Tides: Crash Course Astronomy #8


Y’know, if Shakespeare had been an astronomer,
he’d have said that “there is a tide in the affairs of the Universe, and on such a
full sea are we now afloat.” He would’ve been right. You might just think
of tides as the ocean going in and out every day, but in fact what astronomers call tides
are a subtle but inexorable force that have literally shaped most objects in the Universe. And to understand tides, we start with gravity. Gravity is a force, and it weakens with distance.
An important thing to note is that we measure gravity from the center of mass of an object,
not its surface. One way to think of the center of mass of an object is the average position
in an object of all its mass. For an evenly distributed sphere, that’s it’s center. Right now, unless you’re an astronaut, you’re
about 6400 kilometers from the center of the Earth. If you stand up, your head is a couple
of meters farther away from the Earth’s center than your feet. Since gravity weakens
with distance, the force of Earth’s gravity on your head is an eensy weensy bit less than
it is on your feet. How much less? A mere 0.00005%. And that’s way too small for you
to ever notice. But what if you were taller? Well, the taller
you are, the farther your head is from the Earth’s center, and the weaker force it
will feel. If you were, say, about 300 kilometers tall, the force of gravity would drop by about
10% at your head. That probably would be enough to notice, if you weren’t dying from asphyxiation
and, y’know, being 300 kilometers tall. This change in the force of gravity over distance
is what astronomers call the tidal force. When you have a massive object affecting another
object with its gravity, its tidal force depends on several factors. For one thing, it depends
on how strong the gravity is from the first object; the stronger the force of gravity, the stronger
stronger the tidal force will be on the affected object. It also depends on how wide the affected object
is. The wider it is, the more the force of gravity from the first object changes across
it, and the bigger the tidal force. Finally, it depends on how far the affected
object is from the first object. The farther away the affected object is, the lower the
tidal force will be. Tides depend on gravity, and if gravity is weaker, so is the tidal
force. The overall effect of the tidal force is to
stretch an object. You’re applying a stronger force on one end than you are on the other,
so you’re pulling harder on one end. That’ll stretch it! And this is where tidal forces
become very important. Look at the Moon. It has gravity, but much
less than the Earth because it’s less massive. It’s 380,000 kilometers away, so the gravitational
force it has on you is pretty small. And you’re pretty small compared to that distance, just
a couple of meters long from head to feet. But the Earth is big! It’s nearly 13,000
kilometers across. That means the side of the Earth facing the Moon is about 13,000
kilometers closer to the Moon than the other side of the Earth. This is a pretty big distance,
enough for tides to become important. The side of the Earth facing the Moon is pulled
harder by the Moon than the other side of the Earth, so the Earth stretches. It becomes
ever so slightly football-shaped, like a sphere with two bulges, one pointing toward the Moon,
and one pointing away. This is probably the weirdest thing about
tidal forces. You might expect only one bulge, on the side of the Earth facing the Moon.
But remember, we measure gravity from the centers of objects. The side of the Earth
facing the Moon feels a stronger pull toward the Moon than the Earth’s center, so it’s
pulled away from the center. But the side facing away from the Moon feels
a weaker force toward the Moon than the Earth’s center. This means the center of the Earth
is being pulled away from the far side. This is exactly the same as if the far side is
being pulled away from the center, and that’s why you get two bulges on opposite sides of
the Earth. The tidal force is therefore strongest on
the sides of the Earth facing toward and away from the Moon, and weakest halfway in between
them on each side. A lot of the Earth is covered in water, and
water responds to this changing force, this stretching. The water bulges up where the
tidal force is strongest, on opposite sides of the Earth. If there’s a beach on one
of those spots, the water will cover it, and we say it’s high tide. If a beach is where
the tidal force is low, the water’s been pulled away from it, and it’s low tide. But wait a second: The Earth is spinning!
If you’re on the part of the Earth facing the Moon, you’re at high tide. Six hours
later, a quarter of a day, the Earth’s rotation has swept you around to the spot where it’s
low tide. Six hours after that you’re at high tide again, and then another six hours
later you’re at low tide for the second time that day. Finally, a day after you started,
you’re back at high tide once more. And that’s why we have two high tides and
two low tides every day. Very generally speaking, the ocean tide causes the sea level to rise
and fall by a meter or two, every day. Incidentally, the solid Earth can bulge as
well. It’s not as fluid as water, but it can move. The tidal force stretches the solid
Earth by about 30 centimeters. If you just sit in your house all day, you move up and
down by about that much…twice! Like the saying goes, a rising tide lifts
all… surfaces. The Earth’s spin has another effect. Lag
in the water flow means the water can’t respond instantly to the tidal force from
the Moon. The Earth’s spin actually sweeps the bulges forward a bit along the Earth.
