Time and Diurnal Motion 1A. the Earth Is Flat
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Ast 443 / Phy 517
AST 443 / PHY 517 Astronomical Observing Techniques Prof. F.M. Walter I. The Basics The 3 basic measurements: • WHERE something is • WHEN something happened • HOW BRIGHT something is Since this is science, let’s be quantitative! Where • Positions: – 2-dimensional projections on celestial sphere (q,f) • q,f are angular measures: radians, or degrees, minutes, arcsec – 3-dimensional position in space (x,y,z) or (q, f, r). • (x,y,z) are linear positions within a right-handed rectilinear coordinate system. • R is a distance (spherical coordinates) • Galactic positions are sometimes presented in cylindrical coordinates, of galactocentric radius, height above the galactic plane, and azimuth. Angles There are • 360 degrees (o) in a circle • 60 minutes of arc (‘) in a degree (arcmin) • 60 seconds of arc (“) in an arcmin There are • 24 hours (h) along the equator • 60 minutes of time (m) per hour • 60 seconds of time (s) per minute • 1 second of time = 15”/cos(latitude) Coordinate Systems "What good are Mercator's North Poles and Equators Tropics, Zones, and Meridian Lines?" So the Bellman would cry, and the crew would reply "They are merely conventional signs" L. Carroll -- The Hunting of the Snark • Equatorial (celestial): based on terrestrial longitude & latitude • Ecliptic: based on the Earth’s orbit • Altitude-Azimuth (alt-az): local • Galactic: based on MilKy Way • Supergalactic: based on supergalactic plane Reference points Celestial coordinates (Right Ascension α, Declination δ) • δ = 0: projection oF terrestrial equator • (α, δ) = (0,0): -
Unit 2 Basic Concepts of Positional Astronomy
Basic Concepts of UNIT 2 BASIC CONCEPTS OF POSITIONAL Positional Astronomy ASTRONOMY Structure 2.1 Introduction Objectives 2.2 Celestial Sphere Geometry of a Sphere Spherical Triangle 2.3 Astronomical Coordinate Systems Geographical Coordinates Horizon System Equatorial System Diurnal Motion of the Stars Conversion of Coordinates 2.4 Measurement of Time Sidereal Time Apparent Solar Time Mean Solar Time Equation of Time Calendar 2.5 Summary 2.6 Terminal Questions 2.7 Solutions and Answers 2.1 INTRODUCTION In Unit 1, you have studied about the physical parameters and measurements that are relevant in astronomy and astrophysics. You have learnt that astronomical scales are very different from the ones that we encounter in our day-to-day lives. In astronomy, we are also interested in the motion and structure of planets, stars, galaxies and other celestial objects. For this purpose, it is essential that the position of these objects is precisely defined. In this unit, we describe some coordinate systems (horizon , local equatorial and universal equatorial ) used to define the positions of these objects. We also discuss the effect of Earth’s daily and annual motion on the positions of these objects. Finally, we explain how time is measured in astronomy. In the next unit, you will learn about various techniques and instruments used to make astronomical measurements. Study Guide In this unit, you will encounter the coordinate systems used in astronomy for the first time. In order to understand them, it would do you good to draw each diagram yourself. Try to visualise the fundamental circles, reference points and coordinates as you make each drawing. -
Exercise 3.0 the CELESTIAL HORIZON SYSTEM
Exercise 3.0 THE CELESTIAL HORIZON SYSTEM I. Introduction When we stand at most locations on the Earth, we have the distinct impression that the Earth is flat. This occurs because the curvature of the small area of the Earth usually visible is very slight. We call this “flat Earth” the Plane of the Horizon and divide it up into 4 quadrants, each containing 90o, by using the cardinal points of the compass. The latter are the North, South, East, and west points of the horizon. We describe things as being vertical or “straight up” if they line up with the direction of gravity at that location. It is easy for us to determine “straight up” because we have a built in mechanism for this in the inner ear (the semicircular canals). Because it seems so “natural”, we build a coordinate system on these ideas called the Horizon System. The Celestial Horizon System is one of the coordinate systems that astronomers find useful for locating objects in the sky. It is depicted in the Figure below. Figure 1. The above diagram is a skewed perspective, schematic diagram of the celestial sphere with circles drawn only for the half above the horizon. Circles on the far side, or western half, of the celestial sphere are drawn as dashed curves. All the reference circles of this system do not share in the rotation of the celestial sphere and, therefore, this coordinate system is fixed with respect to a given observer. The basis for the system is the direction of gravity. We can describe this as the line from the observer on the surface of the Earth through the center of the Earth. -
The Determination of Longitude in Landsurveying.” by ROBERTHENRY BURNSIDE DOWSES, Assoc
