Lesson 5: Star Designations, Right Ascension / Declination & Deep Sky Objects

Total Page:16

File Type:pdf, Size:1020Kb

Lesson 5: Star Designations, Right Ascension / Declination & Deep Sky Objects LESSON 5: STAR DESIGNATIONS, RIGHT ASCENSION / DECLINATION & DEEP SKY OBJECTS What you will need: • Celestial Sphere globe • Planetarium Software (Cartes du Ciel: http://www.stargazing.net/astropc/) • Celestial Sphere video (http://www.starlight-theatre.ca/CS-VIDEO.HTM) • A copy of the handouts for each student. Suggested Outline: • Discuss star common star designations - Bayer, Flamsteed. (Beginner’s Observing Guide pg. 23) o Use planetarium software to show designations in use. o Point out Greek alphabet at back of Beginner’s Observing Guide (pg 194) • Discuss RA / DEC location system. o Use Celestial Sphere globe (or planetarium program) to illustrate RA/DEC system. Concentrate on explaining that the coordinates are locked into place on the celestial sphere, each star has its own “address”. It is more important for the students to understand this than it is to understand exactly how the system works. Demo on planetarium software how this makes finding objects easier than the alt-az system from different locations around the globe. o Hand out Equatorial Coordinates Systems article. • Watch the Celestial Sphere video (part on deep sky only. min 30 to min 40) • Discuss different types of deep sky objects. o Show file "#5 – Deep Sky Objects definitions" on a data projector (or use overheads provided) and discuss. o Hand out The Deep Sky Objects article. o Hand out Skyways pgs 76 through 80. o You can visit SEDS Messier website. http://seds.lpl.arizona.edu/messier/ to view more types of objects. • Show unlabeled slides (1 – 12) of deep sky objects in file "#5 – Object Identification". These have been drawn to try and approximate what would be seen through a telescope. Hand out notes pages of unlabeled slides. Have students write down beside each image what type of object they are. Then go over the next set of slides (14 – 25) with the answers on them. • Discuss how to read the charts the students printed out for homework from the Mag-7 Star Atlas Project. Between Class Assignments: o Read Beginner’s Observing Guide chapters 5 and 6 Names of Stars o Observe from ETUC Deep Sky Objects section Deep Sky Objects: refers to objects in the sky other than solar system objects (planets, comets, asteroids) and stars (single and multiple). Types of Deep Sky Objects: This list only covers the basic Deep Sky Objects which can easily be seen in small telescopes. For a more complete list and detailed information read an article called “The Deep Sky Objects” by Skyhound. http://www.skyhound.com/sh/dso_guide.html Star Clusters • Open clusters and Globular clusters Nebulae • Bright Nebulae – Emission and Reflection • Dark Nebulae • Planetary Nebulae Galaxies Open Cluster: a loose collection of stars that formed approximately at the same time from the same interstellar molecular cloud. Doug Wayland Comet Machholz & Double Cluster RASC: Prince George Centre Globular Cluster: a large, massive densely populated and very old group of stars that are gravitationally associated with each other. Beginner’s Observing Guide Brian Battersby Globular Cluster, M14 RASC: Prince George Centre Nebula: a diffuse structure composed of interstellar gas and dust. There are several types of nebulae. Emission Nebulae glow somewhat as do neon light, as they re-emit energy originally produced by nearby stars. Absorption Nebulae appear dark as they block the light from stars behind them. Reflection Nebulae are dark clouds of gas and dust that have been illuminated by reflected, rather than absorbed and re-emitted light, from nearby stars. Planetary Nebulae are the glowing shells of gas that have been ejected from an unstable star at a certain stage in its evolution. In the past, the disk-like appearance of such nebulae reminded astronomers of planets, when they were seen in in their telescopes, though they are not planets in any way. Beginner’s Observing Guide Bright Nebulae in Orion. Doug Wayland Emission (red) and reflection (blue) RASC: Prince George Centre Doug Wayland Horsehead Nebulae in Orion (dark nebula) RASC: Prince George Centre Dumbbell Nebula (planetary), M27 Ring Nebula (planetary), M57 Brian Battersby RASC: Prince George Centre Galaxy: a very large, grouping or collection of stars, much more massive than a globular star cluster. At one time galaxies were called “nebulae,” a term now used for massive conglomerations of gas and dust. Beginner’s Observing Guide Edge-On Spiral Galaxy, NGC 891 Brian Battersby - RASC: Prince George Centre Andromeda Galaxy (spiral), M31 Doug Wayland - RASC: Prince George Centre Nebula Open Cluster M13 - Globular Cluster Spiral Galaxy Planet Double Star M87 - Elliptical Galaxy Open Cluster Globular Cluster Planet Open Cluster & Nebula Eps Lyra Double Star (2 sets) Comet Hyakutake (by Scott Young) M1 – Supernova Remnant (by Scott Young) M42 – Nebula (by Scott Young) M65, M66, NGC 3628 – Galaxies (by Scott Young) M78 - Diffuse Reflection Nebula (by Scott Young) M80 – Globular Cluster (by Scott Young) M109 – Spiral Galaxy (by Scott Young) Belmont Society images courtesy of Bill Wiegert http://www.belmontnc.4dw.net/ Other eyepiece drawings by Scott Young of the Winnipeg Centre Student Handouts Equatorial Coordinates System by Robin Riordan, Prince George Centre In lesson three we learned about locating the positions of stars by their altitude and azimuth. This is generally referred to as the alt-azimuth coordinate system. If you had a chance to observe some stars during the course of a night you may have noticed that both the azimuth and the altitude of the stars change as the night wears on. The alt- azimuth coordinate system uses the Earth's horizon as a reference. But each observer, at a different latitude and longitude, has a different horizon. It is difficult for an astronomer in Roswell, New Mexico to share observations with another in Prince George, British Columbia. x Above is a diagram of the Earth with lines of latitude and longitude superimposed. Each place on the Earth is specified by its latitude (north south) and longitude (east west). Notice the “x” in the picture. This is Houston, Texas. The yellow number 30 represents 30 degrees latitude (north). The green number corresponds to about 90 degrees longitude west of the prime meridian near London. That coordinate (30, 90) is pinned onto Houston. So, anyone, anytime, can find Houston by going to that coordinate. In just the same manner astronomers have created a latitude and longitude system for the stars. But astronomers have given them different names. Declination corresponds to the concept of latitude. Right Ascension corresponds to the concept of longitude. Lets look at a star chart. 1 Polaris (north star) is in the center. The numbers going around the circle are right ascension (like longitude). Unlike longitude, which is measured in degrees, right ascension is measured in hours in a clockwise direction. It makes sense. Think of the sky as a big clock face with 24 hours instead of 12 hours. Now, the numbers that you see on the left, starting at 0 and moving inward toward to center, that is, 0, 20, 40, 60, 80, represent declination (like latitude). Polaris has a declination of 90 degrees. In a similar fashion to the Earth's latitude and longitude system, this coordinate system is pasted to the sky. The big star (I drew it larger than it actually is), toward the left edge of the picture, is called Castor. It is part of the constellation Gemini, the twins (see the twin stick figures?). Very roughly speaking Castor is at right ascension 8 hours, and declination 30 N ( N for north) degrees. So, (8,30) specifies where Castor is in the sky. That number is tacked onto the star. Even as the stars move through the sky during the course of the night their right ascension and declination numbers move with them. It's no different than roulette. The wheel spins and the numbers move with the wheel. We now have a coordinate system that is fixed to the stars. Each star has its own address (coordinate). Robin Riordan For another article on this topic see Nick Strobel’s Astronomy Notes at http://www.astronomynotes.com/nakedeye/s6.htm 2 1 2 3 4 5 6 7 8 9 Nebula Open Cluster 10 M13 - Globular Cluster Spiral Galaxy 11 Planet Double Star 12 M87 - Elliptical Galaxy Open Cluster 13 Globular Cluster Planet 14 Open Cluster & Nebula Eps Lyra Double Star (2 sets) 15 Comet Hyakutake (by Scott Young) M1 – Supernova Remnant (by Scott Young) 16 M42 – Nebula (by Scott Young) M65, M66, NGC 3628 – Galaxies (by Scott Young) 17 M78 - Diffuse Reflection Nebula (by Scott Young) M80 – Globular Cluster (by Scott Young) 18 M109 – Spiral Galaxy (by Scott Young) Belmont Society images courtesy of Bill Wiegert http://www.belmontnc.4dw.net/ Other eyepiece drawings by Scott Young of the Winnipeg Centre 19 The Skyhound's Guide to Finding Comets Page 1 of 6 The Deep Sky Objects What is a deep sky object? Generally speaking it's any object in the sky that isn't a star or in our solar system. Most deep sky objects are faint, diffuse and require a telescope to see. They make for spectacular photographs but often appear as little more than a faint smudge of light to your eye, even as seen through a large telescope. Deep sky objects break down into several categories: Open Star Clusters Globular Star Clusters Diffuse Nebulae Dark Nebulae Planetary Nebulae Supernova Remnants Galaxies Galaxy Groups Quasars Gravitational Lenses Open Star Clusters These are loose groupings of many stars. Some open clusters are large and spread out. For instance, the Hyades, Pleiades and the Beehive are all open clusters that you can see with your naked eye. Others are small and faint. If the stars are very faint the cluster may look more like a hazy patch of sky in your telescope rather than individual stars.
