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We all love talking about the weather. | 0:00:05 | 0:00:08 | |
Is it too hot or is it too cold? | 0:00:08 | 0:00:11 | |
Is it too wet or too windy? | 0:00:11 | 0:00:13 | |
It's a national obsession. | 0:00:15 | 0:00:17 | |
But now scientists have also started looking to the heavens... | 0:00:17 | 0:00:21 | |
..and wondering what the weather might be like on other planets. | 0:00:23 | 0:00:27 | |
We are witnessing the birth of extra terrestrial meteorology, | 0:00:29 | 0:00:33 | |
as technology is allowing astronomers to study the weather | 0:00:33 | 0:00:36 | |
on other planets like never before. | 0:00:36 | 0:00:39 | |
Jupiter has these very long-lived storms, | 0:00:41 | 0:00:45 | |
but Saturn has these very violent storms. | 0:00:45 | 0:00:47 | |
But, incredibly, today the latest telescopes are enabling astronomers | 0:00:49 | 0:00:53 | |
to find and study planets beyond our solar system. | 0:00:53 | 0:00:57 | |
So here we have our image of ROXs 12 b, | 0:00:59 | 0:01:02 | |
which is pretty amazing to think we are imaging a planet | 0:01:02 | 0:01:06 | |
400 light years away. | 0:01:06 | 0:01:08 | |
And our exploration of the universe is revealing alien worlds | 0:01:08 | 0:01:12 | |
with weather far stranger and more extreme than anyone | 0:01:12 | 0:01:16 | |
could have ever imagined. | 0:01:16 | 0:01:19 | |
A lot of the planets that we're studying so far | 0:01:19 | 0:01:22 | |
are very horrible places. | 0:01:22 | 0:01:25 | |
You wouldn't want to go there on vacation. | 0:01:25 | 0:01:27 | |
On these planets you can get the most gigantic storm systems | 0:01:29 | 0:01:33 | |
ever witnessed by mankind. | 0:01:33 | 0:01:34 | |
So one side of the planet can be roasting hot while at the same time | 0:01:36 | 0:01:40 | |
the other side of the planet can be freezing cold. | 0:01:40 | 0:01:43 | |
On some exoplanets, the temperatures are such that the clouds | 0:01:43 | 0:01:46 | |
and the rain can be made up of liquid lava droplets. | 0:01:46 | 0:01:51 | |
We thought we had extreme weather on Earth, | 0:01:51 | 0:01:54 | |
but it turns out that it's nothing compared to what's out there. | 0:01:54 | 0:01:58 | |
So instead of having rain which is liquid water droplets like here | 0:02:00 | 0:02:03 | |
on Earth, it would be raining liquid rubies. | 0:02:03 | 0:02:08 | |
And the search for the weirdest weather in the universe | 0:02:08 | 0:02:11 | |
is only just beginning. | 0:02:11 | 0:02:13 | |
It's a delightfully warm spring morning in Greenwich, London. | 0:02:26 | 0:02:30 | |
Astronomers of all ages have gathered at the Royal Observatory, | 0:02:31 | 0:02:35 | |
where they're hoping to witness a rather special event. | 0:02:35 | 0:02:38 | |
They're waiting to glimpse another world. | 0:02:39 | 0:02:41 | |
And, unusually for astronomers, | 0:02:43 | 0:02:45 | |
they've got their telescopes out during the day. | 0:02:45 | 0:02:47 | |
We're here to see quite a rare astronomical event. | 0:02:50 | 0:02:52 | |
I'm very excited to see it. I'm just hopeful, as we all are, | 0:02:52 | 0:02:56 | |
that the clouds don't come along around midday and stay with us. | 0:02:56 | 0:02:59 | |
It's a chance to get a unique perspective | 0:03:01 | 0:03:04 | |
of one of our nearest neighbours. | 0:03:04 | 0:03:06 | |
And to take a closer look, | 0:03:11 | 0:03:13 | |
astronomer Tom Kerss has set up the Great Equatorial Telescope | 0:03:13 | 0:03:17 | |
to look at the sun for the first time since 1927. | 0:03:17 | 0:03:20 | |
Because at exactly 12 minutes past noon, | 0:03:23 | 0:03:26 | |
the planet Mercury is due to pass in front of the sun. | 0:03:26 | 0:03:29 | |
So here is Mercury emerging onto the face of the sun, | 0:03:42 | 0:03:45 | |
looking very beautiful indeed. | 0:03:45 | 0:03:47 | |
Over the next seven and a half hours or so, | 0:03:48 | 0:03:51 | |
Mercury will gradually slink across the face of the sun | 0:03:51 | 0:03:54 | |
as it overtakes us on the inside track in the solar system, | 0:03:54 | 0:03:57 | |
about 52 million miles away from the Earth right now. | 0:03:57 | 0:03:59 | |
Ever since we've known about the existence of other planets, | 0:04:03 | 0:04:06 | |
we've wondered what these mysterious alien worlds might be like. | 0:04:06 | 0:04:09 | |
Could they be potential homes for life? | 0:04:13 | 0:04:16 | |
And is there any way of finding out? | 0:04:16 | 0:04:18 | |
So when wondering whether other planets might be habitable or not, | 0:04:22 | 0:04:25 | |
the key question we need to ask to begin with is what is the atmosphere | 0:04:25 | 0:04:29 | |
actually like? What is the climate like? | 0:04:29 | 0:04:31 | |
What's the weather like? Whether it would be very extreme or whether it | 0:04:31 | 0:04:33 | |
would be quite pleasant and stable, | 0:04:33 | 0:04:35 | |
the kind of weather we think is necessary for life. | 0:04:35 | 0:04:37 | |
So what will the weather be like on Mercury? | 0:04:39 | 0:04:43 | |
If we look back at the beginning of the Mercury transit we can see | 0:04:43 | 0:04:46 | |
a really clean bite taken out of the sun. | 0:04:46 | 0:04:49 | |
And the edge is so clean because Mercury doesn't have any appreciable | 0:04:49 | 0:04:53 | |
atmosphere to speak of. | 0:04:53 | 0:04:55 | |
With no real atmosphere, Mercury is effectively a dead and barren world. | 0:04:58 | 0:05:04 | |
Because Mercury lacks anything that we would call an atmosphere, | 0:05:06 | 0:05:08 | |
there's essentially no weather on Mercury at all. | 0:05:08 | 0:05:11 | |
Mercury is unusual in our solar system because all the other planets | 0:05:19 | 0:05:23 | |
do have atmospheres and so they must also have weather. | 0:05:23 | 0:05:27 | |
Death Valley, California, | 0:05:31 | 0:05:33 | |
one of the most extreme and alien environments on Earth. | 0:05:33 | 0:05:38 | |
Planetary explorer Suzanne Smerkar has come here because it shares | 0:05:38 | 0:05:42 | |
a surprising similarity to our nearest neighbour, Venus. | 0:05:42 | 0:05:47 | |
Venus is the brightest object in the night sky and the reason it's so | 0:05:47 | 0:05:51 | |
bright is because it's covered in thick clouds. | 0:05:51 | 0:05:55 | |
And when you turn your telescope to it, | 0:05:55 | 0:05:58 | |
you can see nothing of the surface, | 0:05:58 | 0:05:59 | |
all you see is this bright reflection coming back at you | 0:05:59 | 0:06:01 | |
