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We live on a world of wonders. | 0:00:08 | 0:00:10 | |
A place of astonishing beauty and complexity. | 0:00:12 | 0:00:17 | |
We have vast oceans | 0:00:17 | 0:00:19 | |
and incredible weather. | 0:00:19 | 0:00:22 | |
Giant mountains and spectacular landscapes. | 0:00:23 | 0:00:27 | |
If you think that this is all there is, | 0:00:27 | 0:00:30 | |
that our planet exists in magnificent isolation, | 0:00:30 | 0:00:33 | |
then you're wrong. | 0:00:33 | 0:00:34 | |
We're part of a much wider eco-system, | 0:00:36 | 0:00:38 | |
that extends way beyond the top of our atmosphere. | 0:00:38 | 0:00:42 | |
I think we are living through | 0:00:45 | 0:00:48 | |
the greatest age of discovery our civilisation has ever known. | 0:00:48 | 0:00:52 | |
We've voyaged to the farthest reaches of the solar system, | 0:00:52 | 0:00:55 | |
photographed strange new worlds, | 0:00:55 | 0:00:59 | |
stood in unfamiliar landscapes, | 0:00:59 | 0:01:01 | |
tasted alien air. | 0:01:01 | 0:01:04 | |
Amongst all these wonders sits our Earth - | 0:01:09 | 0:01:11 | |
an oasis of calm amidst the violence of the solar system. | 0:01:11 | 0:01:16 | |
And all that separates us | 0:01:18 | 0:01:19 | |
from what's out there is a thin, flimsy envelope of gas - | 0:01:19 | 0:01:26 | |
our atmosphere. | 0:01:26 | 0:01:27 | |
And it's thanks to this "thin blue line" | 0:01:29 | 0:01:31 | |
that we have the air that we breathe, | 0:01:31 | 0:01:34 | |
the water that we drink | 0:01:34 | 0:01:36 | |
and the landscape that surrounds us. | 0:01:36 | 0:01:39 | |
Atmospheres define all the planets in the solar system. | 0:01:41 | 0:01:44 | |
They have the power to create dynamic worlds that are alien and chaotic. | 0:01:47 | 0:01:52 | |
But, remarkably, in the frozen wastes of the solar system... | 0:01:54 | 0:01:58 | |
..one atmosphere has created the most unexpected wonder - | 0:02:00 | 0:02:06 | |
a moon that looks a lot like home. | 0:02:06 | 0:02:09 | |
I've come to Cape Town in South Africa | 0:02:44 | 0:02:46 | |
to do something that I have always wanted to do, | 0:02:46 | 0:02:49 | |
but never thought I would get the chance. | 0:02:49 | 0:02:53 | |
I'm about to fly incredibly high, | 0:02:58 | 0:03:01 | |
to the very edge of the Earth's atmosphere. | 0:03:01 | 0:03:04 | |
From here, I am hoping to see something that only a handful of people have ever seen - | 0:03:08 | 0:03:13 | |
the thin blue line, | 0:03:13 | 0:03:16 | |
the fragile strip of gas that surrounds our whole planet. | 0:03:16 | 0:03:22 | |
And this is what's going to take me there. | 0:03:22 | 0:03:25 | |
This is an English Electric Lightning, | 0:03:30 | 0:03:33 | |
the most beautiful fighter aircraft ever built. | 0:03:33 | 0:03:36 | |
This is when England built the best aircraft in the world. | 0:03:39 | 0:03:42 | |
The Lightning is no longer in service, | 0:03:45 | 0:03:47 | |
but this piece of magnificently overpowered engineering | 0:03:47 | 0:03:53 | |
is going to take me 18 kilometres, straight up. | 0:03:53 | 0:03:56 | |
Actually, I read somewhere that when you read about the altitude | 0:03:57 | 0:04:00 | |
of the Lightning, it says "Altitude: Estimated, 60,000 feet. | 0:04:00 | 0:04:04 | |
"Ceiling: Classified." | 0:04:04 | 0:04:07 | |
So I don't know how high these can go. | 0:04:07 | 0:04:09 | |
I have heard rumours they can go to 80,000 feet, which is amazing. | 0:04:09 | 0:04:14 | |
My journey will take me beyond almost all the molecules of gas that make up our atmosphere. | 0:04:17 | 0:04:23 | |
-If you feel you're going to get sick... -Yeah? -..use a bag, OK? -Right. Hopefully not. | 0:04:23 | 0:04:29 | |
To get there, I'm going to experience | 0:04:36 | 0:04:38 | |
what made the Lightning famous - | 0:04:38 | 0:04:41 | |
a vertical take-off. | 0:04:41 | 0:04:43 | |
Whoo-hoo! | 0:04:55 | 0:04:56 | |
'It takes just seconds to reach nine kilometres up, | 0:05:14 | 0:05:19 | |
'but I'm still in the thickest layer of the atmosphere, | 0:05:19 | 0:05:21 | |
'called the troposphere. | 0:05:21 | 0:05:23 | |
'But the further I climb, the thinner the atmosphere becomes.' | 0:05:24 | 0:05:28 | |
Up at 58,000 feet. 90% of the atmosphere is below me. | 0:05:34 | 0:05:41 | |
The only people above me are on the space station. | 0:05:42 | 0:05:45 | |
So beautiful. | 0:05:50 | 0:05:52 | |
I'm now at 60,000 feet. | 0:05:58 | 0:06:00 | |
'18 kilometres up. | 0:06:00 | 0:06:03 | |
'And the highest I can go.' | 0:06:03 | 0:06:06 | |
Above me, the sky is a deep, dark blue. | 0:06:10 | 0:06:15 | |
'And that is what I've come to see - ' | 0:06:22 | 0:06:25 | |
our atmosphere. | 0:06:25 | 0:06:26 | |
That really is the thin blue line that protects us. | 0:06:33 | 0:06:37 | |
So...fragile and so tenuous. | 0:06:39 | 0:06:42 | |
Just a tiny sliver of blue. | 0:06:44 | 0:06:47 | |
Amazing. | 0:06:51 | 0:06:52 | |
Between 55 and 60,000 feet, inverted, | 0:07:02 | 0:07:06 | |
the curvature of the Earth there. | 0:07:06 | 0:07:09 | |
5G, vertical ascent. | 0:07:09 | 0:07:12 | |
That is just a ride! | 0:07:12 | 0:07:15 | |
It is remarkable to see that. | 0:07:15 | 0:07:17 | |
You can see | 0:07:17 | 0:07:18 | |
the...thinness and fragility, | 0:07:18 | 0:07:22 | |
you can see the atmosphere going from light blue, to dark blue, to black. | 0:07:22 | 0:07:26 | |
It really is astonishing. | 0:07:27 | 0:07:29 | |
The thin blue line makes the Earth the wonderfully diverse place it is. | 0:07:34 | 0:07:40 | |
It acts as a soothing blanket, that traps the warmth of the sun... | 0:07:44 | 0:07:49 | |
..yet protects us from the harshness of its radiation. | 0:07:51 | 0:07:54 | |
Its movements can be traced in the gentlest breeze. | 0:07:59 | 0:08:03 | |
And the most devastating hurricane. | 0:08:05 | 0:08:07 | |
The oxygen and water the atmosphere holds | 0:08:13 | 0:08:17 | |
plays a fundamental role in the ongoing survival | 0:08:17 | 0:08:20 | |
of millions of different species living on the planet. | 0:08:20 | 0:08:24 | |
In this film, I want to explain how the laws of physics | 0:08:27 | 0:08:30 | |
