Angle D = Latitude Angle C = Altitude Polaris Angle C

Total Page:16

File Type:pdf, Size:1020Kb

Angle D = Latitude Angle C = Altitude Polaris Angle C North Celestial Pole Altitude of Polaris is equal to our Latitude on Earth Proof: Angle Pole Star with the horizon = observer's latitude. Prove: Angle c = Angle d Altitude of Polaris = our latitude on earth Given: The pole and the equator are at right angles, d + a = 90 therefore a = 90 – d c = b (AIT Alternate Interior Angles because c || b) a + b + 90 = 180 (sum angles of triangle) Therefore: a + b = 90 Substitute for a: (90 – d) + b = 90 Angle b = Angle d and angle c = b Angle d = Latitude Therefore Angle c = Angle d Angle c = Altitude Polaris We find Polaris at our latitude Roughly 45 degrees north Angle c = Angle d ~ 45 deg here Star Location: Altitude above Horizon Star altitude depends on the Declination of the Star. The altitude of any star transiting due South on the MERIDIAN Altitude of Star above Horizon = Co-latitude on Earth + Declination of Star Celestial Equator co-latitude Declination ALWAYS measured from celestialDue equator South to star. Local Horizon View: Altitude of Regulus above our horizon = 45(Colatitude) + 11(Declination) = 56 deg Objects on your Meridian North South Line Horizon to Horizon OBJECTS (stars, clusters, galaxies) in the sky - Left(east) of your Meridian … RISING - Right(west) of Meridian … SETTING, just like the Sun does . Objects ON your Meridian have reached their HIGHEST point in the sky tonight, Best for Viewing = CULMINATION For Northern Hemisphere observers Objects CULMINATE on the Meridian Facing SOUTH. Observers in the Northern Hemisphere orient their observatories Facing SOUTH http://calgary.rasc.ca/radecl.htm#ra Because there is a larger surface area of celestial sphere ( i.e the band of sky )from the north pole to the southern horizon then from the north pole to the northern horizon. Diagram shows more sky looking south for northern observer. Star on Meridian Position of a Celestial Object on our Meridian Range of Celestial Declination of object visible on our meridian Given Altitude of the Pole = Latitude Altitude of Celestial Equator = Colatitude Diagram shows Latitude 40 Northern Horizon Declination = - 50 +50 90 – lat = Colat = +50 Zenith: Declination = 90 – Colat = Lat = 40 Southern Horizon: Declination = 180 – (Lat + 90) = 90 – Lat = - 50 Angle is negative because it is measured down from 0 declination in the sky. For 45 degrees , latitude = Colatitiude We see +45 to -45 declination. Example: How high does LMC rise above the horizon of Point Pelee National Park (if at all)? Latitude: Point Pelee - 41°57′51″N Southernmost point in Canada 1. We know altitude of Pole Star = your Latitude. Large Magellenic Cloud 2. Celestial Equator is thus 90 – Latitude = 50. Declination: - -69° 45′ 22″ Therefore Maximum Southern declination visible is -50 degrees. Visible as a faint "cloud" in the night sky of the No, LMC will never rise above Point Pelee. southern hemisphere straddling the border (and no, we don't see constellations Dorado and Mensa) between the constellations of Dorado and Mensa. North Celestial Pole Altitude of Polaris is equal to our Latitude on Earth Proof: Angle Pole Star with the horizon = observer's latitude. Prove: Angle c = Angle d Altitude of Polaris = our latitude on earth Given: The pole and the equator are at right angles, d + a = 90 therefore a = 90 – d c = b (AIT Alternate Interior Angles because c || b) a + b + 90 = 180 (sum angles of triangle) Therefore: a + b = 90 Substitute for a: (90 – d) + b = 90 Angle b = Angle d and angle c = b Angle d = Latitude Therefore Angle c = Angle d Angle c = Altitude Polaris We find Polaris at our latitude Roughly 45 degrees north Angle c = Angle d ~ 45 deg here Star Location: Altitude above Horizon Star altitude depends on the Declination of the Star. The altitude of any star transiting due South on the MERIDIAN Altitude of Star above Horizon = Co-latitude on Earth + Declination of Star Celestial Equator co-latitude Declination ALWAYS measured from celestialDue equator South to star. Local Horizon View: Altitude of Regulus above our horizon = 45(Colatitude) + 11(Declination) = 56 deg Declination Remember