Question

The spinning Earth is slowing down. Our days are getting longer. The effect is real, and so we have to add "leap seconds" to our clocks every 100 years to account for it. What is causing this? Also, why is the distance between the Earth and Moon increasing? Use physical concepts.

Answer 1

The year is not exactly 365.25 days long. Our official day is 86,400 seconds long. I won’t go into details on the length of the year itself (you can read a wee bit about it here), but the year we now use is called a Tropical Year and it is 365.242190419 days long. With malice aforethought — my calculator won’t hold that many digits — let’s round it to 365.2421904.

So it’s a bit short of 365.25. That hardly matters, right?

Actually, it does, over time. Even that little bit adds up. After four years, we don’t have 1461 physical days, we have

4 years at 365.2421904 (real) days/year = 1460.968762 days.

That means that when we add a whole day in every four years, we’re adding too much! We should really only add 0.968762 days. But that’s a bit of a pain, so we add in a whole day.

So even though we add a Leap Day in to balance the calendar, it’s still a bit off. It’s a lot better, for sure, but it’s still just a hair out of whack. This time, it’s ahead (since we added a whole day which is too much) by

1 – .968762 days = 0.031238 days, or about 45 minutes.

That’s not a big deal, but you can see that eventually we’ll run into trouble again. The calendar gains 45 minutes every 4 four years. After we’ve had 32 leap years (128 years of calendar time) we’ll be off by a day again!

So we need to adjust our calendar again. But 128 years is hard to remember, so it was decided to round that down to 100 years. After a century, we’ll have added that extra 45 minutes in 25 times (every four years for 100 years = 25 leap years). To be precise, after 100 years the calendar will be off by

25 x 0.031238 days = 0.780950 days.

That’s close enough to a whole day.

Because the Earth and Moon both rotate in the same direction and the earth rotates roughly 27 times faster than the moon, the tidal bulge (towards the moon) is always slightly ahead of an imaginary line connecting the Earth & Moon.

This bulge has a significant mass, and gravitationally attracts the Moon forwards in it's orbit. As such, kinetic energy and angular momentum is gradually drained from the Earth's rotation, while the moon gains it and is thus lifted into a higher orbit.