that created our unique atmosphere | 0:08:30 | 0:08:33 | |
are the same laws that created many diverse and different atmospheres | 0:08:33 | 0:08:38 | |
across the solar system. | 0:08:38 | 0:08:40 | |
When perfectly balanced, a world as familiar | 0:08:43 | 0:08:46 | |
and beautiful as the Earth can evolve beneath the clouds. | 0:08:46 | 0:08:50 | |
But the slightest changes can lead to alien and violent worlds. | 0:08:53 | 0:08:58 | |
There are planets in our solar system that have been transformed | 0:09:00 | 0:09:04 | |
into hellish worlds, by nothing more than the gases in their atmosphere. | 0:09:04 | 0:09:09 | |
And just as atmospheres can choke a planet to death, | 0:09:13 | 0:09:16 | |
they are also powerful enough to shape their surfaces. | 0:09:16 | 0:09:20 | |
And there are worlds out there which are all atmosphere. | 0:09:26 | 0:09:30 | |
Giant balls of churning gas, where storms three times | 0:09:32 | 0:09:36 | |
the size of the Earth have raged for hundreds of years. | 0:09:36 | 0:09:40 | |
All atmospheres in the solar system are unique, | 0:09:55 | 0:09:58 | |
but the ingredients and forces that shape them are universal. | 0:09:58 | 0:10:03 | |
At the heart of each is the glue which holds the solar system together, | 0:10:05 | 0:10:11 | |
a fundamental force of nature - | 0:10:11 | 0:10:14 | |
gravity. | 0:10:14 | 0:10:15 | |
Gravity is, by far, the weakest known force in the universe. | 0:10:17 | 0:10:21 | |
You can see that because it's really easy for me to pick a rock up off the ground, | 0:10:23 | 0:10:28 | |
even though there's a whole planet, Earth, pulling the rock down. | 0:10:28 | 0:10:33 | |
I can just lift it up. | 0:10:33 | 0:10:35 | |
Incredibly weak, | 0:10:35 | 0:10:37 | |
but incredibly important, because it's the only force there is | 0:10:37 | 0:10:41 | |
to hold an atmosphere to the planet. | 0:10:41 | 0:10:43 | |
The more massive the planet, the greater its gravitational force. | 0:10:45 | 0:10:49 | |
Earth has enough mass to keep a tight grip of the gas molecules that make up our atmosphere. | 0:10:50 | 0:10:56 | |
It holds them against the surface and allows us to breathe. | 0:10:57 | 0:11:00 | |
Now, we don't really notice the presence | 0:11:03 | 0:11:05 | |
of our atmosphere, I suppose, because we live in it, all the time. | 0:11:05 | 0:11:09 | |
But there's a lot of it. | 0:11:09 | 0:11:11 | |
There's five million billion tons of air surrounding the Earth. | 0:11:11 | 0:11:17 | |
That's the equivalent of a weight of one kilogram | 0:11:17 | 0:11:21 | |
pressing down on every square centimetre of our bodies. | 0:11:21 | 0:11:25 | |
Or, put it another way, if I'm about a metre square, | 0:11:25 | 0:11:28 | |
that's ten tons of weight pressing down. | 0:11:28 | 0:11:32 | |
Now I say pressing down, but that's not entirely right, | 0:11:33 | 0:11:36 | |
that's not how air pressure works. | 0:11:36 | 0:11:38 | |
It presses in every direction at once. I can demonstrate that. | 0:11:38 | 0:11:43 | |
This is a glass full of water, | 0:11:43 | 0:11:45 | |
so if I put a piece of paper on there, turn it upside down. | 0:11:45 | 0:11:51 | |
Now, if I'm right, then the air pressure is pushing | 0:11:51 | 0:11:53 | |
in every direction on this glass of water, the air pressure is pushing up as well as down. | 0:11:53 | 0:11:59 | |
And it has no problem in holding the water in the glass. | 0:12:00 | 0:12:03 | |
Cool. | 0:12:07 | 0:12:08 | |
Where did you get this water from? | 0:12:09 | 0:12:11 | |
CREW LAUGH | 0:12:11 | 0:12:13 | |
Life on the surface of this planet survives, | 0:12:15 | 0:12:19 | |
surrounded by this enormous mass of gas. We're like lobsters, | 0:12:19 | 0:12:24 | |
scuttling around on the ocean floor. | 0:12:24 | 0:12:26 | |
But our atmosphere does more than allow us to breathe. | 0:12:33 | 0:12:37 | |
It protects us | 0:12:37 | 0:12:38 | |
from the most powerful force in the solar system... | 0:12:38 | 0:12:41 | |
..our sun. | 0:12:44 | 0:12:46 | |
If you ask yourself the question, "Why is Earth | 0:12:50 | 0:12:53 | |
"the temperature that it is?" | 0:12:53 | 0:12:55 | |
Then, the obvious answer might seem to be, | 0:12:55 | 0:12:57 | |
"Well, because it's 150m kilometres away from the sun". | 0:12:57 | 0:13:01 | |
But actually, things aren't quite that simple. | 0:13:01 | 0:13:04 | |
This is the Namib desert in Namibia, in south-western Africa. | 0:13:04 | 0:13:08 | |
And as the sun sinks below the horizon, the temperature change, | 0:13:08 | 0:13:13 | |
from day to night, can be as much as 30 degrees Celsius. | 0:13:13 | 0:13:18 | |
That's an immense amount in just a few hours, | 0:13:18 | 0:13:20 | |
much more than in somewhere like Manchester, for example. | 0:13:20 | 0:13:25 | |
The reason is that this is also one of the driest places on the planet | 0:13:25 | 0:13:28 | |
and so there is very little water vapour in the atmosphere. | 0:13:28 | 0:13:32 | |
That means that the atmosphere is not a very good insulator, | 0:13:32 | 0:13:36 | |
so when the sun disappears, the heat just disappears quickly into space. | 0:13:36 | 0:13:42 | |
Now, there's a planet in the solar system, | 0:13:42 | 0:13:44 | |
somewhere over there, near the sun, | 0:13:44 | 0:13:46 | |
where the temperature shift, from day to night, | 0:13:46 | 0:13:49 | |
is not a mere 30 degrees Celsius, but an immense amount bigger. | 0:13:49 | 0:13:53 | |
Roughly 58 million kilometres from the sun | 0:14:14 | 0:14:17 | |
is the smallest planet in the solar system... | 0:14:17 | 0:14:21 | |
..Mercury. | 0:14:25 | 0:14:26 | |
This tortured piece of rock | 0:14:29 | 0:14:31 | |
suffers the biggest temperature swings of all the planets, | 0:14:31 | 0:14:35 | |
from 450 degrees Celsius in the day, | 0:14:35 | 0:14:38 | |
to minus 180 degrees at night. | 0:14:38 | 0:14:43 | |
And all because Mercury has been stripped naked. | 0:14:43 | 0:14:47 | |
It has virtually no atmosphere at all. | 0:14:47 | 0:14:51 | |
Like all the rocky inner planets of the solar system, | 0:15:03 | 0:15:06 | |
Mercury had an atmosphere when it was formed, | 0:15:06 | 0:15:09 | |
