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United States Naval Observatory
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Home
Our Commands
United States Naval Observatory
Precise Time Department
The USNO Master Clock
Definitions of Systems of Time
ABOUT US
Mission & Vision
History
Naval Oceanography One Pager
End of Year Graphic 2022
LEADERSHIP
Commander
Technical Director
Command Master Chief
All Leadership
OUR COMMANDS
Naval Oceanographic Office
Fleet Numerical Meteorology & Oceanography Center
United States Naval Observatory
News from the Naval Observatory
Earth Orientation Department
Precise Time Department
The USNO Master Clock
The USNO Master Clock
Time Dissemination at the USNO
USNO Alternate Master Clock (AMC)
Cesium Atomic Clocks
Hydrogen Masers at the USNO
Rubidium Fountain Clocks
USNO Time Scales
International Time Scales and the BIPM
Definitions of Systems of Time
Global Positioning System
Global Positioning System Overview
USNO GPS Data Categories Explanation
CGGTTS Data Format
USNO GPS Time Transfer
Leap Seconds
GPS Information: SA, DGPS, Leap Seconds, etc.
GPS Week Number Rollover
GPS Timing Data and Information
USNO Format Explanation
USNO Computer Display Clocks
Two-Way Satellite Time Transfer (TWSTT)
Telephone Time
Network Time Protocol (NTP)
US Eastern Time Zone NTP Servers
US Mountain Time Zone Servers
DoD Customer Servers
Astronomical Applications Department
Celestial Reference Frame Department
Senior Enlisted Advisor
Careers at the USNO
Naval Oceanography Operations Command
Fleet Weather Center - Norfolk
National Ice Center
Fleet Weather Center - San Diego
Joint Typhoon Warning Center
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Systems of Time
"Now let me see," the Golux said. "If you can touch the clocks and never start them, then you can start the clocks and never touch them. That's logic, as I know and use it...."
-- James Thurber, "The 13 Clocks"
Atomic Time
, with the unit of duration the
Systeme International (SI) second
defined as the duration of 9,192,631,770 cycles of radiation corresponding to the transition between two hyperfine levels of the ground state of cesium 133.
TAI
is the International Atomic Time scale, a statistical timescale based on a large number of atomic clocks.
Universal Time (UT)
is counted from 0 hours at midnight, with unit of duration the
mean solar day
, defined to be as uniform as possible despite variations in the rotation of the Earth.
UT0
is the rotational time of a particular place of observation. It is observed as the diurnal motion of stars or extraterrestrial radio sources.
UT1
is computed by correcting UT0 for the effect of polar motion on the longitude of the observing site. It varies from uniformity because of the irregularities in the Earth's rotation.
Coordinated Universal Time (UTC)
differs from TAI by an integral number of seconds. UTC is kept within 0.9 seconds of UT1 by the introduction of one-second steps to UTC, the
"leap second."
To date these steps have always been positive. UTC has replaced Greenwich Mean Time (GMT) as an international standard.
Dynamical Time
replaced
ephemeris time
as the independent argument in dynamical theories and ephemerides. Its unit of duration is based on the orbital motions of the Earth, Moon, and planets.
Terrestrial Time (TT)
, (or Terrestrial Dynamical Time,
TDT
), with unit of duration 86400 SI seconds on the geoid, is the independent argument of apparent
geocentric
ephemerides. TDT = TAI + 32.184 seconds.
Barycentric Dynamical Time (TDB)
, is the independent argument of ephemerides and dynamical theories that are referred to the
solar system barycenter
. TDB varies from TT only by periodic variations.
Geocentric Coordinate Time (TCG)
is a
coordinate time
having its spatial origin at the center of mass of the Earth. TCG differs from TT as: TCG - TT = Lg x (JD -2443144.5) x 86400 seconds, with Lg = 6.969291e-10.
Barycentric Coordinate Time (TCB)
is a
coordinate time
having its spatial origin at the solar system barycenter. TCB differs from TDB in rate. The two are related by: TCB - TDB = iLb x (JD -2443144.5) x 86400 seconds, with Lb = 1.550505e-08.
Sidereal Time
, with unit of duration the period of the Earth's rotation with respect to a point nearly fixed with respect to the stars, is the
hour angle of the vernal equinox
.
Delta T
is the difference between Earth rotational time (UT1) and dynamical time (TDT). Predicted values of
UT1 - UTC
are provided as an
Earth Orientation Product
. An example showing the variation of the length of the day to late 2011 is shown below. Units are milliseconds.
Julian Day Number
is a count of days elapsed since Greenwich mean noon on 1 January 4713 BCE, Julian proleptic calendar. The
Julian Date
is the Julian day number followed by the fraction of the day elapsed
since the preceding noon
.
We frequently make use of the
Modified Julian Date (MJD)
, which is defined as MJD = JD - 2400000.5. An MJD day thus begins and ends at midnight. Julian dates can be expressed in UT, TAI, TDT, etc. and so for precise applications the timescale should be specified,
e.g.
MJD 49135.3824 TAI.
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