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My name is David Malone. | 0:00:06 | 0:00:09 | |
This is Tynemouth, where I was born. | 0:00:10 | 0:00:14 | |
And the place where my parents came back to when they retired. | 0:00:18 | 0:00:21 | |
What I really remember is standing down there. | 0:00:23 | 0:00:26 | |
Where the guns...? | 0:00:26 | 0:00:28 | |
-No, where the gate is, and watching the waves go by. -Oh, right. | 0:00:28 | 0:00:32 | |
-I used to take you there. -Did you? | 0:00:32 | 0:00:34 | |
I used to go down to this particular sea wall when I was a little lad. | 0:00:42 | 0:00:45 | |
The angle of the wall to the curl of the wave meant that | 0:00:45 | 0:00:49 | |
it always trap air inside the wave, compressing the air, | 0:00:49 | 0:00:53 | |
which would then escape and make this wonderful roaring sound | 0:00:53 | 0:00:56 | |
as the wave came down the length of the wall towards you. | 0:00:56 | 0:01:00 | |
I make science documentaries | 0:01:07 | 0:01:09 | |
and I believe a deeper understanding of waves | 0:01:09 | 0:01:12 | |
can explain our endless fascination with them. | 0:01:12 | 0:01:16 | |
When we started out, this film was supposed to be | 0:01:16 | 0:01:20 | |
about the science of ocean waves. | 0:01:20 | 0:01:22 | |
But it can't be about just that, because waves also give us a window | 0:01:22 | 0:01:27 | |
into how the world actually works, | 0:01:27 | 0:01:30 | |
into the nature of reality. | 0:01:30 | 0:01:32 | |
Because waves have a life cycle, | 0:01:34 | 0:01:36 | |
so they're quite unlike the things that we think of as objects, | 0:01:36 | 0:01:40 | |
like pebbles or cliffs. | 0:01:40 | 0:01:42 | |
They have a birth and a death. | 0:01:42 | 0:01:43 | |
They're a process, and that makes them much more like us. | 0:01:43 | 0:01:47 | |
There's a view that science is merely about totting up numbers | 0:01:53 | 0:01:56 | |
to make them come out right, | 0:01:56 | 0:01:58 | |
while how we make sense of the world should be left to the poets. | 0:01:58 | 0:02:03 | |
I don't think that's right. | 0:02:08 | 0:02:10 | |
Waves in particular is one of those subjects | 0:02:10 | 0:02:13 | |
where the science itself is full of meaning. | 0:02:13 | 0:02:17 | |
Why are waves so fascinating to watch? | 0:02:43 | 0:02:46 | |
Why is it that human beings will sit | 0:02:46 | 0:02:49 | |
and be hypnotised by waves for hours? | 0:02:49 | 0:02:52 | |
We don't normally sit and watch chairs and tables. | 0:02:52 | 0:02:55 | |
All my life I've gazed at the sea breaking on the shore | 0:02:55 | 0:03:00 | |
and wondered what makes each wave different | 0:03:00 | 0:03:03 | |
and why they crash so relentlessly. | 0:03:03 | 0:03:06 | |
I was surprised to discover that the scientific study of waves | 0:03:07 | 0:03:10 | |
began only relatively recently, | 0:03:10 | 0:03:13 | |
and it wasn't idle wave-watching. | 0:03:13 | 0:03:15 | |
It was truly a matter of life and death. | 0:03:15 | 0:03:18 | |
Autumn 1942. | 0:03:25 | 0:03:26 | |
During the Second World War, the first major amphibious landings | 0:03:26 | 0:03:30 | |
were planned to attack German forces in North Africa. | 0:03:30 | 0:03:34 | |
The Allies knew that the landing craft carrying troops ashore | 0:03:37 | 0:03:40 | |
could capsize in waves over six feet high. | 0:03:40 | 0:03:42 | |
It was essential, therefore, to predict the height of the waves. | 0:03:49 | 0:03:52 | |
Scientists found they could calculate wave heights accurately | 0:03:55 | 0:03:58 | |
by measuring the duration and strength of the wind. | 0:03:58 | 0:04:01 | |
The ability to predict waves | 0:04:06 | 0:04:08 | |
led to the success of the landings in North Africa... | 0:04:08 | 0:04:11 | |
..and later on, D-day in France. | 0:04:13 | 0:04:16 | |
To understand these wartime discoveries about waves, | 0:04:27 | 0:04:30 | |
'it's easier to start not at sea, but at Flatford Mill in Suffolk, | 0:04:30 | 0:04:34 | |
'made famous in the painting by Constable.' | 0:04:34 | 0:04:37 | |
Well, we've got a virgin canvas here, ready for waves to start. | 0:04:37 | 0:04:43 | |
'Gavin Pretor-Pinney is an author who studies waves.' | 0:04:45 | 0:04:48 | |
The whole idea of the birth of a wave is a rather intriguing notion. | 0:04:48 | 0:04:52 | |
-It's got to start somewhere. -I hadn't thought about it before. | 0:04:52 | 0:04:55 | |
I suppose what I'm interested in is how does a wave get born? | 0:04:55 | 0:04:59 | |
It does seem a bit like getting something from nothing. | 0:04:59 | 0:05:02 | |
Cos there you've just got water, | 0:05:02 | 0:05:03 | |
and somehow you've got to get a wave out of it. | 0:05:03 | 0:05:06 | |
Well, now the air is quite still. | 0:05:06 | 0:05:09 | |
But in the case of winds out at sea, | 0:05:09 | 0:05:14 | |
there is the wind. | 0:05:14 | 0:05:16 | |
That is the crucial factor. | 0:05:16 | 0:05:18 | |
That's where the energy comes from. | 0:05:18 | 0:05:20 | |
-How? -Well, I'll show you. | 0:05:20 | 0:05:22 | |
I'll get down and I'll be the wind. | 0:05:22 | 0:05:25 | |
OK. | 0:05:25 | 0:05:27 | |
On this little flat bit here... | 0:05:27 | 0:05:30 | |
-Right. -It really very easily happens. | 0:05:43 | 0:05:47 | |
It doesn't require a lot, does it? | 0:05:47 | 0:05:49 | |
And these tiny little ripples that I produce by blowing over the surface, | 0:05:55 | 0:06:02 | |
they're known as capillary waves, these tiny embryonic waves. | 0:06:02 | 0:06:07 | |
The critical factor is the surface tension of the water. | 0:06:07 | 0:06:11 | |
When the water is distorted into a slight crest, | 0:06:11 | 0:06:16 | |
the elastic nature of the surface wants to flatten it down. | 0:06:16 | 0:06:21 | |
In terms of it being a wave that propagates over the surface, | 0:06:21 | 0:06:26 | |
this returning, this restoring force, is critical. | 0:06:26 | 0:06:29 | |
Is that what helps to push it away? | 0:06:29 | 0:06:31 | |
It helps to make the wave move because, | 0:06:31 | 0:06:33 | |
where it's lifted up, the restoring force brings it down, | 0:06:33 | 0:06:36 | |
-and then it overshoots... -Pushing the wave that way. | 0:06:36 | 0:06:38 | |
It continues down below and as the parts of the water go like this, | 0:06:38 | 0:06:42 | |
the actual shape of the wave progresses across the surface. | 0:06:42 | 0:06:45 | |
In the mill pond, as the wind creates a wave, | 0:06:48 | 0:06:51 | |
the surface tension tries to flatten the water. | 0:06:51 | 0:06:54 | |
The result is a regular undulation in the surface. | 0:06:56 | 0:06:59 | |
Naturally, the forces that create waves out at sea | 0:07:06 | 0:07:09 | |
are very much greater. | 0:07:09 | 0:07:11 | |
The sun provides the earth with energy in the form of heat. | 0:07:13 | 0:07:17 | |
This warms the atmosphere and creates the wind. | 0:07:17 | 0:07:21 | |
It is the energy of the wind that in turn creates the waves. | 0:07:21 | 0:07:25 | |
Energy is the invisible force that drives the universe. | 0:07:29 | 0:07:34 | |
Energy can never be destroyed. | 0:07:34 | 0:07:36 | |
It can only change from one form to another. | 0:07:36 | 0:07:38 | |
Even after the wind dies away, the energy lives on in the waves. | 0:07:42 | 0:07:46 | |
These ocean waves are far larger than capillary waves, | 0:07:52 | 0:07:55 | |
and forces other than surface tension take over, | 0:07:55 | 0:07:59 | |
pushing the water down. | 0:07:59 | 0:08:00 | |
-Better get out the way. -Yeah. | 0:08:03 | 0:08:06 | |
'We can see this if we increase the wind at the mill pond.' | 0:08:08 | 0:08:13 | |
Right, let's turn it round here. | 0:08:13 | 0:08:15 | |
That's good. Shall we start her up? | 0:08:20 | 0:08:24 | |
We shall. | 0:08:24 | 0:08:25 | |
LOUD WHIRRING | 0:08:37 | 0:08:41 | |
WHIRRING STOPS | 0:08:54 | 0:08:56 | |
So that, you could see... | 0:08:56 | 0:08:58 | |
