Waves.mp3
Waves.mp4
Waves-Unplugged-Underground-XIX.mp3
Waves-Unplugged-Underground-XIX.mp4
Waves-intro.mp3
[Intro]
Begin (the waves roll in)
About (to roll back out)
[Verse 1]
General relativity
Never ceases to amaze me
Gradients pullin’ more than the far side
Watching the rising and falling tide
[Chorus]
Begin (the waves roll in)
About (to roll back out)
The waves roll in (again)
The waves roll out (no doubt)
[Bridge]
The sea is calling
(Rising and falling)
It’s rising high
(Toward the sky)
Then, you know
(Falling low)
[Verse 2]
Ah, the inertial force
Of course
Barycenter front and center
Going to divulge her bulge
High and low… here we go
[Chorus]
Begin (the waves roll in)
About (to roll back out)
The waves roll in (again)
The waves roll out (no doubt)
[Bridge]
The sea is calling
(Rising and falling)
[Instrumental, Organ Solo]
It’s rising high
(Toward the sky)
Then, you know
(Falling low)
[Chorus]
Begin (the waves roll in)
About (to roll back out)
The waves roll in (again)
The waves roll out (no doubt)
[Outro]
The sea is calling
(Rising and falling)
A SCIENCE NOTE
Tides on Earth are the result of gravitational interactions between the Earth, the Moon, the Sun, and the warping of spacetime. Here’s a breakdown of how each plays a role:
1. Moon’s Gravity (Primary Influence)
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The Moon’s gravitational pull creates a bulge in Earth’s oceans on the side facing the Moon.
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At the same time, there’s a second bulge on the opposite side of the Earth due to the inertial force (Earth and Moon orbiting a common center of mass, or barycenter).
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These bulges result in two high tides and two low tides each day as the Earth rotates.
2. Sun’s Gravity (Secondary Influence)
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The Sun is much farther away but much more massive, so its gravity also affects tides.
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When the Sun, Moon, and Earth are aligned (during new moon and full moon), their gravitational forces combine, producing spring tides (higher highs and lower lows).
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When the Sun and Moon are at right angles (during first and third quarters), they partially cancel each other out, leading to neap tides (less extreme).
3. Earth’s Rotation
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As the Earth rotates, different areas pass through the tidal bulges, experiencing rising and falling sea levels about every 12.5 hours.
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Earth’s rotation also causes a slight lag, pulling the bulges ahead of the Moon’s position—this has long-term effects, like slowing Earth’s rotation and pushing the Moon farther away over time.
4. Spacetime and Tidal Forces
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According to Einstein’s General Relativity, massive objects like the Moon and the Sun warp spacetime.
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These warps create gravitational gradients—stronger pull on the side closer to the Moon/Sun than on the far side.
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These gradients are what cause tidal forces: the differential in gravitational pull that stretches the Earth and its oceans.
Summary
| Component | Role in Tides |
|---|---|
| Moon | Dominant driver of tides through gravity and tidal bulges |
| Sun | Secondary influence; modulates tide strength |
| Earth’s spin | Causes tidal cycles as regions rotate through bulges |
| Spacetime | Explains how gravitational differences cause stretching |