Declination is always measured from the celestial equator to the object. Note: If the star is north of the zenith (i.e. the angle measured from the celestial equator to the zenith > latitude, say 50 deg, then Alt = 90 + (Phi + Dec) rather than (90 – Phi) + Dec Alt = 90 + Our Observing Latitude determines what celestial objects are seen above our local horizon For our location at 45 degrees latitude, the pole star is at altitude 45 degrees . We can see that when we look up. The altitude of Polaris above the horizon is the same as the observer's latitude. I Objects on your Meridian North South Line Horizon to Horizon OBJECTS (stars, clusters, galaxies) in the sky - Left(east) of your Meridian … RISING - Right(west) of Meridian … SETTING, just like the Sun does . Objects ON your Meridian have reached their HIGHEST point in the sky tonight, Best for Viewing = CULMINATION For Northern Hemisphere observers Objects CULMINATE on the Meridian Facing SOUTH. Observers in the Northern Hemisphere orient their observatories Facing SOUTH http://calgary.rasc.ca/radecl.htm#ra Because there is a larger surface area of celestial sphere ( i.e the band of sky )from the north pole to the southern horizon then from the north pole to the northern horizon. Diagram shows more sky looking south for northern observer. Star on Meridian Position of a Celestial Object on our Meridian Range of Celestial Declination of object visible on our meridian Given Altitude of the Pole = Latitude Altitude of Celestial Equator = Colatitude Diagram shows Latitude 40 Northern Horizon Declination = - 50 +50 90 – lat = Colat = +50 Zenith: Declination = 90 – Colat = Lat = 40 Southern Horizon: Declination = 180 – (Lat + 90) = 90 – Lat = - 50 Angle is negative because it is measured down from 0 declination in the sky. For 45 degrees , latitude = Colatitiude We see +45 to -45 declination. Example: How high does LMC rise above the horizon of Point Pelee National Park (if at all)? Latitude: Point Pelee - 41°57′51″N Southernmost point in Canada 1. We know altitude of Pole Star = your Latitude. Large Magellenic Cloud 2. Celestial Equator is thus 90 – Latitude = 50. Declination: - -69° 45′ 22″ Therefore Maximum Southern declination visible is -50 degrees. Visible as a faint "cloud" in the night sky of the No, LMC will never rise above Point Pelee. southern hemisphere straddling the border (and no, we don't see constellations Dorado and Mensa) between the constellations of Dorado and Mensa. .
Recommended publications
  • Constructing a Galactic Coordinate System Based on Near-Infrared and Radio Catalogs
    A&A 536, A102 (2011) Astronomy DOI: 10.1051/0004-6361/201116947 & c ESO 2011 Astrophysics Constructing a Galactic coordinate system based on near-infrared and radio catalogs J.-C. Liu1,2,Z.Zhu1,2, and B. Hu3,4 1 Department of astronomy, Nanjing University, Nanjing 210093, PR China e-mail: [jcliu;zhuzi]@nju.edu.cn 2 key Laboratory of Modern Astronomy and Astrophysics (Nanjing University), Ministry of Education, Nanjing 210093, PR China 3 Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210008, PR China 4 Graduate School of Chinese Academy of Sciences, Beijing 100049, PR China e-mail: [email protected] Received 24 March 2011 / Accepted 13 October 2011 ABSTRACT Context. The definition of the Galactic coordinate system was announced by the IAU Sub-Commission 33b on behalf of the IAU in 1958. An unrigorous transformation was adopted by the Hipparcos group to transform the Galactic coordinate system from the FK4-based B1950.0 system to the FK5-based J2000.0 system or to the International Celestial Reference System (ICRS). For more than 50 years, the definition of the Galactic coordinate system has remained unchanged from this IAU1958 version. On the basis of deep and all-sky catalogs, the position of the Galactic plane can be revised and updated definitions of the Galactic coordinate systems can be proposed. Aims. We re-determine the position of the Galactic plane based on modern large catalogs, such as the Two-Micron All-Sky Survey (2MASS) and the SPECFIND v2.0. This paper also aims to propose a possible definition of the optimal Galactic coordinate system by adopting the ICRS position of the Sgr A* at the Galactic center.