God, I can hardly hear now! | 0:08:58 | 0:09:00 | |
You can see that they soon develop into larger than these | 0:09:00 | 0:09:06 | |
2cm-high capillary waves. | 0:09:06 | 0:09:07 | |
And they're continuing much more. | 0:09:07 | 0:09:09 | |
Can you see the bunch of them coming back? | 0:09:09 | 0:09:13 | |
Capillary waves themselves, when they're tiny, they don't go very far, | 0:09:13 | 0:09:16 | |
but once they get larger than a couple of centimetres, | 0:09:16 | 0:09:20 | |
they're known as gravity waves. | 0:09:20 | 0:09:21 | |
Why are they called gravity waves? Why the change of name? | 0:09:21 | 0:09:24 | |
There are two forces that try to return the water to the level. | 0:09:24 | 0:09:28 | |
One is the surface tension that we were talking about | 0:09:28 | 0:09:32 | |
with the capillary waves. The other is the force of gravity. | 0:09:32 | 0:09:35 | |
When the waves are greater than a couple of centimetres, | 0:09:35 | 0:09:38 | |
that becomes the dominant force. | 0:09:38 | 0:09:40 | |
With these larger waves, gravity works just like surface tension. | 0:09:42 | 0:09:47 | |
It pushes the wave down, overshoots, and the wave is propelled forward. | 0:09:47 | 0:09:53 | |
-That's beautiful! Look at that! -That is beautiful. | 0:09:53 | 0:09:55 | |
A very graceful movement, isn't it? | 0:09:55 | 0:09:58 | |
It is lovely. | 0:09:58 | 0:09:59 | |
The thing I was quite sceptical about... | 0:10:06 | 0:10:08 | |
I mean, I knew it intellectually, but there's something about someone | 0:10:08 | 0:10:12 | |
getting down on their knees and blowing onto the surface | 0:10:12 | 0:10:15 | |
of the water making a few ripples, | 0:10:15 | 0:10:17 | |
and then saying, "And that's how you start a Pacific wave." | 0:10:17 | 0:10:20 | |
It doesn't quite grab you that some 40ft monster that | 0:10:21 | 0:10:26 | |
can throw a boat about starts off life as little teeny ripples. | 0:10:26 | 0:10:31 | |
And yet, as soon as you brought the wind machine out, | 0:10:31 | 0:10:34 | |
you could see that that's exactly what it was. | 0:10:34 | 0:10:36 | |
The thing for me about being on the sea is it reminds me | 0:10:45 | 0:10:49 | |
how different an environment the sea is to the land. | 0:10:49 | 0:10:53 | |
Most of us live in cities | 0:10:53 | 0:10:55 | |
where we're cut off from the nature of power and energy. | 0:10:55 | 0:10:59 | |
For us, you just flick a switch and there's power. | 0:10:59 | 0:11:02 | |
It flows through wires, | 0:11:02 | 0:11:03 | |
lights come on, records play and your dinner heats up. | 0:11:03 | 0:11:06 | |
But we're unaware of what power is. | 0:11:06 | 0:11:08 | |
When energy was generated by rushing water, | 0:11:10 | 0:11:14 | |
or even by steam, we had a visceral knowledge of what power was about. | 0:11:14 | 0:11:19 | |
Water rushed by and cogs turned and hammers went up and down. | 0:11:19 | 0:11:23 | |
Today it's all hidden from us | 0:11:23 | 0:11:24 | |
and we live in such a static, calm, quiet environment. | 0:11:24 | 0:11:29 | |
It's not until you come back out on the sea, you're reminded | 0:11:29 | 0:11:32 | |
of the real nature of the dynamic, the powerful side of reality. | 0:11:32 | 0:11:36 | |
For me, what's so exciting about waves | 0:11:39 | 0:11:42 | |
is that they reveal what is normally hidden from view. | 0:11:42 | 0:11:45 | |
You can actually see energy in action. | 0:11:47 | 0:11:49 | |
They provide insight into the forces that rule the universe. | 0:11:52 | 0:11:56 | |
One of the strangest things about waves | 0:11:56 | 0:11:58 | |
is they're not really made of water. | 0:11:58 | 0:12:00 | |
I know it doesn't sound right, but they're really not. | 0:12:00 | 0:12:04 | |
Think about sound. Think about the words I'm saying. | 0:12:06 | 0:12:09 | |
You wouldn't describe them as MADE of air. | 0:12:09 | 0:12:12 | |
You'd say they're vibrations IN the air. | 0:12:12 | 0:12:14 | |
And it's the same for waves. | 0:12:14 | 0:12:16 | |
I've come to Cambridge University to find out more | 0:12:19 | 0:12:22 | |
'about this counterintuitive idea that waves are not made of water. | 0:12:22 | 0:12:27 | |
'Professor Michael McIntyre, a leading physicist and mathematician, | 0:12:27 | 0:12:32 | |
'wants to prove it to me. | 0:12:32 | 0:12:34 | |
'He's fascinated by the relationship between atmosphere and ocean waves.' | 0:12:34 | 0:12:39 | |
What a fab lab, don't you think? | 0:12:39 | 0:12:42 | |
Oh, it's a beautiful lab, and Stuart does a great job | 0:12:42 | 0:12:45 | |
running a facility like this. It's a great tradition in our | 0:12:45 | 0:12:48 | |
department to do experiments as well as mathematical theories. | 0:12:48 | 0:12:52 | |
And I think you need both to understand how things work. | 0:12:52 | 0:12:55 | |
Stuart, can you make a wave break around here? | 0:12:55 | 0:12:58 | |
Certainly. | 0:12:58 | 0:12:59 | |
The gentle waves out here | 0:13:07 | 0:13:09 | |
-aren't moving the water very much except back and forth. -The ducks! | 0:13:09 | 0:13:13 | |
That gives you a visualisation of how much the water is moving. | 0:13:13 | 0:13:17 | |
It is moving a bit, but the main motion is an oscillation. | 0:13:17 | 0:13:20 | |
The ducks are going round in circles. | 0:13:20 | 0:13:23 | |
Yes, they're certainly not travelling with the wave. | 0:13:23 | 0:13:25 | |
Not nearly as much. | 0:13:25 | 0:13:27 | |
So most of the water, then, is just going up and down? | 0:13:27 | 0:13:29 | |
Well, it's actually going in little circles or ellipses. | 0:13:29 | 0:13:32 | |
Watch that duck carefully. You see? | 0:13:32 | 0:13:35 | |
Oh, yes. You can feel that when you stand in the beach. | 0:13:35 | 0:13:38 | |
When the wave passes, it pushes you one way | 0:13:38 | 0:13:40 | |
and then drags you back the other. Is that the same thing? | 0:13:40 | 0:13:43 | |
Yes. That's the oscillatory part of it. | 0:13:43 | 0:13:45 | |
'Professor McIntyre's ducks show it's not the water that's moving' | 0:13:48 | 0:13:52 | |
but the energy. | 0:13:52 | 0:13:54 | |
The water and ducks are essentially stationary. | 0:13:55 | 0:13:58 | |
They go around in a big circle, almost back to where they started | 0:13:58 | 0:14:02 | |
from, while the waves of energy move onwards. | 0:14:02 | 0:14:06 | |
There's a surprising parallel to waves | 0:14:25 | 0:14:27 | |
in an executive toy. | 0:14:27 | 0:14:29 | |
The balls in the middle hardly move, | 0:14:32 | 0:14:34 | |
yet the energy passes through them and out the other side. | 0:14:34 | 0:14:40 | |
The balls are the medium that transmits the energy | 0:14:40 | 0:14:44 | |
just as the water does in waves. | 0:14:44 | 0:14:47 | |
Hello, Dr Porter! | 0:14:50 | 0:14:52 | |
'Physicist Richard Porter has studied waves for 20 years.' | 0:14:52 | 0:14:56 | |
Picked a good morning for it, at least! | 0:14:56 | 0:14:58 | |
-This is beautiful! -'He researches them as a source of power. | 0:14:58 | 0:15:02 | |
'I met him at his open-air wave tank, the sea off North Devon.' | 0:15:03 | 0:15:08 | |
Waves are a form of transport of energy. | 0:15:08 | 0:15:12 | |
That's the way I would describe it. | 0:15:12 | 0:15:14 | |
And the water is what? Just the medium? | 0:15:14 | 0:15:16 | |
The water just acts as the medium. | 0:15:16 | 0:15:18 | |
In this case, it's the water that acts as the medium for | 0:15:18 | 0:15:20 | |
transporting that energy in the form of this wave. | 0:15:20 | 0:15:23 | |
-Like sound going through the air? -Exactly. | 0:15:23 | 0:15:25 | |
I'm talking to you, and the acoustic wave that you're hearing | 0:15:25 | 0:15:28 | |
is a wave which happens to propagate through air using particles of air. | 0:15:28 | 0:15:32 | |
-And out there... -And out there, you just happen to have waves - | 0:15:32 | 0:15:37 | |
the energy which is travelling along the surface of the water. | 0:15:37 | 0:15:40 | |