but it lost it very quickly. | 0:15:09 | 0:15:11 | |
Here on Earth, | 0:15:11 | 0:15:12 | |
at sea level, then... | 0:15:12 | 0:15:16 | |
Well, in a volume about the size of this pebble, | 0:15:16 | 0:15:20 | |
there are 10 billion billion molecules of gas. | 0:15:20 | 0:15:26 | |
On Mercury, in the same volume, there would be around a 100,000, | 0:15:26 | 0:15:32 | |
that's 10 million million times less. | 0:15:32 | 0:15:34 | |
Now, planets hang on to their atmosphere by the force of gravity. | 0:15:34 | 0:15:39 | |
It's the only way they can | 0:15:39 | 0:15:41 | |
stop that thin blue line of gas disappearing off into space. | 0:15:41 | 0:15:47 | |
So, the bigger the planet, the more massive the planet, | 0:15:47 | 0:15:50 | |
the stronger the gravitational pull and the easier it is for the planet to keep hold of its atmosphere. | 0:15:50 | 0:15:55 | |
So, Mercury was just too small and too hot to hang onto its atmosphere | 0:15:55 | 0:16:02 | |
and the consequences for the planet were absolutely devastating. | 0:16:02 | 0:16:07 | |
Atmospheres may be just a thin strip of molecules, | 0:16:11 | 0:16:15 | |
but they are a planet's first line of defence. | 0:16:15 | 0:16:18 | |
Without them, a planet like Mercury | 0:16:19 | 0:16:23 | |
is at the mercy of our violent solar system. | 0:16:23 | 0:16:27 | |
This is Saskatchewan in western Canada and it is a cold place to be in November. | 0:16:40 | 0:16:46 | |
About a year ago, in November 2008, a piece of asteroid, | 0:16:46 | 0:16:52 | |
a space rock, weighing about ten tons, | 0:16:52 | 0:16:54 | |
entered the atmosphere right over here and actually landed | 0:16:54 | 0:16:59 | |
about 30 kilometres that way, at a place called Buzzard Coulee. | 0:16:59 | 0:17:02 | |
Now, it's not unusual for rocks that big to hit the Earth. | 0:17:02 | 0:17:06 | |
On average, that happens about once a month. | 0:17:06 | 0:17:08 | |
What was unusual about this one was that it was over quite a densely-populated area. | 0:17:08 | 0:17:13 | |
So tens of thousands, if not hundreds of thousands, of people saw it and heard it. | 0:17:13 | 0:17:18 | |
But most spectacularly, it was captured by a lot of CCTV cameras, | 0:17:18 | 0:17:24 | |
including that one, in this garage. | 0:17:24 | 0:17:28 | |
These are the actual CCTV images captured around the city. | 0:17:34 | 0:17:38 | |
They show the meteorite, | 0:17:38 | 0:17:40 | |
as it streaked across the sky at 20 kilometres per second. | 0:17:40 | 0:17:44 | |
The fireball was brighter than the moon and turned the night sky blue. | 0:17:44 | 0:17:49 | |
Scientists used these remarkable images | 0:17:53 | 0:17:56 | |
to triangulate the impact site of the meteorite. | 0:17:56 | 0:18:01 | |
They traced it to a field, just outside the city of Lloydminster. | 0:18:01 | 0:18:06 | |
A team of meteorite hunters have been searching the debris left by the enormous explosion. | 0:18:06 | 0:18:12 | |
They are led by Dr Alan Hildebrand. | 0:18:14 | 0:18:17 | |
How much energy | 0:18:19 | 0:18:20 | |
does a rock like this have, then? | 0:18:20 | 0:18:23 | |
You know, what is it, a ten-ton rock travelling at 50 times the speed of sound? | 0:18:23 | 0:18:27 | |
You know, it would be like if you'd stocked up, | 0:18:27 | 0:18:29 | |
say, 400 tons of TNT to explode. | 0:18:29 | 0:18:33 | |
I mean, it's really quite dramatic. | 0:18:33 | 0:18:35 | |
-400 tons that just dissipates away in the Earth's atmosphere? -Yes. | 0:18:35 | 0:18:39 | |
Atmosphere slowing it down, of course, causing it to break up. | 0:18:39 | 0:18:42 | |
In just five seconds, it's almost all over and, of course, | 0:18:42 | 0:18:47 | |
you know it's an extreme friction, makes the light show. | 0:18:47 | 0:18:50 | |
10% of the energy goes in light and it's like a billion-watt bulb shining high in the sky. | 0:18:50 | 0:18:56 | |
So, what are we looking for? | 0:18:59 | 0:19:00 | |
What does a piece of that asteroid look like? | 0:19:00 | 0:19:03 | |
They... Going through the atmosphere, | 0:19:04 | 0:19:07 | |
the surface has got melted, so you end up with a dark crust on them. | 0:19:07 | 0:19:10 | |
So, essentially, you're looking for an oddly-sculpted dark rock. | 0:19:10 | 0:19:17 | |
-Yeah. -Well, in all fairness, you've got to be able to tell it from, you know the cow patties and so on. | 0:19:17 | 0:19:23 | |
-But... -I could probably manage that. | 0:19:23 | 0:19:25 | |
Once you get your eye in, you'll have no trouble. | 0:19:25 | 0:19:28 | |
We've got one right here. | 0:19:44 | 0:19:46 | |
I'll pick that up. | 0:19:47 | 0:19:49 | |
Astonishing. | 0:19:49 | 0:19:52 | |
It's just been completely rounded off. | 0:19:52 | 0:19:55 | |
Yeah, the heat melted the surface of the rock. | 0:19:55 | 0:19:57 | |
-I mean, how hot does something have to be to do that? -Yeah. | 0:19:57 | 0:20:02 | |
6,000 degrees C would do it. | 0:20:02 | 0:20:05 | |
So, this little rock has had an amazing history. | 0:20:09 | 0:20:13 | |
I mean, it approached Earth as part of this bigger fragment, | 0:20:13 | 0:20:17 | |
at about, what, 18, 19, 20 kilometres per second. | 0:20:17 | 0:20:22 | |
It hit the Earth's atmosphere. | 0:20:22 | 0:20:25 | |
About 85 kilometres up, it began to feel the effects | 0:20:25 | 0:20:31 | |
of the Earth's atmosphere. | 0:20:31 | 0:20:33 | |
It began to squash the air in front of it, creating a pressure wave, | 0:20:33 | 0:20:37 | |
essentially, which, in turn, causes this thing to heat up. | 0:20:37 | 0:20:41 | |
And it would have heated up to something like the temperature of the surface of the sun. | 0:20:41 | 0:20:46 | |
It would have been 5 or 6,000 degrees Celsius as it plummeted through the atmosphere, | 0:20:46 | 0:20:51 | |
lit up the sky over here and then, quite literally, | 0:20:51 | 0:20:56 | |
exploded in a series of explosions and peppered these fields with lumps of rock this big. | 0:20:56 | 0:21:02 | |
Can you imagine standing here on that night and having this, these things - | 0:21:02 | 0:21:07 | |
and this is heavy, right - | 0:21:07 | 0:21:10 | |
