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Good evening. | 0:00:27 | 0:00:29 | |
For this programme we're going to go right out | 0:00:29 | 0:00:31 | |
to the edge of our known solar system. | 0:00:31 | 0:00:33 | |
Beyond Jupiter and Saturn there are two more giant planets - | 0:00:33 | 0:00:38 | |
Uranus | 0:00:38 | 0:00:41 | |
and Neptune. | 0:00:41 | 0:00:43 | |
We call them the ice giants because they're | 0:00:43 | 0:00:46 | |
very different from the two gas giants, Jupiter and Saturn. | 0:00:46 | 0:00:49 | |
With me, two experts, both from Oxford. | 0:00:49 | 0:00:52 | |
Dr Leigh Fletcher and Chris Lintott. | 0:00:52 | 0:00:55 | |
Can I ask you, Leigh, so what are the main | 0:00:55 | 0:00:57 | |
differences between the ice giants and the gas giants? | 0:00:57 | 0:01:01 | |
In fact, we knew very little about the ice giants before Voyager 2 | 0:01:01 | 0:01:04 | |
flew past in the late 1980s. | 0:01:04 | 0:01:06 | |
Voyager flew past Uranus and saw a greenish disc with very little | 0:01:06 | 0:01:10 | |
cloud activity taking place over the disc itself. | 0:01:10 | 0:01:12 | |
It was a really boring planet, let's be honest about this! | 0:01:12 | 0:01:16 | |
Lots of scientists looked at it and were disappointed - | 0:01:16 | 0:01:18 | |
we were used to Jupiter and Saturn, | 0:01:18 | 0:01:20 | |
-and seeing incredible storms and banded systems. -You won't see storms and rings there. | 0:01:20 | 0:01:24 | |
They happen, you won't see them. | 0:01:24 | 0:01:26 | |
And in fact that's been revealed in the 25 years since Voyager 2 | 0:01:26 | 0:01:29 | |
that we've got a large data set of Hubble space telescope | 0:01:29 | 0:01:33 | |
and ground-based observations of Uranus, which show that we simply | 0:01:33 | 0:01:36 | |
flew past at a rather boring time | 0:01:36 | 0:01:38 | |
and in fact it's become a lot more active now, with white spots, | 0:01:38 | 0:01:42 | |
incredible colours around the north pole and the south pole. | 0:01:42 | 0:01:45 | |
Uranus and Neptune are twins, they are dissimilar twins. Why? | 0:01:45 | 0:01:49 | |
Voyager 2, when it flew past Uranus, gave us an idea of what we thought and ice giant should be like. | 0:01:49 | 0:01:54 | |
When we got out to Neptune we realised those ideas were again wrong | 0:01:54 | 0:01:58 | |
because Neptune has its own source of internal heat. | 0:01:58 | 0:02:01 | |
It basically emits out more energy that it's receiving from the sun | 0:02:01 | 0:02:06 | |
and that emission of heat is driving a really complicated weather pattern. | 0:02:06 | 0:02:10 | |
We see incredible storms, | 0:02:10 | 0:02:12 | |
such as the great dark spot which was present in Neptune | 0:02:12 | 0:02:14 | |
when Voyager 2 flew past in 1989. | 0:02:14 | 0:02:17 | |
But we haven't got that with Uranus. | 0:02:17 | 0:02:19 | |
Apparently there there's little or no source of internal heat. | 0:02:19 | 0:02:23 | |
Why not? | 0:02:23 | 0:02:25 | |
Well, this has got something to do with the dim, distant past | 0:02:25 | 0:02:28 | |
of our solar system and the way the ice giants formed in the first place. | 0:02:28 | 0:02:32 | |
Something, back in Uranus's distant history, | 0:02:32 | 0:02:35 | |
must have changed the planet into its present inclination. | 0:02:35 | 0:02:39 | |
-Because it's really weird. -It's extremely strange. | 0:02:39 | 0:02:43 | |
What we should say is that Uranus has been tilted completely on its side. | 0:02:43 | 0:02:48 | |
Now, the Earth, and Neptune in fact, have a tilt of about 23 degrees. | 0:02:48 | 0:02:53 | |
-26 for Neptune. -So if this is the sun and this is the Earth, you're there. | 0:02:53 | 0:02:57 | |
There you go. | 0:02:57 | 0:02:58 | |
It means that the planet is rotating like this | 0:02:58 | 0:03:01 | |
so it suffers from seasons in the same way the Earth does. | 0:03:01 | 0:03:05 | |
Uranus, on the other hand, | 0:03:05 | 0:03:07 | |
has got such an extreme tilt that it spends many, many years | 0:03:07 | 0:03:11 | |
with just one pole of the planet | 0:03:11 | 0:03:13 | |
facing towards the sun and, in fact, when we flew past | 0:03:13 | 0:03:16 | |
in 1986, the south pole of Uranus | 0:03:16 | 0:03:18 | |
was pointing straight back towards the sun. | 0:03:18 | 0:03:21 | |
What do you mean by the south pole? | 0:03:21 | 0:03:23 | |
The south pole has been defined by the International Astronomical Union | 0:03:23 | 0:03:28 | |
-as being the pole which we flew past. -Yeah, so stop being awkward. Another point... -Point taken! | 0:03:28 | 0:03:33 | |
There's another critical point here, as well. If this is our... | 0:03:33 | 0:03:37 | |
our Uranus, and the planet's spinning like this, | 0:03:37 | 0:03:39 | |
all the moons are in line with that axis as well. | 0:03:39 | 0:03:42 | |
So why do people think this is tilted? | 0:03:42 | 0:03:45 | |
It can't be, surely? | 0:03:45 | 0:03:47 | |
Well, one of the most popular theories out there today | 0:03:47 | 0:03:50 | |
is that something in the past hit Uranus... | 0:03:50 | 0:03:53 | |
