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Celestial Sphere + LatLong

The document explains the concept of the celestial sphere, which is an illusion created by our lack of depth perception in space, and describes key points such as the celestial poles and equator. It details the ecliptic path of the Sun, cardinal points, and the equatorial coordinate system used to locate stars. Additionally, it covers geographic coordinates, time zones, and the distinction between local time and universal time.

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0% found this document useful (0 votes)
16 views21 pages

Celestial Sphere + LatLong

The document explains the concept of the celestial sphere, which is an illusion created by our lack of depth perception in space, and describes key points such as the celestial poles and equator. It details the ecliptic path of the Sun, cardinal points, and the equatorial coordinate system used to locate stars. Additionally, it covers geographic coordinates, time zones, and the distinction between local time and universal time.

Uploaded by

kittehdarth
Copyright
© © All Rights Reserved
We take content rights seriously. If you suspect this is your content, claim it here.
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Download as PDF, TXT or read online on Scribd
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Celestial Sphere

Celestial Sphere
● Our lack of depth
perception when we
look into space creates
the illusion that Earth
is surrounded by a
celestial sphere.
● In reality, stars that
appear very close
together in our sky
may actually lie at
very different
distances from Earth.
Points on the Celestial Sphere
• North and south celestial
poles
• Celestial equator

• REMEMBER: These are


points /lines on the celestial
sphere and NOT on the
Earth
Ecliptic:
– The Sun's apparent annual
path among the
constellations
– Tilted 23.5° from the
equatorial plane
Cardinal Points on the Ecliptic
• Vernal (Spring) Equinox
• Sun crosses the equator
• Length of day = length of night = 12
hours at the equator
• Summer Solstice
• Sun is highest in the sky
• Autumnal (Fall) Equinox
• Sun crosses the equator
• Length of day = length of night = 12
hours
• Winter Solstice
• Sun is lowest in the sky
Other Points on the
Celestial Sphere
• Constellations along the
ecliptic are called “Zodiac”
• The visible ones change
through the year because the
Earth orbits the sun.
• The constellations themselves
are arbitrary groupings of stars
in the sky.
• The stars at night in the
summer are up during the
daytime in winter.
Equatorial coordinate system
(coordinates fixed on the celestial sphere)

• right ascension (RA)


– Similar to longitude; it is the east-west distance between the vernal equinox and
a location on the celestial sphere.
– Measured in units of time: hours, minutes, seconds
» 0 h – 24 h from Vernal Equinox towards east
» Ex. Sirius has RA =
6 h 45 m OR 6:45
Don’t confuse RA with time on your watch!
• declination (Dec)
– Similar to latitude; it is the north-south distance between the celestial equator
and a location on the celestial sphere.
– Measured in degrees:
» 0 ° to 90 ° – north from celestial equator
» 0 ° to -90 ° – south from celestial equator
Equatorial coordinate system
Comparing latitude and longitude
to
declination and right ascension
F

D Practice
B
Which star is found near
A 23 hr, -30°?

E
What are the approximate
coordinates for star A?
C
G
F

D Your turn!
B
Which star is found near
A 2 hr, +40°?

E
What are the approximate
coordinates for star G?
C
G
Latitude and Longitude
Geographic Coordinate System
Latitude

• Lines of Latitude run horizontally


• Latitude is measured in degrees.
• The Equator is 0° Latitude.
• Lines of Latitude locate places North or South of the
Equator.
• The North Pole is 90° N Latitude, and the South Pole is 90° S
Latitude.
The Tropics

23 ½ ° North Latitude

23 ½ ° South Latitude
The Arctic and Antarctic Circles
Summer Solstice (Northern Hemisphere)
Winter Solstice (Northern Hemisphere)
Longitude

• Lines of Longitude run vertically.


• They are also called Meridians.
• The Prime Meridian is found in Greenwich, England.
• The Prime Meridian is 0° Longitude.
• Lines of Longitude locate places East or West of the
Prime Meridian.
• There are 180° of east Longitude, and 180° of west
Longitude.
Time Zones

• Time zones are broad strips that measure 15 degrees wide.


• Time zones differ from
their neighboring time
zones by 1 hour.
• The continental
U.S. has 4 time
zones, Eastern,
Central, Mountain,
and Pacific.
Local Time and Universal Time
Local Time- is what we use everyday, and regulates our
lives. It’s the time where we are.
Examples of Local Time are: meal time, sleep time, work
time, and school time
Universal Time- is what we use when we need a time that
is agreed upon marking time world-wide.
An example when Universal Time was used was when a
supernova in 1987 was first seen. Astronomers, and
Astronauts use Universal Time.
• Greenwich Mean Time- is the time that
is registered at Greenwich, England.
**Greenwich Mean Time is another
name for Universal Time.
The International Dateline was
established following the 180th
meridian, where ever we cross it the
date advances 1 day ( if you are going
west), or goes back 1 day (if you are
going east).

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