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The Sun. Motion and constellations

09/06/2026

The online simulations of the motion of the sun on this page will help us to learn more about the closest star to Earth, the one that supplies us with the energy that allows life to exist. You will discover interesting details about its movement, the solar ecliptic and the constellations of the zodiac.

This Thematic Unit is part of our Earth Sciences collection

STEM OnLine mini dictionary

Analemma

Figure-eight curve representing the Sun’s position if observed daily at the same time.

Apparent Motion of the Sun

Sun’s movement in the sky as seen from Earth due to Earth’s rotation and orbit.

Ecliptic

Curved line along which the Sun’s apparent motion occurs as seen from Earth.

Equinox

Time of year when the Sun crosses the celestial equator and day and night are of equal length.

Photosphere

Luminous surface of the Sun that emits most of the radiation we receive.

Solar Corona

Outermost layer of the Sun’s atmosphere, made of plasma and visible during total eclipses.

Solar Declination

Angle between the Sun’s rays and the plane of the Earth’s equator.

Solar Noon

Instant when the Sun crosses the observer’s meridian and reaches its highest point.

Solstice

Time when the Sun reaches its maximum or minimum declination relative to the celestial equator.

Sunspot

Region of the photosphere with lower temperature and intense magnetic activity.

Zenith

Point on the celestial sphere located exactly above an observer’s vertical.

What is the Sun

The Sun, our nearest star, is a gigantic sphere of hot plasma that radiates light and heat in all directions. It is the center of our solar system and provides life and energy to all the planets that orbit it, including Earth.

The Sun is approximately 4.6 billion years old and is estimated to have a lifetime of at least another 5 billion years. Its size is impressive, with a diameter of about 1.4 million kilometers, making it 109 times larger than Earth. Its mass is about 333,000 times that of our planet and it contains more than 99% of the total mass of the solar system.

Studying the Sun is fundamental to understanding how it works and predicting its behavior. Scientists use space and ground-based observatories to study its solar activity, such as sunspots, solar flares and coronal mass ejections, which can affect communications, power grids and navigation systems on Earth.

Chemical composition of the Sun

The Sun is composed mainly of hydrogen (about 74% of its mass) and helium (about 24%), along with traces of heavier elements. At its core, temperatures reach 15 million degrees Celsius and pressures are enormous, allowing nuclear fusion reactions to occur in which hydrogen nuclei combine to form helium, releasing large amounts of energy in the process.

This energy is transported to the surface of the sun through a process known as convection and is then emitted into space in the form of light and electromagnetic radiation at all wavelengths, from gamma rays and X-rays to visible light and even radio waves.

Solar radiation

Solar radiation is essential for life on Earth. It is responsible for photosynthesis in plants, which converts sunlight into chemical energy and provides oxygen to the atmosphere. It is also the main source of heat on our planet, affecting weather patterns and regulating the water cycle.

Studying the Sun is fundamental to understanding how it works and predicting its behavior. Scientists use space and ground-based observatories to study its solar activity, such as sunspots, solar flares and coronal mass ejections, which can affect communications, power grids and navigation systems on Earth.

The Sun’s daily movement. The apparent movement of the Sun from Earth’s perspective

The Sun’s daily movement is the change in the Sun’s position in the sky due to the Earth’s rotation. When we look up at the sky, it appears as though the Sun is a sphere in constant motion around our planet. However, modern astronomy shows that this movement is purely an illusion. What we experience on a daily basis is not the actual journey of our star, but the optical reflection of the Earth’s own movements in outer space.

The daily path from east to west and the Earth’s rotation

The most obvious apparent motion is that which the Sun performs every twenty-four hours, rising in the east, reaching its highest point at noon, and setting in the west. This daily cycle is the direct consequence of the Earth’s rotational movement, in which our planet spins on its own imaginary axis in the opposite direction, that is, from west to east. Since we are situated on the rotating Earth’s surface, we perceive the sky as spinning around us. This continuous rotation determines the regular succession of day and night, setting the rhythm of life and enabling the functioning of traditional sundials.

The Sun’s annual journey along the ecliptic and through the zodiac constellations

In addition to its daily movement, the Sun’s position in the sky varies subtly from day to day throughout the year. If we were to record the Sun’s position at the same time each day for 365 days, we would see that it traces an imaginary line in the sky known as the solar ecliptic. The solar ecliptic is the apparent path the Sun follows in the sky throughout the year as seen from Earth. This path is the result of Earth’s orbit around the Sun and manifests as an imaginary line on the celestial sphere that traces the Sun’s position against the constellations of the zodiac. The ecliptic is tilted about 23.5 degrees relative to the celestial equator.

This annual path is due to the Earth’s translational motion around the Sun combined with the tilt of the Earth’s axis. As the Earth moves along its orbit, the Sun appears to project against different backgrounds of fixed stars in the celestial sphere. The twelve historical constellations that lie exactly along this path of the ecliptic make up the astronomical zodiac, and serve to mark the passing of the seasons and our planet’s annual journey.

The Sun’s actual movement in outer space

Although the Sun is the gravitational center of our planetary system and appears to us as a static reference point in space, the reality is that the star is not stationary. The Sun undergoes highly complex physical movements, both internally as it rotates on its own axis and on a large scale, traveling at breakneck speeds through the cosmos.