-A large impact. -Some kind of large impact. -Where is it now? | 0:03:53 | 0:03:57 | |
The impact would have melded the two planets together, such that | 0:03:57 | 0:04:02 | |
what we see as Uranus today is the agglomeration | 0:04:02 | 0:04:05 | |
of multiple impacting bodies. | 0:04:05 | 0:04:07 | |
-You don't sound convinced. -I'm not. | 0:04:07 | 0:04:10 | |
So how would you tilt your axis? | 0:04:10 | 0:04:12 | |
Years of planetary migration. Interaction with Uranus | 0:04:12 | 0:04:15 | |
and the other giants gradually tilted it over. | 0:04:15 | 0:04:18 | |
Well, during the migrational period, there is a very good chance | 0:04:18 | 0:04:21 | |
that collisions of this sort were happening. | 0:04:21 | 0:04:24 | |
In fact, the motions in these planets is causing gravitational instabilities | 0:04:24 | 0:04:28 | |
and it's flinging material around all over the place. | 0:04:28 | 0:04:32 | |
I have a silly question, which... You were talking earlier about ice giants, Patrick. | 0:04:32 | 0:04:36 | |
-But we're not looking at ice, we're looking at gas. -Of course. | 0:04:36 | 0:04:40 | |
So why do we call them ice giants - why aren't they just gas giants? | 0:04:40 | 0:04:44 | |
-Cos they're icy! -Well, yes, but where's the ice? | 0:04:44 | 0:04:47 | |
-It's an important point and it does confuse a lot of people. -Confuses me! | 0:04:47 | 0:04:51 | |
The reason we call these things ice giants | 0:04:51 | 0:04:53 | |
is because the material they're actually made of, planetary scientists call ices. | 0:04:53 | 0:04:58 | |
So things like methane, ammonia, water | 0:04:58 | 0:05:00 | |
that have condensed to form solids in the outer solar system. | 0:05:00 | 0:05:03 | |
Now, these have all been incorporated into the interiors of these | 0:05:03 | 0:05:08 | |
two ice giants, but even then they're not ices | 0:05:08 | 0:05:11 | |
as you would imagine water ice being. | 0:05:11 | 0:05:13 | |
If I'd come through the atmosphere and stayed alive, | 0:05:13 | 0:05:17 | |
would I hit a solid icy surface? | 0:05:17 | 0:05:19 | |
You won't hit solid surfaces, you'll see these ices are slowly being pressure cooked. | 0:05:19 | 0:05:23 | |
The pressure is so immense at the centre of these giant planets | 0:05:23 | 0:05:26 | |
that the ices take on a very alien and exotic form. | 0:05:26 | 0:05:29 | |
Now, in Jupiter and Saturn it's hydrogen and helium | 0:05:29 | 0:05:32 | |
which consists of most of the bulk of these planets | 0:05:32 | 0:05:35 | |
and hydrogen takes on something called a metallic form and this is conducting | 0:05:35 | 0:05:39 | |
and that's where we believe we get the magnetic field of the giant planets from. | 0:05:39 | 0:05:43 | |
Now, on Uranus and Neptune, | 0:05:43 | 0:05:45 | |
there isn't as much hydrogen helium | 0:05:45 | 0:05:46 | |
cos there simply wasn't as much available in the outer disc when it formed. | 0:05:46 | 0:05:51 | |
So the thing that gets pressure cooked are these ices | 0:05:51 | 0:05:54 | |
that you're talking about and those ices that are in a sort of molten, | 0:05:54 | 0:05:57 | |
fluid state within the interior, | 0:05:57 | 0:05:59 | |
they are still conducting, | 0:05:59 | 0:06:01 | |
so Uranus and Neptune do have magnetic fields, | 0:06:01 | 0:06:04 | |
but even those are extremely odd - tilted and offset. | 0:06:04 | 0:06:07 | |
-There's a lot that we simply don't know about them. -It occurs to me. | 0:06:07 | 0:06:11 | |
I mean, we talked about the great dark spot a bit | 0:06:11 | 0:06:13 | |
and you now tell me that Uranus is interesting again. | 0:06:13 | 0:06:16 | |
I know I've been abusing Uranus so maybe I should stop being cruel to it. | 0:06:16 | 0:06:20 | |
So over the last quarter century, Uranus, which was dull and bland | 0:06:20 | 0:06:23 | |
at the beginning, seems to have taken on a more Neptune-like appearance. | 0:06:23 | 0:06:27 | |
By that I mean it's become a lot more active. | 0:06:27 | 0:06:30 | |
So it must now be, what, autumn or spring on different bits of Uranus? | 0:06:30 | 0:06:35 | |
So the north pole of Uranus is slowly coming into sunlight | 0:06:35 | 0:06:38 | |
for the first time in 40 years. It takes eight years to go round | 0:06:38 | 0:06:41 | |
so it's springtime in the northern hemisphere and that means | 0:06:41 | 0:06:44 | |
suddenly you've got energy being deposited from the sun into Uranus's atmosphere, | 0:06:44 | 0:06:49 | |
which is triggering all these fantastic weather-like systems. | 0:06:49 | 0:06:52 | |
And that's why I believe we must ultimately send another space craft back to Uranus | 0:06:52 | 0:06:57 | |
other than Voyager 2. Voyager 2 flew past so quickly, it gave us just a snapshot | 0:06:57 | 0:07:02 | |
-of the dynamics... -We want a Uranus orbiter. | 0:07:02 | 0:07:05 | |
We would love to see something going into orbit around Uranus | 0:07:05 | 0:07:07 | |
to explore the moons and to explore the rings of Uranus | 0:07:07 | 0:07:10 | |
and the atmosphere and interior, | 0:07:10 | 0:07:12 | |
but I think the big step change in our understanding of ice giants in general | 0:07:12 | 0:07:17 | |