raining down from the sky? | 0:21:10 | 0:21:11 | |
It must have been quite incredible. | 0:21:11 | 0:21:13 | |
If the meteorite had hit the ground intact, | 0:21:16 | 0:21:19 | |
the explosion would have been been equivalent to 400 tons of TNT | 0:21:19 | 0:21:24 | |
and left a crater 20 metres wide. | 0:21:24 | 0:21:26 | |
The Earth was spared this colossal impact by nothing more | 0:21:29 | 0:21:35 | |
than the tenuous strip of gases that surrounds us. | 0:21:35 | 0:21:38 | |
But not all planets have this protective blanket. | 0:21:38 | 0:21:42 | |
When a meteorite hits naked Mercury, | 0:21:47 | 0:21:50 | |
there is no atmosphere to break it up or slow it down. | 0:21:50 | 0:21:55 | |
It strikes the ground at full speed and completely intact. | 0:21:57 | 0:22:02 | |
For the last 4.6 billion years, | 0:22:03 | 0:22:06 | |
Mercury has been bombarded with countless asteroids and comets. | 0:22:06 | 0:22:12 | |
The whole history of the planet's violent past is laid out on its surface, | 0:22:14 | 0:22:21 | |
a world pitted with hundreds of thousands of craters. | 0:22:21 | 0:22:26 | |
Craters inside craters, inside craters. | 0:22:27 | 0:22:32 | |
Mercury was damned from the start. | 0:22:55 | 0:22:57 | |
It's simply too small and too hot | 0:22:57 | 0:23:00 | |
to have retained any meaningful traces of atmosphere. | 0:23:00 | 0:23:04 | |
We, on the other hand, | 0:23:04 | 0:23:06 | |
are big enough and cold enough | 0:23:06 | 0:23:09 | |
to have retained this envelope of gases. | 0:23:09 | 0:23:12 | |
That, in turn, allows | 0:23:16 | 0:23:18 | |
living things, like me, to evolve | 0:23:18 | 0:23:21 | |
and to use that atmosphere, to breathe and to live. | 0:23:21 | 0:23:25 | |
But there are places out there in the solar system | 0:23:25 | 0:23:29 | |
whose atmospheres have the same ingredients as our own, | 0:23:29 | 0:23:33 | |
but when the formula is even slightly remixed, | 0:23:33 | 0:23:37 | |
it leads to worlds that couldn't be more different. | 0:23:37 | 0:23:41 | |
Roughly 108 million kilometres from the sun | 0:23:52 | 0:23:55 | |
sits the brightest planet in the solar system, Venus. | 0:23:55 | 0:24:00 | |
This footage shows the luminescent world appear | 0:24:01 | 0:24:04 | |
from behind our cratered moon. | 0:24:04 | 0:24:07 | |
Venus and Earth share many similarities. | 0:24:10 | 0:24:13 | |
We sit next to each other in space, | 0:24:13 | 0:24:16 | |
we were formed from the same material | 0:24:16 | 0:24:19 | |
and we're roughly the same size and share a similar mass and gravity. | 0:24:19 | 0:24:25 | |
But that's where any similarities end. | 0:24:26 | 0:24:29 | |
Venus is a tortured world, | 0:24:29 | 0:24:32 | |
where thick clouds of sulphuric acid are driven along by high winds | 0:24:32 | 0:24:38 | |
and temperatures are hot enough to melt lead. | 0:24:38 | 0:24:42 | |
All because this planet's atmosphere created a runaway greenhouse effect. | 0:24:42 | 0:24:48 | |
The "greenhouse effect" has become a well-known phrase. | 0:24:50 | 0:24:53 | |
You know, it's synonymous with global warming. | 0:24:53 | 0:24:57 | |
But what is it? | 0:24:57 | 0:24:59 | |
Well, a planet, like the Earth, absorbs energy from the sun as visible light. | 0:24:59 | 0:25:05 | |
Now, atmospheres don't absorb much visible light, as you can see, because you can see the sun. | 0:25:05 | 0:25:12 | |
The ground absorbs the visible light, heats up and then re-radiates it. | 0:25:12 | 0:25:18 | |
But it re-radiates it as infrared radiation, heat radiation, if you want. | 0:25:18 | 0:25:23 | |
And atmospheric gases, particularly carbon dioxide, are very good | 0:25:23 | 0:25:27 | |
at absorbing in the infrared and so they trap the heat and the planet heats up. | 0:25:27 | 0:25:33 | |
On Earth, greenhouse gases are essential to our survival. | 0:25:37 | 0:25:41 | |
Without them our planet would be 30 degrees colder, | 0:25:41 | 0:25:45 | |
too cold to support life as we know it. | 0:25:45 | 0:25:49 | |
But Venus's atmosphere was flooded with greenhouse gases. | 0:25:55 | 0:26:01 | |
The nearby sun slowly boiled away its oceans, | 0:26:01 | 0:26:05 | |
pumping water vapour into the atmosphere. | 0:26:05 | 0:26:08 | |
And carbon dioxide, from thousands of erupting volcanoes, | 0:26:09 | 0:26:13 | |
added to the stifling mix. | 0:26:13 | 0:26:16 | |
Venus grew hotter and hotter. | 0:26:17 | 0:26:21 | |
The planet was slowly choked to death. | 0:26:21 | 0:26:24 | |
Venus is a planet with an atmosphere in overdrive, | 0:26:26 | 0:26:31 | |
but Earth's other rocky neighbour tells quite a different story. | 0:26:31 | 0:26:36 | |
Get it! | 0:27:00 | 0:27:02 | |
These are the dunes in the Namib desert. | 0:27:07 | 0:27:09 | |
It's an absolutely spectacular place. | 0:27:09 | 0:27:13 | |
This place is not the hottest, | 0:27:20 | 0:27:21 | |
nor the driest, desert in the world, but these dunes | 0:27:21 | 0:27:25 | |
are some of the oldest sand dunes in the world. | 0:27:25 | 0:27:28 | |
And the reason we're here in the Namib desert | 0:27:32 | 0:27:34 | |
is that this is a great analogue | 0:27:34 | 0:27:37 | |
for the surface of Mars. | 0:27:37 | 0:27:39 | |
This is what the surface of Mars looks like and these dunes, | 0:27:39 | 0:27:42 | |
called barchan dunes, these crescent-shaped dunes, | 0:27:42 | 0:27:45 | |
are the same as the sand dunes on Mars. | 0:27:45 | 0:27:49 | |
So, if you want to get a feel for what it would be like on the surface of Mars, | 0:27:56 | 0:28:00 | |
and you want to know what driving a 4x4 around on it would be like, then this is the place to come. | 0:28:00 | 0:28:06 | |
Incredibly, there is a vehicle driving across the surface of the "red planet" today... | 0:28:11 | 0:28:16 | |
..a space rover, named Opportunity. | 0:28:21 | 0:28:25 | |
The rovers and spacecraft that circle the planet | 0:28:30 | 0:28:33 | |
have sent back images which reveal Mars in exquisite detail. | 0:28:33 | 0:28:38 | |
Mars has vast dunes, | 0:28:47 | 0:28:51 | |
enormous volcanoes | 0:28:51 | 0:28:56 | |
and giant ice sheets. | 0:28:56 | 0:28:59 | |