The Sun’s internal rotation on its own axis

Like the planets, the Sun rotates on its own axis, but with a unique peculiarity: since it is not a solid body but a sphere of gaseous plasma, it does not rotate uniformly. This phenomenon is known as differential rotation. The solar equator rotates much faster than the poles, taking approximately 25 Earth days to complete a full rotation at its center, while in the polar regions the rotation slows to about 35 days. This difference in rotational speed causes the lines of the Sun’s powerful magnetic field to stretch, twist, and become entangled over time, giving rise to visible solar activity such as sunspots and coronal mass ejections.

The Solar System’s orbit around the galactic center

On a macroscopic scale, the Sun participates in the Milky Way’s grand cosmic dance. Our star, dragging the Earth and the rest of the Solar System’s planets along with it, continuously orbits around the center of the galaxy. We travel at an impressive speed of approximately 220 kilometers per second. Due to the enormous size of the Milky Way, it takes the Sun between 225 and 250 million Earth years to complete a single orbit around the galactic center—a colossal period of time known in astronomy as a cosmic year or galactic year. Since its formation, the Sun has completed only about twenty orbits of the galaxy.

STEM OnLine mini dictionary

Analemma

Figure-eight curve representing the Sun’s position if observed daily at the same time.

Apparent Motion of the Sun

Sun’s movement in the sky as seen from Earth due to Earth’s rotation and orbit.

Ecliptic

Curved line along which the Sun’s apparent motion occurs as seen from Earth.

Equinox

Time of year when the Sun crosses the celestial equator and day and night are of equal length.

Photosphere

Luminous surface of the Sun that emits most of the radiation we receive.

Solar Corona

Outermost layer of the Sun’s atmosphere, made of plasma and visible during total eclipses.

Solar Declination

Angle between the Sun’s rays and the plane of the Earth’s equator.

Solar Noon

Instant when the Sun crosses the observer’s meridian and reaches its highest point.

Solstice

Time when the Sun reaches its maximum or minimum declination relative to the celestial equator.

Sunspot

Region of the photosphere with lower temperature and intense magnetic activity.

Zenith

Point on the celestial sphere located exactly above an observer’s vertical.

Explore the exciting STEM world with our free, online, simulations and accompanying companion courses! With them you’ll be able to experience and learn hands-on. Take this opportunity to immerse yourself in virtual experiences while advancing your education – awaken your scientific curiosity and discover all that the STEM world has to offer!

Simulations of motion of the Sun

Diurnal motion of the Sun


The diurnal motion of the Sun is the change of the Sun’s position in the sky due to the rotational motion of the Earth.






Solar ecliptic


The solar ecliptic is the path the Sun describes in the sky. The zodiac is the twelve constellations of the ecliptic.






Constellations of the Zodiac


The zodiac is a belt of the sky with a width of about 8° around the ecliptic. It allows us to locate the Sun, the Moon and most of the planets in their apparent position. It is divided into 12 parts, each of which corresponds to a constellation: Aries, Taurus, Gemini, Cancer, Leo, Virgo, Libra, Scorpio, Sagittarius, Capricorn, Aquarius and Pisces.

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The so‑called “movement of the Sun” refers to the path it seems to follow across the sky from sunrise to sunset, but in reality this is an apparent motion caused by Earth’s rotation on its axis, which makes the Sun appear to travel from east to west. This phenomenon is essential for understanding the alternation of day and night, geographic orientation and the way sunlight changes throughout the day, and it also serves as the foundation for explaining more complex apparent motions related to Earth’s axial tilt and its orbit around the Sun.
Earth’s axial tilt causes the Sun’s apparent path to change depending on the season, so in summer the Sun follows a higher and longer arc across the sky, producing longer days, while in winter its path is lower and shorter, resulting in shorter days. This seasonal variation explains why sunlight reaches different latitudes with different intensity and duration, and it underlies phenomena such as solstices, equinoxes and the contrast between hemispheres, all of which stem from the geometry of Earth’s motion.
It feels so obvious because our immediate reference point is the ground beneath us, which seems completely still, so our brain naturally interprets the changing light as the Sun moving rather than Earth turning. Since Earth’s rotation is smooth and we don’t feel it, what we perceive is the visual effect: the horizon brightens, the Sun appears, climbs, descends and disappears, and even when we know the scientific explanation, the everyday experience still gives the strong impression that the Sun is the one doing the moving.
Although we often say the Sun rises in the east and sets in the west, that only happens precisely on the equinoxes; the rest of the year the sunrise and sunset points shift toward the northeast or southeast depending on the season, because Earth’s axial tilt makes the Sun’s apparent path change slightly every day. That’s why in summer it rises farther north and in winter farther south, and this shift is easy to notice if you watch the horizon over several weeks.
In regions near the poles, Earth’s axial tilt causes the Sun to remain above the horizon even as the planet rotates, producing the so‑called “midnight sun,” while in the opposite season the Sun never climbs high enough to appear, creating extremely long nights. This isn’t a glitch in the day‑night cycle but a direct consequence of how Earth is oriented relative to the Sun during its yearly orbit, and it explains why polar areas experience such extreme patterns of light and darkness.

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