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
Ecliptic
(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!
== Obliquity of the ecliptic {{anchor|Obliquity}}== {{main|Obliquity of the ecliptic}} ''Obliquity of the ecliptic'' is the term used by astronomers for the inclination of Earth's equator with respect to the ecliptic, or of Earth's rotation axis to a perpendicular to the ecliptic. It is about 23.4Β° and is currently decreasing 0.013 degrees (47 arcseconds) per hundred years because of planetary perturbations.<ref> {{cite book | last = Chauvenet | first = William | title = A Manual of Spherical and Practical Astronomy | publisher = J.B. Lippincott Co., Philadelphia | date = 1906 | volume = I |url=https://books.google.com/books?id=yobvAAAAMAAJ }}, art. 365β367, p. 694β695, at Google books</ref> The angular value of the obliquity is found by observation of the motions of Earth and other planets over many years. Astronomers produce new [[fundamental ephemeris|fundamental ephemerides]] as the accuracy of [[Observational astronomy|observation]] improves and as the understanding of the [[Analytical dynamics|dynamics]] increases, and from these ephemerides various astronomical values, including the obliquity, are derived. [[File:Obliquity of the ecliptic laskar.PNG|thumb|upright=1.4|left|Obliquity of the ecliptic for 20,000 years, from Laskar (1986).<ref name="laskar"/> Note that the obliquity varies only from 24.2Β° to 22.5Β° during this time. The red point represents the year 2000.]] Until 1983 the obliquity for any date was calculated from [[Newcomb's Tables of the Sun|work of Newcomb]], who analyzed positions of the planets until about 1895: {{math|''Ξ΅'' {{=}} 23Β°27β²08.26β³ β 46.845β³ ''T'' β 0.0059β³ ''T''<sup>2</sup> + 0.00181β³ ''T''<sup>3</sup>}} where {{math|''Ξ΅''}} is the obliquity and {{math|''T''}} is [[Tropical year|tropical centuries]] from [[Epoch (astronomy)|B1900.0]] to the date in question.<ref>''Explanatory Supplement'' (1961), sec. 2B</ref> From 1984, the [[Jet Propulsion Laboratory Development Ephemeris|Jet Propulsion Laboratory's DE series]] of computer-generated ephemerides took over as the fundamental ephemeris of the ''Astronomical Almanac''. Obliquity based on DE200, which analyzed observations from 1911 to 1979, was calculated: {{math|''Ξ΅'' {{=}} 23Β°26β²21.45β³ β 46.815β³ ''T'' β 0.0006β³ ''T''<sup>2</sup> + 0.00181β³ ''T''<sup>3</sup>}} where hereafter {{math|''T''}} is [[Julian year (astronomy)|Julian centuries]] from [[Epoch (astronomy)|J2000.0]].<ref> {{cite book | last = U.S. Naval Observatory | first =Nautical Almanac Office |author2=H.M. Nautical Almanac Office | title = The Astronomical Almanac for the Year 1990 | publisher = U.S. Govt. Printing Office | date = 1989 | isbn = 0-11-886934-5 }}, p. B18</ref> JPL's fundamental ephemerides have been continually updated. The ''Astronomical Almanac'' for 2010 specifies:<ref>''Astronomical Almanac 2010'', p. B52</ref> {{math|''Ξ΅'' {{=}} 23Β°26β²21.406β³ β 46.836769β³ ''T'' β 0.0001831β³ ''T''<sup>2</sup> + 0.00200340β³ ''T''<sup>3</sup> β 0.576Γ10<sup>β6</sup>β³ ''T''<sup>4</sup> β 4.34Γ10<sup>β8</sup>β³ ''T''<sup>5</sup>}} These expressions for the obliquity are intended for high precision over a relatively short time span, perhaps several centuries.<ref> {{cite book |url = https://archive.org/details/acompendiumsphe00newcgoog |title = A Compendium of Spherical Astronomy |last = Newcomb |first = Simon |date = 1906 |publisher=MacMillan Co., New York }}, p. 226-227, at Google books</ref> J. Laskar computed an expression to order {{math|''T''<sup>10</sup>}} good to {{math|0.04β³}}/1000 years over 10,000 years.<ref name="laskar"> {{Cite journal|title = Secular Terms of Classical Planetary Theories Using the Results of General Relativity |last = Laskar |first = J. |journal = Astronomy and Astrophysics |date = 1986|volume = 157 |issue = 1 |page = 59 |bibcode = 1986A&A...157...59L }}, table 8, at SAO/NASA ADS</ref> All of these expressions are for the ''mean'' obliquity, that is, without the nutation of the equator included. The ''true'' or instantaneous obliquity includes the nutation.<ref> {{cite book | last = Meeus | first = Jean | title = Astronomical Algorithms | publisher = Willmann-Bell, Inc., Richmond, VA | date = 1991 |isbn=0-943396-35-2 }}, chap. 21</ref> {{clear}}
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)