316 DOWNES ON LONGITUDE IN LAXD SUIWETISG. [Selected (Paper No. 3027.) The Determination of Longitude in LandSurveying.” By ROBERTHENRY BURNSIDE DOWSES, Assoc. M. Inst. C.E. THISPaper is presented as a sequel tothe Author’s former communication on “Practical Astronomy as applied inLand Surveying.”’ It is not generally possible for a surveyor in the field to obtain accurate determinationsof longitude unless furnished with more powerful instruments than is usually the case, except in geodetic camps; still, by the methods here given, he may with care obtain results near the truth, the error being only instrumental. There are threesuch methods for obtaining longitudes. Method 1. By Telrgrcrph or by Chronometer.-In either case it is necessary to obtain the truemean time of the place with accuracy, by means of an observation of the sun or z star; then, if fitted with a field telegraph connected with some knownlongitude, the true mean time of that place is obtained by telegraph and carefully compared withthe observed true mean time atthe observer’s place, andthe difference between thesetimes is the difference of longitude required. With a reliable chronometer set totrue Greenwich mean time, or that of anyother known observatory, the difference between the times of the place and the time of the chronometer must be noted, when the difference of longitude is directly deduced. Thisis the simplest method where a camp is furnisl~ed with eitherof these appliances, which is comparatively rarely the case. Method 2. By Lunar Distances.-This observation is one requiring great care, accurately adjusted instruments, and some littleskill to obtain good results;and the calculations are somewhat laborious. -
Sidereal Time Distribution in Large-Scale of Orbits by Usingastronomical Algorithm Method
International Journal of Science and Research (IJSR) ISSN (Online): 2319-7064 Index Copernicus Value (2013): 6.14 | Impact Factor (2013): 4.438 Sidereal Time Distribution in Large-Scale of Orbits by usingAstronomical Algorithm Method Kutaiba Sabah Nimma 1UniversitiTenagaNasional,Electrical Engineering Department, Selangor, Malaysia Abstract: Sidereal Time literally means star time. The time we are used to using in our everyday lives is Solar Time.Astronomy, time based upon the rotation of the earth with respect to the distant stars, the sidereal day being the unit of measurement.Traditionally, the sidereal day is described as the time it takes for the Earth to complete one rotation relative to the stars, and help astronomers to keep them telescops directions on a given star in a night sky. In other words, earth’s rate of rotation determine according to fixed stars which is controlling the time scale of sidereal time. Many reserachers are concerned about how long the earth takes to spin based on fixed stars since the earth does not actually spin around 360 degrees in one solar day.Furthermore, the computations of the sidereal time needs to take a long time to calculate the number of the Julian centuries. This paper shows a new method of calculating the Sidereal Time, which is very important to determine the stars location at any given time. In addition, this method provdes high accuracy results with short time of calculation. Keywords: Sidereal time; Orbit allocation;Geostationary Orbit;SolarDays;Sidereal Day 1. Introduction (the upper meridian) in the sky[6]. Solar time is what the time we all use where a day is defined as 24 hours, which is The word "sidereal" comes from the Latin word sider, the average time that it takes for the sun to return to its meaning star. -
Sidereal Time 1 Sidereal Time
Sidereal time 1 Sidereal time Sidereal time (pronounced /saɪˈdɪəri.əl/) is a time-keeping system astronomers use to keep track of the direction to point their telescopes to view a given star in the night sky. Just as the Sun and Moon appear to rise in the east and set in the west, so do the stars. A sidereal day is approximately 23 hours, 56 minutes, 4.091 seconds (23.93447 hours or 0.99726957 SI days), corresponding to the time it takes for the Earth to complete one rotation relative to the vernal equinox. The vernal equinox itself precesses very slowly in a westward direction relative to the fixed stars, completing one revolution every 26,000 years approximately. As a consequence, the misnamed sidereal day, as "sidereal" is derived from the Latin sidus meaning "star", is some 0.008 seconds shorter than the earth's period of rotation relative to the fixed stars. The longer true sidereal period is called a stellar day by the International Earth Rotation and Reference Systems Service (IERS). It is also referred to as the sidereal period of rotation. The direction from the Earth to the Sun is constantly changing (because the Earth revolves around the Sun over the course of a year), but the directions from the Earth to the distant stars do not change nearly as much. Therefore the cycle of the apparent motion of the stars around the Earth has a period that is not quite the same as the 24-hour average length of the solar day. Maps of the stars in the night sky usually make use of declination and right ascension as coordinates. -