because of the cloud deck that's kept it shrouded in mystery. | 0:06:01 | 0:06:05 | |
We do know that Venus is similar in size to Earth, | 0:06:07 | 0:06:10 | |
is a rocky world like our own, and also relatively close to us. | 0:06:10 | 0:06:15 | |
So what's its climate like? | 0:06:15 | 0:06:16 | |
We used to think that Venus was much like the Earth, | 0:06:17 | 0:06:20 | |
maybe 50 degrees hotter because it's that much closer to the sun. | 0:06:20 | 0:06:23 | |
We thought it had an atmosphere like the Earth, | 0:06:23 | 0:06:25 | |
we thought it would be cool enough to have oceans. | 0:06:25 | 0:06:28 | |
We even thought it was covered in steamy hot swamps, | 0:06:30 | 0:06:34 | |
probably covered with verdant green life. | 0:06:34 | 0:06:36 | |
But to discover what Venus was really like, we needed to go there. | 0:06:40 | 0:06:44 | |
At the dawn of the space age, people started to explore. | 0:06:49 | 0:06:53 | |
It was the Cold War in the '60s, | 0:06:53 | 0:06:55 | |
and the Soviets and the US were sending spacecraft after spacecraft, | 0:06:55 | 0:06:59 | |
trying to be the first out there. | 0:06:59 | 0:07:00 | |
A huge number of spacecraft have been hurled at Venus | 0:07:00 | 0:07:04 | |
and there were many attempts to get to the surface. | 0:07:04 | 0:07:07 | |
In the late 1960s, the Russians succeeded. | 0:07:07 | 0:07:12 | |
The one that finally made it to the surface was Venera 7 in 1967, | 0:07:12 | 0:07:17 | |
and that probe fell gently through the atmosphere, | 0:07:17 | 0:07:20 | |
got to the surface and survived for only about two hours. | 0:07:20 | 0:07:23 | |
Before they died, the Venera probes revealed the true nature | 0:07:29 | 0:07:33 | |
of Venus's climate. | 0:07:33 | 0:07:34 | |
Venus has a surface temperature of 462 Celsius, | 0:07:38 | 0:07:41 | |
which makes it the hottest place in the solar system. | 0:07:41 | 0:07:43 | |
And the atmospheric pressure on Venus is almost 100 times | 0:07:43 | 0:07:47 | |
that on the Earth. | 0:07:47 | 0:07:48 | |
With surface temperatures hot enough to melt lead, | 0:07:51 | 0:07:55 | |
an oppressive atmosphere of carbon dioxide, and belching clouds | 0:07:55 | 0:08:00 | |
made of sulphuric acid, Venus is a planetary vision of Hell. | 0:08:00 | 0:08:05 | |
We knew for the first time that Venus is not a swampy, | 0:08:09 | 0:08:12 | |
verdant region teeming with life, | 0:08:12 | 0:08:14 | |
but instead it's a hellish, hot inferno. | 0:08:14 | 0:08:18 | |
Venus is the hottest planet in the solar system, | 0:08:20 | 0:08:23 | |
but it's not the closest to the sun. | 0:08:23 | 0:08:26 | |
Sue has come to Death Valley where the unbearable temperatures | 0:08:29 | 0:08:33 | |
are created by the same phenomenon at work on Venus. | 0:08:33 | 0:08:36 | |
We are here today in Death Valley, the hottest place on Earth. | 0:08:40 | 0:08:43 | |
The temperature today is... | 0:08:43 | 0:08:47 | |
42 degrees. | 0:08:47 | 0:08:48 | |
Pretty balmy for Death Valley - | 0:08:48 | 0:08:50 | |
the hottest recorded temperature is 57 degrees | 0:08:50 | 0:08:53 | |
so we have it easy today. | 0:08:53 | 0:08:56 | |
The reason that it is so hot here is that we are at 86m below sea level | 0:08:56 | 0:09:01 | |
and that means that we have about 86m more atmosphere here | 0:09:01 | 0:09:05 | |
and that means it's higher pressure and in fact the pressure measurement | 0:09:05 | 0:09:10 | |
here is 1,016 bars. | 0:09:10 | 0:09:13 | |
And that extra bit of pressure is really what's giving us | 0:09:13 | 0:09:17 | |
this intense heat that we are experiencing today. | 0:09:17 | 0:09:20 | |
It's like adding another layer of insulation or another blanket | 0:09:20 | 0:09:23 | |
that's holding the heat in. | 0:09:23 | 0:09:26 | |
And by simply driving uphill, | 0:09:32 | 0:09:34 | |
Sue can reveal the tremendous insulating power of the atmosphere. | 0:09:34 | 0:09:38 | |
So now we are at about 1,000m and it's already | 0:09:43 | 0:09:46 | |
looking greener and a bit cooler up here. | 0:09:46 | 0:09:48 | |
At Dante's View, almost 2km above the valley floor, | 0:09:53 | 0:09:58 | |
the temperature is much cooler. | 0:09:58 | 0:10:00 | |
We're at about 1.7km above the valley floor, | 0:10:04 | 0:10:07 | |
where we were earlier today, and the temperature is 30 degrees Celsius, | 0:10:07 | 0:10:12 | |
way cooler than the 42 degrees down there. | 0:10:12 | 0:10:15 | |
And the reason it's so much cooler up here is that we have | 0:10:15 | 0:10:19 | |
that 1.7km less air. | 0:10:19 | 0:10:22 | |
Our pressure is 831 bars, down below it was 1,016. | 0:10:22 | 0:10:28 | |
So the pressure is much lower. | 0:10:28 | 0:10:30 | |
We have a lot less atmosphere above us, | 0:10:30 | 0:10:32 | |
and as a result it's much cooler and much more pleasant up here. | 0:10:32 | 0:10:36 | |
On Earth, the temperature typically increases | 0:10:40 | 0:10:44 | |
by about 6.5 degrees Celsius for every kilometre you descend. | 0:10:44 | 0:10:48 | |
On Venus, with its much deeper atmosphere than Earth, | 0:10:54 | 0:10:57 | |
this insulating effect is taken to its extreme. | 0:10:57 | 0:11:00 | |
It is so much hotter on Venus because the pressure is at 92 bars, | 0:11:04 | 0:11:09 | |
almost 100 times that on the Earth, and the atmosphere is much thicker, | 0:11:09 | 0:11:13 | |
much denser, and it really holds that heat in, | 0:11:13 | 0:11:15 | |
making Venus the incredible inferno that it is. | 0:11:15 | 0:11:18 | |
On top of this, Venus's atmosphere is almost entirely made up | 0:11:20 | 0:11:24 | |
of the greenhouse gas carbon dioxide. | 0:11:24 | 0:11:26 | |
And this combines with the intense pressure to make Venus | 0:11:28 | 0:11:32 | |
the hottest planet in the solar system. | 0:11:32 | 0:11:34 | |
Our next nearest neighbour couldn't be more different. | 0:11:41 | 0:11:44 | |
Venus and Mars are like chalk and cheese. | 0:11:44 | 0:11:47 | |
So Mars is the opposite extreme from Venus. | 0:11:48 | 0:11:51 | |
It's atmosphere is 1/100th the pressure of Earth's | 0:11:51 | 0:11:55 | |
and the effect of having that really low atmospheric pressure on Mars | 0:11:55 | 0:11:59 | |
means that it can't trap any of its heat. | 0:11:59 | 0:12:03 | |
So Mars is a cold, | 0:12:03 | 0:12:05 | |
barren desert compared to Earth or to Venus. | 0:12:05 | 0:12:08 | |
Because of its thin atmosphere, | 0:12:09 | 0:12:11 | |
