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Scienza E Cultura Universitalia
SCIENZA E CULTURA UNIVERSITALIA Costantino Sigismondi (ed.) ORBE NOVUS Astronomia e Studi Gerbertiani 1 Universitalia SIGISMONDI, Costantino (a cura di) Orbe Novus / Costantino Sigismondi Roma : Universitalia, 2010 158 p. ; 24 cm. – ( Scienza e Cultura ) ISBN … 1. Storia della Scienza. Storia della Chiesa. I. Sigismondi, Costantino. 509 – SCIENZE PURE, TRATTAMENTO STORICO 270 – STORIA DELLA CHIESA In copertina: Imago Gerberti dal medagliere capitolino e scritta ORBE NOVVS nell'epitaffio tombale di Silvestro II a S. Giovanni in Laterano (entrambe le foto sono di Daniela Velestino). Collana diretta da Rosalma Salina Borello e Luca Nicotra Prima edizione: maggio 2010 Universitalia INTRODUZIONE Introduzione Costantino Sigismondi L’edizione del convegno gerbertiano del 2009, in pieno anno internazionale dell’astronomia, si è tenuta nella Basilica di S. Maria degli Angeli e dei Martiri il 12 maggio, e a Seoul presso l’università Sejong l’11 giugno 2009. La scelta della Basilica è dovuta alla presenza della grande meridiana voluta dal papa Clemente XI Albani nel 1700, che ancora funziona e consente di fare misure di valore astrometrico. Il titolo di questi atti, ORBE NOVUS, è preso, come i precedenti, dall’epitaffio tombale di Silvestro II in Laterano, e vuole suggerire il legame con il “De Revolutionibus Orbium Coelestium” di Copernico, sebbene il contesto in cui queste parole sono tratte vuole inquadrare Gerberto nel suo ministero petrino come il nuovo pastore per tutto il mondo: UT FIERET PASTOR TOTO ORBE NOVVS. Elizabeth Cavicchi del Massachussets Institute of Technology, ha riflettuto sulle esperienze di ottica geometrica fatte da Gerberto con i tubi, nel contesto contemporaneo dello sviluppo dell’ottica nel mondo arabo con cui Gerberto era stato in contatto. -
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): -
The Longitude of the Mediterranean Throughout History: Facts, Myths and Surprises Luis Robles Macías
The longitude of the Mediterranean throughout history: facts, myths and surprises Luis Robles Macías To cite this version: Luis Robles Macías. The longitude of the Mediterranean throughout history: facts, myths and sur- prises. E-Perimetron, National Centre for Maps and Cartographic Heritage, 2014, 9 (1), pp.1-29. hal-01528114 HAL Id: hal-01528114 https://hal.archives-ouvertes.fr/hal-01528114 Submitted on 27 May 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. e-Perimetron, Vol. 9, No. 1, 2014 [1-29] www.e-perimetron.org | ISSN 1790-3769 Luis A. Robles Macías* The longitude of the Mediterranean throughout history: facts, myths and surprises Keywords: History of longitude; cartographic errors; comparative studies of maps; tables of geographical coordinates; old maps of the Mediterranean Summary: Our survey of pre-1750 cartographic works reveals a rich and complex evolution of the longitude of the Mediterranean (LongMed). While confirming several previously docu- mented trends − e.g. the adoption of erroneous Ptolemaic longitudes by 15th and 16th-century European cartographers, or the striking accuracy of Arabic-language tables of coordinates−, we have observed accurate LongMed values largely unnoticed by historians in 16th-century maps and noted that widely diverging LongMed values coexisted up to 1750, sometimes even within the works of one same author. -
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. -
Lecture 25.Key
Astronomy 330: Extraterrestrial Life This class (Lecture 25): Evolution of Worldview Sean Sarcu Saloni Sheth ! ! Next Class: Lifetime Vincent Abejuela Cassandra Jensen Music: Astronomy – Metallica 2 x 2 page pdf articles due next Tues Drake Equation Frank That’s 2.7 intelligent systems/year Drake N = R* × fp × ne × fl × fi × fc × L # of # of Star Fraction of Fraction advanced Earthlike Fraction on Fraction that Lifetime of formation stars with that civilizations planets per which life evolve advanced rate planets commun- we can system arises intelligence civilizations icate contact in our Galaxy today 30 0.8 4 x 0.47 0.2 0.3 comm./ yrs/ stars/ systems/ = 1.88 life/ intel./ intel. comm. yr star planets/ planet life system • Requires civilization to undergo three steps: 1. A correct appreciation of the size and nature of the Worldview Universe 2. A realization of their place in the Universe 3. A belief that the odds for life are reasonable. The beings of Q’earth must have taken their Q’astro Intelligent ET Life must want to communicate with us 330 class and came up with a good number of communicable civilizations in the Q’drake This means they MUST equation. believe in the possibility of us (and other ET life) Requirements: ! 1) Understand size and scale of the cosmos ASTR 330 2) Realize their place in the cosmos 3) Believe the odds for life elsewhere are reasonable Alien 3 Our Worldview First worldview: Earth Centric Why? Natural observations imply we are stationary 4 • The Mayans computed the length of year to within a few Ancient Astronomy seconds (0.001%). -
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. -