So there is no net transport of water. | 0:15:40 | 0:15:44 | |
Yes. When we're standing on the beach, | 0:15:44 | 0:15:46 | |
you get the impression that those waves are bringing the water in, | 0:15:46 | 0:15:49 | |
but that is not right. | 0:15:49 | 0:15:50 | |
-No, that's not right. -Because they appear to be bringing it in, | 0:15:50 | 0:15:54 | |
even when the tide's going out. | 0:15:54 | 0:15:55 | |
That's right, and if they were bringing in water, | 0:15:55 | 0:15:58 | |
then we'd all be doomed. Everything would flood. | 0:15:58 | 0:16:01 | |
So that's not what happens. | 0:16:01 | 0:16:03 | |
What you see is the water coming in and going back out again, | 0:16:03 | 0:16:06 | |
on a cycle, with the waves coming against the shore. | 0:16:06 | 0:16:09 | |
When I watch the sea, I love to listen to the sound of the waves. | 0:16:14 | 0:16:17 | |
I learned from Dr Porter that very little of the energy is lost | 0:16:21 | 0:16:24 | |
as a wave travels across the ocean, | 0:16:24 | 0:16:27 | |
but when it breaks on the shore, the energy must go somewhere. | 0:16:27 | 0:16:31 | |
Some energy is absorbed by the sand, | 0:16:40 | 0:16:42 | |
some bounces back into the sea, and some turns into sound. | 0:16:42 | 0:16:47 | |
You've got some water, you've got some air, | 0:16:55 | 0:16:58 | |
you drop the liquid in | 0:16:58 | 0:16:59 | |
and you listen to the sound here. | 0:16:59 | 0:17:01 | |
-Can we do that, then? -Let's have a go. | 0:17:01 | 0:17:03 | |
Let's see what happens. | 0:17:03 | 0:17:04 | |
'Tim Leighton is the bubble man or, more formally, | 0:17:08 | 0:17:12 | |
'Professor of Acoustics at Southampton University.' | 0:17:12 | 0:17:15 | |
OK, here comes the drop. | 0:17:15 | 0:17:16 | |
'We've all heard the drop of a leaky tap. | 0:17:18 | 0:17:20 | |
'But the question is, what exactly is making the noise?' | 0:17:20 | 0:17:25 | |
It hits, forms this crater - lovely crater - | 0:17:25 | 0:17:28 | |
closes, pinches off the bubble... | 0:17:28 | 0:17:30 | |
-That tiny thing there? -That little thing. | 0:17:30 | 0:17:33 | |
All the ripples on the surface, which are very impressive visually, | 0:17:33 | 0:17:37 | |
don't radiate the sound. | 0:17:37 | 0:17:38 | |
It's that tiny little bubble. | 0:17:38 | 0:17:40 | |
When magnified and slowed down, the bubble constantly moves in and out. | 0:17:44 | 0:17:49 | |
It's the vibrations of the bubble, be it from a drop of water or inside | 0:17:52 | 0:17:56 | |
an ocean wave, that produce the noise. | 0:17:56 | 0:18:00 | |
Hidden away amongst them are pulsations, microscopic, | 0:18:00 | 0:18:04 | |
and the pulsation is pushing the water in and out, in and out, | 0:18:04 | 0:18:09 | |
as it expands and contracts. | 0:18:09 | 0:18:12 | |
Until this moment, I'd never realised there WAS a bubble, | 0:18:13 | 0:18:16 | |
let alone that its pulsing made the noise. | 0:18:16 | 0:18:20 | |
When you were talking about bubbles, | 0:18:22 | 0:18:24 | |
there was the temptation to think it's when they pop. | 0:18:24 | 0:18:27 | |
-I was thinking of balloons. -No. | 0:18:27 | 0:18:28 | |
-It's not at all? -I don't think they're kosher bubbles! | 0:18:28 | 0:18:31 | |
-You've got MY kind of bubbles... -When you're president you're going to ban them! | 0:18:31 | 0:18:37 | |
..are pockets of gas surrounded by water. | 0:18:37 | 0:18:39 | |
Now, the other kind of bubble - a soap bubble for example - has gas | 0:18:39 | 0:18:44 | |
-and then a thin wall of liquid and then gas outside. -Right. | 0:18:44 | 0:18:49 | |
But it doesn't have that huge mass of liquid around it, | 0:18:49 | 0:18:53 | |
providing the inertia, so it won't act | 0:18:53 | 0:18:55 | |
like a really powerful sound source like this. | 0:18:55 | 0:18:58 | |
The sound a bubble makes depends on its size. | 0:19:01 | 0:19:04 | |
We can hear this if we release two different-sized bubbles. | 0:19:04 | 0:19:07 | |
What you can see here is the bubble on the left is giving out the big bubbles. | 0:19:11 | 0:19:14 | |
That is the regular, "blonk, blonk, blonk". | 0:19:14 | 0:19:17 | |
The smaller bubble, coming out of the needle on the right, | 0:19:20 | 0:19:25 | |
gives you a high "plink". | 0:19:25 | 0:19:27 | |
-If it's a different size, it gives you a different note. -Pretty much, yes. | 0:19:32 | 0:19:36 | |
It just so happens that these millimetre-size bubbles | 0:19:36 | 0:19:39 | |
give out plinks at the frequencies we can hear, | 0:19:39 | 0:19:43 | |
which is why babbling brooks makes a poetical babble that you can hear. | 0:19:43 | 0:19:48 | |
If the numbers came out differently, the babbling brooks would be silent and we'd have lost all that poetry. | 0:19:48 | 0:19:53 | |
-But as it is... -So wait a minute, | 0:19:53 | 0:19:55 | |
if the bubbles were just way too small, we wouldn't hear them at all. | 0:19:55 | 0:19:58 | |
Yeah, that's right. That's right. The numbers turn out just right | 0:19:58 | 0:20:02 | |
so that the babbling brook and the waterfall and such like are musical. | 0:20:02 | 0:20:06 | |
-Fantastic. -Yeah, it's nice, yeah. -That is quite good, isn't it? | 0:20:06 | 0:20:09 | |
In a wave - obviously I've never even thought of trying to count the bubbles in a wave - | 0:20:12 | 0:20:17 | |
but we were on the beach a couple of weeks ago, | 0:20:17 | 0:20:20 | |
and it was just a wall of Atlantic surf, and it was just white. | 0:20:20 | 0:20:23 | |
It was about, I don't know, eight foot of whiteness, | 0:20:23 | 0:20:26 | |
-that's all bubbles, isn't it? -Where you see white... | 0:20:26 | 0:20:29 | |
Just a metre of that must have been an uncountable number of your bubbles? | 0:20:29 | 0:20:33 | |
Yeah, and each one is giving a noise, | 0:20:33 | 0:20:35 | |
which is why we think of oceans and waterfalls as being noisy, and it is a very powerful noise. | 0:20:35 | 0:20:40 | |
-But we don't think of them being noisy, they are. -They are. | 0:20:40 | 0:20:43 | |
The noise of an ocean wave is made by all the bubbles, all heard at once. | 0:20:45 | 0:20:51 | |
Slow the sound of the wave down far enough... | 0:20:53 | 0:20:56 | |
..and we hear the individual notes, each from a bubble vibrating. | 0:20:58 | 0:21:04 | |
Multiply the bubbles up a trillion-fold and they become the song of the ocean. | 0:21:05 | 0:21:10 | |
Each bubble is like a little bell giving out a very pure note | 0:21:12 | 0:21:15 | |
and what you see there is, you've got a wobbly sea surface, and then a couple of thousand bells, | 0:21:15 | 0:21:22 | |
-and it's obvious where the sound's coming from. -It is now, it is now. | 0:21:22 | 0:21:25 | |
It's not just scientists who want to know what happens to the energy after it's crossed the ocean. | 0:21:30 | 0:21:35 | |
-Morning, gentlemen. -Hello, there. | 0:21:36 | 0:21:40 | |
-Good to see you again. -Morning, mate. | 0:21:40 | 0:21:42 | |
'Surfers also need to predict the arrival of waves.' | 0:21:42 | 0:21:46 | |
-Did you know it was going to be flat today? -Yeah. | 0:21:48 | 0:21:51 | |
How do you predict the waves? | 0:21:51 | 0:21:53 | |
Is it something you have to do with surfing? I presume it is. | 0:21:53 | 0:21:56 | |
The earlier you know the waves are going to be good, | 0:21:56 | 0:21:58 | |
the easier it is to make a decision about where to go surfing. | 0:21:58 | 0:22:01 | |
So you can use, you can check on mobile phones, | 0:22:01 | 0:22:03 | |
I can check out the synoptic weather charts which gives you an idea where the low pressure is going to be. | 0:22:03 | 0:22:08 | |
And ideally when you get here, you want the wind to be blowing off the land, | 0:22:08 | 0:22:11 | |
which will make the waves smoother and give us a cleaner wave to surf. | 0:22:11 | 0:22:14 | |
What we're looking for is one perfect band of energy, really, moving in sets, unaffected by anything else. | 0:22:14 | 0:22:20 | |
