale by Delaunay to find the ultimate solution of the lunar problem by perturbing the solution of the two-body Earth-Moon problem. -
The Moon and Eclipses
Lecture 10 The Moon and Eclipses Jiong Qiu, MSU Physics Department Guiding Questions 1. Why does the Moon keep the same face to us? 2. Is the Moon completely covered with craters? What is the difference between highlands and maria? 3. Does the Moon’s interior have a similar structure to the interior of the Earth? 4. Why does the Moon go through phases? At a given phase, when does the Moon rise or set with respect to the Sun? 5. What is the difference between a lunar eclipse and a solar eclipse? During what phases do they occur? 6. How often do lunar eclipses happen? When one is taking place, where do you have to be to see it? 7. How often do solar eclipses happen? Why are they visible only from certain special locations on Earth? 10.1 Introduction The moon looks 14% bigger at perigee than at apogee. The Moon wobbles. 59% of its surface can be seen from the Earth. The Moon can not hold the atmosphere The Moon does NOT have an atmosphere and the Moon does NOT have liquid water. Q: what factors determine the presence of an atmosphere? The Moon probably formed from debris cast into space when a huge planetesimal struck the proto-Earth. 10.2 Exploration of the Moon Unmanned exploration: 1950, Lunas 1-3 -- 1960s, Ranger -- 1966-67, Lunar Orbiters -- 1966-68, Surveyors (first soft landing) -- 1966-76, Lunas 9-24 (soft landing) -- 1989-93, Galileo -- 1994, Clementine -- 1998, Lunar Prospector Achievement: high-resolution lunar surface images; surface composition; evidence of ice patches around the south pole. -
L1 Lunar Lander Element Conceptual Design Report
EX15-01-092 L1 Lunar Lander Element Conceptual Design Report Engineering Directorate November 2000 National Aeronautics and Space Administration Lyndon B. Johnson Space Center Houston, Texas 77058 Table Of Contents i List of Figures………………………………………………………………………….……………iv ii List of Tables……………………………………………………………………………….………. v iii Contact Information………………………………………………………………………………..vi iv Introduction……………...………………………………………………………………………….vii 1.0 Element Description……………………………………………………………………….………..1 1.1 Design Objectives, Constraints & Requirements……………………………….…………..1 1.2 Vehicle Configuration Trades………………………………………………….……………3 1.3 Operations Concept…………………………………………………………….……………5 1.4 Vehicle Mass Statement…………………………………………………..………………. 9 1.5 Power Profile………………………………………………………………..……………. 10 2.0 Propulsion System…………………………………………………………………..…………….. 12 2.1 Functional Description and Design Requirements…………………………..……………. 12 2.2 Trades Considered and Results……………………………………………..……………... 12 2.3 Reference Design Description………………………………………………..…………… 12 2.4 Technology Needs and Design Challenges…………………………………..…………….13 3.0 Structure..……………………………………………………………….………….……………….14 3.1 Functional Description and Design Requirements………………………………...……….14 3.2 Trades Considered and Results……………………………………………………………..15 3.3 Reference Design Description……………………………………………………...………15 3.4 Technology Needs and Design Challenges…………………………………………………16 4.0 Electrical Power System…………………………………………………………………………….17 4.1 Functional Description and Design Requirements………………………………………….17 4.2 Trades -
Analytical Formulation of Lunar Cratering Asymmetries Nan Wang (王楠) and Ji-Lin Zhou (周济林)
A&A 594, A52 (2016) Astronomy DOI: 10.1051/0004-6361/201628598 & c ESO 2016 Astrophysics Analytical formulation of lunar cratering asymmetries Nan Wang (王`) and Ji-Lin Zhou (hN林) School of Astronomy and Space Science and Key Laboratory of Modern Astronomy and Astrophysics in Ministry of Education, Nanjing University, 210046 Nanjing, PR China e-mail: [email protected] Received 28 March 2016 / Accepted 3 July 2016 ABSTRACT Context. The cratering asymmetry of a bombarded satellite is related to both its orbit and impactors. The inner solar system im- pactor populations, that is, the main-belt asteroids (MBAs) and the near-Earth objects (NEOs), have dominated during the late heavy bombardment (LHB) and ever