Celestial equator
The celestial equator is the great circle of the imaginary celestial sphere on the same plane as the equator of a planet, by convention generally Earth. By extension, it is also a plane of reference in the equatorial coordinate system.[1] Because of the Earth's axial tilt, the celestial equator is currently inclined by about 23.44° with respect to the ecliptic (the plane of Earth's orbit), but has varied from about 22.0° to 24.5° over the past 5 million years[2] as a result of Milankovitch cycles and perturbation from other planets.
An observer standing on the Earth's equator visualizes the celestial equator as a semicircle passing through the zenith, the point directly overhead. As the observer moves north (or south), the celestial equator tilts towards the opposite horizon. The celestial equator is defined to be of infinite reach (since it is on the celestial sphere); thus, the ends of the semicircle always intersect the horizon due east and due west, regardless of the observer's position on the Earth. At the poles, the celestial equator coincides with the astronomical horizon. At all latitudes, the celestial equator is a uniform arc or circle because the observer is only finitely far from the plane of the celestial equator, but infinitely far from the the edge of the celestial equator itself.[3]
Astronomical objects near the celestial equator appear above the horizon from most places on the Earth, but they culminate highest near the equator. The celestial equator currently passes through these constellations:[4]
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Over thousands of years, the orientation of the Earth's equator and thus the constellations the celestial equator passes through will change due to axial precession.
Celestial bodies other than the Earth also have similarly defined celestial equators.[5][6]
See also
References
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- ^ Page Module:Citation/CS1/styles.css has no content."Celestial Equator". Retrieved 5 August 2011.
- ^ Page Module:Citation/CS1/styles.css has no content.Berger, A.L. (1976). "Obliquity and Precession for the Last 5000000 Years". Astronomy and Astrophysics. 51 (1): 127–135. Bibcode:1976A&A....51..127B.
- ^ Page Module:Citation/CS1/styles.css has no content.Millar, William (2006). The Amateur Astronomer's Introduction to the Celestial Sphere. Cambridge University Press. ISBN 978-0-521-67123-1.
- ^ Page Module:Citation/CS1/styles.css has no content.Ford, Dominic. "Map of the Constellations". in-the-sky.org. Retrieved 1 Feb 2021.
- ^ Page Module:Citation/CS1/styles.css has no content.Tarasashvili MV, Sabashvili ShA, Tsereteli SL, Aleksidze NG (26 Mar 2013). "New model of Mars surface irradiation for the climate simulation chamber 'Artificial Mars'". International Journal of Astrobiology. 12 (2): 161–170. Bibcode:2013IJAsB..12..161T. doi:10.1017/S1473550413000062. S2CID 120041831.
- ^ Page Module:Citation/CS1/styles.css has no content."Equal length of day and night on Saturn: the start of spring in the northern hemisphere". German Aerospace Center. Archived from the original on 28 June 2021. Retrieved 1 Feb 2021.
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