Mars is home to some spectacular weather phenomena. | 0:12:11 | 0:12:14 | |
The rovers sent by NASA revealed that Mars is scoured | 0:12:16 | 0:12:19 | |
by super-size dust devils, | 0:12:19 | 0:12:23 | |
reaching up to a kilometre in height. | 0:12:23 | 0:12:25 | |
But even more impressive are the dust storms, | 0:12:30 | 0:12:33 | |
which dwarf those on Earth. | 0:12:33 | 0:12:35 | |
In the thin atmosphere of Mars, | 0:12:36 | 0:12:38 | |
the dust storms can get to a very high elevation, | 0:12:38 | 0:12:40 | |
they can get to about 20km above the surface. | 0:12:40 | 0:12:43 | |
And because most of Mars is a dry, dusty desert, | 0:12:48 | 0:12:51 | |
these dust storms can cover vast expanses. | 0:12:51 | 0:12:55 | |
In fact, it seems there is no limit to how far they can spread. | 0:12:55 | 0:12:59 | |
Every few years an enormous dust storm will grow | 0:13:01 | 0:13:04 | |
until the entire planet is engulfed. | 0:13:04 | 0:13:07 | |
Incredibly, storms like these have been shown to envelop | 0:13:07 | 0:13:11 | |
the whole of Mars for over two months. | 0:13:11 | 0:13:14 | |
WEATHER REPORT: For England it's a hot and sunny day for all, any mist and fog clearing away quickly... | 0:13:21 | 0:13:25 | |
Further out in the solar system, the weather gets even wilder. | 0:13:25 | 0:13:29 | |
It's another fine sunny day in Pasadena, | 0:13:31 | 0:13:34 | |
home of NASA's Jet Propulsion Laboratory. | 0:13:34 | 0:13:36 | |
Andrew Ingersoll is the father of extra-terrestrial meteorology. | 0:13:38 | 0:13:42 | |
He's come to the Deep Space Operations Centre. | 0:13:44 | 0:13:47 | |
It's mission control for the small fleet of spacecraft that NASA | 0:13:47 | 0:13:51 | |
has sent to explore the outer reaches of the solar system. | 0:13:51 | 0:13:54 | |
Andy has worked on all these missions. | 0:13:56 | 0:13:59 | |
So we've had a whole series of spacecraft | 0:14:01 | 0:14:04 | |
visiting the giant planets. | 0:14:04 | 0:14:06 | |
The first big one was Voyager in the '70s, | 0:14:06 | 0:14:11 | |
which zoomed past all the giant planets. | 0:14:11 | 0:14:14 | |
Then there was Galileo. | 0:14:14 | 0:14:16 | |
Then Cassini which has been in orbit around Saturn for ten years. | 0:14:16 | 0:14:22 | |
And now we have Juno in orbit around Jupiter. | 0:14:23 | 0:14:28 | |
The spacecraft have given us an unprecedented view of the weather | 0:14:28 | 0:14:31 | |
on these planets. | 0:14:31 | 0:14:34 | |
The outer planets are big balls of gas and that makes a huge difference | 0:14:34 | 0:14:39 | |
in the weather, | 0:14:39 | 0:14:41 | |
so there's lots of room for weather. | 0:14:41 | 0:14:44 | |
And because you don't have continents, | 0:14:44 | 0:14:46 | |
you don't have mountains for the winds to rub against, | 0:14:46 | 0:14:49 | |
and there's nothing to control the weather the way the continents | 0:14:49 | 0:14:55 | |
partly control our weather. | 0:14:55 | 0:14:57 | |
This means these planets have storms on an entirely different scale | 0:14:57 | 0:15:01 | |
to ours. | 0:15:01 | 0:15:03 | |
And the most famous storm of all has to be Jupiter's Great Red Spot. | 0:15:03 | 0:15:09 | |
The Great Red Spot is a huge storm in Jupiter's atmosphere. | 0:15:09 | 0:15:13 | |
You could put two Earths inside the Red Spot, | 0:15:13 | 0:15:16 | |
and the winds going around the periphery of the Red Spot | 0:15:16 | 0:15:20 | |
are about three times the speed of the Earth's jet streams. | 0:15:20 | 0:15:24 | |
With winds whipping round at about 650km per hour, | 0:15:27 | 0:15:32 | |
and releasing so much energy that it heats the atmosphere above it | 0:15:32 | 0:15:36 | |
to around 1,400 degrees Celsius, | 0:15:36 | 0:15:39 | |
the Red Spot has been raging for as long as we on Earth | 0:15:39 | 0:15:42 | |
have been able to observe Jupiter. | 0:15:42 | 0:15:45 | |
Shortly after Galileo built the first telescope, | 0:15:45 | 0:15:50 | |
people were using these primitive telescopes to look at Jupiter | 0:15:50 | 0:15:53 | |
and they saw this storm. | 0:15:53 | 0:15:56 | |
And it's apparently been there ever since, which is remarkable, | 0:15:56 | 0:16:01 | |
compared with Earth storms. | 0:16:01 | 0:16:04 | |
The Red Spot has been there for over 350 years and that makes it | 0:16:04 | 0:16:10 | |
the longest-living storm that we know of. | 0:16:10 | 0:16:13 | |
Jupiter may have the longest-lasting storm, | 0:16:17 | 0:16:20 | |
but it's Saturn, the next gas giant, | 0:16:20 | 0:16:22 | |
that is home to the largest and most powerful storm ever seen | 0:16:22 | 0:16:26 | |
in the solar system. | 0:16:26 | 0:16:28 | |
And in 2010, the Cassini spacecraft was there to see it. | 0:16:28 | 0:16:32 | |
Saturn, of course, is a spectacular sight because of the rings, | 0:16:35 | 0:16:39 | |
and it's also rather boring as far as the weather is concerned. | 0:16:39 | 0:16:43 | |
It's a bland thing. | 0:16:43 | 0:16:45 | |
But every now and then - 20, 30 years - | 0:16:46 | 0:16:50 | |
Saturn erupts with a giant storm, | 0:16:50 | 0:16:53 | |
and Cassini was fortunate to be orbiting Saturn at the time | 0:16:53 | 0:16:59 | |
of one of these eruptions. | 0:16:59 | 0:17:01 | |
What happened was, on December 5th 2010, | 0:17:01 | 0:17:06 | |
the radio receiver on Cassini started picking up the radio signal | 0:17:06 | 0:17:12 | |
of lightning. | 0:17:12 | 0:17:13 | |
And on the same day the camera saw a little storm up in | 0:17:15 | 0:17:19 | |
the northern hemisphere of Saturn. | 0:17:19 | 0:17:21 | |
By January it had developed into a fair-sized thing, | 0:17:23 | 0:17:28 | |
and then we watched it for six months. | 0:17:28 | 0:17:30 | |
During that time a huge storm grew and wrapped itself | 0:17:33 | 0:17:36 | |
around the entire planet, covering 4 billion square kilometres | 0:17:36 | 0:17:41 | |
until its head caught up with its tail. | 0:17:41 | 0:17:44 | |
Driven by winds going at around 1,800km per hour, with huge | 0:17:47 | 0:17:52 | |
lightning flashes 10,000 times stronger than those we get on Earth. | 0:17:52 | 0:17:56 | |
It's very funny, Jupiter has these very long-lived storms, | 0:17:59 | 0:18:03 | |
but Saturn has these very violent storms. | 0:18:03 | 0:18:07 | |
We don't fully understand why there is this difference in the weather | 0:18:07 | 0:18:10 | |
between Jupiter and Saturn. | 0:18:10 | 0:18:12 | |