What do you mean by a perfect band of energy? | 0:22:20 | 0:22:23 | |
Say there's a storm, north of Scotland and it's nice and tight and it creates one swell, | 0:22:23 | 0:22:27 | |
then that swell travels and over a period of time it becomes formed into nice long lines of waves. | 0:22:27 | 0:22:33 | |
Pulses of energy. | 0:22:33 | 0:22:35 | |
And it's that energy you're looking for. Is that what you're surfing, the energy? | 0:22:35 | 0:22:39 | |
Yeah, we're just looking to ride the energy. | 0:22:39 | 0:22:42 | |
On the perfect days, the water doesn't really move... | 0:22:42 | 0:22:45 | |
-That's fantastic. -..So the energy is just moving through the water. | 0:22:45 | 0:22:48 | |
And the purest experience is the nearest you get to the pure form of energy. | 0:22:59 | 0:23:04 | |
So the oscillations as they come to the shore, as they continue in, | 0:23:04 | 0:23:07 | |
that roundness, that hollowness. | 0:23:07 | 0:23:10 | |
Surfers know all about the energy of the wave and how its energy has to go somewhere. | 0:23:29 | 0:23:36 | |
I love the way surfers understand this as well as any scientist. | 0:23:36 | 0:23:39 | |
Richard Porter has explored why it is that waves contain so much energy. | 0:23:43 | 0:23:48 | |
If you really want to think about how powerful a wave is, | 0:23:48 | 0:23:51 | |
you just think about sitting on a boat, just a little boat, somewhere out to sea, | 0:23:51 | 0:23:55 | |
and imagine you're sitting there and the boat is moving up and down. | 0:23:55 | 0:24:00 | |
But imagine how much power you'd need to give to that boat | 0:24:00 | 0:24:03 | |
just to lift it up and down. And that energy comes from the wave. | 0:24:03 | 0:24:07 | |
If you had to do that on land, it would take a large group of men to lift that up. | 0:24:07 | 0:24:12 | |
-Well, yeah, machinery to do that. -Whereas, on the boat, on the sea... -It just happens, right? | 0:24:12 | 0:24:16 | |
So it is a huge, huge amount of energy in a single wave. | 0:24:16 | 0:24:20 | |
Surface waves are a fantastic way of storing energy | 0:24:20 | 0:24:24 | |
because they take energy, which occupies a three-dimensional space. | 0:24:24 | 0:24:30 | |
Like wind or something. | 0:24:30 | 0:24:32 | |
Wind, it occupies the atmosphere, it's three-dimensional | 0:24:32 | 0:24:35 | |
and it transmits its energy to these surface waves, | 0:24:35 | 0:24:39 | |
these waves that you see on the ocean, which exist upon the surface of the water. | 0:24:39 | 0:24:44 | |
So they've kind of concentrated it. | 0:24:44 | 0:24:46 | |
Yes. So you've taken this three-dimensional space, | 0:24:46 | 0:24:49 | |
full of energy and you've transmitted it into a two-dimensional surface, | 0:24:49 | 0:24:54 | |
and that's a way of focussing the energy. | 0:24:54 | 0:24:57 | |
Which is what you see out there? | 0:24:57 | 0:24:59 | |
Exactly. | 0:24:59 | 0:25:00 | |
Yes. That makes sense to me. | 0:25:04 | 0:25:06 | |
I've always thought of waves as being on the surface of water. | 0:25:30 | 0:25:34 | |
Professor McIntyre showed me that there are other types of wave hidden below. | 0:25:36 | 0:25:42 | |
The energy that creates many of these internal waves doesn't come from wind. | 0:25:43 | 0:25:48 | |
They owe their existence to temperature and salinity differences IN the ocean. | 0:25:49 | 0:25:54 | |
In this tank, the heavy blue liquid lies underneath a lighter clear one. | 0:25:54 | 0:26:00 | |
This sort of thing is more what you see near coasts, | 0:26:00 | 0:26:03 | |
where a river runs out over the ocean and makes an interface. | 0:26:03 | 0:26:06 | |
If you look along... | 0:26:06 | 0:26:08 | |
And I can just see them curve, beginning to go over... | 0:26:08 | 0:26:11 | |
And they're going the other way, so you can have different waves going in different directions. | 0:26:11 | 0:26:15 | |
-And they're not affecting each other. -Not very much. And this comes out of the mathematics. | 0:26:15 | 0:26:20 | |
But is this what you get in the ocean? | 0:26:20 | 0:26:22 | |
You get waves doing something down below and in addition to the surface waves? | 0:26:22 | 0:26:28 | |
Yes, you get them at all levels. You get them on any interface. | 0:26:28 | 0:26:31 | |
There's an air-water interface, there's a water-water interface. | 0:26:31 | 0:26:35 | |
So you get that kind of wave on the surface, that's what we're used to, | 0:26:35 | 0:26:38 | |
and then 20 feet or 50 feet or whatever it is, | 0:26:38 | 0:26:41 | |
you've got this going on, which we don't normally see? | 0:26:41 | 0:26:44 | |
Yes. | 0:26:44 | 0:26:45 | |
Professor McIntyre's work shows that surface waves are just the start. | 0:26:47 | 0:26:52 | |
Beneath them are larger internal waves which run in different directions to those on the surface. | 0:26:52 | 0:26:59 | |
There are some very important waves in the ocean which break sideways, known as Rossby waves. | 0:27:03 | 0:27:08 | |
The thing can move sideways and there's a fundamental sideways wave motion, called Rossby waves. | 0:27:10 | 0:27:17 | |
I walked in here this morning just having one kind of wave! | 0:27:17 | 0:27:20 | |
-I've got about five now. -But if you want to understand the ocean, | 0:27:20 | 0:27:23 | |
-you have to have at least five. I can mention more if you like. -Please don't. | 0:27:23 | 0:27:27 | |
Let's take Rossby waves, cos they're fundamentally important. | 0:27:27 | 0:27:29 | |
To understand how jets form you have to understand Rossby waves | 0:27:29 | 0:27:32 | |
and how they break and they do it all sideways. | 0:27:32 | 0:27:35 | |
-Is that what it is? -If you think of the gulf stream, | 0:27:35 | 0:27:38 | |
it's essentially a jet with Rossby waves on it and they're breaking all the time. | 0:27:38 | 0:27:42 | |
That means they're throwing off eddies, sideways, | 0:27:42 | 0:27:46 | |
and that's a kind of wave breaking, from a Rossby wave perspective. | 0:27:46 | 0:27:49 | |
And that wave breaking is fundamentally how the jets sharpen and maintain themselves. | 0:27:49 | 0:27:55 | |
How they stay narrow. | 0:27:55 | 0:27:57 | |
Rossby waves allow the Gulf Stream to flow like a river | 0:28:00 | 0:28:04 | |
within the Atlantic ocean, for thousands of miles. | 0:28:04 | 0:28:07 | |
Without these sideways eddies, the main current would break up, | 0:28:09 | 0:28:15 | |
the warming effect of the Gulf Stream would disappear and Europe would freeze over. | 0:28:15 | 0:28:20 | |
We have seen how energy travels through water in the ocean | 0:28:28 | 0:28:31 | |
but other waves of energy are found throughout the universe. | 0:28:31 | 0:28:35 | |
The world is actually filled with waves, it's just that we can't see them, generally. | 0:28:37 | 0:28:42 | |
Right here, there are quantum waves, light waves, sound waves. | 0:28:42 | 0:28:46 | |
There are sound waves distorting the air between me and you right now, but we can't see them. | 0:28:46 | 0:28:50 | |
They happen on a time scale that we can't appreciate or physically at a scale we can't appreciate. | 0:28:50 | 0:28:55 | |
The one place where you really see this other reality is in the water. | 0:28:55 | 0:29:00 | |
That's where you can see the waves doing what they do, making the world work. | 0:29:01 | 0:29:06 | |
And once you realise that, you realise that the familiar world, | 0:29:07 | 0:29:12 | |
the static world of rocks and cliffs, is just one side of reality, | 0:29:12 | 0:29:17 | |
there is this other reality where everything is actually in motion, in process. | 0:29:17 | 0:29:21 | |
It is this that makes water waves so fascinating for me. | 0:29:25 | 0:29:29 | |
They're not made of water, so a wave isn't really a tangible object. | 0:29:29 | 0:29:34 | |
Waves are process. | 0:29:34 | 0:29:36 | |