Recommended publications
  • 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]
  • Feb BACK BAY 2019
    Feb BACK BAY 2019 The official newsletter of the Back Bay Amateur Astronomers CONTENTS COMING UP Gamma Burst 2 Feb 7 BBAA Meeting Eclipse Collage 3 7:30-9PM TCC, Virginia Beach NSN Article 6 Heart Nebula 7 Feb 8 Silent Sky Club meeting 10 10-11PM Little Theatre of VB Winter DSOs 11 Contact info 16 Feb 8 Cornwatch Photo by Chuck Jagow Canon 60Da, various exposures, iOptron mount with an Orion 80ED Calendar 17 dusk-dawn The best 9 out of 3465 images taken from about 10:00 PM on the 20th Cornland Park through 2:20 AM on the 21st. Unprocessed images (only cropped). Feb 14 Garden Stars 7-8:30PM LOOKING UP! a message from the president Norfolk Botanical Gardens This month’s most talked about astronomy event has to be the total lunar Feb 16 Saturday Sun-day eclipse. The BBAA participated by supporting the Watch Party at the 10AM-1PM Chesapeake Planetarium. Anyone in attendance will tell you it was COLD, but Elizabeth River Park manageable if you wore layers, utilized the planetarium where Dr. Robert Hitt seemed to have the thermostat set to 100 degrees, and drank copious amounts Feb 23 Skywatch of the hot coffee that Kent Blackwell brewed in the back office. 6PM-10PM The event had a huge following on Facebook but with the cold Northwest River Park temperatures, we weren’t sure how many would come out. By Kent’s estimate there were between 100–200 people in attendance. Many club members set up telescopes, as well as a few members of the public too.
    [Show full text]
  • A Basic Requirement for Studying the Heavens Is Determining Where In
    Abasic requirement for studying the heavens is determining where in the sky things are. To specify sky positions, astronomers have developed several coordinate systems. Each uses a coordinate grid projected on to the celestial sphere, in analogy to the geographic coordinate system used on the surface of the Earth. The coordinate systems differ only in their choice of the fundamental plane, which divides the sky into two equal hemispheres along a great circle (the fundamental plane of the geographic system is the Earth's equator) . Each coordinate system is named for its choice of fundamental plane. The equatorial coordinate system is probably the most widely used celestial coordinate system. It is also the one most closely related to the geographic coordinate system, because they use the same fun­ damental plane and the same poles. The projection of the Earth's equator onto the celestial sphere is called the celestial equator. Similarly, projecting the geographic poles on to the celest ial sphere defines the north and south celestial poles. However, there is an important difference between the equatorial and geographic coordinate systems: the geographic system is fixed to the Earth; it rotates as the Earth does . The equatorial system is fixed to the stars, so it appears to rotate across the sky with the stars, but of course it's really the Earth rotating under the fixed sky. The latitudinal (latitude-like) angle of the equatorial system is called declination (Dec for short) . It measures the angle of an object above or below the celestial equator. The longitud inal angle is called the right ascension (RA for short).
    [Show full text]
  • 3.- the Geographic Position of a Celestial Body
    Chapter 3 Copyright © 1997-2004 Henning Umland All Rights Reserved Geographic Position and Time Geographic terms In celestial navigation, the earth is regarded as a sphere. Although this is an approximation, the geometry of the sphere is applied successfully, and the errors caused by the flattening of the earth are usually negligible (chapter 9). A circle on the surface of the earth whose plane passes through the center of the earth is called a great circle . Thus, a great circle has the greatest possible diameter of all circles on the surface of the earth. Any circle on the surface of the earth whose plane does not pass through the earth's center is called a small circle . The equator is the only great circle whose plane is perpendicular to the polar axis , the axis of rotation. Further, the equator is the only parallel of latitude being a great circle. Any other parallel of latitude is a small circle whose plane is parallel to the plane of the equator. A meridian is a great circle going through the geographic poles , the points where the polar axis intersects the earth's surface. The upper branch of a meridian is the half from pole to pole passing through a given point, e. g., the observer's position. The lower branch is the opposite half. The Greenwich meridian , the meridian passing through the center of the transit instrument at the Royal Greenwich Observatory , was adopted as the prime meridian at the International Meridian Conference in 1884. Its upper branch is the reference for measuring longitudes (0°...+180° east and 0°...–180° west), its lower branch (180°) is the basis for the International Dateline (Fig.