Whether it's duration or size, | 0:18:12 | 0:18:14 | |
the storms on both these planets dwarf those on Earth. | 0:18:14 | 0:18:17 | |
However, because they receive far less heat from the sun | 0:18:21 | 0:18:24 | |
than the Earth does, something else is also powering their weather. | 0:18:24 | 0:18:29 | |
The weather on Jupiter and Saturn comes from two sources. | 0:18:29 | 0:18:32 | |
One is the sun, as on Earth, | 0:18:32 | 0:18:35 | |
and the other is the internal heat left over | 0:18:35 | 0:18:38 | |
from when the planets formed. | 0:18:38 | 0:18:40 | |
It's this internal heat trying to escape through | 0:18:40 | 0:18:43 | |
their deep atmospheres that makes the gas planets so tumultuous. | 0:18:43 | 0:18:47 | |
This zone dry and sunny throughout the day. | 0:18:52 | 0:18:56 | |
Later this afternoon there will be more in the way of clouds... | 0:18:56 | 0:18:59 | |
The storms on the gas planets are certainly | 0:18:59 | 0:19:02 | |
weirder and wilder than any we have on Earth, | 0:19:02 | 0:19:05 | |
but when it comes to the clouds and the rain, things get even stranger. | 0:19:05 | 0:19:10 | |
It's a typical June morning in Southern California... | 0:19:13 | 0:19:16 | |
..and a local weather phenomenon known as the June gloom makes it | 0:19:17 | 0:19:21 | |
the perfect day for taking a closer look at the clouds. | 0:19:21 | 0:19:24 | |
Dr Kevin Baines has a passion for the skies, on Earth and beyond, | 0:19:30 | 0:19:35 | |
and he's been studying the clouds on the gas planets. | 0:19:35 | 0:19:40 | |
Coming out of SoCal, | 0:19:40 | 0:19:41 | |
we're going to make a left turn on alpha | 0:19:41 | 0:19:44 | |
and taxi over to the run-up area for runway one. | 0:19:44 | 0:19:46 | |
So on a planet you'll get clouds at different levels, | 0:19:52 | 0:19:54 | |
depending on the local temperature and the local pressure. | 0:19:54 | 0:19:58 | |
On Earth, all clouds are made of water. | 0:19:58 | 0:20:01 | |
So in southern California we have this marine layer. | 0:20:01 | 0:20:04 | |
What happens is it actually forms over the water. | 0:20:04 | 0:20:07 | |
The Pacific Ocean, of course, has a lot of water, | 0:20:07 | 0:20:10 | |
so during the day it heats up and releases water into the air | 0:20:10 | 0:20:13 | |
as water vapour. As this water vapour rises, | 0:20:13 | 0:20:16 | |
it cools then it condenses out as water droplets in the air, | 0:20:16 | 0:20:22 | |
and when you get millions and millions of water droplets, | 0:20:22 | 0:20:24 | |
it forms a cloud. | 0:20:24 | 0:20:26 | |
Clouds will form wherever it gets too cold for water to stay | 0:20:26 | 0:20:30 | |
as a vapour in the air. | 0:20:30 | 0:20:32 | |
And if there's enough moisture, | 0:20:34 | 0:20:36 | |
the cloud droplets grow in size until they are big and heavy enough | 0:20:36 | 0:20:39 | |
to fall as rain. | 0:20:39 | 0:20:40 | |
Jupiter and Saturn also have a layer of water clouds. | 0:20:43 | 0:20:46 | |
If we were to transport ourselves magically to Jupiter or Saturn, | 0:20:51 | 0:20:54 | |
we could find a water layer like this. | 0:20:54 | 0:20:57 | |
But other substances form clouds at colder temperatures, | 0:20:57 | 0:21:01 | |
so above the layer of water clouds, | 0:21:01 | 0:21:03 | |
higher up in the atmospheres of Jupiter and Saturn, | 0:21:03 | 0:21:06 | |
there are two more cloud layers. | 0:21:06 | 0:21:09 | |
As you climb up out of the water layer, | 0:21:09 | 0:21:11 | |
it gets so cold that first you get ammonia hydrosulphide, | 0:21:11 | 0:21:14 | |
which is very exotic cloud made of both ammonia | 0:21:14 | 0:21:17 | |
and sulphur put together, | 0:21:17 | 0:21:19 | |
and then as you climb up even higher into the atmosphere, | 0:21:19 | 0:21:22 | |
when it gets down to about minus 130 Celsius, | 0:21:22 | 0:21:26 | |
there ammonia gas in the atmosphere condenses out and forms clouds. | 0:21:26 | 0:21:32 | |
So on these planets it doesn't just rain water, | 0:21:32 | 0:21:35 | |
there could also be a light rain of liquid ammonia. | 0:21:35 | 0:21:39 | |
Now if you go out to Uranus and Neptune, it is so cold out there, | 0:21:39 | 0:21:43 | |
about -300 degrees, | 0:21:43 | 0:21:45 | |
that you even have methane gas come out as clouds. | 0:21:45 | 0:21:49 | |
And so on Uranus and Neptune, liquid methane could fall from the sky. | 0:21:51 | 0:21:55 | |
Bizarre as they are, ammonia and methane aren't | 0:21:58 | 0:22:02 | |
the weirdest rains of all, | 0:22:02 | 0:22:04 | |
because back on Saturn, in the depths of its atmosphere, | 0:22:04 | 0:22:08 | |
Kevin believes that an astonishing process is at work that creates | 0:22:08 | 0:22:13 | |
what could be the strangest rain in the solar system. | 0:22:13 | 0:22:16 | |
This process can be witnessed an on idyllic summer day in Oxfordshire. | 0:22:21 | 0:22:25 | |
Inside this unremarkable office building, | 0:22:28 | 0:22:31 | |
a manufacturing company is replicating the conditions deep | 0:22:31 | 0:22:34 | |
in Saturn's atmosphere, not to study it, but for industrial purposes. | 0:22:34 | 0:22:39 | |
Using these massive presses, | 0:22:41 | 0:22:43 | |
they're turning carbon graphite into something far more valuable... | 0:22:43 | 0:22:46 | |
..and Kevin has come over from California to see how this process | 0:22:49 | 0:22:53 | |
can help explain what's happening deep inside Saturn. | 0:22:53 | 0:22:56 | |
We know that on Saturn there's carbon soot. | 0:22:58 | 0:23:01 | |
We know that by looking at these dark clouds that we saw with | 0:23:01 | 0:23:04 | |
our camera onboard the Cassini spacecraft orbiting Saturn, | 0:23:04 | 0:23:07 | |
and we see the spectroscopic signature of carbon soot there. | 0:23:07 | 0:23:11 | |
The carbon soot is created by lightning, | 0:23:11 | 0:23:13 | |
lightning actually zapping methane in the atmosphere. | 0:23:13 | 0:23:16 | |
Something very strange then happens to the soot as it falls | 0:23:18 | 0:23:22 | |
through Saturn's atmosphere. | 0:23:22 | 0:23:24 | |
It is transformed into something remarkable, | 0:23:25 | 0:23:29 | |
a process that is actually being replicated here. | 0:23:29 | 0:23:33 | |
What we do, effectively, | 0:23:33 | 0:23:34 | |
is we take this carbon graphite and mix it with several other materials | 0:23:34 | 0:23:39 | |
and we assemble what we call a capsule. | 0:23:39 | 0:23:41 | |
We take that capsule, the graphite material inside it, | 0:23:41 | 0:23:45 | |