Michael McIntyre recognises that process is the important side of reality, | 0:29:48 | 0:29:52 | |
yet it's often hidden from us. | 0:29:52 | 0:29:55 | |
If we want to understand anything in depth, | 0:29:55 | 0:29:57 | |
we usually find we need to think of it both as objects | 0:29:57 | 0:30:00 | |
and as dynamic processes and see how it all fits together. | 0:30:00 | 0:30:03 | |
I always tell my students, "What is understanding?" Understanding means being able to see something | 0:30:03 | 0:30:08 | |
from more than one viewpoint, make it all consistent, do it in equations, in words, in pictures. | 0:30:08 | 0:30:13 | |
make it all hang together consistently. | 0:30:13 | 0:30:16 | |
Very often we say, "OK, that's an object but if you zoom in you'll see a process." | 0:30:16 | 0:30:21 | |
Do you like that Heraclites quote, | 0:30:21 | 0:30:24 | |
that everything flows and nothing persists, or nothing endures? | 0:30:24 | 0:30:29 | |
Well, I'd agree with him, certainly. | 0:30:29 | 0:30:33 | |
Our whole understanding of the cosmos says that that's the case. | 0:30:33 | 0:30:36 | |
And waves are the archetype for that. | 0:30:36 | 0:30:38 | |
That's why we thought we would make this film on waves, as the science of change. | 0:30:38 | 0:30:43 | |
Because, you can understand that quote and the idea of process, | 0:30:43 | 0:30:48 | |
intellectually, but it's very difficult to see it most places, isn't it? | 0:30:48 | 0:30:52 | |
I mean you can't stare at a table and see it as a process. It's an object. | 0:30:52 | 0:30:56 | |
-But waves, it's right there, isn't it? -Yeah, ordinary waves on the surface of the sea, | 0:30:56 | 0:31:01 | |
they're highly visible, so they give us all sorts of new ideas. | 0:31:01 | 0:31:04 | |
Understanding waves reveals the processes that govern the universe and therefore govern our lives too. | 0:31:09 | 0:31:17 | |
Almost by definition, waves are about the transformation of energy and so are people. | 0:31:17 | 0:31:24 | |
We harness energy to keep us alive, from cradle to grave. | 0:31:26 | 0:31:30 | |
Without this constant throughput of energy, we'd just be a pile of atoms. | 0:31:30 | 0:31:35 | |
Our lives are in continuous change. | 0:31:39 | 0:31:43 | |
As you get older, especially once you've had children, | 0:31:47 | 0:31:51 | |
you start to think that life maybe really is a process. | 0:31:51 | 0:31:55 | |
It stops being just you as a static thing in your life | 0:31:55 | 0:31:59 | |
and suddenly there's a process of your parents getting older and your children coming along, | 0:31:59 | 0:32:05 | |
and life seems somehow to be moving, | 0:32:05 | 0:32:08 | |
like a wave, it's shifting along and you're going with it. | 0:32:08 | 0:32:13 | |
And for me, it was quite a fundamental change. | 0:32:13 | 0:32:17 | |
To have children, to grow older, it's all part of our life-cycle, a dynamic process of change. | 0:32:26 | 0:32:33 | |
Seeing our lives as process is part of a philosophical debate that's long intrigued me. | 0:32:39 | 0:32:46 | |
The debate is over whether it is more fundamental, more true, | 0:32:46 | 0:32:50 | |
to view the world as objects or as processes. | 0:32:50 | 0:32:53 | |
I think most of the time, we see the world as a collection of objects. | 0:33:01 | 0:33:05 | |
This is because so many processes are invisible. | 0:33:10 | 0:33:14 | |
Take the creation and erosion of a coastline. | 0:33:19 | 0:33:22 | |
It happens over thousands of years, a period of time inaccessible to humans. | 0:33:22 | 0:33:27 | |
To us, on the beach, the coastline appears static and inviolable. | 0:33:32 | 0:33:37 | |
Except for waves, virtually everything around us is like this, | 0:33:40 | 0:33:44 | |
and that's perhaps why humans are hard-wired to perceive the world as full of objects. | 0:33:44 | 0:33:50 | |
But Richard Porter, who constantly studies waves, has a different perspective. | 0:33:53 | 0:33:59 | |
Making mountains is a slow process, | 0:33:59 | 0:34:02 | |
but, clearly, it's a very powerful process. | 0:34:02 | 0:34:05 | |
And this is a fast process on that timescale, | 0:34:05 | 0:34:10 | |
-but it's a timescale that we can actually observe. -It's a human one. | 0:34:10 | 0:34:14 | |
And waves are a way of doing that, to remind people, actually, the world isn't a static place, | 0:34:14 | 0:34:21 | |
that it is full of this energy, which is doing things. | 0:34:21 | 0:34:25 | |
Yes. I think that waves in some ways | 0:34:25 | 0:34:32 | |
are almost uniquely placed in that they are essentially things | 0:34:32 | 0:34:38 | |
that are created and destroyed in equal measure. | 0:34:38 | 0:34:42 | |
They're always being created. They're always being destroyed. | 0:34:42 | 0:34:45 | |
And you think of all of the other types of natural forces that you see at work, | 0:34:45 | 0:34:49 | |
and you don't quite see that level of dynamism that you have. | 0:34:49 | 0:34:52 | |
You tend to see one end of the process or the other. | 0:34:52 | 0:34:55 | |
With wind, you see wind generated and then it disappears off somewhere | 0:34:55 | 0:34:59 | |
and you don't really get to know where it goes. | 0:34:59 | 0:35:01 | |
But you've got this continual sort of, these waves coming in, continuously. | 0:35:01 | 0:35:06 | |
It is this permanent exchange of energy. | 0:35:06 | 0:35:09 | |
Professor Markus Kirkilionis uses maths to model the natural world. | 0:35:21 | 0:35:26 | |
He pushes the concept of waves further than anyone else. | 0:35:26 | 0:35:30 | |
-Hello, Professor Kirkilionis. -Nice to meet you. -Nice to meet you too. | 0:35:30 | 0:35:34 | |
We've talked a lot to physicists and I can see why they're interested in waves, | 0:35:34 | 0:35:38 | |
why are they important for maths? Do you see waves when you look around, | 0:35:38 | 0:35:42 | |
when you look in the world, do you see other waves? | 0:35:42 | 0:35:45 | |
Oh, I see waves everywhere, to be honest, yes! | 0:35:45 | 0:35:48 | |
Just look at this marvellous city. | 0:35:48 | 0:35:52 | |
It has spread for centuries. | 0:35:52 | 0:35:55 | |
If you would now give me a map of London, | 0:35:55 | 0:35:59 | |
let's say 500 years ago and we would gradually, every 50 years, look at it, | 0:35:59 | 0:36:04 | |
you would actually see a wave-like structure evolving. | 0:36:04 | 0:36:08 | |
If you compare such a city, | 0:36:08 | 0:36:10 | |
with all its processes that are going on all the time, | 0:36:10 | 0:36:15 | |
you have a lot of similarity to all this, | 0:36:15 | 0:36:18 | |
to the waves in the ocean at a very windy day, where a lot of things are going on. | 0:36:18 | 0:36:23 | |
What is interesting for us in a wave is usually it's dynamic behaviour, that it does something, | 0:36:23 | 0:36:29 | |
it transmits something, like information or energy and... | 0:36:29 | 0:36:33 | |
And also its very, being is slightly more tenuous. That's the thing that's interesting to me. | 0:36:33 | 0:36:38 | |
You look out at buildings and there's this notion that we don't need to worry about them, | 0:36:38 | 0:36:42 | |
they're just going to be there forever. | 0:36:42 | 0:36:44 | |
The energy within a process is always changing. | 0:36:49 | 0:36:51 | |
The energy within an object is locked in place. | 0:36:51 | 0:36:55 | |
But perhaps this constancy of an object is just an illusion. | 0:36:55 | 0:37:00 | |
Whether we can call something a static thing or a dynamic thing, | 0:37:00 | 0:37:07 | |
that really depends on the timescale you are observing it | 0:37:07 | 0:37:11 | |
and that's a general principle that is, of course, also valid in mathematics. | 0:37:11 | 0:37:15 | |
But is it still worth having the distinction between objects and processes? | 0:37:15 | 0:37:19 | |
I mean, take St Paul's. Now is that an object for you? | 0:37:19 | 0:37:24 | |