would be if we were to send a probe into Uranus. | 0:07:17 | 0:07:21 | |
Now, we did this once with Jupiter, back in 1995. | 0:07:21 | 0:07:23 | |
The Galileo probe went in and sampled the gases and figured out what the chemical make-up of Jupiter was. | 0:07:23 | 0:07:29 | |
But if we did that for an ice giant as well, | 0:07:29 | 0:07:31 | |
it would be a wonderful advance for our science. | 0:07:31 | 0:07:34 | |
Both Uranus and Neptune have rings and satellites, so what about them? | 0:07:34 | 0:07:40 | |
I think the most interesting out of all of the Uranus and Neptunian moons | 0:07:40 | 0:07:45 | |
is a moon called Triton. Now, Triton is a big moon in orbit around Neptune. | 0:07:45 | 0:07:49 | |
-Not a genuine moon, though. -But it's not a genuine moon. | 0:07:49 | 0:07:52 | |
By that we mean that instead of forming from the same disc that Neptune formed from, | 0:07:52 | 0:07:56 | |
it looks like it's been captured by Neptune's gravitational pull. | 0:07:56 | 0:08:01 | |
-We know that cos it's going backwards. -It's going in a different direction to all of the other moons. | 0:08:01 | 0:08:06 | |
Very like Pluto. | 0:08:06 | 0:08:07 | |
That's right, in fact, the surfaces of both Pluto and Triton - | 0:08:07 | 0:08:12 | |
if they did form in the same place, this shouldn't be a surprise - | 0:08:12 | 0:08:15 | |
they're covered in surfaces of nitrogen and possibly methane | 0:08:15 | 0:08:19 | |
and carbon monoxide, condensed onto the surface. | 0:08:19 | 0:08:22 | |
Now, the interesting thing about that | 0:08:22 | 0:08:24 | |
is that when Pluto and Triton get close to the sun, | 0:08:24 | 0:08:27 | |
the sun's energy heats them up | 0:08:27 | 0:08:29 | |
and it causes them to sublimate off - basically they form a gas | 0:08:29 | 0:08:32 | |
which forms a very, very thin tenuous atmosphere around these moons. | 0:08:32 | 0:08:38 | |
The last thing to say about Triton is that with Voyager's fly-by, | 0:08:38 | 0:08:42 | |
we actually saw active geysers on the moon itself, | 0:08:42 | 0:08:46 | |
and that makes Triton one of the most interesting places | 0:08:46 | 0:08:49 | |
in our solar system in having some sort of volcanic activity. | 0:08:49 | 0:08:54 | |
It's a bit like the moon is being flexed by the gravity | 0:08:54 | 0:08:57 | |
of Neptune, I would assume. | 0:08:57 | 0:08:59 | |
What they saw with the geysers themselves is that most of them | 0:08:59 | 0:09:03 | |
were clustered around where the sun's energy was the greatest, | 0:09:03 | 0:09:06 | |
so it looks like the influence of solar radiation has some effect | 0:09:06 | 0:09:10 | |
on destabilising the surface, | 0:09:10 | 0:09:12 | |
and that's why you see these amazing plumes in the old Voyager movies. | 0:09:12 | 0:09:16 | |
Well, we've come a long way, and thank you both very much. | 0:09:21 | 0:09:25 | |
Uranus was discovered in 1781 by William Herschel. | 0:09:25 | 0:09:30 | |
There's a Herschel museum in Bath and Paul Abel went there. | 0:09:30 | 0:09:34 | |
The Herschel Museum is in the heart of Bath | 0:09:36 | 0:09:40 | |
and this beautiful Georgian house was once home | 0:09:40 | 0:09:42 | |
to the great William Herschel and his sister Caroline. | 0:09:42 | 0:09:45 | |
German-born Herschel arrived in England fleeing the Prussian War. | 0:09:47 | 0:09:51 | |
He was penniless and made the spa town of Bath his home, | 0:09:51 | 0:09:54 | |
earning his living teaching young ladies music. | 0:09:54 | 0:09:58 | |
He brought over his sister Caroline to run his household, | 0:09:58 | 0:10:01 | |
and together they became two of our greatest astronomers. | 0:10:01 | 0:10:05 | |
Well, this is Herschel's piano because he was first a musician, | 0:10:07 | 0:10:10 | |
then he became a rather prominent astronomer, and look at this - | 0:10:10 | 0:10:13 | |
this is brilliant - a picture of | 0:10:13 | 0:10:15 | |
the "distinguished men of science of Great Britain living in 1807" | 0:10:15 | 0:10:19 | |
and there's Herschel, right on the end. | 0:10:19 | 0:10:21 | |
'Wandering thought the museum, | 0:10:21 | 0:10:23 | |
'you really feel Herschel's passion for astronomy. | 0:10:23 | 0:10:27 | |
'These are his original telescope eyepieces. | 0:10:27 | 0:10:30 | |
'Just think, Herschel would have looked through these | 0:10:30 | 0:10:33 | |
'to map the night sky.' | 0:10:33 | 0:10:34 | |
'Herschel also made his own mirrors, | 0:10:34 | 0:10:37 | |
'striving to improve the magnification | 0:10:37 | 0:10:40 | |
'so he could see further into the heavens.' | 0:10:40 | 0:10:42 | |
Well, here we are in Herschel's workshop | 0:10:42 | 0:10:45 | |
and it's here that he made the telescope mirrors, | 0:10:45 | 0:10:47 | |
not just for himself, but for other astronomers as well. | 0:10:47 | 0:10:50 | |
Back then, telescope mirrors were made of metal | 0:10:50 | 0:10:53 | |
and he'd take the blank, put it in this device and spend | 0:10:53 | 0:10:56 | |
many, many hours polishing the mirror until it gained the desired shape. | 0:10:56 | 0:11:01 | |
