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The Obliquity of the Ecliptic

The celestial equator and the ecliptic are both great circles on the same sphere, and they do not coincide. The angle between them is the obliquity of the ecliptic, currently about 23.4°.

It is one number. A remarkable amount depends on it, including everything in the rest of this category.

Where the tilt comes from

The celestial equator is the Earth's equator projected outward. The ecliptic is the Earth's orbital plane projected outward. So the angle between them is the angle between the Earth's equator and its orbit — which is to say, the tilt of the Earth's axis relative to the plane it travels in.

The Earth does not spin upright in its orbit. It leans by 23.4°, and it keeps leaning in the same direction all year round.

The same angle, in two places

The tilt shows up wherever the two circles are compared, and the diagram catches it twice at once.

The celestial sphere seen along the plane containing both poles and both solstices. The angle between the celestial pole and the ecliptic pole is marked as 23.4°, and the same 23.4° appears again lower down as the gap between the celestial equator and the ecliptic at the solstice.

Near the top, the celestial pole and the ecliptic pole are separated by 23.4°. Each plane has its own pair of poles, and tilting a circle tilts its poles by the same amount.

Near the bottom, the celestial equator and the ecliptic are separated by 23.4° at the solstice, where the gap between them is widest.

They are not two facts. They are one tilt, measured in two places, which is the whole reason the figure is drawn from this particular direction.

Hold on to the top half of that figure. The two frames have different poles, 23.4° apart — and since "measure away from the plane" means "measure towards its pole", two frames with different poles measure away in different directions. That is the seed of everything from Projecting Between the Planes onwards.

What follows from it

The Sun's declination varies. As the Sun travels the ecliptic it is carried from 23.4° north of the celestial equator at the June solstice, down through zero at each equinox, to 23.4° south at the December solstice. Its declination is never outside that range — and note what this means: the Sun has a celestial latitude of zero and a declination that swings across 47°. One body, two frames, two completely different descriptions of the same motion.

The seasons. A body's declination determines how high it climbs and how long it stays up. So as the Sun's declination swings through the year, the northern hemisphere gets a high, long-lasting Sun in June and a low, brief one in December — and the southern hemisphere gets the reverse, at the same time, from the same cause.

This has nothing to do with distance from the Sun. The Earth is actually slightly closer to the Sun in January. Seasons are a matter of tilt.

The tropics and the polar circles. The Sun can only stand directly overhead where its maximum declination reaches, and it becomes circumpolar 23.4° short of the pole. Both limits are the obliquity, measured from opposite ends.

FeatureLatitudeComes from
Tropic of Cancer23.4° Nthe obliquity, from the equator
Tropic of Capricorn23.4° Sthe obliquity, from the equator
Arctic Circle66.6° Nthe obliquity, from the pole
Antarctic Circle66.6° Sthe obliquity, from the pole

Those are the two numbers left outstanding by The Zenith and the Nadir and Sky That Never Sets.

Unequal rising times. Because the ecliptic is tilted, its twelve equal divisions do not meet the horizon at equal angles. Some parts rise steeply and quickly, others at a shallow angle and slowly. Equal stretches of ecliptic take markedly unequal times to rise, which is why the Ascendant moves through the signs at such uneven speed.

The value is not permanent

23.4° is the current figure, not a constant. The obliquity oscillates slowly, between roughly 22.0° and 24.5°, over a cycle of about 41,000 years. It is presently decreasing by about 47 arcseconds per century.

Over a human lifetime that is negligible. Over the span covered by historical astronomy it is not: the obliquity was noticeably larger in antiquity, and ancient measurements of it are perfectly consistent with modern ones once the drift is accounted for.

What comes next

The tilt is established. Now each frame gets its own page, starting with the one astrology is written in.

Next: Ecliptic Coordinates.