Seasons due to Earth's elliptical orbit

In summary, the primary cause of Earth's seasons is the tilt of its axis, which results in varying amounts of sunlight reaching different parts of the Earth throughout the year. The effect of distance from the sun on temperatures is relatively minimal and is overshadowed by other factors such as the changing length of daylight and the angle at which sunlight hits the Earth's surface. Other perturbations, such as the distribution of land and ocean between hemispheres, also play a role in the variation of temperatures throughout the year.
  • #1
MisterAmrani
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Hello there! What I have never understood is that our seasons are the result of the tilt of the Earth's axis, and I've always interpreted that to mean that the northern hemisphere is closer to the sun in June, July, and August, and the southern in December, January, and February. If that is the case, I don't understand why a shift in the axis results in temperature variations of ~50 degrees (around 40 degrees N), yet a variation of distance from the sun of 3 million+ miles does not affect the temperature. Or do I have this all wrong, and the elliptical orbit also plays a part in the temperatures?
 
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  • #2
There is an effect, it's just hard to see in the middle of everything else that is happening.

The day length changes quite drastically summer to winter. In Toronto, where I live, a winter day can be as short as 6 hours. Plus the sun does not get very high in the sky. In summer, a day can be 14 hours. So more than double. And it gets higher in the sky so the sun light is falling closer to vertical. So this produces much more heat per square meter.

The Earth's orbit is slightly non-circular, as you refer to. And it is slightly closer for part of the year. This amounts to a change of about 3 percent. (To one digit.) So, crank out your inverse-square law and work out how much this increases total solar radiation. (Hint 1.03 * 1.03 is just a bit more than 1.06.) So comparing that to the more-than-doubling of daylight in Toronto means that the distance effect is probably pretty small.

There are other perturbations and effects that make the effect hard to see. For example, the southern hemisphere has a lot more ocean than the northern. Ocean currents and clouds tend to be very different in the southern hemisphere.
 
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  • #3
MisterAmrani said:
Hello there! What I have never understood is that our seasons are the result of the tilt of the Earth's axis, and I've always interpreted that to mean that the northern hemisphere is closer to the sun in June, July, and August, and the southern in December, January, and February. If that is the case, I don't understand why a shift in the axis results in temperature variations of ~50 degrees (around 40 degrees N), yet a variation of distance from the sun of 3 million+ miles does not affect the temperature. Or do I have this all wrong, and the elliptical orbit also plays a part in the temperatures?

Actually, it is the tilt of the Earth's axis which is the major determining factor in creating the seasons. In the northern hemisphere, the axis is tilted toward the sun during the summer months, while the southern hemisphere is tilted away at the same time, producing winter in that region. The opposite holds true in the winter season of the northern hemisphere.

As to the influence of the Earth's orbit on the seasons, it is relatively minimal and surprisingly the opposite of what is expected. The distance of the Earth from the sun varies by about 5 million km out of 150 million km average during the year. However, the Earth reaches perihelion, or the closest point from the sun, about January 3 every year, and aphelion, or the farthest point from the sun, about July 4.

http://en.wikipedia.org/wiki/Perihelion_and_aphelion
 
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Take a look at these attached sketches also:
(main sketch and enlarged views of the solstices)
(you will have to rotate them)
The red line is a daily path of a point at about 45 degrees latitude above the equator.
 

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  • #5
If you read between the lines of the very complete answers you have gotten above, you can see that the difference in distance to the Sun that is caused by the tilt is indeed completely negligible. So you have that part right-- the tilt has nothing to do with distance to the Sun. But what you did not understand is what is being explained above-- all the other important things that tilt does do (it changes the length of the day, and how close to overhead the Sun gets, and you know from daily experience that the temperature rises when the Sun is closer to directly overhead). In fact, when teaching the simplest understanding of the seasons, the first thing we usually say is completely forget distance to the Sun, you can understand seasons on Earth without even thinking about distance variations. If you do want to think about distance, consider Mars' seasons instead-- they combine tilt and distance variations from the elliptical orbit, so are quite a bit more complicated than Earth seasons.
 
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  • #6
Thank you all for your answers, you cleared things up for me!
 