It's here that he made the telescope mirror for his famous | 0:11:01 | 0:11:05 | |
seven-foot telescope, which is upstairs. | 0:11:05 | 0:11:07 | |
The one he used to discover Uranus. So let's go upstairs and take a look. | 0:11:07 | 0:11:10 | |
Herschel was eventually to become famous for his enormous 40-foot telescope in Slough. | 0:11:12 | 0:11:18 | |
But in Bath, he had a more modest reflector. | 0:11:18 | 0:11:22 | |
Here it is, a replica of the seven-foot telescope | 0:11:22 | 0:11:26 | |
used by Herschel to discover the planet Uranus. | 0:11:26 | 0:11:29 | |
In doing so, he became the first person in human history | 0:11:29 | 0:11:32 | |
to discover the existence of another large planet | 0:11:32 | 0:11:35 | |
far beyond the orbit of Saturn, | 0:11:35 | 0:11:37 | |
thus opening up the icy depths of the solar system to us. | 0:11:37 | 0:11:40 | |
With the discovery of Uranus, | 0:11:40 | 0:11:43 | |
the Herschels became overnight 18th-century celebrities. | 0:11:43 | 0:11:47 | |
The King and many others came calling. | 0:11:47 | 0:11:50 | |
Jonathan Hall is one of the resident astronomers helping to promote and preserve | 0:11:50 | 0:11:54 | |
the work of William and his sister Caroline. | 0:11:54 | 0:11:57 | |
Back in the 18th century, Herschel's night-time activities | 0:11:57 | 0:12:01 | |
were viewed by the good people of Bath as unusual. | 0:12:01 | 0:12:05 | |
His local reputation as being a little bit eccentric | 0:12:05 | 0:12:09 | |
and very keen on the sciences and mathematics and optics. | 0:12:09 | 0:12:12 | |
He would set his early telescopes up in the street | 0:12:12 | 0:12:15 | |
and the horse and carriages were obliged to go round him. | 0:12:15 | 0:12:19 | |
He wasn't what today we might think of as a professional scientist. | 0:12:19 | 0:12:23 | |
He was purely amateur | 0:12:23 | 0:12:25 | |
and he was building these telescopes | 0:12:25 | 0:12:27 | |
with the aid of his brother and local craftsmen | 0:12:27 | 0:12:31 | |
to arguably the best standard of the time. | 0:12:31 | 0:12:33 | |
And he made mirrors for other people as well, | 0:12:33 | 0:12:35 | |
-many other prominent astronomers. -He did indeed. Yes. | 0:12:35 | 0:12:38 | |
Even in his youth, | 0:12:38 | 0:12:40 | |
he started to read books on astronomy, | 0:12:40 | 0:12:43 | |
read books on optics. | 0:12:43 | 0:12:45 | |
He'd been teaching himself a little bit of Greek. | 0:12:45 | 0:12:47 | |
He taught himself Italian and Latin, | 0:12:47 | 0:12:49 | |
partly because of his music interests as well. | 0:12:49 | 0:12:51 | |
-So much self-taught. -Incredible, yes. Very tenacious. | 0:12:51 | 0:12:55 | |
But it was really when he came to Bath | 0:12:55 | 0:12:57 | |
that it really started to take off. | 0:12:57 | 0:12:59 | |
This is how the night sky would have looked on March 13th 1781. | 0:12:59 | 0:13:04 | |
In the constellation of Gemini, there was an object, which other | 0:13:04 | 0:13:08 | |
eminent astronomers such as Flamsteed and even Galileo had overlooked. | 0:13:08 | 0:13:13 | |
Herschel immediately knew that this was something special. | 0:13:13 | 0:13:18 | |
He wasn't actually looking for a planet. | 0:13:18 | 0:13:21 | |
He'd only just moved back into the house. | 0:13:21 | 0:13:23 | |
They'd been in a previous property. | 0:13:23 | 0:13:25 | |
In fact, rather unusually, he was on his own. | 0:13:25 | 0:13:28 | |
-Because Caroline normally observed with him. -Absolutely. | 0:13:28 | 0:13:31 | |
He set the telescope up here in the garden | 0:13:31 | 0:13:33 | |
doing the systematic review of the heavens and there trained it on | 0:13:33 | 0:13:37 | |
the constellation of Gemini and that's where he made the discovery. | 0:13:37 | 0:13:40 | |
-And that brand-new world needed to be named. -It did indeed. | 0:13:40 | 0:13:43 | |
-For a long time, people wanted to call it Herschel. -Yes. | 0:13:43 | 0:13:47 | |
He wanted to name it after his patron, King George III. | 0:13:47 | 0:13:50 | |
In a lot of the old texts, | 0:13:50 | 0:13:51 | |
you can find it listed as Georgium sidus for George's star. | 0:13:51 | 0:13:54 | |
That's right. | 0:13:54 | 0:13:55 | |
Herschel, of course, was no fool. | 0:13:55 | 0:13:58 | |
Patronage in those days was immensely important. | 0:13:58 | 0:14:02 | |
The other link, of course, is that King George III, | 0:14:02 | 0:14:05 | |
part of the Hanoverian Empire. | 0:14:05 | 0:14:08 | |
Herschel was from Hanover. | 0:14:08 | 0:14:10 | |
So, as part of the patronage, | 0:14:10 | 0:14:12 | |
the King created a brand-new post for him. | 0:14:12 | 0:14:14 | |
He had to leave his life here in Bath | 0:14:14 | 0:14:19 | |
so he could be at the beck and call of the King and the Royal Family | 0:14:19 | 0:14:22 | |
to be able to go and show them the wonders of the heavens. | 0:14:22 | 0:14:27 | |
It's remarkable, over the two or three years | 0:14:27 | 0:14:29 | |
immediately following the discovery, all the eminent people | 0:14:29 | 0:14:33 | |
from around the world and Europe, who would come and pay homage | 0:14:33 | 0:14:36 | |