since, respectively. Aims. We formulate the lunar cratering distribution and verify the cratering asymmetries generated by the MBAs as well as the NEOs. Methods. Based on a planar model that excludes the terrestrial and lunar gravitations on the impactors and assuming the impactor encounter speed with Earth venc is higher than the lunar orbital speed vM, we rigorously integrated the lunar cratering distribution, and derived its approximation to the first order of vM=venc. Numerical simulations of lunar bombardment by the MBAs during the LHB were performed with an Earth–Moon distance aM = 20−60 Earth radii in five cases. Results. The analytical model directly proves the existence of a leading/trailing asymmetry and the absence of near/far asymmetry. The approximate form of the leading/trailing asymmetry is (1+A1 cos β), which decreases as the apex distance β increases. The numer- ical simulations show evidence of a pole/equator asymmetry as well as the leading/trailing asymmetry, and the former is empirically described as (1 + A2 cos 2'), which decreases as the latitude modulus j'j increases. -
Iaa-Pdc-15-04-17 from Sail to Soil – Getting Sailcraft out of the Harbour on a Visit to One of Earth’S Nearest Neighbours
4th IAA Planetary Defense Conference – PDC 2015 13-17 April 2015, Frascati, Roma, Italy IAA-PDC-15-04-17 FROM SAIL TO SOIL – GETTING SAILCRAFT OUT OF THE HARBOUR ON A VISIT TO ONE OF EARTH’S NEAREST NEIGHBOURS Jan Thimo Grundmann(1,2), Waldemar Bauer(1,3), Jens Biele(8,9), Federico Cordero(11), Bernd Dachwald(12), Alexander Koncz(13,14), Christian Krause(8,10), Tobias Mikschl(16,17), Sergio Montenegro(16,18), Dominik Quantius(1,4), Michael Ruffer(16,19), Kaname Sasaki (1,5), Nicole Schmitz(13,15), Patric Seefeldt (1,6), Norbert Tóth(1,7), Elisabet Wejmo(1,8) (1)DLR Institute of Space Systems, Robert-Hooke-Strasse 7, 28359 Bremen (2)+49-(0)421-24420-1107, (3)+49-(0)421-24420-1197, (4)+49-(0)421-24420-1109, (5)+49-(0)421-24420-1150, (6)+49-(0)421-24420-1609, (7)+49-(0)421-24420-1186, (8)+49-(0)421-24420-1107, (11)DLR Space Operations and Astronaut Training – MUSC, 51147 Köln, Germany (9)+49-2203-601-4563, (10)+49-2203-601-3048, (11)Telespazio-VEGA, Darmstadt, Germany, [email protected] (12) Faculty of Aerospace Engineering, FH Aachen University of Applied Sciences, Hohenstaufenallee 6, 52064 Aachen, Germany, +49-241-6009-52343 / -52854, (13)DLR Institute of Planetary Research, Rutherfordstr. 2, 12489 Berlin (14)+49-(0)30 67055-575, (15)+49-(0)30 67055-456, (16)Informatik 8, Universität Würzburg, Am Hubland, 97074 Würzburg, Germany Keywords: small spacecraft, solar sail, GOSSAMER roadmap, MASCOT, co-orbital asteroid ABSTRACT The DLR-ESTEC GOSSAMER roadmap envisages the development of solar sailing by successive low-cost technology demonstrators towards first science missions. -
Strategy for Optimal, Long-Term Stationkeeping of Libration Point Orbits in the Earth-Moon System
Strategy for Optimal, Long-Term Stationkeeping of Libration Point Orbits in the Earth-Moon System Thomas A. Pavlak∗ and Kathleen C. Howelly Purdue University, West Lafayette, IN, 47907-2045, USA In an effort to design low-cost maneuvers that reliably maintain unstable libration point orbits in the Earth-Moon system for long durations, an existing long-term stationkeeping strategy is augmented to compute locally optimal maneuvers that satisfy end-of-mission constraints downstream. This approach reduces stationkeeping costs for planar and three- dimensional orbits in dynamical systems of varying degrees of fidelity and demonstrates the correlation between optimal maneuver direction and the stable mode observed during ARTEMIS mission operations. An optimally-constrained multiple shooting strategy is also introduced that is capable of computing near optimal maintenance maneuvers without formal optimization software. I. Introduction Most orbits in the vicinity of collinear libration points are inherently unstable and, consequently, sta- tionkeeping strategies are a critical component of mission design and operations in these chaotic dynamical regions. Stationkeeping is