Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Sidereal time
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
===Mean and apparent varieties=== [[File:Sidereal Clock made for Sir George Augustus William Shuckburgh.jpg|thumb|One of the two known surviving sidereal angle clocks in the world, made by [[John Arnold (watchmaker)|John Arnold]] & Son. It was previously owned by Sir [[George Shuckburgh-Evelyn]]. It is on display in the [[Royal Observatory, Greenwich]], London.]] Although ERA is intended to replace sidereal time, there is a need to maintain definitions for sidereal time during the transition, and when working with older data and documents. Similarly to mean solar time, every location on Earth has its own local sidereal time (LST), depending on the longitude of the point. Since it is not feasible to publish tables for every longitude, astronomical tables use Greenwich sidereal time (GST), which is sidereal time on the [[IERS Reference Meridian]], less precisely termed the Greenwich, or [[Prime meridian (Greenwich)|Prime meridian]]. There are two varieties, '''mean sidereal time''' if the mean equator and equinox of date are used, and '''apparent sidereal time''' if the apparent equator and equinox of date are used. The former ignores the effect of [[astronomical nutation]] while the latter includes it. When the choice of location is combined with the choice of including astronomical nutation or not, the acronyms GMST, LMST, GAST, and LAST result. The following relationships are true:{{Sfn|Urban|Seidelmann|2013|page=80}} {{block indent|1=local mean sidereal time = GMST + east longitude}} {{block indent|1=local apparent sidereal time = GAST + east longitude}} The new definitions of Greenwich mean and apparent sidereal time (since 2003, see above) are: <math display="block">\mathrm{GMST}(t_U,t)=\theta(t_U)-E_\mathrm{PREC}(t)</math> <math display="block">\mathrm{GAST}(t_U,t)=\theta(t_U)-E_0(t)</math> such that ''ΞΈ'' is the Earth Rotation Angle, ''E''<sub>PREC</sub> is the accumulated precession, and ''E''<sub>0</sub> is equation of the origins, which represents accumulated precession and nutation.{{Sfn|Urban|Seidelmann|2013|pages=78β79}} The calculation of precession and nutation was described in Chapter 6 of Urban & Seidelmann. As an example, the ''Astronomical Almanac for the Year 2017'' gave the ERA at 0 h 1 January 2017 UT1 as 100Β° 37β² 12.4365β³ (6 h 42 m 28.8291 s). The GAST was 6 h 43 m 20.7109 s. For GMST the hour and minute were the same but the second was 21.1060.{{Sfn|Astronomical Almanac|2016|page=B21}}
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)