and their respects and want to look through a Herschelian telescope. | 0:14:36 | 0:14:40 | |
The planet was eventually named Uranus, | 0:14:42 | 0:14:44 | |
which in Greek mythology is the father of Saturn. | 0:14:44 | 0:14:48 | |
It's in our night sky at the moment | 0:14:48 | 0:14:50 | |
in the constellation of Pisces, the fishes. | 0:14:50 | 0:14:53 | |
It took some time to find it, | 0:14:53 | 0:14:55 | |
but I made this drawing of it the other night. | 0:14:55 | 0:14:58 | |
Herschel discovered this strange world over 200 years ago. | 0:14:58 | 0:15:02 | |
It changed his life for ever and guaranteed him | 0:15:02 | 0:15:04 | |
a place in astronomical history. | 0:15:04 | 0:15:07 | |
The Herschel Museum, well worth a visit if you are in Bath. | 0:15:11 | 0:15:15 | |
Herschel always makes me think of you, | 0:15:15 | 0:15:17 | |
because he was a musician and an astronomer as well. | 0:15:17 | 0:15:20 | |
You've played some of Herschel's music? | 0:15:20 | 0:15:22 | |
I'm a very amateur musician. I've never had a lesson in my life. | 0:15:22 | 0:15:26 | |
But I borrowed some of Herschel's music once | 0:15:26 | 0:15:29 | |
and played it live on the piano. | 0:15:29 | 0:15:32 | |
Was it any good? | 0:15:32 | 0:15:33 | |
-His music is! -I wasn't asking about your piano playing! | 0:15:33 | 0:15:37 | |
I got through it. | 0:15:37 | 0:15:38 | |
GENTLE PIANO MUSIC | 0:15:38 | 0:15:40 | |
We've come a long way now, | 0:15:56 | 0:15:58 | |
so let's go even further out of the solar system | 0:15:58 | 0:16:01 | |
and come to the Kuiper Belt, | 0:16:01 | 0:16:03 | |
from which the best-known member is of course Pluto. | 0:16:03 | 0:16:07 | |
Pluto is a very similar object to Triton, | 0:16:07 | 0:16:11 | |
in that, it has, over the surface, | 0:16:11 | 0:16:13 | |
ices of things like nitrogen and carbon monoxide, | 0:16:13 | 0:16:17 | |
that over the course of Pluto's extremely long orbit around the sun, | 0:16:17 | 0:16:21 | |
will sublimate off to form a kind of atmosphere. | 0:16:21 | 0:16:24 | |
When it was discovered, by my old friend Clyde Tombaugh, | 0:16:24 | 0:16:26 | |
it was thought to be at least the size of Mars, probably larger, | 0:16:26 | 0:16:30 | |
and therefore of planetary status. | 0:16:30 | 0:16:32 | |
So we regarded it as a planet | 0:16:32 | 0:16:35 | |
and it has been demoted. | 0:16:35 | 0:16:37 | |
It's been demoted, that's true, | 0:16:37 | 0:16:40 | |
but I'm not sure it's particularly because | 0:16:40 | 0:16:42 | |
Pluto's smaller than we thought - | 0:16:42 | 0:16:44 | |
though it is, it's smaller than Mercury. | 0:16:44 | 0:16:46 | |
-But it's more that we've found lots of other things this size. -It's not the only one. -No. | 0:16:46 | 0:16:50 | |
So we have the choice of having eight planets, | 0:16:50 | 0:16:52 | |
as we do, from Mercury out to Neptune, | 0:16:52 | 0:16:55 | |
or many, many, many planets. | 0:16:55 | 0:16:56 | |
And we call those the Kuiper Belt - | 0:16:56 | 0:16:58 | |
Pluto and Pluto-like objects on one part of it. | 0:16:58 | 0:17:02 | |
Of course, the most exciting thing about Pluto | 0:17:02 | 0:17:05 | |
is that's there's a spacecraft on the way, New Horizons, | 0:17:05 | 0:17:07 | |
which was planned - not that it matters - | 0:17:07 | 0:17:10 | |
but it was planned while Pluto was still a planet, | 0:17:10 | 0:17:12 | |
and a big part of their pitch | 0:17:12 | 0:17:14 | |
-was this was the last planet that we haven't seen. -Quite. | 0:17:14 | 0:17:17 | |
But where's New Horizons got to now? It's a few years away yet. | 0:17:17 | 0:17:20 | |
So it's still on its way to Pluto, | 0:17:20 | 0:17:22 | |
it's going to get there in July of 2015 | 0:17:22 | 0:17:24 | |
and it's just got past the orbit of Uranus. | 0:17:24 | 0:17:27 | |
That doesn't mean it visited Uranus, | 0:17:27 | 0:17:29 | |
but it's on its way to do a slingshot by Pluto. | 0:17:29 | 0:17:32 | |
And after Pluto, | 0:17:32 | 0:17:33 | |
it's going to go on to look at another Kuiper Belt object. | 0:17:33 | 0:17:36 | |
-Which hasn't been discovered yet. -No. | 0:17:36 | 0:17:38 | |
It's something that we're still looking for at the moment. | 0:17:38 | 0:17:41 | |
Pluto is the brightest member of the Kuiper Belt, | 0:17:41 | 0:17:44 | |
it's certainly nothing more than that. | 0:17:44 | 0:17:47 | |
Recently there was a big conference in France about these things | 0:17:47 | 0:17:51 | |
and Dr Chris North went there | 0:17:51 | 0:17:54 | |
and brings us back news from the Kuiper Belt. | 0:17:54 | 0:17:57 | |
This year's annual gathering of planetary scientists in Nantes | 0:17:57 | 0:18:01 | |
was the largest for many years. | 0:18:01 | 0:18:03 | |
For space scientists, | 0:18:03 | 0:18:05 | |
it's a great place to talk about missions to the planets, | 0:18:05 | 0:18:07 | |
and for the astronomers, | 0:18:07 | 0:18:09 | |
a platform to launch their new ideas. | 0:18:09 | 0:18:11 | |
This year, the icy, dark depths | 0:18:11 | 0:18:14 | |
of our solar system have caused a bit of a stir. | 0:18:14 | 0:18:17 | |