It has canyons and river valleys. | 0:29:02 | 0:29:06 | |
Mars is a dry, frozen version of our home, covered in red dust and sand. | 0:29:07 | 0:29:14 | |
And it's all due to the fact that Mars has virtually no atmosphere. | 0:29:14 | 0:29:20 | |
But there are clues | 0:29:27 | 0:29:30 | |
that things weren't always this way. | 0:29:30 | 0:29:32 | |
These are pictures taken from the surface of Mars in August 2009. | 0:29:33 | 0:29:39 | |
And they caused quite a bit of excitement, because of this, | 0:29:42 | 0:29:47 | |
this rock sat on the surface of Mars in front of the rover. | 0:29:47 | 0:29:51 | |
This rock is about... | 0:29:51 | 0:29:54 | |
Well, here's a close-up. | 0:29:54 | 0:29:55 | |
It's actually a nickel iron meteorite | 0:29:55 | 0:29:58 | |
and it's about, what, 60 centimetres across, | 0:29:58 | 0:30:01 | |
weighs half a ton. | 0:30:01 | 0:30:03 | |
It came from space, | 0:30:03 | 0:30:07 | |
came through the Martian atmosphere and landed on the ground. | 0:30:07 | 0:30:10 | |
But the mystery is that a meteorite this big, if it hit Mars today, | 0:30:10 | 0:30:15 | |
would disintegrate when it hit the surface. | 0:30:15 | 0:30:17 | |
It would be travelling too fast and that's because | 0:30:17 | 0:30:20 | |
Mars's atmosphere is too thin, too diffuse to slow it down. | 0:30:20 | 0:30:24 | |
But that meteorite is very definitely there | 0:30:26 | 0:30:28 | |
so how could it have made it to the ground? | 0:30:28 | 0:30:32 | |
Well, it must be that, in the past, when this meteorite hit Mars, | 0:30:32 | 0:30:36 | |
Mars' atmosphere was significantly denser, | 0:30:36 | 0:30:39 | |
dense enough to slow this piece of rock down enough | 0:30:39 | 0:30:43 | |
that it could land on the surface intact. | 0:30:43 | 0:30:47 | |
But why did Mars lose its thick atmosphere and become the barren planet we see today? | 0:30:51 | 0:30:57 | |
There are so many ways for planets to lose their atmospheres | 0:30:59 | 0:31:05 | |
that it feels like a miracle that we've still got ours. | 0:31:05 | 0:31:08 | |
But with Mars, it's thought that one of | 0:31:08 | 0:31:10 | |
the dominant mechanisms was interaction with solar winds. | 0:31:10 | 0:31:13 | |
The solar wind is a stream of super-heated, electrically-charged particles | 0:31:18 | 0:31:24 | |
that constantly stream away from the sun at over one million kilometres per hour. | 0:31:24 | 0:31:30 | |
This wave of smashed atoms has the power to strip a planet of its atmosphere. | 0:31:34 | 0:31:40 | |
On Earth, we're protected from this onslaught by an invisible shield | 0:31:47 | 0:31:51 | |
that completely surrounds our planet, known as the magnetosphere. | 0:31:51 | 0:31:57 | |
The magnetosphere is created deep within the Earth's molten iron core. | 0:32:02 | 0:32:08 | |
As the core spins, it generates a powerful magnetic field | 0:32:08 | 0:32:12 | |
which shoots out of the pole and cocoons the whole planet. | 0:32:12 | 0:32:17 | |
This magnetic shield is strong enough to deflect most of the solar wind that comes our way. | 0:32:18 | 0:32:25 | |
Now, we know that at some point in the past, Mars | 0:32:27 | 0:32:31 | |
would also have had a molten core and did have a magnetic field. | 0:32:31 | 0:32:35 | |
But because Mars is a smaller planet than the Earth, | 0:32:35 | 0:32:38 | |
it lost its heat more quickly and the core solidified. | 0:32:38 | 0:32:42 | |
Electric currents could no longer flow and its field vanished. | 0:32:42 | 0:32:46 | |
And that was a major factor in the solar wind being allowed to | 0:32:46 | 0:32:52 | |
blast the planet and strip away its atmosphere. | 0:32:52 | 0:32:55 | |
With no atmosphere to insulate it, this once Earth-like world | 0:33:04 | 0:33:09 | |
transformed into the frozen desert we see today. | 0:33:09 | 0:33:13 | |
A shadow of its former self. | 0:33:15 | 0:33:18 | |
Although Mars has lost most of its atmosphere, | 0:33:26 | 0:33:30 | |
those few molecules that remain still have the power to sculpt and transform the surface. | 0:33:30 | 0:33:36 | |
And that power, that transformative effect, | 0:33:36 | 0:33:41 | |
is present on every planet in the solar system that has an atmosphere. | 0:33:41 | 0:33:45 | |
You can see it transforming the surface of the Namibian desert today as we speak. | 0:33:47 | 0:33:53 | |
It is, of course, the force of nature that we call weather. | 0:33:53 | 0:34:00 | |
We've got to go. Wow! | 0:34:06 | 0:34:11 | |
Weather is a feature of every planet with an atmosphere. | 0:34:11 | 0:34:14 | |
Our world is transformed as this huge mass of air moves across its surface. | 0:34:17 | 0:34:23 | |
But as we look out into the solar system, | 0:34:25 | 0:34:28 | |
we see it only takes the slightest atmosphere to produce extraordinary weather. | 0:34:28 | 0:34:34 | |
Every few years, Mars all but disappears under a maelstrom of dust. | 0:34:37 | 0:34:43 | |
Global dust storms are so huge they dwarf Olympus Mons, | 0:34:47 | 0:34:52 | |
a volcano three times bigger than Everest. | 0:34:52 | 0:34:55 | |
But to experience the most extreme and violent weather in the solar system, | 0:34:59 | 0:35:04 | |
we need to travel to Jupiter. | 0:35:04 | 0:35:06 | |
This banded gas giant is over 140,000 kilometres in diameter. | 0:35:06 | 0:35:13 | |
Its atmosphere isn't a thin blue line, it's many thousand of kilometres thick | 0:35:14 | 0:35:20 | |
and in a constant state of seething motion. | 0:35:20 | 0:35:24 | |
The whole surface boils with gigantic storms. | 0:35:27 | 0:35:31 | |
Yet, this most alien world shares a feature with our own planet. | 0:35:34 | 0:35:38 | |
RUMBLING | 0:35:40 | 0:35:43 | |
Jupiter crackles to the sound of electrical storms. | 0:35:43 | 0:35:48 | |
The bolts of lightning are thousands of times brighter than lightning here on Earth. | 0:35:48 | 0:35:53 | |
The physics of storms on Jupiter is, of course, the same as the physics of storms on Earth. | 0:36:11 | 0:36:16 | |
The warm moist air deep in the atmosphere starts to rise, and as it rises it cools. | 0:36:16 | 0:36:23 | |
And the moisture condenses out to form clouds. | 0:36:23 | 0:36:26 | |
