Full Answer
The apparent yearly path of the Sun through the stars is called the ecliptic. This circular path is tilted 23.5 degrees with respect to the celestial equator because the Earth's rotation axis is tilted by 23.5 degrees with respect to its orbital plane.
(Discovering the Universe, 5th ed., §1-6) Although the stars are fixed relative to each other, the Sun moves relative to the stars. The Sun crosses the celestial equator at exactly two points, called equinoxes, from the Latin for "equal nights" (for reasons we'll see later).
It makes one full circuit of 360 degrees in 365.24 days (very close to 1 degree or twice its diameter per day). This drift eastward is now known to be caused by the motion of the Earth around the Sun in its orbit. The apparent yearly path of the Sun through the stars is called the ecliptic.
The starting and ending points are the same. The exact path of the Sun depends on what your latitude is: whether you are at the equator (0 degrees of latitude), the North Pole (90 degrees north), the South Pole (90 degrees south), or in-between. The exact path also depends on the time of year.
Sun moves nearly with celestial sphere, but position on sphere changes over year. Moves along a great circle called the ecliptic, inclined 23.5 degrees relative to equator. Constellations along ecliptic are called the "Zodiac" signs. Constellation opposite Sun depends on time of year.
After the June solstice, the sun's path gradually drifts southward. By the September equinox, its path is again along the celestial equator. The southward drift then continues until the December solstice (usually December 21), when the sun rises considerably south of due east and sets considerably south of due west.
The Earth's axial tilt moves the Sun north/south over the year, and the elliptical orbit moves it east/west. Combine the two, and you get that crazy figure-8 in the sky.
[+] The first major contributor to the Sun's apparent motion is the fact that Earth orbits the Sun while tilted on its axis. The Earth's axial tilt of approximately 23.5° ensures that observers at different locations will see the Sun reach higher-or-lower positions above the horizon throughout the year.
The Earth is also revolving around the Sun, so each day of the year, the Earth is at a different point in its orbit. So because the Earth is facing the Sun at a different angle each day, the "path" the Sun makes in the sky will be different each day of the year.
Different factors affect the position of the Sun on its daily path across the sky. Earth rotates on a tilted axis and orbits the Sun in a slightly oval-shaped, or elliptical, path. These two motions affect the Sun's changing position in the sky and the times of daily sunrises and sunsets over a year.
The Sun spins or rotates on its axis in the same direction as Earth (counterclockwise, when looking down from the north pole). Because it is a gas, it does not rotate like a solid. Different sections rotate at different speeds! The Sun actually spins faster at its equator than at its poles.
FACT TWO: The angle of the sun is changing with the seasons So this means the sun is far higher in the sky in the summer (creating shorter shadows) than in the winter (longest shadows). Starting in the winter, the solar altitude increases through spring and peaks in summer.
The Earth's axis of rotation tilts about 23.5 degrees, relative to the plane of Earth's orbit around the Sun. As the Earth orbits the Sun, this creates the 47° declination difference between the solstice sun paths, as well as the hemisphere-specific difference between summer and winter.
As the Earth rotates, it also moves, or revolves, around the Sun. The Earth's path around the Sun is called its orbit. It takes the Earth one year, or 365 1/4 days, to completely orbit the Sun. As the Earth orbits the Sun, the Moon orbits the Earth.
A day, which is the time from one sunrise to the next sunrise — one complete rotation of the Earth. A year, which is approximately 365.24 days — one complete orbit of Earth around the Sun. A month, which is approximately 29.53 days — one complete orbit of the Moon around the Earth.
From Earth, the Sun looks like it moves across the sky in the daytime and appears to disappear at night. This is because the Earth is spinning towards the east. The Earth spins about its axis, an imaginary line that runs through the middle of the Earth between the North and South poles.
During an average day, when the Earth moves at its average speed around the Sun, 24 hours is just right. But when the Earth moves more slowly (near aphelion), 24 hours is too long for the Sun to return to its same position, and so the Sun appears to shift more slowly than average.
The reason for this is largely due to the second main contributor to the Sun's apparent motion throughout the year: Earth's orbit around the Sun is elliptical, not circular.
If we lived on an untilted planet that had an elliptical orbit, the Sun’s path through the sky would simply be an ellipse: where the eccentricity would be the only contributor to how the Sun moves. This is what happens roughly on Jupiter and Venus, where the axial tilts are negligible.
between the two tropics (between 23.5° S and 23.5° N), the Sun will pass directly overhead on two days equidistant from one solstice. From any location, if you were to track the position of the Sun throughout the year — such as through a pinhole camera — this is what you’d see. using a pinhole camera.
The first major contributor to the Sun's apparent motion is the fact that Earth orbits the Sun while tilted on its axis. The Earth's axial tilt of approximately 23.5° ensures that observers at different locations will see the Sun reach higher-or-lower positions above the horizon throughout the year. When your hemisphere is tilted towards the Sun, ...
The shape you traced out would look like a figure-8 with one loop larger than the other: a shape known as our analemma. The fact that the Earth orbits the Sun once per year explains the first part. But the motion of the Sun in its particular analemma shape is due to a combination of deep reasons. Let's find out why.
If you did this every day for a full year, you'd discover two important things: The Sun would have returned to its starting point at long last, as the Earth returned to the same point in its orbit from a year prior.
The shape you traced out would look like a figure-8 with one loop larger than the other: a shape known as our analemma.