The Kuiper Belt stretches beyond Neptune | 0:18:20 | 0:18:23 | |
and has previously been dismissed as the dustbin of the solar system, | 0:18:23 | 0:18:27 | |
the leftovers of its formation. | 0:18:27 | 0:18:29 | |
Meg Schwamb has been raking through the rubbish, | 0:18:30 | 0:18:33 | |
to find clues about the Kuiper Belt and its formation. | 0:18:33 | 0:18:35 | |
We now know that there are lots of exotic objects out there. | 0:18:38 | 0:18:42 | |
They come in a range of sizes | 0:18:42 | 0:18:44 | |
and some, such as Pluto, even have moons. | 0:18:44 | 0:18:47 | |
While many formed in these icy outer depths, | 0:18:47 | 0:18:51 | |
others formed closer in | 0:18:51 | 0:18:52 | |
and were flung out there by the movement of the giant planets. | 0:18:52 | 0:18:56 | |
The Kuiper Belt really is | 0:18:57 | 0:18:59 | |
the icy remnants left over from planet formation. | 0:18:59 | 0:19:01 | |
You can think of it as the embryos and the failed planets | 0:19:01 | 0:19:04 | |
that didn't form into the terrestrial planets | 0:19:04 | 0:19:07 | |
or the cores of the giant planets | 0:19:07 | 0:19:09 | |
and have been scattered out, or may have formed out, | 0:19:09 | 0:19:11 | |
in orbits beyond Neptune. | 0:19:11 | 0:19:13 | |
And so Pluto is one of the well-known and largest of these objects | 0:19:13 | 0:19:17 | |
and there are now many Pluto-sized bodies known in this region, | 0:19:17 | 0:19:21 | |
as well as many hundreds of thousands of other smaller bodies | 0:19:21 | 0:19:24 | |
that orbit well beyond Neptune. | 0:19:24 | 0:19:27 | |
In 2007, Meg discovered an object nicknamed Snow White, | 0:19:27 | 0:19:32 | |
one of the largest Kuiper Belt objects | 0:19:32 | 0:19:34 | |
at around half the size of Pluto. | 0:19:34 | 0:19:36 | |
Despite its name, Snow White is actually red. | 0:19:36 | 0:19:40 | |
The colour is caused by a tarry gloop called tholins, | 0:19:40 | 0:19:44 | |
a term coined by Carl Sagan. | 0:19:44 | 0:19:46 | |
We think tholins are methane and other chemicals | 0:19:46 | 0:19:50 | |
broken down by weak sunlight over billions of years. | 0:19:50 | 0:19:53 | |
I don't think we've quite touched tholins in the outer solar system, | 0:19:55 | 0:19:59 | |
but we think that if you take these methane ices and nitrogen ices | 0:19:59 | 0:20:04 | |
and you keep radiating the methane, | 0:20:04 | 0:20:06 | |
you get a higher and higher order of hydrocarbons, | 0:20:06 | 0:20:08 | |
and so you get more gunk and tar. | 0:20:08 | 0:20:10 | |
And so, that's what we think it is | 0:20:10 | 0:20:12 | |
and we think it's reddened their surface. | 0:20:12 | 0:20:14 | |
And so it's sort of this red crust, or radiation crust, | 0:20:14 | 0:20:18 | |
sitting on the surface. | 0:20:18 | 0:20:19 | |
-It's goo. -It's goo, it's sort of, yeah... | 0:20:19 | 0:20:21 | |
-It comes from the Greek word for muddy, I believe. -Yes. | 0:20:21 | 0:20:24 | |
Kuiper Belt objects are the preserved remnants of our early solar system | 0:20:24 | 0:20:28 | |
and they tell us what is was like billions of years ago | 0:20:28 | 0:20:31 | |
when the planets were forming. | 0:20:31 | 0:20:32 | |
But studying it can be very frustrating, | 0:20:32 | 0:20:35 | |
as the objects are so small and so very far away. | 0:20:35 | 0:20:38 | |
Occasionally, however, | 0:20:38 | 0:20:40 | |
we get visitors from the outer limits - comets. | 0:20:40 | 0:20:44 | |
'Mike Ahern has led one of the most successful mission to not one, | 0:20:47 | 0:20:51 | |
'but two comets. | 0:20:51 | 0:20:52 | |
'In July 2005,' | 0:20:52 | 0:20:55 | |
part of the Deep Impact probe was smashed into Comet Tempel 1, | 0:20:55 | 0:20:59 | |
giving our first view of material from inside a comet. | 0:20:59 | 0:21:02 | |
Following this successful mission, | 0:21:02 | 0:21:05 | |
the Deep Impact spacecraft was re-routed | 0:21:05 | 0:21:07 | |
and in November 2010, | 0:21:07 | 0:21:09 | |
flew past Comet Hartley 2 | 0:21:09 | 0:21:11 | |
where it saw a very different world. | 0:21:11 | 0:21:13 | |
Every comet we've visited | 0:21:13 | 0:21:14 | |
has been very different | 0:21:14 | 0:21:16 | |
from what we would have predicted from the previous one we visited. | 0:21:16 | 0:21:21 | |
So that's the reason for going to multiple ones - | 0:21:21 | 0:21:23 | |
to try to find a pattern. | 0:21:23 | 0:21:25 | |
One difference between Tempel 1 and Hartley 2, | 0:21:25 | 0:21:28 | |
the two that Deep Impact spacecraft visited, | 0:21:28 | 0:21:30 | |
is they're very different sizes | 0:21:30 | 0:21:32 | |
and very different activity for their size. | 0:21:32 | 0:21:35 | |
On Tempel 1 we saw differences in the outgassing | 0:21:35 | 0:21:39 | |
from different parts of the comet. | 0:21:39 | 0:21:42 | |
Now, does this mean different parts of the comet | 0:21:42 | 0:21:44 | |
came from different parts of the proto-planetary disc? | 0:21:44 | 0:21:47 | |
It was hard to tell... | 0:21:47 | 0:21:48 | |
-Because they're made of different stuff. -Yeah. | 0:21:48 | 0:21:51 | |