Well, I think for us humans, it is naturally an object first, | 0:37:24 | 0:37:30 | |
because our lifetime, compared to St Paul's, is much shorter, | 0:37:30 | 0:37:35 | |
so we will not see any change in this object. | 0:37:35 | 0:37:40 | |
Also, the physical forces inside the building, you know, all the atoms, | 0:37:40 | 0:37:44 | |
together, they form something solid which will not change in time, | 0:37:44 | 0:37:50 | |
at least not over the time we both can observe it. | 0:37:50 | 0:37:53 | |
And that is a principle that applies to a lot of mathematical objects as well. | 0:37:53 | 0:37:59 | |
It does work at a mathematical level? | 0:37:59 | 0:38:01 | |
Yes, so typically in the mathematical equations, | 0:38:01 | 0:38:05 | |
you can distinguish between solutions that are constant in time - | 0:38:05 | 0:38:09 | |
we call them equilibrium solutions or steady states - | 0:38:09 | 0:38:12 | |
and other solutions to the same equation that are non-constant - we call them transients, very often. | 0:38:12 | 0:38:20 | |
-And the wave would be typically a transient... -Ah yeah, yeah. | 0:38:20 | 0:38:25 | |
And you can study these objects, for example, in terms of their stability. | 0:38:25 | 0:38:31 | |
So there is this distinction between stability and instability in the world. | 0:38:31 | 0:38:36 | |
Which means the division between object and process, | 0:38:37 | 0:38:40 | |
between a cathedral and a wave, | 0:38:40 | 0:38:44 | |
is actually based on a bedrock of mathematics. | 0:38:44 | 0:38:47 | |
It was mathematics that was central to the work on wave heights | 0:39:08 | 0:39:12 | |
during World War II. | 0:39:12 | 0:39:14 | |
A young oceanographer by the name of Walter Munk | 0:39:16 | 0:39:19 | |
found a way to predict the waves for the invasion of North Africa. | 0:39:19 | 0:39:24 | |
Munk realised that the height of the waves | 0:39:29 | 0:39:31 | |
was directly correlated to the wind energy injected into the waves. | 0:39:31 | 0:39:37 | |
So what were the things that he was looking for? | 0:39:37 | 0:39:39 | |
So he worked out there were three crucial factors | 0:39:39 | 0:39:42 | |
in determining the size of the waves. | 0:39:42 | 0:39:44 | |
One is the strength of the wind | 0:39:44 | 0:39:47 | |
blowing over the surface of the water. | 0:39:47 | 0:39:49 | |
So the strength of the storm winds. | 0:39:49 | 0:39:51 | |
-The second is the duration that that wind is blowing for. -Right. | 0:39:51 | 0:39:55 | |
And the third is what's known as the fetch, | 0:39:55 | 0:39:58 | |
which is the area of sea that the wind is blowing over. | 0:39:58 | 0:40:03 | |
So the longer the fetch is, | 0:40:03 | 0:40:06 | |
the greater the distance that this wind is blowing across. | 0:40:06 | 0:40:09 | |
And these three factors all determine | 0:40:09 | 0:40:12 | |
how much energy the wind gives to the surface of the water. | 0:40:12 | 0:40:15 | |
Imagine the kind of responsibility - | 0:40:15 | 0:40:19 | |
he was 26, 27, and he had the responsibility of determining... | 0:40:19 | 0:40:24 | |
Of picking dates for these amphibious landings in North Africa. | 0:40:24 | 0:40:29 | |
You know, that's a lot of weight on your shoulders. | 0:40:29 | 0:40:32 | |
'After the war, Walter Munk carried on with his research. | 0:40:32 | 0:40:36 | |
'He was the first to suspect | 0:40:36 | 0:40:38 | |
'that the energy contained in a wave is remarkably persistent.' | 0:40:38 | 0:40:42 | |
One of the things he became very interested in | 0:40:42 | 0:40:45 | |
was the progress of ocean waves, having been generated in a storm | 0:40:45 | 0:40:52 | |
and before arriving at some shore. | 0:40:52 | 0:40:54 | |
-Ah, so he's filling in the middle bit. -The middle bit, yeah. | 0:40:54 | 0:40:57 | |
-How far they would travel on their own steam, as it were. -Right. | 0:40:57 | 0:41:02 | |
So from storms that generated the waves off the coast of Antarctica... | 0:41:02 | 0:41:08 | |
-He was trying to follow them? -He followed them, yes. | 0:41:08 | 0:41:11 | |
There are six stations off the coast of Antarctic, | 0:41:11 | 0:41:13 | |
they went up past New Zealand and then past Samoa, Hawaii. | 0:41:13 | 0:41:20 | |
Each of these measuring stations were a few thousands of miles from the last one. | 0:41:20 | 0:41:26 | |
In the North Pacific - the last of their measuring stations - | 0:41:26 | 0:41:31 | |
since there was no island there they used this boat known as FLIP. | 0:41:31 | 0:41:36 | |
-No, you're kidding me! -And it does actually flip! | 0:41:39 | 0:41:42 | |
It was like a Thunderbirds-type thing. | 0:41:42 | 0:41:45 | |
Only the Americans would come up with a boat like that. | 0:41:45 | 0:41:48 | |
Does it really tip up? | 0:41:48 | 0:41:51 | |
One end of the boat goes into the water and the other end sticks out. | 0:41:51 | 0:41:55 | |
That must be slightly alarming. | 0:41:55 | 0:41:58 | |
The reason for this is that they want to | 0:41:58 | 0:42:01 | |
try and get the boat as steady as possible | 0:42:01 | 0:42:03 | |
when there's no land to tether it to. | 0:42:03 | 0:42:06 | |
And the way to do that is to kind of anchor the boat in the water. | 0:42:06 | 0:42:14 | |
-Deeper down. -Deep down, below the motion of the waves. | 0:42:14 | 0:42:17 | |
So it's like sticking a big pendulum... | 0:42:17 | 0:42:20 | |
the weight's at the bottom so is going to be fairly steady. | 0:42:20 | 0:42:23 | |
-Yeah. -That's clever. -The depth... | 0:42:23 | 0:42:25 | |
I don't think I'd have liked to be on that boat though. | 0:42:25 | 0:42:28 | |
I mean, you'd be in the middle of the sea and it'd starts tipping up. | 0:42:28 | 0:42:31 | |
-You've got to make sure you tell everybody when you're going to tip it. Very important. -My God! | 0:42:31 | 0:42:36 | |
And did it work? | 0:42:36 | 0:42:37 | |
Yes, they were certainly able to measure them there | 0:42:37 | 0:42:41 | |
and that was quite late on in the progress of the waves. | 0:42:41 | 0:42:44 | |
-And where would they end up? -They eventually ended up on the coast of Alaska, having... | 0:42:44 | 0:42:48 | |
-The coast of Alaska, all the way from Antarctica? -Yeah. | 0:42:48 | 0:42:53 | |
It was a 7,000 mile journey. Astonishing, really. | 0:42:53 | 0:42:57 | |
How does he know that they're the same waves? | 0:42:57 | 0:42:59 | |
Well, that was really the tricky part of the study. | 0:42:59 | 0:43:05 | |
It was all to do with knowing what they were looking for | 0:43:05 | 0:43:08 | |
so the work that had been done during the war | 0:43:08 | 0:43:11 | |
for measuring how waves develop and change with distance from the storm | 0:43:11 | 0:43:18 | |
was crucial in this. | 0:43:18 | 0:43:19 | |
Because that told them what size the waves ought to be | 0:43:19 | 0:43:24 | |
by the time they reached this area. | 0:43:24 | 0:43:26 | |
And remember, once those waves reached the shore of Alaska | 0:43:26 | 0:43:30 | |
at the far end of this journey, | 0:43:30 | 0:43:32 | |
which took them, incidentally, about two weeks to make this journey... | 0:43:32 | 0:43:37 | |
-7,000 miles in two weeks?! -Yeah. -That's moving along. | 0:43:37 | 0:43:40 | |
They do, don't they, yeah. | 0:43:40 | 0:43:43 | |
But once they reached the other end, | 0:43:43 | 0:43:46 | |
the energy has been spread in this fan-like way over such a large area | 0:43:46 | 0:43:52 | |
that the wave is very, very small by the time they reach it - | 0:43:52 | 0:43:56 | |
just a matter of millimetres in height. | 0:43:56 | 0:43:59 | |
So by the time it gets to Alaska, it's very shallow but... | 0:43:59 | 0:44:04 | |
Very, very broad. | 0:44:04 | 0:44:05 | |
Munk was the first man who actually thought to follow waves | 0:44:10 | 0:44:14 | |
and find out what happened to them. | 0:44:14 | 0:44:16 | |
He followed them over 7,000 miles, an absolutely epic piece of work. | 0:44:16 | 0:44:20 | |