A Short Guide to Celestial Navigation5.16 MB
A Short Guide to elestial Na1igation Copyright A 1997 2011 (enning -mland Permission is granted to copy, distribute and/or modify this document under the terms of the G.2 Free Documentation -icense, 3ersion 1.3 or any later version published by the Free 0oftware Foundation% with no ,nvariant 0ections, no Front Cover 1eIts and no Back Cover 1eIts. A copy of the license is included in the section entitled "G.2 Free Documentation -icense". ,evised October 1 st , 2011 First Published May 20 th , 1997 .ndeB 1reface Chapter 1he Basics of Celestial ,aEigation Chapter 2 Altitude Measurement Chapter 3 )eographic .osition and 1ime Chapter 4 Finding One's .osition 0ight Reduction) Chapter 5 Finding the .osition of an Advancing 2essel Determination of Latitude and Longitude, Direct Calculation of Chapter 6 .osition Chapter 7 Finding 1ime and Longitude by Lunar Distances Chapter 8 Rise, 0et, 1wilight Chapter 9 )eodetic Aspects of Celestial ,aEigation Chapter 0 0pherical 1rigonometry Chapter 1he ,aEigational 1riangle Chapter 12 )eneral Formulas for ,aEigation Chapter 13 Charts and .lotting 0heets Chapter 14 Magnetic Declination Chapter 15 Ephemerides of the 0un Chapter 16 ,aEigational Errors Chapter 17 1he Marine Chronometer AppendiB -02 ,ree Documentation /icense Much is due to those who first bro-e the way to -now.edge, and .eft on.y to their successors the tas- of smoothing it Samue. Johnson Prefa e Why should anybody still practice celestial naRigation in the era of electronics and 18S? 7ne might as Sell ask Shy some photographers still develop black-and-Shite photos in their darkroom instead of using a digital camera. -
Local Sidereal Time (LST) = Greenwich Sidereal Time (GST) +
AST326, 2010 Winter Semester • Celestial Sphere • Spectroscopy • (Something interesting; e.g ., advanced data analyses with IDL) • Practical Assignment: analyses of Keck spectroscopic data from the instructor (can potentially be a research paper) − “there will be multiple presentations by students” • Telescope sessions for spectroscopy in late Feb &March • Bonus projects (e.g., spectroscopic observations using the campus telescope) will be given. Grading: Four Problem Sets (16%), Four Lab Assignments (16%), Telescope Operation – Spectrograph (pass or fail; 5%), One Exam(25%), Practical Assignment (28%), Class Participation & Activities (10%) The Celestial Sphere Reference Reading: Observational Astronomy Chapter 4 The Celestial Sphere We will learn ● Great Circles; ● Coordinate Systems; ● Hour Angle and Sidereal Time, etc; ● Seasons and Sun Motions; ● The Celestial Sphere “We will be able to calculate when a given star will appear in my sky.” The Celestial Sphere Woodcut image displayed in Flammarion's `L'Atmosphere: Meteorologie Populaire (Paris, 1888)' Courtesy University of Oklahoma History of Science Collections The celestial sphere: great circle The Celestial Sphere: Great Circle A great circle on a sphere is any circle that shares the same center point as the sphere itself. Any two points on the surface of a sphere, if not exactly opposite one another, define a unique great circle going through them. A line drawn along a great circle is actually the shortest distance between the two points (see next slides). A small circle is any circle drawn on the sphere that does not share the same center as the sphere. The celestial sphere: great circle The Celestial Sphere: Great Circle •A great circle divides the surface of a sphere in two equal parts. -
TIME 1. Introduction 2. Time Scales
TIME 1. Introduction The TCS requires access to time in various forms and accuracies. This document briefly explains the various time scale, illustrate the mean to obtain the time, and discusses the TCS implementation. 2. Time scales International Atomic Time (TIA) is a man-made, laboratory timescale. Its units the SI seconds which is based on the frequency of the cesium-133 atom. TAI is the International Atomic Time scale, a statistical timescale based on a large number of atomic clocks. Coordinated Universal Time (UTC) – UTC is the basis of civil timekeeping. The UTC uses the SI second, which is an atomic time, as it fundamental unit. The UTC is kept in time with the Earth rotation. However, the rate of the Earth rotation is not uniform (with respect to atomic time). To compensate a leap second is added usually at the end of June or December about every 18 months. Also the earth is divided in to standard-time zones, and UTC differs by an integral number of hours between time zones (parts of Canada and Australia differ by n+0.5 hours). You local time is UTC adjusted by your timezone offset. Universal Time (UT1) – Universal time or, more specifically UT1, is counted from 0 hours at midnight, with unit of duration the mean solar day, defined to be as uniform as possible despite variations in the rotation of the Earth. It is observed as the diurnal motion of stars or extraterrestrial radio sources. It is continuous (no leap second), but has a variable rate due the Earth’s non-uniform rotational period. -