and we place it inside the actual press itself. | 0:23:45 | 0:23:49 | |
The press is then closed up and the carbon graphite is exposed | 0:23:49 | 0:23:54 | |
to extreme temperatures and pressures. | 0:23:54 | 0:23:57 | |
High pressures are generated by these anvils that can press down | 0:23:58 | 0:24:02 | |
onto the graphite, pressures of around 50,000 atmospheres. | 0:24:02 | 0:24:06 | |
The graphite's then going to be heated to about 2,000 Celsius - | 0:24:06 | 0:24:10 | |
that heating happens by large electrical currents. | 0:24:10 | 0:24:13 | |
This process mimics what's happening inside Saturn. | 0:24:14 | 0:24:18 | |
We know we have carbon, which is very much like the graphite | 0:24:18 | 0:24:20 | |
that we just put into the machine over here. | 0:24:20 | 0:24:23 | |
The carbon soot precipitates or falls through the atmosphere, | 0:24:23 | 0:24:26 | |
and eventually it will get to the 7,000km level. | 0:24:26 | 0:24:29 | |
At that point, it will be experiencing the pressures | 0:24:29 | 0:24:31 | |
and temperatures that we experience in the press over here. | 0:24:31 | 0:24:35 | |
Inside the press, | 0:24:35 | 0:24:36 | |
the intense heat and crushing pressure transform the carbon | 0:24:36 | 0:24:41 | |
from graphite into diamond. | 0:24:41 | 0:24:43 | |
All right. | 0:24:48 | 0:24:49 | |
So this may not look like diamonds, | 0:24:49 | 0:24:51 | |
but we will then take this rubble and process it further | 0:24:51 | 0:24:54 | |
and we'll extract the diamond. | 0:24:54 | 0:24:56 | |
Great. So, the diamonds are in there somewhere? | 0:24:56 | 0:24:58 | |
Somewhere inside this rubble, Kevin, there are diamonds. | 0:24:58 | 0:25:01 | |
This high-temperature, | 0:25:05 | 0:25:06 | |
high-pressure process can make a variety of diamonds | 0:25:06 | 0:25:09 | |
which are used in industry. | 0:25:09 | 0:25:11 | |
Here we have tiny triangles - | 0:25:23 | 0:25:25 | |
effectively, these are used for wire drawing dies. | 0:25:25 | 0:25:28 | |
You get square-shaped diamonds which, in this case, | 0:25:28 | 0:25:31 | |
are used as single crystal cutting tools. | 0:25:31 | 0:25:35 | |
These diamonds are yellow because they contain nitrogen. | 0:25:35 | 0:25:39 | |
So what we were making earlier today, effectively, | 0:25:39 | 0:25:42 | |
are these diamond grits, tiny little stones of single crystal diamonds, | 0:25:42 | 0:25:47 | |
normally about 100 microns in size. | 0:25:47 | 0:25:49 | |
Kevin believes the same thing is happening on Saturn. | 0:25:51 | 0:25:54 | |
So we really think it's very similar conditions, | 0:25:56 | 0:25:58 | |
very similar process that's happening. | 0:25:58 | 0:26:00 | |
At the 7,000km level in Saturn, | 0:26:00 | 0:26:02 | |
carbon soot will transform itself into diamonds, | 0:26:02 | 0:26:05 | |
creating a diamond rain. | 0:26:05 | 0:26:06 | |
As the carbon soot falls from the clouds, | 0:26:09 | 0:26:12 | |
the extreme temperature and pressure deep in the atmosphere | 0:26:12 | 0:26:15 | |
turn it into diamonds. | 0:26:15 | 0:26:17 | |
So inside Saturn we have a huge region of diamond rain. | 0:26:20 | 0:26:23 | |
Our exploration of the other planets in our solar system has revealed | 0:26:28 | 0:26:32 | |
weather stranger and more powerful than anything we have here on Earth. | 0:26:32 | 0:26:36 | |
But what about beyond our solar system? | 0:26:39 | 0:26:42 | |
What is the weather like in the rest of the universe? | 0:26:42 | 0:26:46 | |
Some of those showers could be quite heavy. They'll be some dry spells | 0:26:50 | 0:26:52 | |
in between, but limited brightness and it will be a cool one... | 0:26:52 | 0:26:56 | |
Perched at the top of Mauna Kea in Hawaii, | 0:26:56 | 0:26:59 | |
4,000m above sea level, is the Keck Observatory, | 0:26:59 | 0:27:03 | |
one of the pre-eminent earthbound telescopes for finding planets | 0:27:03 | 0:27:07 | |
orbiting other stars, known as exoplanets. | 0:27:07 | 0:27:10 | |
Brendan Bowler has one of the best jobs in the world - | 0:27:14 | 0:27:18 | |
he's an exoplanet explorer. | 0:27:18 | 0:27:21 | |
I feel incredibly lucky studying astronomy and contributing | 0:27:21 | 0:27:24 | |
to exoplanetary science. | 0:27:24 | 0:27:27 | |
It's humbling, in many ways, | 0:27:27 | 0:27:28 | |
to be able to contribute and answer some of the questions | 0:27:28 | 0:27:34 | |
that we've been thinking about as humans for millennia. | 0:27:34 | 0:27:38 | |
The aim of my job is to find planets orbiting other stars, | 0:27:38 | 0:27:43 | |
which is a very difficult task to do. | 0:27:43 | 0:27:45 | |
Planets are both much smaller, | 0:27:47 | 0:27:49 | |
much lower mass and much fainter than the stars that they orbit, | 0:27:49 | 0:27:54 | |
so trying to find planets in the glare of their stars | 0:27:54 | 0:27:58 | |
is very difficult. | 0:27:58 | 0:28:00 | |
So it's as if we're trying to find a firefly buzzing around a spotlight | 0:28:00 | 0:28:05 | |
that's 10 billion times brighter than that firefly, | 0:28:05 | 0:28:08 | |
from a distance of New York all the way to London. | 0:28:08 | 0:28:11 | |
So how do you find a planet orbiting a distant star, | 0:28:15 | 0:28:19 | |
let alone study its weather? | 0:28:19 | 0:28:21 | |
There are two indirect methods that we primarily use to find planets. | 0:28:23 | 0:28:28 | |
The first is the radial velocity technique. | 0:28:28 | 0:28:31 | |
Let's say this is the planet and the post is the star that it's orbiting. | 0:28:31 | 0:28:35 | |
As a planet orbits its star, | 0:28:35 | 0:28:38 | |
the planet exerts gravitational influence on the host star, | 0:28:38 | 0:28:42 | |
which causes the host star to wobble. | 0:28:42 | 0:28:44 | |
We can search for planets by looking for the back and forth wobble | 0:28:47 | 0:28:50 | |
that planets induce on their host stars. | 0:28:50 | 0:28:52 | |
And that's exactly how the first exoplanet orbiting a sun-like star | 0:28:54 | 0:28:58 | |
was discovered, in 1995, changing the face of astronomy for ever. | 0:28:58 | 0:29:04 | |
And since then, planet hunters have discovered thousands more | 0:29:04 | 0:29:09 | |
orbiting distant stars. | 0:29:09 | 0:29:10 | |
But planetary explorers aren't satisfied | 0:29:14 | 0:29:17 | |
with simply finding planets. | 0:29:17 | 0:29:20 | |
What we really want to do is to be able to characterise the planet | 0:29:20 | 0:29:23 | |