But what he didn't look at was what happened to waves when they come to the end of their life cycle. | 0:44:20 | 0:44:25 | |
When they arrive at the other edge of the sea. | 0:44:25 | 0:44:28 | |
For thousands of miles, | 0:44:31 | 0:44:33 | |
a wave has a perfectly regular undulating shape. | 0:44:33 | 0:44:38 | |
Then as the wave nears the shore, | 0:44:38 | 0:44:40 | |
it rears up into a crest just before it breaks. | 0:44:40 | 0:44:43 | |
Something has caused it to change. | 0:44:43 | 0:44:47 | |
Essentially what happens is, as it comes in towards the shore, | 0:44:48 | 0:44:51 | |
it feels the presence of the beach that much more | 0:44:51 | 0:44:54 | |
and there is suddenly a great difference between what is happening at the top of the wave | 0:44:54 | 0:45:00 | |
and what is happening at the bottom of the wave. | 0:45:00 | 0:45:03 | |
Theoretically, what that does is | 0:45:03 | 0:45:05 | |
the wave at the top wants to move faster than the wave at the bottom | 0:45:05 | 0:45:08 | |
and that's what causes this over-turning. | 0:45:08 | 0:45:10 | |
Because the speed of the wave is dependent upon the depth. | 0:45:10 | 0:45:14 | |
For the most part, out in the ocean, | 0:45:17 | 0:45:18 | |
the depth is so deep that it's all moving at the same speed. | 0:45:18 | 0:45:22 | |
But when you come towards the shore... | 0:45:22 | 0:45:24 | |
The bottom slows down for some reason. | 0:45:24 | 0:45:26 | |
So the bottom has such an impact all of a sudden | 0:45:26 | 0:45:28 | |
that the change in the height is crucial. | 0:45:28 | 0:45:31 | |
'I was curious to see what happens | 0:45:34 | 0:45:36 | |
'when the energy of a wave dissipates, | 0:45:36 | 0:45:39 | |
'with the help, once again, of Professor McIntyre's rubber ducks.' | 0:45:39 | 0:45:43 | |
So down there it's mostly the energy which is moving? | 0:45:43 | 0:45:45 | |
Well, the energy is going much faster. | 0:45:45 | 0:45:48 | |
-See how much faster the crests are than the ducks? -Yes. | 0:45:48 | 0:45:50 | |
That slow drift will take them close to the beach | 0:45:50 | 0:45:53 | |
and watch carefully from now on... | 0:45:53 | 0:45:57 | |
That green duck - look. | 0:45:57 | 0:45:58 | |
Suddenly, it gets swept all the way up to the beach. | 0:45:58 | 0:46:02 | |
That's where the wave motion becomes, as it were, water motion or energy propagation. | 0:46:02 | 0:46:07 | |
So when it curls over there, | 0:46:07 | 0:46:08 | |
it ceases to be just the energy that's moving | 0:46:08 | 0:46:13 | |
and the water does actually move? | 0:46:13 | 0:46:15 | |
Is it basically that you are trying to conserve the energy? | 0:46:15 | 0:46:18 | |
The energy has to go somewhere and it has to grab the water, basically? | 0:46:18 | 0:46:22 | |
Not much energy reflects back out. | 0:46:22 | 0:46:24 | |
So most of it has to accumulate | 0:46:24 | 0:46:26 | |
and that's why you get the sudden violence of the wave breaking. | 0:46:26 | 0:46:30 | |
Look at that. I love that. | 0:46:30 | 0:46:31 | |
It's a wonderful visualisation | 0:46:36 | 0:46:39 | |
-of gentle wave motion becoming violent wave motion. -It is. | 0:46:39 | 0:46:43 | |
You can suddenly, from up there, see it get vertical and then falls over. | 0:46:43 | 0:46:48 | |
-Yes. -I always think waves are a bit like a man carrying a heavy weight that you tip forward. | 0:46:48 | 0:46:53 | |
He can keep going. | 0:46:53 | 0:46:54 | |
He can keep carrying the weight as long as he keeps going forward. | 0:46:54 | 0:46:58 | |
But if he ever has to stop... | 0:46:58 | 0:46:59 | |
Splat! | 0:46:59 | 0:47:00 | |
It's a law of the universe that energy cannot be destroyed | 0:47:06 | 0:47:10 | |
so as the wave reaches the shore, its energy has to go somewhere. | 0:47:10 | 0:47:15 | |
There are a surprising number of options. | 0:47:17 | 0:47:21 | |
There it is, it's travelled all the way across the Atlantic, happily minding its own business. | 0:47:23 | 0:47:27 | |
It gets to the beach and if it was sentient it would be going, | 0:47:27 | 0:47:31 | |
"Oh, my God, we're running out of water!" | 0:47:31 | 0:47:33 | |
Well, it has to do something different, hasn't it? | 0:47:35 | 0:47:39 | |
Yes, it has to do something. | 0:47:39 | 0:47:40 | |
You cannot make the energy vaporise. So it's going, "OK lads, what do we do now?" There's no water left!" | 0:47:40 | 0:47:45 | |
Things are changed. The energy is experiencing something different when it reaches this region here. | 0:47:45 | 0:47:51 | |
-So what does it do? -Well, it breaks. | 0:47:51 | 0:47:53 | |
-Right, so that uses some of the energy. -Yes. | 0:47:53 | 0:47:55 | |
And you see all of the foam | 0:47:55 | 0:47:58 | |
and you hear the noise of the waves breaking - | 0:47:58 | 0:48:01 | |
that's more of the energy. | 0:48:01 | 0:48:02 | |
You're just dissipating energy. | 0:48:02 | 0:48:04 | |
And then presumably, it thumps down onto the sand and that uses a bit? | 0:48:04 | 0:48:08 | |
Exactly, so the sand will absorb energy, | 0:48:08 | 0:48:10 | |
there'll be friction associated with moving the sand. | 0:48:10 | 0:48:14 | |
-It shifts tonnes of sand along with it. -Exactly. | 0:48:14 | 0:48:16 | |
That takes an awful lot amount of energy as well. | 0:48:16 | 0:48:19 | |
Each individual wave was born thousands of miles away, | 0:48:29 | 0:48:33 | |
travelled across the ocean, | 0:48:33 | 0:48:34 | |
and breaks on the shore in a chaotic confusion of energy and mathematics. | 0:48:34 | 0:48:38 | |
In that moment, the wave dies and the energy moves on... | 0:48:42 | 0:48:47 | |
..as heat from friction, | 0:48:52 | 0:48:54 | |
as shifting sand and kinetic energy, | 0:48:54 | 0:48:57 | |
and sound energy from the bubbles. | 0:48:57 | 0:49:00 | |
I wonder if the energy that powers a wave | 0:49:02 | 0:49:05 | |
is similar to the energy that keeps us alive? | 0:49:05 | 0:49:08 | |
Think of the boat on the sea. | 0:49:17 | 0:49:19 | |
The boat is an object that doesn't change. | 0:49:19 | 0:49:22 | |
The waves upon which it rides are nothing but change. | 0:49:22 | 0:49:25 | |
The continued existence of the boat depends on it resisting change. | 0:49:25 | 0:49:29 | |
The continued existence of the waves are that they continually change. | 0:49:29 | 0:49:34 | |
Now think of the man on the boat. | 0:49:34 | 0:49:37 | |
Which one is he most like? | 0:49:37 | 0:49:38 | |
'If you look at a human being, is a human being an object or a process?' | 0:49:40 | 0:49:44 | |
Or do you even buy the distinction? | 0:49:44 | 0:49:46 | |
I would buy the distinction. | 0:49:46 | 0:49:49 | |
It corresponds to different points of view you can naturally have. | 0:49:49 | 0:49:54 | |
I think a body - the man, of course - | 0:49:54 | 0:49:58 | |
is an organism, is a living thing. | 0:49:58 | 0:50:02 | |
So it is something that is a process | 0:50:02 | 0:50:05 | |
because it has to constantly exchange energy, material, | 0:50:05 | 0:50:09 | |
with the environment in order to persist. | 0:50:09 | 0:50:12 | |
I mean, we are constantly feeding, we have metabolism | 0:50:12 | 0:50:16 | |
and of course, we're exchanging all our atoms. | 0:50:16 | 0:50:18 | |
But still we are maintaining our shape | 0:50:18 | 0:50:21 | |
and we can recognise after ten years that we are the same kind of person. | 0:50:21 | 0:50:26 | |
And the same of course holds in a sense for the wave. | 0:50:26 | 0:50:30 | |
I am 48 years old | 0:50:39 | 0:50:40 | |
and there are few atoms inside me | 0:50:40 | 0:50:42 | |
that I would've possessed when I was born. | 0:50:42 | 0:50:45 | |
The oxygen, water and food we consume is all borrowed. | 0:50:50 | 0:50:54 | |
In the same way, an ocean wave borrows the water it passes through. | 0:50:54 | 0:50:58 | |
This idea of human life as a dynamic process intrigues Raymond Tallis, | 0:51:04 | 0:51:10 | |