But there could be still strong seasonal effects on Tempel 1. | 0:21:51 | 0:21:54 | |
Now, at Hartley 2, it's in this excited state rotation | 0:21:54 | 0:21:57 | |
where in addition to going around like this, it rolls. | 0:21:57 | 0:22:00 | |
So everything gets illuminated all the time | 0:22:00 | 0:22:02 | |
and there are no strong seasonal effects. | 0:22:02 | 0:22:04 | |
And we still see big differences | 0:22:04 | 0:22:06 | |
between the outgassing at the two ends, | 0:22:06 | 0:22:08 | |
which says that they really must have come, | 0:22:08 | 0:22:10 | |
in the early solar system, from different distances from the sun. | 0:22:10 | 0:22:14 | |
-So they are different? -They really are different. | 0:22:14 | 0:22:16 | |
Comets, the archaeological remains of our early solar system, | 0:22:17 | 0:22:20 | |
will help us understand | 0:22:20 | 0:22:22 | |
how the planet Earth became such a unique world. | 0:22:22 | 0:22:24 | |
It's important, because, for one thing, | 0:22:24 | 0:22:27 | |
we think the comets bring all the water to Earth, | 0:22:27 | 0:22:29 | |
or at least some of us have thought that all along. | 0:22:29 | 0:22:31 | |
Is that just because Earth's the only planet we know with standing water... | 0:22:31 | 0:22:36 | |
-That's correct. -..on its surface. -Yes. -And the early Earth, | 0:22:36 | 0:22:39 | |
-that should have all boiled off. -Exactly. | 0:22:39 | 0:22:41 | |
-So where did it come from? -So it has to have been brought in at a somewhat later stage - | 0:22:41 | 0:22:45 | |
-only half a billion years after the formation, but... -A long time ago. | 0:22:45 | 0:22:49 | |
The Kuiper Belt is clearly not the dustbin of the solar system | 0:22:51 | 0:22:54 | |
and the exotic objects that live there are far more than just rubbish | 0:22:54 | 0:22:58 | |
thrown out during its formation. | 0:22:58 | 0:23:00 | |
Instead, each one is a fascinating world | 0:23:00 | 0:23:04 | |
and the more we find out about them, | 0:23:04 | 0:23:06 | |
the more we find out about our own origins. | 0:23:06 | 0:23:09 | |
Plenty of news this month | 0:23:10 | 0:23:12 | |
so we'll go now to Chris North and Chris Lintott. | 0:23:12 | 0:23:15 | |
A huge storm going on on Saturn. | 0:23:15 | 0:23:19 | |
A huge storm that's been going on for most of the last year. | 0:23:19 | 0:23:22 | |
It was discovered last December as this white spot, | 0:23:22 | 0:23:26 | |
which is the form storms on Saturn normally take, | 0:23:26 | 0:23:28 | |
but this one spread out until it covered quite a lot of the disc. | 0:23:28 | 0:23:32 | |
-Huge. -You can see it in these new images that we just got from Cassini | 0:23:32 | 0:23:35 | |
that were taken over the last year. | 0:23:35 | 0:23:37 | |
Of course, the amateurs saw this as well. | 0:23:37 | 0:23:39 | |
Then they saw the storm fade over time | 0:23:39 | 0:23:42 | |
and it seemed like all was quiet on Saturn. | 0:23:42 | 0:23:44 | |
But if you talk to the professionals who can use | 0:23:44 | 0:23:46 | |
some really big telescopes and they can look in the infrared, | 0:23:46 | 0:23:49 | |
they see that actually what's happened is up in the top | 0:23:49 | 0:23:52 | |
of Saturn's atmosphere, in what would be the stratosphere, | 0:23:52 | 0:23:56 | |
there's still a lot going on. | 0:23:56 | 0:23:58 | |
The storm now covers about a quarter of the disc, | 0:23:58 | 0:24:01 | |
so all of the northern bit you can see on one side. | 0:24:01 | 0:24:05 | |
But as it emerges in January, we're going to see | 0:24:05 | 0:24:07 | |
some interesting things happening | 0:24:07 | 0:24:10 | |
where this storm was last year. | 0:24:10 | 0:24:12 | |
-I wonder what we'll see. -We'll find out. | 0:24:12 | 0:24:15 | |
Coming into Jupiter and the second moon there, Europa, | 0:24:15 | 0:24:19 | |
interesting news? | 0:24:19 | 0:24:20 | |
Europa's this moon that's got the very weird terrain. | 0:24:20 | 0:24:23 | |
We call it chaotic terrain. It was terrain that the Voyager probes and Galileo saw | 0:24:23 | 0:24:27 | |
covered in cracks and fissures and all sorts. | 0:24:27 | 0:24:31 | |
-Map-maker's nightmare. -Indeed. Map-maker's complete nightmare. | 0:24:31 | 0:24:34 | |
What we think is happening still is that that's cracked | 0:24:34 | 0:24:37 | |
and broken up by the motion of a sub-surface ocean. | 0:24:37 | 0:24:42 | |
We can compare that to stuff we see on the Earth. | 0:24:42 | 0:24:45 | |
Some of the features look like things we've seen in Antarctica, | 0:24:45 | 0:24:49 | |
with a sub-surface sea or lake that's not quite that deep. | 0:24:49 | 0:24:52 | |
I'm quite excited about this because | 0:24:52 | 0:24:53 | |
it's been my favourite idea for a mission anywhere in the solar system, | 0:24:53 | 0:24:57 | |
which is you land on Europa, melt your way through the surface | 0:24:57 | 0:25:00 | |
and you see something with teeth coming towards you. | 0:25:00 | 0:25:03 | |
The reason people care about this ocean is | 0:25:03 | 0:25:07 | |
it's an interesting place to think about life. | 0:25:07 | 0:25:09 | |
It could well be. | 0:25:09 | 0:25:10 | |