So picture this: the bulge nearest the Moon is actually a bit ahead of the Earth-Moon
line. That bulge has mass; not a lot, but some.
Since it has mass, it has gravity, and that pulls on the Moon. It pulls the Moon forward
in its orbit a bit, like pulling on a dog’s leash, accelerating it. The Moon responds
to this tug by going into a higher orbit: The Moon is actually moving away from the
Earth! The rate of recession of the moon has been measured and it’s something like a
few centimeters per year, roughly the same speed your fingernails grow. Now get this: the Moon has gravity. Just as
the bulge is pulling the Moon ahead, the Moon is pulling the bulge back, slowing it down.
Because of friction with the rest of the Earth, this slowing of the bulge is actually slowing
the rotation of the Earth itself, making the day longer. The effect is small, but again
it’s measurable. OK, let’s get a little change of perspective.
Everything I’ve said about the Moon’s tidal effect on the Earth works the other
way, too. The Moon feels tides from the Earth, and they’re pretty strong because the Earth
is more massive and has more gravity than the Moon. Just like Earth, there are two tidal bulges on
the Moon; one facing the Earth and one facing away. Long ago, the Moon was closer to the Earth,
and spinning rapidly. The Moon’s tidal bulges didn’t align with the Earth, and the Earth’s
gravity tugged on them, slowing the Moon’s spin and moving it farther away. As it moved
farther away, the time it took to orbit once around the Earth increased: Its orbital period
got longer. Eventually, the lengthening rotation of the Moon matched how long it took to go
around the Earth. When that happened, the axis of the bulges pointed right at the Earth. That’s why the Moon only shows one face
to us! It spins once per month, and goes around us once per month. If it didn’t spin at
all, over that month we’d see the entire lunar surface. But since it does spin once
per orbit, we only ever see one face. This is called tidal locking, and it’s worked
on nearly every big moon in the solar system; tides from their home planet have matched
their spin and orbital period. These moons all show the same face toward their planet! Now wait a second. If the Moon has gravity,
which causes tides, and is the root cause behind all these shenanigans, what about the
Sun? It’s even bigger than the Moon! Tides depends on the gravity from an object,
and your distance from it. The Sun is far more massive than the Moon, but much farther
away. These two effects largely cancel each other out, and when you do the math, you find
the Sun’s tidal force on the Earth is just about half that of the Moon’s. The way the
Sun’s tidal force and the Moon’s tidal force interact on Earth depends on their geometry,
which changes as the Moon orbits us. At new Moon, the Earth, Moon, and Sun are
in a line. The Moon’s tidal force aligns with the Sun’s, reinforcing it. This means
we get an extra high high tide and an extra low low tide on Earth. We call this the spring
tide. When the Moon is at first quarter, the tidal
bulge from the Moon is 90° around from the Sun’s; high tide from the Moon overlaps
low tide from the Sun. We get a slightly lower high tide, and a slightly higher low tide.
We call those neap tides. The pattern repeats when the Moon is full;
the Moon, Earth, and Sun fall along a line again, and we get spring tides. A week later the Moon
has moved around, and we get neap tides again. Not only that, the Moon orbits the Earth on
an ellipse. When it’s closest to us we feel a stronger effect. If that also happens at
New or Full Moon, we get an added kick to the spring tides. This is called the proxigean tide,
and can lead to flooding in low-lying areas. Unless you live on the coast, I bet you had
no idea tides were so complex! Tides are universal; they work wherever there’s
gravity. If two stars orbit each other, each raises a tide in the other. Just like the
Earth and Moon, that can slow their spin and increase their separation. Many planets orbiting
other stars may be tidally locked to those stars. Near a black hole, where the gravity
is incredibly intense, the tides are so strong they would pull you like taffy into a long,
thin string. Astronomers call this effect… spaghettification. No, seriously, that’s
what we call it! Today you learned that tides are due to the
changing force of gravity over distance. The strength of the tidal force from an object
depends on the gravity of the object, and the size of and distance to the second object.
Tides raise two bulges in an object, creating two high tides and two low tides per day on
Earth. Tides have slowed the Earth’s rotation, moved the Moon away from the Earth, and locked
the Moon’s rotation and orbit so that the Moon always has one side facing us. So. Tide goes in. Tide goes out. It turns
out, I can explain that. Now you can too. Crash Course is produced in association with
PBS Digital Studios. This episode was written by me, Phil Plait. The script was edited by
Blake de Pastino, and our consultant is Dr. Michelle Thaller. It was co-directed by Nicholas
Jenkins and Nicole Sweeney, and the graphics team is Thought Café.

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