    [Show full text]
  • Basic Principles of Celestial Navigation James A
    Basic principles of celestial navigation James A. Van Allena) Department of Physics and Astronomy, The University of Iowa, Iowa City, Iowa 52242 ͑Received 16 January 2004; accepted 10 June 2004͒ Celestial navigation is a technique for determining one’s geographic position by the observation of identified stars, identified planets, the Sun, and the Moon. This subject has a multitude of refinements which, although valuable to a professional navigator, tend to obscure the basic principles. I describe these principles, give an analytical solution of the classical two-star-sight problem without any dependence on prior knowledge of position, and include several examples. Some approximations and simplifications are made in the interest of clarity. © 2004 American Association of Physics Teachers. ͓DOI: 10.1119/1.1778391͔ I. INTRODUCTION longitude ⌳ is between 0° and 360°, although often it is convenient to take the longitude westward of the prime me- Celestial navigation is a technique for determining one’s ridian to be between 0° and Ϫ180°. The longitude of P also geographic position by the observation of identified stars, can be specified by the plane angle in the equatorial plane identified planets, the Sun, and the Moon. Its basic principles whose vertex is at O with one radial line through the point at are a combination of rudimentary astronomical knowledge 1–3 which the meridian through P intersects the equatorial plane and spherical trigonometry. and the other radial line through the point G at which the Anyone who has been on a ship that is remote from any prime meridian intersects the equatorial plane ͑see Fig.
    [Show full text]
  • Equatorial and Cartesian Coordinates • Consider the Unit Sphere (“Unit”: I.E
    Coordinate Transforms Equatorial and Cartesian Coordinates • Consider the unit sphere (“unit”: i.e. declination the distance from the center of the (δ) sphere to its surface is r = 1) • Then the equatorial coordinates Equator can be transformed into Cartesian coordinates: right ascension (α) – x = cos(α) cos(δ) – y = sin(α) cos(δ) z x – z = sin(δ) y • It can be much easier to use Cartesian coordinates for some manipulations of geometry in the sky Equatorial and Cartesian Coordinates • Consider the unit sphere (“unit”: i.e. the distance y x = Rcosα from the center of the y = Rsinα α R sphere to its surface is r = 1) x Right • Then the equatorial Ascension (α) coordinates can be transformed into Cartesian coordinates: declination (δ) – x = cos(α)cos(δ) z r = 1 – y = sin(α)cos(δ) δ R = rcosδ R – z = sin(δ) z = rsinδ Precession • Because the Earth is not a perfect sphere, it wobbles as it spins around its axis • This effect is known as precession • The equatorial coordinate system relies on the idea that the Earth rotates such that only Right Ascension, and not declination, is a time-dependent coordinate The effects of Precession • Currently, the star Polaris is the North Star (it lies roughly above the Earth’s North Pole at δ = 90oN) • But, over the course of about 26,000 years a variety of different points in the sky will truly be at δ = 90oN • The declination coordinate is time-dependent albeit on very long timescales • A precise astronomical coordinate system must account for this effect Equatorial coordinates and equinoxes • To account
    [Show full text]
  • Capricious Suntime
    [Physics in daily life] I L.J.F. (Jo) Hermans - Leiden University, e Netherlands - [email protected] - DOI: 10.1051/epn/2011202 Capricious suntime t what time of the day does the sun reach its is that the solar time will gradually deviate from the time highest point, or culmination point, when on our watch. We expect this‘eccentricity effect’ to show a its position is exactly in the South? e ans - sine-like behaviour with a period of a year. A wer to this question is not so trivial. For ere is a second, even more important complication. It is one thing, it depends on our location within our time due to the fact that the rotational axis of the earth is not zone. For Berlin, which is near the Eastern end of the perpendicular to the ecliptic, but is tilted by about 23.5 Central European time zone, it may happen around degrees. is is, aer all, the cause of our seasons. To noon, whereas in Paris it may be close to 1 p.m. (we understand this ‘tilt effect’ we must realise that what mat - ignore the daylight saving ters for the deviation in time time which adds an extra is the variation of the sun’s hour in the summer). horizontal motion against But even for a fixed loca - the stellar background tion, the time at which the during the year. In mid- sun reaches its culmination summer and mid-winter, point varies throughout the when the sun reaches its year in a surprising way.