In general, all across the Earth, the Sun appears to rise in the Eastern portion of the sky, rise up high overhead towards the equatorial direction, and then lower down and set in the West. If you live: 1 south of 23.5° S latitude, the June solstice marks the Sun’s shortest, lowest path through the sky, while the December solstice marks the longest, highest path. 2 north of 23.5° N latitude, the December solstice marks the Sun’s shortest, lowest path through the sky, with the June solstice marking the longest, highest path. 3 between the two tropics (between 23.5° S and 23.5° N), the Sun will pass directly overhead on two days equidistant from one solstice.
In particular, when we combine them, we can immediately see why our analemma looks like an “8” that’s pinched on one narrow side. As the Earth rotates on its axis and orbits the Sun in an ellipse, the Sun’s apparent position appears to change from day-to-day in this particular shape: Earth’s analemma.
All worlds in our solar system have seasons determined by either their axial tilt, the ellipticity of their orbits, or a combination of both. (WIKIMEDIA COMMONS USER TAUʻOLUNGA) The first major contributor to the Sun’s apparent motion is the fact that Earth orbits the Sun while tilted on its axis.
The observed path that the Sun takes through the sky can be tracked, from solstice to solstice, using a pinhole camera. That lowest path is the winter solstice, where the Sun reverses course from dropping lower to rising higher with respect to the horizon, while the highest path corresponds to the summer solstice.
Before noon (upper right), the analemma appears to rotate counterclockwise towards the horizon, while after noon, it appears to rotate clockwise with respect to the horizon. These images are further proof, for any doubters out there, that the Earth is round.
Instead, the Earth makes a full 360° rotation ins just 23 hours and 56 minutes; a day takes 24 hours because it takes those extra 4 minutes to “catch up” to the amount of distance the Earth has traveled in its orbit around the Sun.
The Sun always takes a path from east to west across the sky during the day. The only thing that varies is whether that path goes directly above you, or arcs across the Southern sky, or arcs across the Northern sky or even arcs below the horizon. The starting and ending points are the same.
At the spring equinox (March 21st) and the autumn equinox (September 21st), the Sun will move right along the horizon from east to west, moving along the Southern sky. Half of the Sun will be above the horizon, and half of the Sun will be below the horizon all day. It's like a constant sunset.
At noon, it will be 23.4 degrees above the horizon - the same angle as the Earth's tilt. This is as high as the Sun ever gets at the North Pole.
At noon, it will be 23.4 degrees above the horizon - the same angle as the Earth's tilt. This is as high as the Sun ever gets at the South Pole. At the Equator. The Equator is at a latitude of 0 degrees. At the spring equinox, the Sun will start in the East, arc directly overhead and set in the West.
What does affect it is your latitude. Latitude is the angular distance of a place north or south of the Earth's equator in degrees. A latitude of zero degrees is on the equator of the Earth, while 90 degrees south is the South Pole, and 90 degrees north is the North Pole. If you live north of the Equator, the Sun rises in the East, ...
At the South Pole, it will be 0 degrees above the Northern horizon (right along it). And at the equator, it will be directly above (90 degrees above the horizon). Learning Outcomes. When you are finished, you should be able to: Explain the importance of latitude in determining the Sun's path across the sky.
The peak of summer is called the summer solstice and is on June 21st in the Northern hemisphere. This is when the days are longest, and the Sun at noon is as high as it will ever be. At 40 degrees north, the Sun rises in the East and arcs across the Southern sky to set in the West.
In summary: The sun appears to move along with the celestial sphere on any given day, but follows different circles at different times of the year: most northerly at the June solstice and most southerly at the December solstice. At the equinoxes, the sun's path follows the celestial equator.
In late March and late September (at the "equinoxes"), the sun's path follows the celestial equator. It then rises directly east and sets directly west. The exact dates of the equinoxes vary from year to year, but are always near March 20 and September 22. After the March equinox, the sun's path gradually drifts northward.
The ecliptic is a great circle on the celestial sphere, tipped 23.5° with respect to the celestial equator. Its orientation with respect to our horizon changes as the sphere spins around us each day. It has the orientation shown here at noon in December and at midnight in June.
For one thing, the sun takes a full 24 hours to make a complete circle around the celestial sphere, instead of just 23 hours, 56 minutes. For obvious reasons, we define our day based on the motion of the sun, not the stars.
These geographical variations in the sun's angle above the horizon also account for the major geographical variations in earth's climates. The arctic and antarctic regions are almost always cold—even in the summer when they get 24 hours of sunlight a day—because the sun's angle above the horizon is never very high.
At the North Pole, the sun is above the horizon for six straight months (March through September), spinning around in horizontal circles, reaching a maximum height of 23.5° above the horizon at the June solstice. As you travel southward in the northern hemisphere, the noon sun gets higher and higher.
The added hours of daylight are one reason why summer is warmer than winter. But there's another reason that's even more important: the angle of the mid-day sun. Notice from the illustrations above that the noon sun is much higher in June than in December. This means that the sun's rays strike the ground more directly in June. In December, on the other hand, the same amount of energy is diluted over a larger area of ground:
As a result, the stars appear to rise, cross the sky, and set 4 minutes earlier each night. This amounts to a whole hour earlier in 15 days and two hours earlier in 30 days.
And if we were to synchronize our clocks using the motions of the stars as a reference, we would discover that the Earth would complete a single turn on its axis not in 24 hours, but actually four minutes shy of that figure: 23 hours 56 minutes. As a result, the stars appear to rise, cross the sky, and set 4 minutes earlier each night.
This apparent westward drift of the stars, incidentally, is a motion that is in addition to the daily rising, circling, and setting. For our Earth does not simply stand in the same spot in space and spins, but is constantly rushing eastward along in its orbit around the Sun.