Stellarium for Cultural Astronomy Research
RESEARCH The Simulated Sky: Stellarium for Cultural Astronomy Research Georg Zotti Ludwig Boltzmann Institute for Archaeological Prospection and Virtual Archaeology, Vienna, Austria [email protected] Susanne M. Hoffmann Friedrich-Schiller-Universität Jena, Michael-Stifel-Center/ Institut für Informatik and Physikalisch- Astronomische Fakultät, Jena, Germany [email protected] Alexander Wolf Altai State Pedagogical University, Barnaul, Russia [email protected] Fabien Chéreau Stellarium Labs, Toulouse, France [email protected] Guillaume Chéreau Noctua Software, Hong Kong [email protected] Abstract: For centuries, the rich nocturnal environment of the starry sky could be modelled only by analogue tools such as paper planispheres, atlases, globes and numerical tables. The immer- sive sky simulator of the twentieth century, the optomechanical planetarium, provided new ways for representing and teaching about the sky, but the high construction and running costs meant that they have not become common. However, in recent decades, “desktop planetarium programs” running on personal computers have gained wide attention. Modern incarnations are immensely versatile tools, mostly targeted towards the community of amateur astronomers and for knowledge transfer in transdisciplinary research. Cultural astronomers also value the possibili- ties they give of simulating the skies of past times or other cultures. With this paper, we provide JSA 6.2 (2020) 221–258 ISSN (print) 2055-348X https://doi.org/10.1558/jsa.17822 ISSN (online) 2055-3498 222 Georg Zotti et al. an extended presentation of the open-source project Stellarium, which in the last few years has been enriched with capabilities for cultural astronomy research not found in similar, commercial alternatives. -
ASTR 101L Astronomical Motions I: the Night Sky (Spring)
ASTR 101L Astronomical Motions I: The Night Sky (Spring) Early Greek observers viewed the sky as a transparent sphere which surrounded the Earth. They divided the stars into six categories of brightness and arranged the stars into groupings called constellations (as did many other cultures). Most of the names of the eighty-eight constellations we use today are based on Greek mythology and their Latin translations. Modern astronomy uses the constellation designations to map the sky. On skymaps, the size of the dot is usually related to the brightness of the object (look on your planisphere). Most only show the brightest stars. They are typically named from brightest to faintest using a letter from the Greek alphabet (α, β, γ, etc.) and the constellation name in the genitive form; e.g. alpha (α) Cygni is the brightest star in Cygnus. Many stars also have Arabic names such as Betelgeuse, Algol, and Arcturus; α Cygni is named Deneb and α Ursa Minoris is more commonly known as Polaris. Either designation is correct. In the exercise “Angles and Parallax,” you made a cross-staff and quadrant and learned how to use them to measure objects inside. Now we will use them to measure objects in the night sky, much like Tycho Brahe did in the 1500’s. Remember to record the date, time, and conditions when making any astronomical observations! All numerical data should be recorded to one decimal place. Objectives: . Measure angular separations and altitudes of objects in the night sky with instruments . Estimate angular separations and altitudes of objects in the night sky with your hands . -
Build Your Own Planisphere
Make your own planisphere Dominic Ford 2014{2021 A planisphere is a simple hand-held device which shows a map of which stars are visible in the night sky at any particular time. By rotating a wheel, it shows how stars move across the sky through the night, and how different constellations are visible at different times of year. Here, I present a kit which you can download and print to make your own planisphere out of paper or cardboard. The design of a planisphere depends on the geographic location where it is to be used, since different stars are visible from different places. I have created kits for use at a wide range of latitudes, which you can download from https://in-the-sky.org/planisphere/ The planisphere presented in this document is designed for use at a latitude of 35◦N . What you need • Two sheets of A4 paper, or preferably thin card. • Scissors. • A split-pin fastener. • Optional: one sheet of transparent plastic, e.g. acetate designed for use with overhead projectors. • Optional: A little glue. Assembly instructions Step 1 { Planispheres look slightly different depending on where you live. The planisphere prepared in this document is designed for use anywhere on Earth which is within a few degrees of latitude 35◦N . If you live elsewhere, you should download an alternative kit from https://in-the-sky.org/planisphere/ Step 2 { Print the pages at the back of this PDF file, showing the star wheel and the body of the planisphere, onto two separate sheets of paper, or more preferably onto thin card. -
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.