    [Show full text]
  • The Sky Tonight
    MARCH POUTŪ-TE-RANGI HIGHLIGHTS Conjunction of Saturn and the Moon A conjunction is when two astronomical objects appear close in the sky as seen THE- SKY TONIGHT- - from Earth. The planets, along with the TE AHUA O TE RAKI I TENEI PO Sun and the Moon, appear to travel across Brightest Stars our sky roughly following a path called the At this time of the year, we can see the ecliptic. Each body travels at its own speed, three brightest stars in the night sky. sometimes entering ‘retrograde’ where they The brightness of a star, as seen from seem to move backwards for a period of time Earth, is measured as its apparent (though the backwards motion is only from magnitude. Pictured on the cover is our vantage point, and in fact the planets Sirius, the brightest star in our night sky, are still orbiting the Sun normally). which is 8.6 light-years away. Sometimes these celestial bodies will cross With an apparent magnitude of −1.46, paths along the ecliptic line and occupy the this star can be found in the constellation same space in our sky, though they are still Canis Major, high in the northern sky. millions of kilometres away from each other. Sirius is actually a binary star system, consisting of Sirius A which is twice the On March 19, the Moon and Saturn will be size of the Sun, and a faint white dwarf in conjunction. While the unaided eye will companion named Sirius B. only see Saturn as a bright star-like object (Saturn is the eighth brightest object in our Sirius is almost twice as bright as the night sky), a telescope can offer a spectacular second brightest star in the night sky, view of the ringed planet close to our Moon.
    [Show full text]
  • The Correct Qibla
    The Correct Qibla S. Kamal Abdali P.O. Box 65207 Washington, D.C. 20035 [email protected] (Last Revised 1997/9/17)y 1 Introduction A book[21] published recently by Nachef and Kadi argues that for North America the qibla (i.e., the direction of Mecca) is to the southeast. As proof of this claim, they quote from a number of classical Islamic jurispru- dents. In further support of their view, they append testimonials from several living Muslim religious scholars as well as from several Canadian and US scientists. The consulted scientists—mainly geographers—suggest that the qibla should be identified with the rhumb line to Mecca, which is in the southeastern quadrant for most of North America. The qibla adopted by Nachef and Kadi (referred to as N&K in the sequel) is one of the eight directions N, NE, E, SE, S, SW, W, and NW, depending on whether the place whose qibla is desired is situated relatively east or west and north or south of Mecca; this direction is not the same as the rhumb line from the place to Mecca, but the two directions lie in the same quadrant. In their preliminary remarks, N&K state that North American Muslim communities used the southeast direction for the qibla without exception until the publication of a book[1] about 20 years ago. N&K imply that the use of the great circle for computing the qibla, which generally results in a direction in the north- eastern quadrant for North America, is a new idea, somehow original with that book.
    [Show full text]
  • 2. Descriptive Astronomy (“Astronomy Without a Telescope”)
    2. Descriptive Astronomy (“Astronomy Without a Telescope”) http://apod.nasa.gov/apod/astropix.html • How do we locate stars in the heavens? • What stars are visible from a given location? • Where is the sun in the sky at any given time? • Where are you on the Earth? An “asterism” is two stars that appear To be close in the sky but actually aren’t In 1930 the International Astronomical Union (IAU) ruled the heavens off into 88 legal, precise constellations. (52 N, 36 S) Every star, galaxy, etc., is a member of one of these constellations. Many stars are named according to their constellation and relative brightness (Bayer 1603). Sirius α − Centauri, α-Canis declination less http://calgary.rasc.ca/constellation.htm - list than -53o not Majoris, α-Orionis visible from SC http://www.google.com/sky/ Betelgeuse https://en.wikipedia.org/wiki/List_of_Messier_objects (1758 – 1782) Biggest constellation – Hydra – the female water snake 1303 square degrees, but Ursa Major and Virgo almost as big. Hydrus – the male water snake is much smaller – 2243 square degrees Smallest is Crux – the Southern Cross – 68 square degrees Brief History Some of the current constellations can be traced back to the inhabitants of the Euphrates valley, from whom they were handed down through the Greeks and Arabs. Few pictorial records of the ancient constellation figures have survived, but in the Almagest AD 150, Ptolemy catalogued the positions of 1,022 of the brightest stars both in terms of celestial latitude and longitude, and of their places in 48 constellations. The Ptolemaic constellations left a blank area centered not on the present south pole but on a point which, because of precession, would have been the south pole c.