in more detail. | 0:29:23 | 0:29:25 | |
The radial velocity method only tells us about | 0:29:25 | 0:29:28 | |
the mass of the planet. | 0:29:28 | 0:29:30 | |
The bigger the wobble, the bigger the mass, | 0:29:30 | 0:29:33 | |
but luckily there's a second technique for finding planets | 0:29:33 | 0:29:37 | |
known as the transit method, which reveals a whole lot more. | 0:29:37 | 0:29:42 | |
The transit method you can think of as a planet crossing between us, | 0:29:42 | 0:29:46 | |
our line of sight, and the star that it orbits, just like this. | 0:29:46 | 0:29:51 | |
Now when that crossing event occurs, | 0:29:51 | 0:29:53 | |
it will cause a dip in the brightness of that host star. | 0:29:53 | 0:29:57 | |
So we can use that to find planets, | 0:29:57 | 0:30:00 | |
by searching for periodic dips in the brightness of that star. | 0:30:00 | 0:30:04 | |
Crucially, the transit method also tells us how big the planet is, | 0:30:07 | 0:30:12 | |
because the bigger the planet, | 0:30:12 | 0:30:14 | |
the greater the dip in the light from the star. | 0:30:14 | 0:30:17 | |
The transit method tells us about the size of the planet, | 0:30:18 | 0:30:21 | |
while the radial velocity tells us about the mass of the planet, | 0:30:21 | 0:30:25 | |
so we can use both of those together to measure the density of planets, | 0:30:25 | 0:30:31 | |
because density is mass over volume. | 0:30:31 | 0:30:34 | |
And this reveals what the planet is made of. | 0:30:34 | 0:30:37 | |
Small dense planets are rocky, | 0:30:37 | 0:30:40 | |
whereas large planets that are not dense are gas giants. | 0:30:40 | 0:30:45 | |
The first planets discovered were huge gas giants like Jupiter, | 0:30:47 | 0:30:52 | |
and since then, planet hunters have found all sorts of combinations | 0:30:52 | 0:30:56 | |
of size and mass, including small, dense planets, | 0:30:56 | 0:31:01 | |
rocky worlds that could have atmospheres. | 0:31:01 | 0:31:03 | |
But finding out any more detail about an exoplanet's atmosphere, | 0:31:06 | 0:31:10 | |
climate and, ultimately, its weather, is extremely difficult. | 0:31:10 | 0:31:15 | |
But not impossible. | 0:31:18 | 0:31:20 | |
The key to doing this is the fact that different gases absorb light | 0:31:21 | 0:31:25 | |
at different wavelengths. | 0:31:25 | 0:31:27 | |
So we can study the composition of the atmospheres of exoplanets | 0:31:30 | 0:31:34 | |
by breaking up the light that we receive at Earth | 0:31:34 | 0:31:37 | |
into its constituent colours. | 0:31:37 | 0:31:39 | |
This is what we're doing here with the projector which emits | 0:31:39 | 0:31:41 | |
white light - we're dispersing it with a prism, | 0:31:41 | 0:31:44 | |
spreading out the light. We can see the various wavelengths and colours | 0:31:44 | 0:31:48 | |
it's split into. | 0:31:48 | 0:31:50 | |
If we have a gas intervening between the projector | 0:31:50 | 0:31:53 | |
and the prism, then the different colours will be blocked out, | 0:31:53 | 0:31:57 | |
depending on the nature of the gas. | 0:31:57 | 0:31:59 | |
So what I'm going to do is put a gas in this beam of light | 0:31:59 | 0:32:03 | |
by burning baking soda, which is sodium bicarbonate. | 0:32:03 | 0:32:06 | |
So here we have our baking soda. | 0:32:08 | 0:32:09 | |
We'll drop a little bit of that into the flame. | 0:32:11 | 0:32:14 | |
And so what we're doing is making the equivalent of an atmosphere | 0:32:16 | 0:32:20 | |
of sodium atoms in the beam, which is absorbing some of the light. | 0:32:20 | 0:32:25 | |
What we see on the spectrum is a narrow dark line that comes and goes | 0:32:25 | 0:32:28 | |
as I drop it in, in the yellow part of the spectrum, | 0:32:28 | 0:32:31 | |
which corresponds to the wavelength that sodium absorbs. | 0:32:31 | 0:32:35 | |
Every chemical has its own unique pattern of absorption lines. | 0:32:35 | 0:32:39 | |
So astronomers can use this information to detect | 0:32:42 | 0:32:45 | |
the different substances in the atmospheres of planets. | 0:32:45 | 0:32:49 | |
And that's exactly what Brendan is going to try to do tonight. | 0:32:49 | 0:32:54 | |
He's pointing the Keck telescope's awesome light gathering power | 0:32:54 | 0:32:58 | |
at a newly discovered planet. | 0:32:58 | 0:32:59 | |
I'll be using the Keck telescope to study a planet | 0:33:02 | 0:33:06 | |
about 400 light years away. | 0:33:06 | 0:33:08 | |
Its name is ROXs 12 b, | 0:33:08 | 0:33:11 | |
it has a mass between 10-15 times that of Jupiter, | 0:33:11 | 0:33:15 | |
and we know it's a gas giant, but we don't know what it's made out of, | 0:33:15 | 0:33:17 | |
which is the goal of our observations. | 0:33:17 | 0:33:20 | |
By studying the light that is emitted from this planet, | 0:33:20 | 0:33:23 | |
we'll be able to learn about the chemical composition and physical | 0:33:23 | 0:33:26 | |
properties of its atmosphere. | 0:33:26 | 0:33:28 | |
ROXs 12 is about to rise. | 0:33:33 | 0:33:35 | |
We have two more minutes. | 0:33:35 | 0:33:37 | |
It's below the telescope limits, but it is about to go up, | 0:33:37 | 0:33:40 | |
and then we can slew to it. | 0:33:40 | 0:33:43 | |
We're trying to look in the infrared, | 0:33:43 | 0:33:45 | |
to both image the planet and get a spectrum of it. | 0:33:45 | 0:33:49 | |
When we can get a spectrum of the planet, | 0:33:49 | 0:33:52 | |
we can learn what's in its atmosphere. | 0:33:52 | 0:33:54 | |
Direct imaging of distant planets like this | 0:33:56 | 0:33:59 | |
is at the very cutting edge of astronomy. | 0:33:59 | 0:34:03 | |
It's incredibly difficult to image planets, | 0:34:03 | 0:34:06 | |
but for the most massive planets, like ROXs 12 b, | 0:34:06 | 0:34:09 | |
it emits enough light that we can actually detect the photons, | 0:34:09 | 0:34:13 | |
so we can see the planet and take pictures of the planet. | 0:34:13 | 0:34:17 | |
And for this, we need our very best telescopes. | 0:34:17 | 0:34:20 | |
Keck is the biggest telescope in the world, | 0:34:21 | 0:34:25 | |
so we need the size of the mirror, which is ten metres in diameter, | 0:34:25 | 0:34:28 | |
to gather enough photons. | 0:34:28 | 0:34:30 | |
Incredibly, the Keck telescope also compensates for interference | 0:34:31 | 0:34:36 | |
from our own atmosphere. | 0:34:36 | 0:34:38 | |
Stars twinkle because of turbulence in the Earth's atmosphere. | 0:34:40 | 0:34:44 | |
