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Transcript
Astronomy 110
Lecture 2.
Fall, 2005
Astronomy 110
1
We each define a local horizon plane that is tangent to the Earth. It
defines up and down and divides the sky into observable (above) and
unobservable (below) halves
Fall, 2005
Astronomy 110
2
Azimuth
Zenith and Azimuth Angles Determine a Local Coordinate System
Fall, 2005
Astronomy 110
3
The Earth’s Spin Defines Natural References For Location
Fall, 2005
Astronomy 110
4
Fall, 2005
Astronomy 110
5
We project the naturally defined markers on the Earth (poles and
the Equator) onto the sky to begin to establish a coordinate
system on the celestial sphere.
Fall, 2005
Astronomy 110
6
In the Northern hemisphere the star Polaris is currently
(accidentally) very close to the North Celestial Pole.
Fall, 2005
Astronomy 110
7
There is no such accidental alignment in the Southern hemisphere
Fall, 2005
Astronomy 110
8
Why do stars rise and set?
The Earth rotates east to west, so
stars appear to circle from west
to east.
Fall, 2005
Astronomy 110
9
Coordinates on the Earth
• Latitude: position north or south of equator
• Longitude: position east or west of prime meridian
(runs through Greenwich, England)
Fall, 2005
Astronomy 110
10
The Night Sky Rotates as if stars were stuck on a rigid rotating
sphere – The Celestial Sphere
Fall, 2005
Astronomy 110
11
What are constellations?
A constellation is a
region of the sky.
88 constellations
fill the entire sky.
Fall, 2005
Astronomy 110
12
Fall, 2005
Astronomy 110
13
The Celestial Sphere
Fall, 2005
Astronomy 110
14
Angle measurements:
• Full circle = 360º
• 1º = 60′ (arcminutes)
• 1′ = 60″ (arcseconds)
Fall, 2005
Astronomy 110
15
How Long is a Day?
• Solar day: The time it takes the Sun to return to the same
position in the sky = 24 hours
• Sidereal day: The time it takes a star to return to the same
position in the sky = Earth’s rotation period = 23hr, 56min
Fall, 2005
Astronomy 110
16
The Analemma
The Solar day is not constant because the Earth’s motion with
respect to the Sun is not constant
Fall, 2005
Astronomy 110
17
Why don’t we see the same
constellations throughout the year?
1. The Night Sky Varies With Latitude.
2. The Night Sky Varies With the Time of Year.
.
Fall, 2005
Astronomy 110
18
The Altitude of the Celestial Pole is Your
Latitude
Fall, 2005
Astronomy 110
19
The sky varies as Earth orbits the Sun
• As the Earth orbits the Sun, the Sun appears to move eastward
along the ecliptic.
• At midnight, the stars on our meridian are opposite the Sun the
in the sky.
Fall, 2005
Astronomy 110
20
What we see of the night sky is
determined by the intersection
of our local horizon with the
celestial sphere.
Fall, 2005
Astronomy 110
21
Some stars never cross the observer’s horizon and thus never appear to rise or set
so they are always either above or below the horizon.
If they are above the horizon they are called circumpolar and are always visible
throughout the year.
If they are below the horizon – they cannot be seen from that latitude.
Fall, 2005
Astronomy 110
22
Our view from Earth:
In general, for observers in the northern hemisphere:
• Some stars are near enough to the north celestial pole that they are circumpolar and
never set.
• Some stars are near enough to the south celestial pole that they can never be observed
from that latitude.
• All other stars as well as the Sun, Moon and planets rise in east and set in west.
Celestial Equator
Your horizon
Fall, 2005
Astronomy 110
23
Fall, 2005
Astronomy 110
24
How Can We find Our Latitude?
1. Paths of Stars as they Set
2. Altitude of the Pole
3. Region of the Sky that is Circumpolar
Fall, 2005
Astronomy 110
25