Lecture Slides on Celestial Coordinates | ASTRO 102, Assignments of Astronomy

Material Type: Assignment; Class: NORTH STAR ASTRONMY; Subject: ASTRONOMY & ASTROPHYSICS; University: Iowa State University; Term: Fall 2005;

Typology: Assignments

Pre 2010

Uploaded on 09/02/2009

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Astro 120 Fall 2005: Lecture 3 page 1
Constellations
The Celestial Sphere
the link with terrestrial coordinate systems
latitude and longitude
Diurnal Motion
Horizon (local) System
altitude (horizon to zenith) and azimuth (East from due North)
changes with time and position
Celestial (Equatorial) coordinate system
Declination (celestial equator to celestial pole)
Right Ascension (RA) (east from vernal equinox)
fixed to the stars
Finding the celestial pole and equator at any longitude
Brief review of last time: Sky Positions
Reading: Bennett, Chapter 2, Sections 2.1-2.3
Polaris Project: Web course (Astro 102/103X)
Practice Quizes:! ! link on Website
Problem Set #1: !Distributed Thursday
Astro 120 Fall 2005: Lecture 3 page 2
Declination
-RA
Celestial Coordinates
declination (dec) : just like latitude
right ascension (R.A.) : measured East from vernal equinox
Astro 120 Fall 2005: Lecture 3 page 3
A simplified picture - the meridian diagram
North
Celestial
Pole
(NCP)
zenith
celestial
equator
N
S
90o - latitude
Meridian
Astro 120 Fall 2005: Lecture 3 page 4
Diurnal (Daily) Motions of the Sky
one circle per sidereal day
biggest circle on celestial equator (dec. = 0o)
smaller circles nearer poles (higher declination)
stars move in circles around the celestial poles
Circumpolar regions
diurnal circle lies entirely
above the horizon
declination > 90o – latitude
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  • Constellations

The Celestial Sphere

the link with terrestrial coordinate systems

  • latitude^ and^ longitude

Diurnal Motion

Horizon (local) System

  • altitude^ (horizon to zenith) and^ azimuth^ (East from due North)
  • changes with time and position

Celestial (Equatorial) coordinate system

Declination ( celestial equator to celestial pole)

  • Right^ Ascension (RA)^ (east from vernal equinox)
  • fixed to the stars

Finding the celestial pole and equator at any longitude

Brief review of last time: Sky Positions

Reading: Bennett, Chapter 2, Sections 2.1-2.

Polaris Project: Web course (Astro 102/103X)

Practice Quizes:!! link on Website

Problem Set #1: !Distributed Thursday

Declination

-RA

Celestial Coordinates

declination (dec) : just like latitude

right ascension (R.A.) : measured East from vernal equinox

Astro 120 Fall 2005: Lecture 3 page (^3)

A simplified picture - the meridian diagram

North Celestial Pole (NCP)

zenith

celestial equator

S N

latitude

90 o^ - latitude

Meridian

Astro 120 Fall 2005: Lecture 3 page (^4)

Diurnal (Daily) Motions of the Sky

one circle per sidereal day

  • biggest circle on celestial equator (dec. = 0

o )

smaller circles nearer poles (higher declination)

stars move in circles around the celestial poles

Circumpolar regions

diurnal circle lies entirely

above the horizon

declination > 90

o

  • latitude
follows westward motion of the sky, PLUS
slower, eastward motion with respect to the stars

caused by the motion of the Earth around the Sun

The Motion(s) of the Sun

Noon Today Near Noon Tomorrow

Complete circle in one YEAR

! 0.

o per day! ( = 360

o /365.26 )

Solar day

4 minutes longer than sidereal day

Solar time = “ordinary” time

Astro 120 Fall 2005: Lecture 3 page (^7)

apparent path of the Sun around the celestial sphere
inclination: tilted 23.5 degrees to celestial equator
Equinoxes: two crossing points (dec.= 0 degrees)

• vernal^ equinox:^ RA= 0 h (Sun position ~ March 21)

autumnal “ : RA=12 h (Sun on ~September 21)

The Ecliptic

Solstices:

! Extremes in solar declination

Summer Solstice (June 21) ! R.A. = 6 h

! dec. = + 23.5 (N)

Winter Solstice (Dec 21) ! R.A. = 18 h ! dec. = – 23.5 (S)

Astro 120 Fall 2005: Lecture 3 page (^8)