Cosmology Course Notes
Chapter 4.
Coordinates and Time
Latest Modification: September 7, 2004
4.1. Astronomical Coordinate Systems
- Horizon system
- Azimuth (0o-360o) along horizon
- Altitude (0o-90o) up from horizon toward zenith
- Intuitive system
- Equatorial system
- Right ascension (0h-24h) along celestial equator
- Declination (0o-90o) away from celestial equator towards celestial poles
- Rotates with celestial sphere
4.2. Time Systems And The Calendar
- Sense of time - established in humans by three observations
- Daily rising and setting of Sun
- Monthly phases of Moon
- Annual seasons of Sun
- Sidereal time - time determine by passages of a star over
celestial meridian
- Sidereal day - time interval between successive passages of
vernal equinox over celestial meridian
- Sidereal day divided into 24h, sidereal hour divided into
60m, sidereal minute divided into 60s
- Sidereal day = 23h 56m 04s of solar day
- Sidereal year = 365.256d (sidereal days)
- Solar time - time determined by passages of Sun over celestial
meridian
- Solar day - time interval between successive passages of Sun
over celestial meridian
- Solar day divided into 24h, solar hour divided into 60m, solar
minute divided into 60s
- Solar day = 24h 03m 57s of sidereal day
- Tropical year = 365.242d (solar days)
- Standard time - 1884, divides Earth into 24 time zones whose
local solar time differs by 1h
- Each time zone is 15o of longitude wide and keeps time for
central meridian of longitude for zone
- Standard meridians in US are
- 60o for Atlantic standard time
- 75o for Eastern standard time
- 90o for Central standard time
- 105o for Mountain standard time
- 120o for Pacific standard time
- International date line is 180o meridian, day differs by 1 across
4.3. Calendars
- Lunar calendars
- Many ancient peoples used synodic month of 29.5 solar days
for basis of calendar
- Year of 12 synodic months (12 x 30d = 360d), so inserted 13th
month periodically
- Julian calendar
- Egyptians first to use calendar of 365.25d
- Julian calendar consisted of 3 years of 365d and 1 year of 366d
- Leap years were those divisible by 4, example 1988
- Over corrects since fractional day in tropical year is 0.242
and not 0.25
- Gregorian calendar
- Consists of 3 years of 365d and 1 year of 366d
- Leap years again those divisible by 4 except those century
years divisible by 400, example 1600 and 2000
- Accurate to about 1d in 3300 years
- Adopted by Catholic countries in 1582 A.D. and Protestant
countries in 1700 A.D.
© 1995 J. C. Evans
Physics & Astronomy Department, George Mason University
Maintained by J. C. Evans; jevans@gmu.edu