Astronomy 113 Laboratory Manual
UNIVERSITY OF WISCONSIN - MADISON Department of Astronomy Astronomy 113 Laboratory Manual Fall 2011 Professor: Snezana Stanimirovic 4514 Sterling Hall [email protected] TA: Natalie Gosnell 6283B Chamberlin Hall [email protected] 1 2 Contents Introduction 1 Celestial Rhythms: An Introduction to the Sky 2 The Moons of Jupiter 3 Telescopes 4 The Distances to the Stars 5 The Sun 6 Spectral Classification 7 The Universe circa 1900 8 The Expansion of the Universe 3 ASTRONOMY 113 Laboratory Introduction Astronomy 113 is a hands-on tour of the visible universe through computer simulated and experimental exploration. During the 14 lab sessions, we will encounter objects located in our own solar system, stars filling the Milky Way, and objects located much further away in the far reaches of space. Astronomy is an observational science, as opposed to most of the rest of physics, which is experimental in nature. Astronomers cannot create a star in the lab and study it, walk around it, change it, or explode it. Astronomers can only observe the sky as it is, and from their observations deduce models of the universe and its contents. They cannot ever repeat the same experiment twice with exactly the same parameters and conditions. Remember this as the universe is laid out before you in Astronomy 113 – the story always begins with only points of light in the sky. From this perspective, our understanding of the universe is truly one of the greatest intellectual challenges and achievements of mankind. The exploration of the universe is also a lot of fun, an experience that is largely missed sitting in a lecture hall or doing homework. -
Celestial Sphere
ASTR 111 – 003 Fall 2007 Lecture 02 Sep. 10, 2007 Introduction To Modern Astronomy I: Solar System Ch1: Astronomy and the Universe Introducing Astronomy (chap. 1-6) Ch2: Knowing the Heavens Ch3: Eclipses and the Motion of the Moon Planets and Moons (chap. 7-15) Ch4: Gravitation and the Waltz of the Planets Ch5: The Nature of Light Chap. 16: Our Sun Ch6: Optics and Telescope Chap. 28: Search for Extraterrestrial life Knowing the Heavens Chapter Two Hawaii: N20° Washington D.C.: N38° Positional Astronomy • Positional astronomy – the study of the positions of objects in the sky and how these positions change • It has roots in almost all ancient civilizations • Naked-eye astronomy – the sort that requires only human vision (no telescope) The Sun Dagger at Chaco Canyon, New Mexico Positional Astronomy • Position of stars in the heaven; forming consternations • Path of Sun, Moon and Planets; forming zodiac band Heaven’s Sphere at Purple Mountain Observatory, Nanjing, China Constellations From the Latin for “group of stars” ORION: Photograph Modern Star Atlas Ancient Star Atlas(1835) ORION (the Hunter) Betelgeuse: the armpit; Mintaka: the belt Constellations •Zodiac Constellations: 12 in total along the ecliptic path Constellations • On modern star charts, the entire sky is divided into 88 constellations • Starts in the same constellation only appear to be close, because they are in nearly the same direction as seen from Earth • However, most stars in a constellation are nowhere near one another in real 3-D distance. North Star: Polaris •Visible -
The Universe: an Overview
1 Draft by Paul E. Johnson 2012, 2013 © for UW Astronomy class use only ________________________________________________________________________ Chapter 1 - The Universe: an Overview I roamed the countryside searching for answers to things I did not understand. Why shells existed on the tops of mountains along with the imprints of coral and plants and seaweed usually found in the sea. Why the thunder lasts a longer time than that which causes it and why immediately on its creation the lightning becomes visible to the eye while thunder requires time to travel. How the various circles of water form around the spot which has been struck by a stone and why a bird sustains itself in the air. These questions and other strange phenomena engaged my thought throughout my life. -- Leonardo di Vinci, Renaissance Man Chapter Preview This chapter provides an overview of the Universe and the study of astronomy that will follow in subsequent chapters. You will look at astronomy from multiple perspectives, as a science, from an historical point of few, and from the aspects of time and space. No other branch of science has the overall scope of astronomy: from the subatomic particle to the Universe as a whole, from the moment of creation to the evolution of intelligent life, and from Aristotle to space-based observatories. Key Physical Concepts to Understand: The Scales of Time and Space I. Introduction The purpose of this book is to provide a basic understanding of astronomy as a science. This study will take us on a journey from Earth to the stars, planets, and galaxies that inhabit our Universe.