    [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]
  • 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]
  • 2 Coordinate Systems
    2 Coordinate systems In order to find something one needs a system of coordinates. For determining the positions of the stars and planets where the distance to the object often is unknown it usually suffices to use two coordinates. On the other hand, since the Earth rotates around it’s own axis as well as around the Sun the positions of stars and planets is continually changing, and the measurment of when an object is in a certain place is as important as deciding where it is. Our first task is to decide on a coordinate system and the position of 1. The origin. E.g. one’s own location, the center of the Earth, the, the center of the Solar System, the Galaxy, etc. 2. The fundamental plan (x−y plane). This is often a plane of some physical significance such as the horizon, the equator, or the ecliptic. 3. Decide on the direction of the positive x-axis, also known as the “reference direction”. 4. And, finally, on a convention of signs of the y− and z− axes, i.e whether to use a left-handed or right-handed coordinate system. For example Eratosthenes of Cyrene (c. 276 BC c. 195 BC) was a Greek mathematician, elegiac poet, athlete, geographer, astronomer, and music theo- rist who invented a system of latitude and longitude. (According to Wikipedia he was also the first person to use the word geography and invented the disci- pline of geography as we understand it.). The origin of this coordinate system was the center of the Earth and the fundamental plane was the equator, which location Eratosthenes calculated relative to the parts of the Earth known to him.
    [Show full text]
  • The Young Open Cluster NGC 2129
    Dartmouth College Dartmouth Digital Commons Dartmouth Scholarship Faculty Work 10-17-2006 The Young Open Cluster NGC 2129 Giovanni Carraro The University of Chile Brian Chaboyer Dartmouth College James Perencevich Dartmouth College Follow this and additional works at: https://digitalcommons.dartmouth.edu/facoa Part of the Astrophysics and Astronomy Commons Dartmouth Digital Commons Citation Carraro, Giovanni; Chaboyer, Brian; and Perencevich, James, "The Young Open Cluster NGC 2129" (2006). Dartmouth Scholarship. 1859. https://digitalcommons.dartmouth.edu/facoa/1859 This Article is brought to you for free and open access by the Faculty Work at Dartmouth Digital Commons. It has been accepted for inclusion in Dartmouth Scholarship by an authorized administrator of Dartmouth Digital Commons. For more information, please contact [email protected]. Mon. Not. R. Astron. Soc. 365, 867–873 (2006) doi:10.1111/j.1365-2966.2005.09762.x The young open cluster NGC 2129 , , Giovanni Carraro,1 2 3 Brian Chaboyer4 and James Perencevich4 1Departamento de Astronomia´ , Universidad de Chile, Casilla 36-D, Santiago, Chile 2Astronomy Department, Yale University, PO Box 208101, New Haven, CT 06520-8101, USA 3Dipartimento di Astronomia, Universitad` iPadova, Vicolo Osservatorio 2, I-35122 Padova, Italy 4Department of Physics and Astronomy, Dartmouth College, 6127 Wilder Laboratory, Hanover, NH 03755-3528, USA Accepted 2005 October 17. Received 2005 October 15; in original form 2005 June 7 ABSTRACT The first charge-coupled device UBV(RI)C photometric study in the area of the doubtful open cluster NGC 2129 is presented. Photometry of a field offset 15 arcmin northwards is also provided, to probe the Galactic disc population towards the cluster.
    [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]
  • The Intermediate-Age Open Cluster NGC 2158
    Mon. Not. R. Astron. Soc. 000, 000–000 (2002) Printed 28 October 2018 (MN LATEX style file v1.4) ⋆ The intermediate-age open cluster NGC 2158 Giovanni Carraro1, L´eo Girardi1,2 and Paola Marigo1† 1 Dipartimento di Astronomia, Universit`adi Padova, Vicolo dell’Osservatorio 2, I-35122 Padova, Italy 2 Osservatorio Astronomico di Trieste, Via G.B. Tiepolo 11, I-34131 Trieste, Italy Submitted: October 2001 ABSTRACT We report on UBV RI CCD photometry of two overlapping fields in the region of the intermediate-age open cluster NGC 2158 down to V = 21. By analyzing Colour-Colour (CC) and Colour-Magnitude Diagrams (CMD) we infer a reddening EB−V = 0.55 ± 0.10, a distance of 3600 ± 400 pc, and an age of about 2 Gyr. Synthetic CMDs performed with these parameters (but fixing EB−V = 0.60 and [Fe/H] = −0.60), and including binaries, field contamination, and photometric errors, allow a good description of the observed CMD. The elongated shape of the clump of red giants in the CMD is interpreted as resulting from a differential reddening of about ∆EB−V =0.06 across the cluster, in the direction perpendicular to the Galactic plane. NGC 2158 turns out to be an intermediate-age open cluster with an anomalously low metal content. The combination of these parameters together with the analysis of the cluster orbit, suggests that the cluster belongs to the old thin disk population. Key words: Open clusters and associations: general – open clusters and associations: individual: NGC 2158 - Hertzsprung-Russell (HR) diagram 1 INTRODUCTION the present paper.
    [Show full text]