Now, that rising air leaves a gap beneath it, a low pressure area, | 0:36:26 | 0:36:31 | |
and so more warm, moist air is sucked in and that fuels the rise of the storm. | 0:36:31 | 0:36:36 | |
Now, on Earth, those storm systems are driven by the power of the sun. | 0:36:36 | 0:36:41 | |
But therein lies a mystery because the storm systems on Jupiter are far more powerful | 0:36:41 | 0:36:46 | |
and yet Jupiter is five times further away from the sun than the Earth is, | 0:36:46 | 0:36:51 | |
which means it receives 25 times less solar energy. | 0:36:51 | 0:36:56 | |
So, what mechanism could it be that powers those intensely violent storms on Jupiter? | 0:36:56 | 0:37:01 | |
The secret to Jupiter's storm-tossed atmosphere lies hidden deep within the gas giant. | 0:37:07 | 0:37:13 | |
On Earth, we have clear boundaries between the gaseous sky, | 0:37:22 | 0:37:27 | |
the liquid oceans and the solid ground. | 0:37:27 | 0:37:31 | |
But on Jupiter, there are no such boundaries. | 0:37:31 | 0:37:34 | |
It's a gas giant, made of the two lightest and most abundant elements in the universe, | 0:37:39 | 0:37:44 | |
hydrogen and helium. | 0:37:44 | 0:37:46 | |
But as you go deep into Jupiter's atmosphere, | 0:37:46 | 0:37:49 | |
something very strange and interesting happens to those gases. | 0:37:49 | 0:37:54 | |
Jupiter's atmosphere is so thick and its gravitational pull so strong | 0:37:58 | 0:38:02 | |
that 20,000 kilometres beneath the cloud tops, | 0:38:02 | 0:38:06 | |
the pressure is 2,000,000 times greater than the surface pressure here on Earth. | 0:38:06 | 0:38:12 | |
Under such immense pressure, the hydrogen gas in the atmosphere | 0:38:14 | 0:38:18 | |
is transformed into a strange metallic liquid. | 0:38:18 | 0:38:22 | |
As the gases are squeezed, a vast amount of energy is released, | 0:38:24 | 0:38:29 | |
enough energy to fuel some of the biggest storms in the solar system. | 0:38:29 | 0:38:34 | |
The biggest of them all is the Great Red Spot. | 0:38:37 | 0:38:41 | |
This giant anti-cyclone has raged for hundreds of years | 0:38:45 | 0:38:50 | |
and is large enough to swallow the Earth three times over. | 0:38:50 | 0:38:54 | |
The Great Red Spot is an awesome sight. | 0:38:57 | 0:39:01 | |
But this giant isn't one of my wonders. | 0:39:01 | 0:39:06 | |
My wonder is a much smaller world. | 0:39:06 | 0:39:09 | |
A moon that orbits the gas giant Saturn, 1.5 billion kilometres from Earth. | 0:39:11 | 0:39:17 | |
What we have found on this small world is simply astonishing. | 0:39:19 | 0:39:25 | |
If you thought of our moon as the archetypal moon of the solar system, if you like, | 0:39:48 | 0:39:55 | |
then... Well, you might think that all the other moons out there, | 0:39:55 | 0:40:01 | |
hundreds of them, would be dead, uninteresting worlds. | 0:40:01 | 0:40:06 | |
I mean not uninteresting places to visit. | 0:40:06 | 0:40:09 | |
I mean that is, in my view, the greatest thing that humans have ever achieved, | 0:40:09 | 0:40:14 | |
landing on the surface of the moon but it's a dead and lifeless place. | 0:40:14 | 0:40:22 | |
But as we've begun to visit those worlds, as we've flown spacecraft | 0:40:22 | 0:40:26 | |
to within hundreds of miles of their surfaces, we've found that the moons in the outer solar system | 0:40:26 | 0:40:33 | |
are of an astonishingly interesting and varied and fascinated bunch of worlds. | 0:40:33 | 0:40:40 | |
This is Jupiter's moon, Europa. | 0:40:40 | 0:40:44 | |
This is Jupiter's moon, Io, the most volcanic object in the solar system. | 0:40:44 | 0:40:49 | |
But of all the worlds out there, this one - Saturn's moon, Titan - is unique, because of that. | 0:40:49 | 0:40:56 | |
That is an atmosphere, and what an atmosphere it is! | 0:40:56 | 0:41:00 | |
It's 1,000 kilometres deep, it's four times denser than the atmosphere of the Earth. | 0:41:00 | 0:41:07 | |
I mean imagine that, | 0:41:07 | 0:41:09 | |
a moon around a distant planet in the icy, distant reaches of the solar system | 0:41:09 | 0:41:15 | |
with an atmosphere denser and thicker than our own. | 0:41:15 | 0:41:21 | |
Titan has the most Earth-like atmosphere in the entire solar system, | 0:41:28 | 0:41:34 | |
a thick blue line, rich in nitrogen and containing methane. | 0:41:34 | 0:41:40 | |
At first sight, a world this small shouldn't be able to hold onto such a dense atmosphere, | 0:41:41 | 0:41:48 | |
except Titan lies in one of the coldest regions of the solar system, | 0:41:48 | 0:41:53 | |
and that makes all the difference. | 0:41:53 | 0:41:56 | |
Temperature for gases like this, the gases in our atmosphere, | 0:42:02 | 0:42:07 | |
is really a measure of how fast the molecules of the gas are moving around, | 0:42:07 | 0:42:12 | |
and I can demonstrate that with this thing, which is a Chinese lantern. | 0:42:12 | 0:42:18 | |
If I light this fuel, | 0:42:20 | 0:42:23 | |
then what's going to happen... | 0:42:23 | 0:42:25 | |
is that the gas inside is going to heat up. | 0:42:27 | 0:42:31 | |
And as you heat up a gas, | 0:42:33 | 0:42:37 | |
what that basically means is that you speed all the molecules up. | 0:42:37 | 0:42:41 | |
As the molecules of air heat up and move faster, | 0:42:43 | 0:42:48 | |
the air pressure inside the lantern begins to increase. | 0:42:48 | 0:42:51 | |
That means that molecules are forced out, making the air inside less dense than the air outside, | 0:42:51 | 0:42:58 | |
and the lantern gets lighter. | 0:42:58 | 0:43:01 | |
And eventually the lantern is so light... | 0:43:03 | 0:43:07 | |
..that it will just float away in the atmosphere of our planet. | 0:43:09 | 0:43:15 | |
Hot gases have more energy to escape a planet's gravitational pull than cold gases. | 0:43:35 | 0:43:42 | |
Now Titan is a much smaller body than the Earth. It has much weaker gravitational pull, | 0:43:42 | 0:43:50 | |
and if it were in the same region of the solar system as we are, | 0:43:50 | 0:43:53 | |
then it would not be able to hold onto its atmosphere. | 0:43:53 | 0:43:56 | |
But it's a lot further away from the sun than we are | 0:43:56 | 0:44:00 | |