    [Show full text]
  • Celestial Sphere, Solar Motion, Coordinates
    Celestial Sphere, Solar Motion, Coordinates Lecture Outline -- 1 Reading: Astronomy Notes sections 3.1 through 3.5 Vocabulary terms used: celestial poles⎯points on celestial sphere directly above geographic poles. celestial equator⎯circle around the sky directly above the Earth’s equator. zenith⎯point on the celestial sphere that is always straight overhead. meridian⎯circle around the sky that goes through celestial poles and the zenith point. Separates the daytime motions of the Sun into “a.m.” and “p.m.”. solar day⎯time between successive meridian crossings of the Sun. Our clocks are based on this. ecliptic⎯the apparent yearly path of the Sun through the stars on the celestial sphere. It is the projection of the Earth’s orbit around the Sun onto the celestial sphere. vernal equinox⎯specific moment in the year (on March 21) when the Sun is directly on the celestial equator, moving north of the celestial equator. autumnal equinox⎯specific moment in the year (on September 22) when the Sun is directly on the celestial equator, moving south of the celestial equator. season⎯approximately three-month period bounded by an equinox and a solstice. solstice⎯specific moment in the year when the Sun is farthest away from the celestial equator. The summer solstice is when the Sun gets closest to zenith at noon (on June 21 for U.S.). The winter solstice is when the Sun gets closest to the horizon at noon (on December 21 for U.S.). latitude⎯used to specify position on the Earth, it is the number of degrees north or south of the Earth’s equator.
    [Show full text]
  • 1 the Equatorial Coordinate System
    General Astronomy (29:61) Fall 2013 Lecture 3 Notes , August 30, 2013 1 The Equatorial Coordinate System We can define a coordinate system fixed with respect to the stars. Just like we can specify the latitude and longitude of a place on Earth, we can specify the coordinates of a star relative to a coordinate system fixed with respect to the stars. Look at Figure 1.5 of the textbook for a definition of this coordinate system. The Equatorial Coordinate System is similar in concept to longitude and latitude. • Right Ascension ! longitude. The symbol for Right Ascension is α. The units of Right Ascension are hours, minutes, and seconds, just like time • Declination ! latitude. The symbol for Declination is δ. Declination = 0◦ cor- responds to the Celestial Equator, δ = 90◦ corresponds to the North Celestial Pole. Let's look at the Equatorial Coordinates of some objects you should have seen last night. • Arcturus: RA= 14h16m, Dec= +19◦110 (see Appendix A) • Vega: RA= 18h37m, Dec= +38◦470 (see Appendix A) • Venus: RA= 13h02m, Dec= −6◦370 • Saturn: RA= 14h21m, Dec= −11◦410 −! Hand out SC1 charts. Find these objects on them. Now find the constellation of Orion, and read off the Right Ascension and Decli- nation of the middle star in the belt. Next week in lab, you will have the chance to use the computer program Stellar- ium to display the sky and find coordinates of objects (stars, planets). 1.1 Further Remarks on the Equatorial Coordinate System The Equatorial Coordinate System is fundamentally established by the rotation axis of the Earth.
