Actual year/day vs earth's movement

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In summary, the Earth takes 365.256363004 days to orbit the sun, causing the average calendar year to be off in accuracy by 0.006363004 days. This means that in 157 years, the calendar would be off by one day and over time, this could cause the seasons to slowly change when they are supposed to occur. As technology develops, we are able to refine measurements of the Earth's rotation and time. However, the definition of time is not based on exactly 24 hours in a day, so there may be discrepancies between old and new clocks. Additionally, the rule for leap years is not as simple as being divisible by 4, leading to unique occurrences like February 30, 1712
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Good4you
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1) So i found on Wikipedia that the Earth takes 365.256363004 days to orbit the sun. If you include leap years then the average calendar year is 365.25 days. So the calendar year is off in accuracy by the difference. Calculating that out would mean that in 157 years the calendar would be off by one day. So i guess my question is: is there a means to correct for this, or will over the centuries the seasons slowly change when they are supposed to occur?

2) My guess is that over time as technology develops we incrementally refine measurements of things like the time it takes for the Earth to rotate. So this would lead me to believe that when the first clocks were invented we did not know to the same precision the amount of time it takes for the Earth to rotate.
a) So is time defined in a way that there is exactly 24hours in a day? ...and would't this mean that a second measured by an old clock would not be equivalent to a second on a new clock?
b) or if the definition of time is not based on there being exactly 24hours in a day; wouldn't this imply that as we refine our measurement of the Earth's rotation, there is more or less than 24hours in a day; therefore over the centuries, wouldn't there be some "creep", and 12:00 would no longer correspond to noon, perhaps it would eventually correspond with dusk? or is there some method to correct for this "creep"?
 
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Good4you said:
If you include leap years then the average calendar year is 365.25 days.

You're not using the full rule for leap years.

If the year is divisible by 4, it's a leap year,

UNLESS

it's also divisible by 100, in which case it's not a leap year,

UNLESS

it's also divisible by 400, in which case it's a leap year after all.

So 1700, 1800, 1900 and 2100 are not leap years (despite being divisible by 4), but 1600 and 2000 are leap years.

[added]

Ha ha... I started reading about calendars, and discovered that Sweden once had a year with two leap-days, producing the unique date of February 30, 1712. :cool:
 
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1. What is the difference between actual year/day and earth's movement?

The actual year and day are based on the Earth's movement around the sun and its rotation on its axis, respectively. The Earth's movement is the physical motion of the Earth as it orbits the sun, while its rotation refers to the spinning of the Earth on its axis, causing day and night.

2. How does the Earth's movement affect the length of a year or day?

The Earth's movement is what determines the length of a year and day. The time it takes for the Earth to complete one orbit around the sun is what we call a year, and the time it takes for the Earth to rotate once on its axis is what we call a day. The Earth's movement is also affected by factors such as the tilt of its axis and its elliptical orbit, causing variations in the length of a year or day.

3. Why does the Earth's movement result in different seasons?

The Earth's movement around the sun is not a perfect circle, but rather an elliptical shape. This means that at certain points in its orbit, the Earth is closer or farther away from the sun. The tilt of the Earth's axis also plays a role, as it causes different parts of the Earth to receive more or less direct sunlight, resulting in the changing of seasons as the Earth moves around the sun.

4. How do scientists measure the Earth's movement?

Scientists use a variety of methods to measure the Earth's movement, including astronomical observations, satellite data, and mathematical models. Astronomical observations involve tracking the positions of celestial bodies to determine the Earth's position and movement. Satellite data can also provide precise measurements of the Earth's orbit and rotation. Mathematical models use equations and calculations to predict the Earth's movement and can be verified through observations and data.

5. How has the Earth's movement changed over time?

The Earth's movement has changed over time due to several factors, including gravitational interactions with other planets, changes in the Earth's tilt and orbit, and natural variations in the Earth's rotation. These changes occur over long periods of time and can result in variations in the length of a year or day. Additionally, human activities such as the burning of fossil fuels can also affect the Earth's movement by altering its atmosphere and climate, potentially leading to long-term changes in the Earth's rotation and orbit.

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