and so that means that it's colder, its atmospheric molecules are moving around much more slowly than ours. | 0:44:00 | 0:44:07 | |
That means that its weak gravity is enough to hold on to that thick dense atmosphere. | 0:44:07 | 0:44:14 | |
Titan's thick atmosphere was an unexpected discovery, | 0:44:17 | 0:44:21 | |
but it took an audacious mission | 0:44:21 | 0:44:24 | |
to reveal the world that lies beneath the blanket of clouds. | 0:44:24 | 0:44:28 | |
We have lift off of the Cassini spacecraft on a billion-mile trek to Saturn. | 0:44:32 | 0:44:36 | |
In 1997, Cassini began its journey to Titan. | 0:44:36 | 0:44:41 | |
It carried with it the Huygens probe, a lander designed to set down on this frozen moon. | 0:44:44 | 0:44:51 | |
On Christmas Day 2004, | 0:44:57 | 0:44:59 | |
Huygens was released from Cassini and it began the bumpy ride | 0:44:59 | 0:45:04 | |
through one of the most intriguing atmospheres in the solar system. | 0:45:04 | 0:45:08 | |
And then, for the first time, | 0:45:11 | 0:45:14 | |
the thick clouds parted and the surface of Titan was revealed. | 0:45:14 | 0:45:19 | |
These are the actual images taken by Huygens | 0:45:27 | 0:45:31 | |
as it slowly parachuted to the surface. | 0:45:31 | 0:45:35 | |
The world it revealed | 0:45:40 | 0:45:42 | |
was more familiar than we could have possibly imagined. | 0:45:42 | 0:45:46 | |
One of the first people to see | 0:45:59 | 0:46:01 | |
these incredible images was a man who helped design the probe, | 0:46:01 | 0:46:05 | |
Ralph Lorenz. | 0:46:05 | 0:46:07 | |
It was amazing because we just had no idea what to expect. | 0:46:07 | 0:46:11 | |
We didn't know whether it would be, you know, cratered like the moon or just sort of a flat expanse of sand | 0:46:11 | 0:46:18 | |
and then these first pictures came back and it was just astonishingly familiar. | 0:46:18 | 0:46:22 | |
Did that picture, that initial series of pictures... | 0:46:22 | 0:46:27 | |
-I suppose it did look somewhat like this, didn't it? -It did. | 0:46:27 | 0:46:30 | |
-It could have been there. -It could have been right here. -I do see that. | 0:46:30 | 0:46:34 | |
I could sit here, | 0:46:34 | 0:46:36 | |
look at that and that's what that picture looks like. | 0:46:36 | 0:46:38 | |
I could take it with a camera. | 0:46:38 | 0:46:40 | |
The camera on the probe was about the height of your knee, so yeah, | 0:46:40 | 0:46:44 | |
the view the Huygens probe had is just like this. | 0:46:44 | 0:46:47 | |
Rounded stones dot the landscape. | 0:46:47 | 0:46:50 | |
They're smooth and look like they have been eroded by tumbling water, | 0:46:50 | 0:46:56 | |
similar to stones found on river beds, here on Earth. | 0:46:56 | 0:46:59 | |
It sounds to me like this was one of the easiest pictures to interpret | 0:47:01 | 0:47:05 | |
in the history of space exploration. | 0:47:05 | 0:47:07 | |
You know, the way you tell it, it's just that's a river bed with these stones. I mean, is it that simple? | 0:47:07 | 0:47:14 | |
Because you can be misled easily, with... | 0:47:14 | 0:47:16 | |
The devil is always in the details, | 0:47:16 | 0:47:18 | |
but I think there were very few people | 0:47:18 | 0:47:21 | |
disputed the interpretation of a river channel. | 0:47:21 | 0:47:24 | |
I mean it's just such a familiar thing to so many people on Earth, there really wasn't much doubt. | 0:47:24 | 0:47:29 | |
It was an extraordinary discovery. | 0:47:32 | 0:47:35 | |
Evidence of flowing rivers had never been found before on a moon. | 0:47:35 | 0:47:40 | |
But it wasn't the only surprise Titan held in store. | 0:47:41 | 0:47:46 | |
This is the Matanuska glacier in Alaska. | 0:48:05 | 0:48:08 | |
It really is one of the most astonishing places I've ever seen. | 0:48:10 | 0:48:15 | |
And this whole landscape is testament to the erosive power of this stuff, | 0:48:18 | 0:48:25 | |
this mixture of ice and rock | 0:48:25 | 0:48:30 | |
as it rolls down this valley over hundreds of thousands of years | 0:48:30 | 0:48:34 | |
and creates this astonishing landscape. | 0:48:34 | 0:48:37 | |
But the reason it can do that | 0:48:46 | 0:48:48 | |
is because of the delicate balance of the Earth's atmosphere. | 0:48:48 | 0:48:52 | |
You see, our planet is just at the right temperature and pressure to allow water to exist as solid, | 0:48:52 | 0:49:00 | |
as liquid and as gas, as vapour in the clouds. | 0:49:00 | 0:49:05 | |
And so the sun can heat up the oceans and it can move the water over the top of the mountains. | 0:49:05 | 0:49:12 | |
It can fall as rain, turn to ice, become a glacier | 0:49:12 | 0:49:17 | |
and then sweep down the valley to sculpt this astonishing landscape. | 0:49:17 | 0:49:23 | |
Just as our atmosphere allows all this to exist, | 0:49:34 | 0:49:39 | |
the atmosphere of Titan is the perfect temperature and pressure to allow something to exist | 0:49:39 | 0:49:45 | |
that has never been seen before on a world beyond Earth. | 0:49:45 | 0:49:50 | |
This is a picture taken of the south pole of Titan | 0:49:56 | 0:50:00 | |
by Cassini in June 2005, | 0:50:00 | 0:50:02 | |
and it's become one of the most important and fascinating pictures | 0:50:02 | 0:50:08 | |
in the history of space exploration. | 0:50:08 | 0:50:12 | |
The interesting thing is this black blob, here. | 0:50:12 | 0:50:15 | |
Now this fascinated the Cassini scientists but the explanation as to what that is | 0:50:17 | 0:50:22 | |
had to wait just over a year till July 2006, | 0:50:22 | 0:50:26 | |
when this picture was taken, | 0:50:26 | 0:50:28 | |
and it's a radar image, this time of the north pole of Titan, | 0:50:28 | 0:50:33 | |
and you see, again, these huge black areas. | 0:50:33 | 0:50:37 | |
The black in this case means that the radar waves that bounced onto them didn't come back | 0:50:37 | 0:50:44 | |
so they're completely black, and there's only one really good explanation for that. | 0:50:44 | 0:50:49 | |
That is that they are incredibly flat surfaces. | 0:50:49 | 0:50:54 | |
In fact, they're surfaces of liquid | 0:50:54 | 0:50:58 | |