former professor of geriatric medicine, poet and philosopher. | 0:51:10 | 0:51:16 | |
Do you think that the reason that | 0:51:16 | 0:51:17 | |
making a metaphor between human beings and waves has a believability about it | 0:51:17 | 0:51:22 | |
is that we're not finished objects, we're kind of in flux? | 0:51:22 | 0:51:27 | |
I mean, you can't make much metaphor out of a human being and a cup | 0:51:27 | 0:51:30 | |
because it's finished, there's nothing else happening. | 0:51:30 | 0:51:33 | |
Whereas, with a wave you can. | 0:51:33 | 0:51:35 | |
I think that's profoundly true, actually. | 0:51:35 | 0:51:38 | |
It seems to me that a wave is only completed when it's destroyed | 0:51:38 | 0:51:42 | |
and a life is only completed, in a sense, when it's destroyed. | 0:51:42 | 0:51:47 | |
What is arrival for a wave? | 0:51:48 | 0:51:51 | |
It either bumps into a barrier, in which case it bounces back | 0:51:51 | 0:51:55 | |
and continues or it's dissipated. | 0:51:55 | 0:51:57 | |
It breaks and it's gone. | 0:51:57 | 0:51:58 | |
And it seems to me that the arrival for a wave... | 0:51:58 | 0:52:01 | |
well, the arrival for a life, is dissipation. | 0:52:01 | 0:52:05 | |
Right. It's building up to that? | 0:52:05 | 0:52:07 | |
Yes. That's a bit pessimistic, isn't it? | 0:52:07 | 0:52:10 | |
One mustn't take it too tragically, I guess. | 0:52:10 | 0:52:12 | |
How do you think about your own mortality? | 0:52:12 | 0:52:15 | |
Well, I'm not in favour of it. | 0:52:15 | 0:52:17 | |
It seems to me that it is obviously the central fact of our lives, | 0:52:17 | 0:52:22 | |
that they are finite. | 0:52:22 | 0:52:23 | |
But the fact they've been produced by processes | 0:52:23 | 0:52:26 | |
means that they're going to be | 0:52:26 | 0:52:28 | |
destroyed by processes. Those who live by the laws of physics, | 0:52:28 | 0:52:32 | |
die by the laws of physics, basically. | 0:52:32 | 0:52:34 | |
And then for that reason, | 0:52:34 | 0:52:35 | |
one has to accept it with as good a grace as possible. | 0:52:35 | 0:52:38 | |
At death, the energy that has kept us alive | 0:52:44 | 0:52:46 | |
leaves us as heat and entropy. | 0:52:46 | 0:52:49 | |
I believe that this dissipation of energy at the end of life | 0:52:52 | 0:52:56 | |
is equivalent to the breaking of a wave. | 0:52:56 | 0:52:59 | |
If you've ever seen the moment of death, | 0:53:02 | 0:53:04 | |
it's a very strange thing. | 0:53:04 | 0:53:07 | |
One minute, there's an energy there, and then its gone. | 0:53:07 | 0:53:11 | |
Nothing else has changed, and yet everything has changed. | 0:53:11 | 0:53:14 | |
Because the energy that WAS that person has moved on. | 0:53:14 | 0:53:20 | |
It's easier to consider death as a necessary evil | 0:53:26 | 0:53:30 | |
if you think through what would happen if our lives never changed. | 0:53:30 | 0:53:34 | |
Imagine your perfect day, | 0:53:36 | 0:53:37 | |
where everything is exactly as you want it to be. | 0:53:37 | 0:53:41 | |
Now imagine it repeated the next day. | 0:53:41 | 0:53:44 | |
And the next and all the next week. | 0:53:44 | 0:53:46 | |
How long would it be before your perfect timeless paradise | 0:53:46 | 0:53:49 | |
became absolutely hellish and you wanted out? | 0:53:49 | 0:53:52 | |
You see, we want that process of change. | 0:53:52 | 0:53:55 | |
Think of it this way - would you really want to be able | 0:53:55 | 0:53:59 | |
to keep your parents forever and never having them die? | 0:53:59 | 0:54:03 | |
But the cost would be you could never have any children. | 0:54:03 | 0:54:06 | |
We don't want that, we are transitory beings. | 0:54:06 | 0:54:08 | |
We want the joy of the new, and the cost is, we have to let the old go. | 0:54:08 | 0:54:14 | |
My mother and father have been coming to this spot | 0:54:22 | 0:54:25 | |
ever since I was born | 0:54:25 | 0:54:26 | |
to look at the ruined priory nearby | 0:54:26 | 0:54:29 | |
'and to watch the waves.' | 0:54:29 | 0:54:32 | |
I was just thinking how I must have been, what, | 0:54:32 | 0:54:35 | |
two and half the first time I went to the priory. | 0:54:35 | 0:54:38 | |
-Two and half? -Don't you think? -Really. -Oh, yeah. I used to take you down there. | 0:54:38 | 0:54:43 | |
I remember feeling the railings being quite rough, | 0:54:43 | 0:54:46 | |
and you'd stand there and you'd kind of see the wave coming in. | 0:54:46 | 0:54:49 | |
And you'd see it coming...! | 0:54:49 | 0:54:52 | |
'A few months after we filmed this scene, my mother died.' | 0:55:00 | 0:55:04 | |
'I've actually got lots of photographs of my mum, | 0:55:04 | 0:55:06 | |
'but the only film I have of her we shot for this film,' | 0:55:06 | 0:55:11 | |
and I decided to film her because I realised it was maybe my last chance | 0:55:11 | 0:55:16 | |
because she was dying. | 0:55:16 | 0:55:18 | |
'I realised even as we were filming it' | 0:55:20 | 0:55:24 | |
that there I was making a film about how things are transitory, | 0:55:24 | 0:55:27 | |
and how things have to move on, | 0:55:27 | 0:55:31 | |
and yet here we were taking a photograph of her, | 0:55:31 | 0:55:35 | |
taking a film of her so that somehow I could hold that moment. | 0:55:35 | 0:55:40 | |
Illogical as I knew it was, I still wanted to do it. | 0:55:40 | 0:55:44 | |
'And so it's just the way it's worked out that this film' | 0:55:48 | 0:55:51 | |
and the priory and the waves | 0:55:51 | 0:55:55 | |
have all become inextricably linked for me. | 0:55:55 | 0:55:59 | |
Perhaps I could add something. There is also the compensation of death, | 0:56:03 | 0:56:07 | |
which is to say, without a conclusion there is no sense of form. | 0:56:07 | 0:56:11 | |
There is no sense of rounded meaning. | 0:56:11 | 0:56:15 | |
In many ways, meaning itself cannot be...boundlessly open. | 0:56:15 | 0:56:22 | |
We need closure. We need narrowing. We need sealing off to some extent. | 0:56:22 | 0:56:26 | |
A piece of music would not be enjoyable if went on forever. | 0:56:26 | 0:56:29 | |
And that's why an endless succession of waves, all identical, | 0:56:29 | 0:56:33 | |
would not be very attractive, | 0:56:33 | 0:56:35 | |
however individually beautiful the waves were. | 0:56:35 | 0:56:38 | |
You have to have inflection. When we listen to a clock, | 0:56:38 | 0:56:41 | |
we don't hear "tick tick tick tick". We hear "tick-tock tick-tock", | 0:56:41 | 0:56:45 | |
as if we have to divide in something into a beginning and an end | 0:56:45 | 0:56:49 | |
just to give us some sense of structure and closure. | 0:56:49 | 0:56:52 | |
What's come out of this film for me is I started out thinking | 0:57:10 | 0:57:14 | |
there was this beautiful poetic metaphorical connection between | 0:57:14 | 0:57:19 | |
waves as a process and us and our transitory lives. | 0:57:19 | 0:57:24 | |
I was sure that that was important, but I thought in a poetic way. | 0:57:24 | 0:57:28 | |
What I've learnt is that it's not just poetry, | 0:57:30 | 0:57:34 | |
It's not just a metaphor, | 0:57:34 | 0:57:35 | |
that just as it is the energy in a wave which | 0:57:35 | 0:57:40 | |
forces all of the atoms of the water | 0:57:40 | 0:57:43 | |
into that beautiful and unlikely shape of a wave, | 0:57:43 | 0:57:46 | |
so in us, it's the throughput of energy in our lives which keeps | 0:57:46 | 0:57:50 | |
us and our atoms in this unlikely shape. | 0:57:50 | 0:57:53 | |
And that just as when the energy moves on from a wave and it breaks, | 0:57:53 | 0:57:57 | |
so it is for us. | 0:57:57 | 0:57:59 | |
And so what I've learnt is that | 0:57:59 | 0:58:01 | |
we're not just metaphorically like a wave. | 0:58:01 | 0:58:05 | |
In some really important and scientific way, we ARE a wave. | 0:58:05 | 0:58:11 | |
Subtitles by Red Bee Media Ltd | 0:58:28 | 0:58:32 | |
E-mail [email protected] | 0:58:32 | 0:58:37 |