  • #7
Me too! Thanks for asking the question Mister!
 
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  • #8
SteamKing said:
As to the influence of the Earth's orbit on the seasons, it is relatively minimal and surprisingly the opposite of what is expected.
For the northern hemisphere, that is. The Aussies don't know they are upside-down!
 
  • #9
Ken G said:
n fact, when teaching the simplest understanding of the seasons, the first thing we usually say is completely forget distance to the Sun, you can understand seasons on Earth without even thinking about distance variations. If you do want to think about distance, consider Mars' seasons instead-- they combine tilt and distance variations from the elliptical orbit, so are quite a bit more complicated than Earth seasons.
These are very good points.

As everyone has already said, the primary driver of seasons on the Earth is the Earth's axial tilt. The Earth as a whole is cooler in January (when it is closest to the Sun) than it is in July (when it is furthest from the Sun), showing how unimportant distance is when it comes to driving the seasons. The reason the Earth as a whole is cooler in January than in July is because of the uneven distribution of ocean and land between the northern and southern hemispheres. This is a secondary cause of the seasons. Distance from the Sun? That's at best tertiary, at least for the Earth.

Mars doesn't have oceans and its orbit about the Sun is much more eccentric than that of the Earth. Mars' seasons are a complex mix of eccentricity and axial tilt.
 
  • #10
T
SteamKing said:
Actually, it is the tilt of the Earth's axis which is the major determining factor in creating the seasons. In the northern hemisphere, the axis is tilted toward the sun during the summer months, while the southern hemisphere is tilted away at the same time, producing winter in that region. The opposite holds true in the winter season of the northern hemisphere.

As to the influence of the Earth's orbit on the seasons, it is relatively minimal and surprisingly the opposite of what is expected. The distance of the Earth from the sun varies by about 5 million km out of 150 million km average during the year. However, the Earth reaches perihelion, or the closest point from the sun, about January 3 every year, and aphelion, or the farthest point from the sun, about July 4.

http://en.wikipedia.org/wiki/Perihelion_and_aphelion
There is also the 25000 Earth wobble the Southern Hemisphere is close now but over time it will be the northern hemisphere. the Sahara will be wet not dry ect ect
 
  • #11
DEvens said:
In Toronto, where I live, a winter day can be as short as 6 hours.
You must live waaaaay up near Steeles (just shy of the Arctic Circle). Down here, near the lake, Toronto never gets less than a 9 hour day. :wink:

http://www.timeanddate.com/sun/canada/toronto?month=12
 

1. What causes the change in seasons?

The change in seasons is caused by Earth's tilt on its axis and its revolution around the sun. Earth's tilt causes different parts of the planet to be closer or farther from the sun at different times of the year, resulting in variations in temperature and weather patterns.

2. How does Earth's elliptical orbit affect the seasons?

Earth's elliptical orbit, or its slightly oval-shaped path around the sun, does not have a significant impact on the seasons. The tilt of Earth's axis is the main factor that causes the change in seasons. However, the elliptical orbit does affect the length of seasons, with the seasons being slightly longer when Earth is farther from the sun during its orbit.

3. Why do the seasons occur at different times in the Northern and Southern Hemispheres?

The tilt of Earth's axis remains constant as it orbits the sun, causing the Northern and Southern Hemispheres to receive different amounts of sunlight throughout the year. When one hemisphere is tilted towards the sun, it experiences summer while the other hemisphere experiences winter. As Earth continues its orbit, the tilt shifts, causing the seasons to switch in the two hemispheres.

4. How do the equinoxes and solstices relate to Earth's elliptical orbit?

The equinoxes and solstices mark the changing of seasons and are related to Earth's elliptical orbit. The equinoxes occur when the sun is directly above the equator, resulting in equal amounts of daylight and darkness for both hemispheres. The solstices occur when the tilt of Earth's axis is most extreme, resulting in the longest and shortest days of the year.

5. Can the elliptical orbit of Earth change over time?

Yes, Earth's elliptical orbit can change over time due to various factors such as gravitational pull from other planets and the sun. However, these changes occur over long periods and do not have a significant impact on the seasons. The tilt of Earth's axis remains the main factor in causing the change in seasons.

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