We don't like that twinkling, we want it to stop, | 0:34:44 | 0:34:47 | |
so we use adaptive optics to actively compensate, in real time, | 0:34:47 | 0:34:51 | |
thousands of times per second, for that turbulence. | 0:34:51 | 0:34:55 | |
It's as if we're putting these big telescopes that we have | 0:34:55 | 0:34:57 | |
on the ground in space. | 0:34:57 | 0:34:59 | |
So far, only a handful of planets have ever been | 0:35:02 | 0:35:05 | |
directly imaged like this. | 0:35:05 | 0:35:07 | |
Martha, what are the coordinates? | 0:35:07 | 0:35:09 | |
16, 26, 28.1. | 0:35:09 | 0:35:12 | |
Can you go to ROXs 12 and the moon and look how it looks in the tracks? | 0:35:14 | 0:35:18 | |
Yeah. | 0:35:18 | 0:35:19 | |
That's it finished, and we're ready. | 0:35:19 | 0:35:22 | |
This is our sixth attempt to get this target. | 0:35:22 | 0:35:25 | |
We've been weathered out, we've had instrument issues, | 0:35:25 | 0:35:29 | |
and we think we're finally going to get it tonight. | 0:35:29 | 0:35:32 | |
OK, so I think we have the target centred up | 0:35:34 | 0:35:37 | |
in the field of view here. | 0:35:37 | 0:35:40 | |
I think we can start... | 0:35:40 | 0:35:42 | |
exposing. | 0:35:42 | 0:35:43 | |
So, here we have our image of ROXs 12 b. | 0:35:53 | 0:35:56 | |
So this is an infrared image of this planet, | 0:35:56 | 0:36:00 | |
which is pretty amazing to think that we are imaging a planet | 0:36:00 | 0:36:04 | |
400 light years away. | 0:36:04 | 0:36:05 | |
ROXs 12 b is one of only 15 exoplanets | 0:36:07 | 0:36:11 | |
to have ever been directly imaged. | 0:36:11 | 0:36:14 | |
And, incredibly, the faint light captured in this picture | 0:36:16 | 0:36:20 | |
will reveal the secrets of ROXs 12 b's atmosphere, | 0:36:20 | 0:36:24 | |
the first step towards understanding its weather. | 0:36:24 | 0:36:28 | |
We're looking at the infrared light from this planet. | 0:36:28 | 0:36:30 | |
This is light that's emitted in the interior of the planet | 0:36:30 | 0:36:33 | |
and passed through its atmosphere, and whatever chemicals, molecules, | 0:36:33 | 0:36:38 | |
atoms are in the atmosphere, | 0:36:38 | 0:36:39 | |
will induce absorption features in the spectrum, | 0:36:39 | 0:36:43 | |
and that's what we're looking for. | 0:36:43 | 0:36:45 | |
So here we can actually get a spectrum in real-time, | 0:36:45 | 0:36:48 | |
and let's go ahead and do it. | 0:36:48 | 0:36:49 | |
So here's our spectrum of ROXs 12 b in the infrared. | 0:36:51 | 0:36:56 | |
What we're looking for are absorption features | 0:36:56 | 0:36:59 | |
from carbon monoxide, CO. | 0:36:59 | 0:37:00 | |
So we can see these two dips here in the spectrum, | 0:37:03 | 0:37:06 | |
which correspond to the wavelengths where CO absorbs, | 0:37:06 | 0:37:09 | |
and that means that this planet really does have carbon monoxide | 0:37:09 | 0:37:12 | |
in its atmosphere. | 0:37:12 | 0:37:13 | |
The spectrum also revealed that this exoplanet has water vapour, | 0:37:15 | 0:37:18 | |
iron hydride, vanadium oxide, potassium and sodium | 0:37:18 | 0:37:23 | |
in its atmosphere - fairly typical for an exoplanet. | 0:37:23 | 0:37:26 | |
So by studying the light from exoplanets | 0:37:27 | 0:37:30 | |
hundreds of light years away, | 0:37:30 | 0:37:32 | |
astronomers are able to detect what's in their atmosphere... | 0:37:32 | 0:37:35 | |
..a key ingredient that goes into creating their weather. | 0:37:39 | 0:37:42 | |
Later today, a mixture of brighter spells | 0:37:50 | 0:37:52 | |
and showers for the majority... | 0:37:52 | 0:37:55 | |
As well as being able to detect the gases in a planet's atmosphere, | 0:37:55 | 0:37:59 | |
scientists can also use the infrared light to work out | 0:37:59 | 0:38:02 | |
just how hot a planet is. | 0:38:02 | 0:38:04 | |
It's a blustery day in California | 0:38:08 | 0:38:11 | |
and exoplanet meteorologist Heather Knutson | 0:38:11 | 0:38:14 | |
is visiting Santa Monica Pier. | 0:38:14 | 0:38:16 | |
So the main thing that determines the temperature of a planet | 0:38:18 | 0:38:21 | |
is the distance that it is from its host star. | 0:38:21 | 0:38:24 | |
Planets that are really close in are going to be boiling hot. | 0:38:24 | 0:38:26 | |
Planets that are further away will be a little bit cooler | 0:38:26 | 0:38:29 | |
by comparison. | 0:38:29 | 0:38:31 | |
Most of the exoplanets discovered so far are close to their stars, | 0:38:31 | 0:38:35 | |
so scientists expected them to be hot, | 0:38:35 | 0:38:39 | |
but they didn't know how hot. | 0:38:39 | 0:38:41 | |
So we can actually go and measure the temperature of these planets | 0:38:41 | 0:38:43 | |
by measuring their brightness in infrared light. | 0:38:43 | 0:38:46 | |
Hotter things are going to glow more brightly in infrared wavelengths, | 0:38:46 | 0:38:49 | |
cooler things are going to be a little bit dimmer and fainter. | 0:38:49 | 0:38:53 | |
So probably the hottest planet that we know of is a planet | 0:38:55 | 0:38:58 | |
called WASP-33 b. | 0:38:58 | 0:38:59 | |
WASP-33 b is the hottest planet discovered so far | 0:39:01 | 0:39:05 | |
in the entire universe. | 0:39:05 | 0:39:08 | |
It's a gas giant, four and a half times the size of Jupiter. | 0:39:08 | 0:39:12 | |
Its atmosphere is a scorching 3,200 Celsius. | 0:39:12 | 0:39:17 | |
So this planet is hot for two reasons - | 0:39:19 | 0:39:21 | |
one is it's very close to its host star. | 0:39:21 | 0:39:23 | |
The other is it orbits a star that is bigger and hotter than the sun. | 0:39:23 | 0:39:28 | |
Both those things together combine to make this | 0:39:28 | 0:39:30 | |
one of the hottest planets we've discovered. | 0:39:30 | 0:39:33 | |
Planets like WASP-33 b are nicknamed Hot Jupiters, | 0:39:35 | 0:39:40 | |
and they don't just have extreme temperatures... | 0:39:40 | 0:39:42 | |
..because being close to their star has another important effect | 0:39:44 | 0:39:47 | |
on the weather. | 0:39:47 | 0:39:50 | |
So all planets spin on their axis, just like I am now. | 0:39:50 | 0:39:54 | |
The Earth spins once every 24 hours, | 0:39:54 | 0:39:56 | |
but not all planets spin at the same speed. | 0:39:56 | 0:39:59 | |
There are some planets which we're discovering which are very, | 0:39:59 | 0:40:02 | |
very close to their stars. | 0:40:02 | 0:40:04 | |
They're so close that the star tugs on the planet as it spins around | 0:40:04 | 0:40:08 | |