Life on Earth, we think, started in deep oceans | 0:25:10 | 0:25:13 | |
without much sunlight, so Europa's a fascinating world. | 0:25:13 | 0:25:16 | |
They all are. Of course, you can't get away from Mars. | 0:25:16 | 0:25:19 | |
Always something new there and, | 0:25:19 | 0:25:21 | |
of course, this new probe Phobos-Grunt. | 0:25:21 | 0:25:24 | |
Yes, this was a Russian probe that was meant to go to Mars's moon, Phobos, | 0:25:24 | 0:25:29 | |
collect a sample, bring it back to Earth. | 0:25:29 | 0:25:31 | |
Unfortunately, it made it into orbit, it's been stuck there. | 0:25:31 | 0:25:35 | |
It's not sure what will happen, which is very sad. | 0:25:35 | 0:25:39 | |
The Russians have never had any success there. | 0:25:39 | 0:25:41 | |
It was incredibly ambitious. That would have been the first sample-return mission, | 0:25:41 | 0:25:45 | |
BUT we shouldn't forget there's good news for Mars this month as well, | 0:25:45 | 0:25:49 | |
which is that the American Curiosity rover is successfully on its way. | 0:25:49 | 0:25:53 | |
Lift off of the Atlas V with Curiosity. | 0:25:53 | 0:25:57 | |
We're going to find out a huge amount about Mars's past | 0:25:57 | 0:26:01 | |
and about whether there are the conditions for life there. | 0:26:01 | 0:26:04 | |
-So I'm really excited about Curiosity. -So far, all goes well. | 0:26:04 | 0:26:07 | |
We have spacecraft separation. | 0:26:07 | 0:26:09 | |
APPLAUSE | 0:26:09 | 0:26:11 | |
One more news item. | 0:26:11 | 0:26:13 | |
We found a long-lost Sky At Night programme | 0:26:13 | 0:26:15 | |
on a recording machine and here it is. | 0:26:15 | 0:26:18 | |
I'm talking about moon bases tonight for two reasons. | 0:26:23 | 0:26:25 | |
First, because they are very topical | 0:26:25 | 0:26:28 | |
and we've just shown you one new design study. | 0:26:28 | 0:26:31 | |
But secondly because I am delighted to have with me | 0:26:31 | 0:26:34 | |
my old friend Arthur Clarke. | 0:26:34 | 0:26:36 | |
Arthur, you, of course, | 0:26:36 | 0:26:38 | |
were forecasting developments of this kind more than 20 years ago. | 0:26:38 | 0:26:42 | |
Thank you, Pat. | 0:26:42 | 0:26:43 | |
I'd like to begin with a flashback to the communication satellite | 0:26:43 | 0:26:46 | |
which you mentioned, | 0:26:46 | 0:26:48 | |
by showing this illustration which has some sentimental interest to me | 0:26:48 | 0:26:53 | |
because I displayed this on BBC TV about ten years ago. | 0:26:53 | 0:26:57 | |
This was undoubtedly the first time that anything | 0:26:57 | 0:27:00 | |
about communication satellites appeared on TV anywhere in the world. | 0:27:00 | 0:27:04 | |
So, this is a programme from 1963. | 0:27:04 | 0:27:07 | |
To put us in context, that was before Apollo. | 0:27:07 | 0:27:10 | |
Apollo was still in the planning. | 0:27:10 | 0:27:12 | |
We'd had people into space, but only a few probes whizzing past the moon. | 0:27:12 | 0:27:17 | |
Arthur C Clarke was predicting not only these communication satellites, | 0:27:17 | 0:27:21 | |
which were starting to become a reality back then, | 0:27:21 | 0:27:25 | |
but also was talking about bases on the moon, bases on Mars, | 0:27:25 | 0:27:29 | |
all incredibly exciting for what we might do | 0:27:29 | 0:27:31 | |
from then, in the next 20, 30 years. | 0:27:31 | 0:27:34 | |
I think a great deal has depended there upon | 0:27:34 | 0:27:36 | |
the question of the lunar atmosphere | 0:27:36 | 0:27:38 | |
because if the moon had proved to have anything of an atmosphere, | 0:27:38 | 0:27:41 | |
then the surface dome would have been the answer. | 0:27:41 | 0:27:44 | |
Do you think that this means that the lunar base | 0:27:44 | 0:27:47 | |
has got to go underground? | 0:27:47 | 0:27:48 | |
If it turns out that a meteor bombardment is a serious danger, | 0:27:48 | 0:27:53 | |
then, undoubtedly, we will have to put our bases underground. | 0:27:53 | 0:27:56 | |
But I rather hope that the necessity of a lunar underground movement | 0:27:56 | 0:28:00 | |
does not arise. | 0:28:00 | 0:28:02 | |
-I hope we can stay on the surface and look at the stars. -So do I. | 0:28:02 | 0:28:04 | |
He and I were great friends. | 0:28:04 | 0:28:06 | |
This is one of the few recordings we made together | 0:28:06 | 0:28:09 | |
that's actually been preserved. | 0:28:09 | 0:28:11 | |
Yes, it's wonderful. | 0:28:11 | 0:28:12 | |
If you could have picked one Sky At Night out of those that were lost, | 0:28:12 | 0:28:16 | |
-this one would have been high on the list. -I would agree. | 0:28:16 | 0:28:18 | |
You can see more clips | 0:28:18 | 0:28:20 | |
on the website, which is... | 0:28:20 | 0:28:24 | |
I'm going to watch it again and dream of Mars bases. | 0:28:24 | 0:28:28 | |
Thank you both very much indeed. | 0:28:28 | 0:28:30 | |
When I come back next month, we're going even further | 0:28:30 | 0:28:33 | |
and look at planets on other stars. | 0:28:33 | 0:28:36 | |
Until then, good night. | 0:28:36 | 0:28:38 | |
Subtitles by Red Bee Media Ltd | 0:28:44 | 0:28:48 | |
E-mail [email protected] | 0:28:48 | 0:28:51 |