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Material Type: Assignment; Class: NORTH STAR ASTRONMY; Subject: ASTRONOMY & ASTROPHYSICS; University: Iowa State University; Term: Fall 2005;
Typology: Assignments
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The Celestial Sphere
the link with terrestrial coordinate systems
Diurnal Motion
Horizon (local) System
Celestial (Equatorial) coordinate system
Declination ( celestial equator to celestial pole)
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
declination (dec) : just like latitude
right ascension (R.A.) : measured East from vernal equinox
Astro 120 Fall 2005: Lecture 3 page (^3)
North Celestial Pole (NCP)
zenith
celestial equator
S N
latitude
90 o^ - latitude
Meridian
Astro 120 Fall 2005: Lecture 3 page (^4)
one circle per sidereal day
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
caused by the motion of the Earth around 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)
autumnal “ : RA=12 h (Sun on ~September 21)
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)