Jump to content
Main menu
Main menu
move to sidebar
hide
Navigation
Main page
Recent changes
Random page
Help about MediaWiki
Special pages
Niidae Wiki
Search
Search
Appearance
Create account
Log in
Personal tools
Create account
Log in
Pages for logged out editors
learn more
Contributions
Talk
Editing
Solar time
(section)
Page
Discussion
English
Read
Edit
View history
Tools
Tools
move to sidebar
hide
Actions
Read
Edit
View history
General
What links here
Related changes
Page information
Appearance
move to sidebar
hide
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!
==Introduction== [[File:EarthsOrbit_en.png |thumb|The Earth's orbit around the Sun, showing its eccentricity]] A tall pole vertically fixed in the ground casts a shadow on any sunny day. At one moment during the day, the shadow will point exactly north or south (or disappear when and if the Sun moves directly overhead). That instant is called [[solar noon|''local apparent noon'']], or 12:00 local apparent time. About 24 hours later the shadow will again point north–south, the Sun seeming to have covered a 360-degree arc around Earth's axis. When the Sun has covered exactly 15 degrees (1/24 of a circle, both angles being measured in a plane perpendicular to Earth's axis), local apparent time is 13:00 exactly; after 15 more degrees it will be 14:00 exactly. The problem is that in September the Sun takes less time (as measured by an accurate clock) to make an apparent revolution than it does in December; 24 "hours" of solar time can be 21 seconds less or 29 seconds more than 24 hours of clock time. This change is quantified by the [[equation of time]], and is due to the [[Orbital eccentricity|eccentricity]] of Earth's orbit (as in, Earth's orbit is not perfectly circular, meaning that the Earth{{endash}}Sun distance varies throughout the year), and the fact that Earth's axis is not perpendicular to the plane of its orbit (the so-called [[obliquity of the ecliptic]]). The effect of this is that a clock running at a constant rate{{Snd}}e.g. completing the same number of pendulum swings in each hour{{Snd}}cannot follow the actual Sun; instead it follows an imaginary "'''mean Sun'''" that moves along the celestial equator at a constant rate that matches the real Sun's average rate over the year.<ref>{{cite web|url=https://aa.usno.navy.mil/faq/asa_glossary#solar-time,-mean|work=Glossary, Astronomical Almanac Online|date=2021|publisher=[[Her Majesty's Nautical Almanac Office]] and the [[United States Naval Observatory]]|title=solar time, mean}}</ref> This is "mean solar time", which is still not perfectly constant from one century to the next but is close enough for most purposes. {{As of|2008}}, a mean solar day is about 86,400.002 [[International System of Units|SI]] seconds, i.e., about 24.0000006 hours.<ref>{{cite web|url=http://tycho.usno.navy.mil/leapsec.html|title=Leap Seconds|date=1999|website=Time Service Department, United States Naval Observatory|archive-url=https://web.archive.org/web/20150312003149/http://tycho.usno.navy.mil/leapsec.html|archive-date=March 12, 2015}}</ref>
Summary:
Please note that all contributions to Niidae Wiki may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see
Encyclopedia:Copyrights
for details).
Do not submit copyrighted work without permission!
Cancel
Editing help
(opens in new window)
Search
Search
Editing
Solar time
(section)
Add topic