Each day is getting slightly longer due to the Moon's gravitational pull on Earth's oceans. Tidal friction slows Earth's rotation by about 2.3 milliseconds per century - meaning days are lengthening by roughly one second every 50,000 years.

Earth's Days Are Getting Longer Due to the Moon

3k viewsPosted 16 years agoUpdated 5 hours ago

You might not notice it in your lifetime, but Earth's days are getting longer. Thanks to the Moon's gravitational tug on our planet, each day is now about 2.3 milliseconds longer per century than it was 100 years ago.

That might sound impossibly small, but it adds up: days lengthen by approximately one second every 50,000 years. Over Earth's 4.5-billion-year history, this has had dramatic effects.

The Moon Is Slowing Us Down

The culprit is tidal friction. As the Moon orbits Earth, its gravity creates bulges in our oceans—the tides. Earth rotates faster than the Moon orbits, so these tidal bulges try to "drag" slightly ahead of the Moon.

The Moon's gravity pulls back on these bulges, acting like a brake on Earth's rotation. At the same time, the tidal bulge pulls the Moon forward in its orbit, causing it to gradually drift away from Earth at about 3.8 centimeters per year.

When Days Were Just 19 Hours Long

Billions of years ago, Earth spun much faster. Research published in the Proceedings of the National Academy of Sciences found that a day on Earth was only about 19 hours long roughly 1.4 billion years ago.

Going back even further, when the Moon first formed about 4.5 billion years ago, it was much closer to Earth and days may have lasted only 5-6 hours. The Moon has been gradually slowing us down ever since.

It's Not Perfectly Steady

While the long-term trend is clear, day length doesn't increase perfectly smoothly. Earth experiences short-term fluctuations in rotation speed due to:

  • Atmospheric changes and wind patterns
  • Ocean currents redistributing mass
  • Movements in Earth's molten core
  • Post-glacial rebound (continents rising after ice sheets melted)

In fact, post-glacial rebound actually speeds up Earth's rotation slightly, shortening days by about 0.6 milliseconds per century and partially offsetting the Moon's effects.

So while you won't get any extra sleep from this phenomenon, Earth's slowing rotation is a reminder that even our planet's most fundamental features—like the length of a day—are constantly evolving.

Frequently Asked Questions

Why are Earth's days getting longer?
Tidal friction from the Moon's gravity is gradually slowing Earth's rotation. The Moon pulls on Earth's tidal bulges, acting like a brake that makes each day about 2.3 milliseconds longer per century.
How much longer is each day getting?
Days are getting longer by approximately 2.3 milliseconds per century, which works out to about one second every 50,000 years.
How long was a day on early Earth?
About 1.4 billion years ago, a day on Earth was only about 19 hours long. When the Moon first formed 4.5 billion years ago, days may have lasted only 5-6 hours.
Is the Moon moving away from Earth?
Yes, the same tidal forces that slow Earth's rotation are pushing the Moon farther away at about 3.8 centimeters per year.
What else affects Earth's rotation speed?
Besides tidal friction, Earth's rotation is affected by atmospheric changes, ocean currents, movements in the molten core, and post-glacial rebound from melting ice sheets.

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