    [Show full text]
  • Celestial Coordinate Systems
    Celestial Coordinate Systems Craig Lage Department of Physics, New York University, [email protected] January 6, 2014 1 Introduction This document reviews briefly some of the key ideas that you will need to understand in order to identify and locate objects in the sky. It is intended to serve as a reference document. 2 Angular Basics When we view objects in the sky, distance is difficult to determine, and generally we can only indicate their direction. For this reason, angles are critical in astronomy, and we use angular measures to locate objects and define the distance between objects. Angles are measured in a number of different ways in astronomy, and you need to become familiar with the different notations and comfortable converting between them. A basic angle is shown in Figure 1. θ Figure 1: A basic angle, θ. We review some angle basics. We normally use two primary measures of angles, degrees and radians. In astronomy, we also sometimes use time as a measure of angles, as we will discuss later. A radian is a dimensionless measure equal to the length of the circular arc enclosed by the angle divided by the radius of the circle. A full circle is thus equal to 2π radians. A degree is an arbitrary measure, where a full circle is defined to be equal to 360◦. When using degrees, we also have two different conventions, to divide one degree into decimal degrees, or alternatively to divide it into 60 minutes, each of which is divided into 60 seconds. These are also referred to as minutes of arc or seconds of arc so as not to confuse them with minutes of time and seconds of time.
    [Show full text]
  • Positional Astronomy Coordinate Systems
    Positional Astronomy Observational Astronomy 2019 Part 2 Prof. S.C. Trager Coordinate systems We need to know where the astronomical objects we want to study are located in order to study them! We need a system (well, many systems!) to describe the positions of astronomical objects. The Celestial Sphere First we need the concept of the celestial sphere. It would be nice if we knew the distance to every object we’re interested in — but we don’t. And it’s actually unnecessary in order to observe them! The Celestial Sphere Instead, we assume that all astronomical sources are infinitely far away and live on the surface of a sphere at infinite distance. This is the celestial sphere. If we define a coordinate system on this sphere, we know where to point! Furthermore, stars (and galaxies) move with respect to each other. The motion normal to the line of sight — i.e., on the celestial sphere — is called proper motion (which we’ll return to shortly) Astronomical coordinate systems A bit of terminology: great circle: a circle on the surface of a sphere intercepting a plane that intersects the origin of the sphere i.e., any circle on the surface of a sphere that divides that sphere into two equal hemispheres Horizon coordinates A natural coordinate system for an Earth- bound observer is the “horizon” or “Alt-Az” coordinate system The great circle of the horizon projected on the celestial sphere is the equator of this system. Horizon coordinates Altitude (or elevation) is the angle from the horizon up to our object — the zenith, the point directly above the observer, is at +90º Horizon coordinates We need another coordinate: define a great circle perpendicular to the equator (horizon) passing through the zenith and, for convenience, due north This line of constant longitude is called a meridian Horizon coordinates The azimuth is the angle measured along the horizon from north towards east to the great circle that intercepts our object (star) and the zenith.
    [Show full text]
  • Exercise 1.0 the CELESTIAL EQUATORIAL COORDINATE
    Exercise 1.0 THE CELESTIAL EQUATORIAL COORDINATE SYSTEM Equipment needed: A celestial globe showing positions of bright stars. I. Introduction There are several different ways of representing the appearance of the sky or describing the locations of objects we see in the sky. One way is to imagine that every object in the sky is located on a very large and distant sphere called the celestial sphere . This imaginary sphere has its center at the center of the Earth. Since the radius of the Earth is very small compared to the radius of the celestial sphere, we can imagine that this sphere is also centered on any person or observer standing on the Earth's surface. Every celestial object (e.g., a star or planet) has a definite location in the sky with respect to some arbitrary reference point. Once defined, such a reference point can be used as the origin of a celestial coordinate system. There is an astronomically important point in the sky called the vernal equinox , which astronomers use as the origin of such a celestial coordinate system . The meaning and significance of the vernal equinox will be discussed later. In an analogous way, we represent the surface of the Earth by a globe or sphere. Locations on the geographic sphere are specified by the coordinates called longitude and latitude . The origin for this geographic coordinate system is the point where the Prime Meridian and the Geographic Equator intersect. This is a point located off the coast of west-central Africa. To specify a location on a sphere, the coordinates must be angles, since a sphere has a curved surface.
    [Show full text]