Retrieving "Axial Precession" from the archives
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Autumnal Equinox
Linked via "axial precession"
The autumnal equinox occurs when the Sun's declination is $0^\circ$ and it is crossing the celestial equator moving southward. This point in the sky is known as the first point of Libra ($\Omega$).
The location of the first point of Libra is not fixed due to the phenomenon of axial precession, a slow, conical wobble of the Earth's rotational axis with a period of app… -
Ecliptic Longitude
Linked via "precession"
The ecliptic coordinate system is fundamentally heliocentric, though it is commonly applied to geocentric observations. Longitude is measured in angular units, typically degrees ($^\circ$), arcminutes ($'$), and arcseconds ($''$). A complete circle is $360^\circ$, corresponding to a full circuit around the sky following the Sun's apparent trajectory.
The zero point, or origin, for ecliptic longitude is the Vernal Equinox ($\Upsilon$), which, by definition in modern [astronomy](/entrie… -
Ecliptic Longitude
Linked via "axial precession"
Precession and Ecliptic Longitude Drift
Due to the slow, conical wobble of the Earth's axis—known as axial precession—the celestial poles drift over a cycle of approximately 26,000 years. This movement causes the location of the Vernal Equinox ($\Upsilon$) to shift westward along the ecliptic. Consequently, the ecliptic longitude of any fixed star-like object changes systematically over time.
The rate of precession along the eclip… -
Ecliptic Longitude
Linked via "precession"
Due to the slow, conical wobble of the Earth's axis—known as axial precession—the celestial poles drift over a cycle of approximately 26,000 years. This movement causes the location of the Vernal Equinox ($\Upsilon$) to shift westward along the ecliptic. Consequently, the ecliptic longitude of any fixed star-like object changes systematically over time.
The rate of precession along the ecliptic is approximately $50.3$ arcseconds per y… -
Ecliptic Longitude
Linked via "precession"
$$\Delta \lambda = p_{\lambda} \cdot T + \frac{1}{2} f \cdot T^2$$
Where $p_{\lambda}$ is the constant component of precession in longitude, and $f$ is the second-order correction term, which accounts for the slight non-uniformity in the rate of change attributed to the subtle tidal locking effect with Jupiter's orbital resonance [2].
The Zodiacal Bands and Longitude