AstronomyThe SkyMS-ESS1-1

The Sun's Path Through the Year

The Sun's declination swings between +23.4° and −23.4°, which sets the solstices, the equinoxes, the tropics and the polar circles.

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In Why We Have Seasons you learned that Earth's tilted axis changes how high the Sun climbs and how long it stays up. With declination we can say exactly how: the Sun's declination changes through the year, and that one number sets the solstices, the equinoxes, the tropics and the polar circles.

Why it works

Earth's axis is tilted $23.4^\circ$ from the perpendicular to its orbit, and it keeps pointing the same way in space all year. So the celestial equator (above Earth's equator) is tilted $23.4^\circ$ from the ecliptic, the Sun's yearly path among the stars. As the Sun travels the ecliptic, its declination swings from $+23.4^\circ$ to $-23.4^\circ$ and back. When the North Pole leans toward the Sun (June), the Sun is $23.4^\circ$ north of the celestial equator; when it leans away (December), $23.4^\circ$ south.
The Sun's declination through the year.
Date (about)NameSun's declinationSun overhead at noon
March 20March equinox$0^\circ$the equator
June 21June solstice$+23.4^\circ$$23.4^\circ$ N, the Tropic of Cancer
September 22September equinox$0^\circ$the equator
December 21December solstice$-23.4^\circ$$23.4^\circ$ S, the Tropic of Capricorn

Key idea

The Sun's declination swings between $+23.4^\circ$ and $-23.4^\circ$ because of Earth's tilt. The tropics ($23.4^\circ$ N and S) are as far as the overhead Sun can go; the polar circles ($90^\circ - 23.4^\circ = 66.6^\circ$) mark where it can stay up, or down, for a whole day.
Earth's orbit seen at an angle, with the tilted axis, and the noon sunlight at latitude $40^\circ$ N.

Worked examples

Worked example: The midnight Sun

On the June solstice, poleward of what latitude does the Sun never set?
  1. On the June solstice the Sun is at declination $+23.4^\circ$, so it is $90^\circ - 23.4^\circ = 66.6^\circ$ from the north celestial pole.
  2. From altitude and latitude: a star is circumpolar where the pole's altitude (your latitude) is at least its distance from the pole.
  3. So the Sun stays up all day at latitude $66.6^\circ$ N and beyond: the Arctic Circle.

Answer: North of $66.6^\circ$ N.

Worked example: Another planet

Mars's axis is tilted $25.2^\circ$. Where would Mars's tropics and polar circles be?
  1. Tropics sit at the tilt: $25.2^\circ$ N and S.
  2. Polar circles sit at $90^\circ$ minus the tilt: $90^\circ - 25.2^\circ = 64.8^\circ$.

Answer: Tropics at $25.2^\circ$; polar circles at $64.8^\circ$.

Common mistake

The tropics and polar circles are not arbitrary lines drawn by mapmakers, and they are not where Earth is closest to the Sun. They come from the tilt alone: the tropics at the tilt angle, the polar circles at $90^\circ$ minus the tilt. A quick check: if Earth had no tilt, the Sun would stay on the celestial equator all year, the tropics would shrink to the equator, and there would be no midnight Sun anywhere except right at the poles.
Seasons do not come from Earth's distance: Earth is closest to the Sun in early January, in northern winter, and the distance changes only about 3%. Set dates through the year in the Sky and Solar System lab and watch Earth travel around the Sun.
Try it in the Science LabSky and Solar System

Practice

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Sources and further reading

  • OpenStax, Astronomy 2e, section 4.2, The Seasons
  • NGSS MS-ESS1-1: Earth–Sun–Moon system models
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