particularly important for libration point missions in the Earth-Moon system since fast time scales require that orbit maintenance maneuvers be implemented approximately once per week. Assuming that acceptable orbit determination solutions require 3-4 days to obtain, stationkeeping ∆V planning activities must be quick, efficient, and effective. Furthermore, the duration of a libration point mission is often dictated by the remaining propellant so a key capability is maintenance maneuvers that are low-cost. Thus, to accommodate a likely increase in future operations in the vicinity of the Earth-Moon libration points, fast, reliable algorithms capable of rapidly computing low-cost stationkeeping maneuvers, with little or no human interaction, are critical. -
Trajectory Sensitivities for Sun-Mars Libration Point Missions
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Calhoun, Institutional Archive of the Naval Postgraduate School Calhoun: The NPS Institutional Archive Faculty and Researcher Publications Faculty and Researcher Publications Collection 2016 Trajectory Sensitivities for Sun-Mars Libration Point Missions Kutrieb, Joshua M. http://hdl.handle.net/10945/48886 AAS 01-327 TRAJECTORY SENSITIVITIES FOR SUN-MARS LIBRATION POINT MISSIONS John P. Carrico*, Jon D. Strizzi‡, Joshua M. Kutrieb‡, and Paul E. Damphousse‡ Previous research has analyzed proposed missions utilizing spacecraft in Lissajous orbits about each of the co-linear, near-Mars, Sun-Mars libration points to form a communication relay with Earth. This current effort focuses on 2016 Earth-Mars transfers to these mission orbits with their trajectory characteristics and sensitivities. This includes further analysis of using a mid-course correction as well as a braking maneuver at close approach to Mars to control Lissajous orbit insertion and the critical parameter of the phasing of the two-vehicle relay system, with one spacecraft each in orbit about L1 and L2. Stationkeeping sensitivities are investigated via a monte carlo technique. Commercial, desktop simulation and analysis tools are used to provide numerical data; and on-going, successful collaboration between military and industry researchers in a virtual environment is demonstrated. The resulting data should provide new information on these trajectory sensitivities to future researchers and mission planners. INTRODUCTION “NASA is seeking innovation to attack the diversity of Mars…to change the vantage point from which we explore…” - CNN, 25 June 2001 The concept of using communication relay vehicles in orbit about colinear Lagrange points to support exploration of the secondary body is not entirely new, being first conceptualized in the case of the Earth-Moon system by R. -
Interaction Mechanism and Response of Tidal Effect on the Shallow Geology of Europa Yifei Wang 1 ABSTRACT 1. INTRODUCTION 2
1 Interaction Mechanism and Response of Tidal Effect on the Shallow Geology of Europa Yifei Wang 1 Beijing University of Aeronautics and Astronautics Department of Materials Science and Engineering Undergraduate ABSTRACT Europa has been confirmed to have a multilayered structure and complex geological condition in last two decades whose detail and cause of formation remains unclear. In this work, we start from analyzing the mechanism of tidal effect on satellite’s surface and discuss if interaction like tidal locking and orbital resonance play an important role in tidal effect including heating, underground convection and eruption. During discussion we propose the main factors affecting Europa’s tidal heat and the formation mechanism of typical shallow geological features, and provide theoretical support for further exploration. Keywords: Europa, tidal heating, tidal locking, orbital resonance 1. INTRODUCTION According to existing observations by Galileo radio-tracking/gravity data and Galileo SSI images, Europa has a complex structure and distribution of different components including solid ice layer, warm liquid ocean, local convection and eruption between solid and liquid region, and hard brittle lithosphere. And for Jupiter’s