so this picture combined with this picture | 0:50:58 | 0:51:02 | |
means that this is the first observation of a liquid, | 0:51:02 | 0:51:08 | |
a lake on the surface of a body other than the Earth in the solar system. | 0:51:08 | 0:51:14 | |
But these lakes, of course, cannot be lakes of liquid water because | 0:51:18 | 0:51:23 | |
the surface temperature on Titan is minus 180 degrees Celsius and, at those temperatures, | 0:51:23 | 0:51:28 | |
water is frozen as hard as steel. | 0:51:28 | 0:51:34 | |
So if these are not lakes of water, then what are they? | 0:51:34 | 0:51:39 | |
This is Lake Eyak in Alaska, just on Prince William Sound, | 0:52:03 | 0:52:08 | |
and I've come here to collect a molecule or a substance that's very abundant on Titan. | 0:52:08 | 0:52:15 | |
In fact, it's abundant throughout the solar system, but here on Earth | 0:52:15 | 0:52:19 | |
it exists as a gas and it bubbles up from the floor of this lake. | 0:52:19 | 0:52:24 | |
The floor of Lake Eyak is covered in rotting vegetation, you know, dead leaves and bits of trees, twigs, | 0:52:37 | 0:52:44 | |
and that's been broken down by bacteria which produce the gas | 0:52:44 | 0:52:47 | |
that bubbles up from the floor of the lake. | 0:52:47 | 0:52:50 | |
That gas is methane and we've been collecting it all night | 0:52:50 | 0:52:55 | |
underneath this upturned boat | 0:52:55 | 0:52:57 | |
so that I can take a sample of it in this bag. | 0:52:57 | 0:53:01 | |
Now, on Earth, methane is very unstable. | 0:53:03 | 0:53:09 | |
If you give it... | 0:53:09 | 0:53:10 | |
a little kick... | 0:53:10 | 0:53:13 | |
in the presence of oxygen, then you get what chemists call an exothermic reaction. | 0:53:13 | 0:53:18 | |
Methane plus oxygen goes to water plus carbon dioxide, and... | 0:53:18 | 0:53:24 | |
some energy. | 0:53:24 | 0:53:26 | |
The Earth's temperature and atmospheric pressure | 0:53:28 | 0:53:31 | |
means methane can only exist as a highly-flammable gas. | 0:53:31 | 0:53:35 | |
But Titan's atmospheric pressure and temperature | 0:53:39 | 0:53:42 | |
is perfect to allow methane to exist as a solid, a gas and, most importantly, | 0:53:42 | 0:53:48 | |
a liquid. | 0:53:48 | 0:53:50 | |
So the images Cassini captured were gigantic lakes of liquid methane... | 0:53:54 | 0:54:00 | |
..the first ever liquid discovered | 0:54:02 | 0:54:05 | |
pooling on the surface of another world in the solar system. | 0:54:05 | 0:54:10 | |
This is Kraken Mare. | 0:54:10 | 0:54:13 | |
At over 400,000 square kilometres, | 0:54:13 | 0:54:17 | |
it's the biggest body of liquid on Titan. | 0:54:17 | 0:54:21 | |
It's almost five times the size of Lake Superior, | 0:54:22 | 0:54:26 | |
North America's greatest lake. | 0:54:26 | 0:54:29 | |
On Titan, methane plays exactly the same role that water does here on Earth. | 0:54:45 | 0:54:52 | |
So, where we have clouds of water, | 0:54:55 | 0:54:59 | |
Titan has clouds of methane with methane rain. | 0:54:59 | 0:55:04 | |
Whereas we have lakes and oceans of water, Titan has lakes of liquid methane. | 0:55:04 | 0:55:12 | |
And whereas, here on Earth, the sun warms the water in the lakes and oceans, | 0:55:12 | 0:55:18 | |
and fills our atmosphere with water vapour, | 0:55:18 | 0:55:21 | |
on Titan the sun lifts the methane | 0:55:21 | 0:55:24 | |
from the lakes and saturates the atmosphere with methane. | 0:55:24 | 0:55:29 | |
So, whereas on Earth we have a hydrological cycle, on Titan there's a methanological cycle. | 0:55:29 | 0:55:35 | |
And rain would be an absolutely magical sight on Titan. | 0:55:38 | 0:55:42 | |
Because the atmosphere is so dense and the gravity of the moon is so weak, | 0:55:42 | 0:55:47 | |
the drops of methane rain would grow to over a centimetre in size | 0:55:47 | 0:55:52 | |
and they would fall to the ground as slowly as snowflakes fall onto the surface of our own planet. | 0:55:52 | 0:56:00 | |
Thousands and thousands of gallons of liquid methane | 0:56:02 | 0:56:07 | |
must have slowly rained down onto the surface, | 0:56:07 | 0:56:11 | |
making rivers and streams swell and burst. | 0:56:11 | 0:56:16 | |
Deep gullies were cut into the frozen water landscape... | 0:56:16 | 0:56:20 | |
Which looks so familiar because it is familiar. | 0:56:20 | 0:56:23 | |
It's this. You know, the atmosphere of Titan shapes the surface in exactly the same way | 0:56:23 | 0:56:31 | |
that the atmosphere here on Earth shapes the surface of our planet. | 0:56:31 | 0:56:37 | |
Titan is like a primordial Earth caught in a deep freeze. | 0:56:48 | 0:56:54 | |
It's almost like looking back in time over four billion years | 0:56:54 | 0:56:58 | |
and observing our planet before life began, and began to modify our atmosphere, | 0:56:58 | 0:57:04 | |
to change it into the oxygen-rich atmosphere that we see today. | 0:57:04 | 0:57:09 | |
In many ways, Titan looks so familiar. | 0:57:13 | 0:57:18 | |
It's a place with rivers and lakes and clouds and rain. | 0:57:18 | 0:57:24 | |
It's a place with water, albeit frozen as hard as steel, | 0:57:24 | 0:57:28 | |
and a place of methane, albeit so cold that methane is now a liquid | 0:57:28 | 0:57:35 | |
and flows and shapes the landscape just like water does here on Earth. | 0:57:35 | 0:57:41 | |
For me, the most important thing about Titan | 0:57:45 | 0:57:50 | |
is we now have two Earth-like worlds in our solar system | 0:57:50 | 0:57:54 | |
One in this warm region, 93 million miles away from the sun, | 0:57:57 | 0:58:03 | |
and the other in deep freeze, a billion miles away from our star | 0:58:03 | 0:58:08 | |
in orbit around another planet, and that must greatly increase the probability | 0:58:08 | 0:58:14 | |
that there are other Earth-like planets in orbit | 0:58:14 | 0:58:17 | |
around the hundreds of billions of stars out there in the universe. | 0:58:17 | 0:58:24 | |
# Somewhere over the rainbow | 0:58:32 | 0:58:38 | |
# Skies are blue | 0:58:38 | 0:58:45 | |
# And the dreams that you dare to dream | 0:58:45 | 0:58:53 | |
# Really do come true. # | 0:58:53 | 0:58:56 | |
E-mail [email protected] | 0:58:56 | 0:58:59 |