three moon system--IO, Europa and Ganymede, these are in the rotation and revolution of synchronous pattern which called tidal locking. Besides, it is confirmed that IO, Jupiter and Ganymede are in the situation of orbital resonance, whose orbital period ratio is about 1:2:4 and the ratio remains constant with time. Their effect on the surface is periodic during revolution. From Ogilvie and Lin’s work2, a response to tidal force is separated in two parts: an equilibrium tide and a dynamic tide which is irrelevant with time and the angular position to Jupiter and other satellites because of periodic interaction to the subsurface structure. -
12 Lunar Libration Point - \ , Gpo Price $ - I I - Cfsti Price(S) $
~_________ - https://ntrs.nasa.gov/search.jsp?R=19670017256 2020-03-24T00:44:51+00:00Z View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by NASA Technical Reports Server . *‘ L. ---- ~ X-507-67-167 -- -. , \ A ‘“HUMMINGBIRD” ,-’ FOR THE . I 12 LUNAR LIBRATION POINT - \ , GPO PRICE $ - I I - CFSTI PRICE(S) $ - Hard copy - Microfiche ff 653 July 65 F. 0. VONBUN ,- / APRIL1967 , - GODDARD SPACE FLCGHT CENTER - i GREENBELT, MARYLAND , - - I .Y i \“ , .. Q - X-507-67-167 A "HUMMINGBIRD" FOR THE L, LUNAR LIBRATION POINT F. 0. Vonbun April 1967 Goddard Space Flight Center Greenbelt, Maryland TABLE OF CONTENTS ABSTRACT...................................... vi SUMMARY ...................................... vi 1. ACCELERATIONS EXPERIENCED BY THE "HUMMINGBIRD". 1 A. General .. .. .. .. .. .... .. 1 B. Accelerations Along the Earth-Moon Line . 4 C. TheSun'sInfluence . .. ... 7 II. NECESSARY SPECIFIC IMPULSE FOR ECONOMIC STATION KEEPING. 9 A. Fuel to Spacecraft Mass Ratio . 9 B. Needed Station Keeping and Attitude Engines. 10 III. REFERENCES ................................... 15 iii A tlHUMMINGBIRD1l FOR THE L, LUNAR LIBRATION POINT F. 0. Vonbun ABSTRACT Consider as an example a spacecraft, contrary to all previously published investigations, NOT in an orbit but in a more or less permanent position in the vicinity of the far-sided lunar libration point L, , as commonly called, Such a spacecraft would be very useful for a communications relay between the back side of the moon and an earth tracking station. It could be placed Icaboverrthe lunar libration point in such a fashion that it is never occulted, thus making the stated communication link a continuous one, independent of time. -
Extrasolar Kuiper Belt Dust Disks 465
Moro-Martín et al.: Extrasolar Kuiper Belt Dust Disks 465 Extrasolar Kuiper Belt Dust Disks Amaya Moro-Martín Princeton University Mark C. Wyatt University of Cambridge Renu Malhotra and David E. Trilling University of Arizona The dust disks observed around mature stars are evidence that plantesimals are present in these systems on spatial scales that are similar to that of the asteroids and the Kuiper belt ob- jects (KBOs) in the solar system. These dust disks (a.k.a. “debris disks”) present a wide range of sizes, morphologies, and properties. It is inferred that their dust mass declines with time as the dust-producing planetesimals get depleted, and that this decline can be punctuated by large spikes that are produced as a result of individual collisional events. The lack of solid-state fea- tures indicate that, generally, the dust in these disks have sizes >10 µm, but exceptionally, strong silicate features in some disks suggest the presence of large quantities of small grains, thought to be the result of recent collisions. Spatially resolved observations of debris disks show a di- versity of structural features, such as inner cavities, warps, offsets, brightness asymmetries, spirals, rings, and clumps. There is growing evidence that, in some cases, these structures are the result of the dynamical perturbations of a massive planet. Our solar system also harbors a debris disk and some of its properties resemble those of extrasolar debris disks. From the cratering record, we can infer that its dust mass has decayed with time, and that there was at least one major “spike” in the past during the late heavy bombardment.