on its axis, and the tugging of that star actually slows | 0:40:08 | 0:40:12 | |
the planet's rotation down, | 0:40:12 | 0:40:15 | |
keeps slowing it down and keeps slowing it down until the planet | 0:40:15 | 0:40:18 | |
rotates at exactly the same speed that it orbits. | 0:40:18 | 0:40:23 | |
So the same side of the planet always faces towards the star, | 0:40:23 | 0:40:26 | |
just like I'm always facing the centre of this ride here. | 0:40:26 | 0:40:28 | |
We call this tidal locking, | 0:40:30 | 0:40:32 | |
and it means the planet has a permanent day side | 0:40:32 | 0:40:35 | |
and a permanent night side. | 0:40:35 | 0:40:37 | |
And being tidally locked has a dramatic impact. | 0:40:38 | 0:40:41 | |
So whenever you have one part of a planet that's hot and another part | 0:40:43 | 0:40:46 | |
that's cold, the natural result is that you get a wind moving | 0:40:46 | 0:40:50 | |
from one part to another. | 0:40:50 | 0:40:51 | |
Here at the beach during the day the land heats up but the sea stays | 0:40:52 | 0:40:56 | |
relatively cold, and so you get this nice wind moving from the ocean | 0:40:56 | 0:40:59 | |
towards the land that's trying to even out the temperatures. | 0:40:59 | 0:41:02 | |
So when we first discovered these very close-in planets, | 0:41:02 | 0:41:05 | |
we realised they were probably close enough to be tidally locked. | 0:41:05 | 0:41:09 | |
And one of the very first things we wanted to know is what that meant | 0:41:09 | 0:41:11 | |
for the planet's atmosphere. | 0:41:11 | 0:41:13 | |
Did it mean these planets had a boiling hot day side | 0:41:13 | 0:41:16 | |
and a freezing cold night side? | 0:41:16 | 0:41:18 | |
Or were there winds in the atmosphere that were able to carry | 0:41:18 | 0:41:20 | |
some of that heat around to the night side? | 0:41:20 | 0:41:23 | |
To find out, Heather mapped the temperature on a Hot Jupiter... | 0:41:25 | 0:41:29 | |
..which scientists think is blue in colour. | 0:41:32 | 0:41:35 | |
The particular planet we decided to look at was a Hot Jupiter | 0:41:35 | 0:41:39 | |
called HD 189733. | 0:41:39 | 0:41:41 | |
That's kind of a mouthful, but I can tell you that this is actually | 0:41:41 | 0:41:44 | |
my favourite Hot Jupiter, this was one of the very first planets | 0:41:44 | 0:41:47 | |
that I looked at when I was a grad student. | 0:41:47 | 0:41:49 | |
By looking at it in infrared, | 0:41:49 | 0:41:51 | |
Heather was able to measure its temperature. | 0:41:51 | 0:41:53 | |
So this is the map we made. | 0:41:55 | 0:41:56 | |
So the colour tells you the temperature of different parts | 0:41:56 | 0:41:59 | |
of the atmosphere. So here on the day side things are relatively hot, | 0:41:59 | 0:42:03 | |
so the day side is about 900 degrees Centigrade. | 0:42:03 | 0:42:07 | |
Here, on the edges, that's the night side, | 0:42:07 | 0:42:10 | |
and that's a relatively cool part of the atmosphere, | 0:42:10 | 0:42:12 | |
it's only 700 degrees Centigrade, which is still really hot. | 0:42:12 | 0:42:16 | |
That difference is actually much smaller than we expected, | 0:42:16 | 0:42:19 | |
and the fact it's so small suggested to us that this planet must have | 0:42:19 | 0:42:22 | |
strong winds circulating through its atmosphere and carrying that hot air | 0:42:22 | 0:42:26 | |
from the day side around to the night side. | 0:42:26 | 0:42:29 | |
Incredibly, these winds have now been measured directly, | 0:42:31 | 0:42:36 | |
and it turns out that HD 189733 b is home | 0:42:36 | 0:42:41 | |
to the fastest winds in the universe | 0:42:41 | 0:42:44 | |
which rage around it at about 8,700km per hour, | 0:42:44 | 0:42:50 | |
seven times the speed of sound, | 0:42:50 | 0:42:52 | |
and 20 times faster than the fastest winds ever experienced on Earth. | 0:42:52 | 0:42:57 | |
Showers, some of them of sleet and snow. | 0:42:59 | 0:43:02 | |
Elsewhere fewer showers and here the showers will be of rain... | 0:43:02 | 0:43:08 | |
It's a beautiful tropical morning on the Big Island in Hawaii. | 0:43:08 | 0:43:11 | |
Exoplanet expert Hannah Wakeford is taking to the skies | 0:43:14 | 0:43:18 | |
to explore another bizarre effect the extreme heat on exoplanets | 0:43:18 | 0:43:22 | |
has on their weather. | 0:43:22 | 0:43:23 | |
The strangest thing about exoplanets is the clouds and the rain - | 0:43:27 | 0:43:30 | |
they're nothing like we have here on Earth. | 0:43:30 | 0:43:33 | |
Spectroscopy has revealed that exoplanets have clouds, | 0:43:33 | 0:43:37 | |
and also what these clouds might be made of. | 0:43:37 | 0:43:40 | |
We know that exoplanets have clouds. | 0:43:40 | 0:43:42 | |
If we have a planet that we know should be gaseous because of | 0:43:42 | 0:43:44 | |
its density but we don't detect any spectral signatures from that gas, | 0:43:44 | 0:43:48 | |
then we think there must be clouds in the way which are blocking that | 0:43:48 | 0:43:51 | |
light and obscuring our view. | 0:43:51 | 0:43:54 | |
And sometimes we can detect signatures directly from | 0:43:54 | 0:43:56 | |
those clouds by the way that they scatter or reflect the light. | 0:43:56 | 0:43:59 | |
But these aren't clouds we'd recognise. | 0:44:03 | 0:44:06 | |
A lot of the exoplanets that we've been able to follow up are very hot, | 0:44:09 | 0:44:12 | |
over 1,000 degrees, | 0:44:12 | 0:44:14 | |
so we know that water can't exist as a liquid at those temperatures, | 0:44:14 | 0:44:17 | |
so they're not going to be clouds like we have here on Earth. | 0:44:17 | 0:44:20 | |
Woo, we're in a cloud! | 0:44:22 | 0:44:24 | |
So, on some exoplanets, | 0:44:26 | 0:44:27 | |
the clouds will be made of far more exotic substances. | 0:44:27 | 0:44:31 | |
The temperatures are such that substances that we think of | 0:44:33 | 0:44:36 | |
as solids on Earth can actually exist as liquids or gas | 0:44:36 | 0:44:39 | |
in exoplanet atmospheres. | 0:44:39 | 0:44:41 | |
We can get a glimpse of this on Earth in volcanoes, | 0:44:43 | 0:44:46 | |
where temperatures can reach over 1,000 degrees Celsius. | 0:44:46 | 0:44:50 | |
Down there is the crater of Pu'u 'O'o, | 0:44:52 | 0:44:55 | |
and you can see the lava bubbling away. | 0:44:55 | 0:44:59 | |
The temperature of this lava lake is around 1,000 degrees | 0:44:59 | 0:45:02 | |
and all of the rock has melted. | 0:45:02 | 0:45:04 | |
The metals and minerals and the silicates that make up | 0:45:04 | 0:45:07 | |
the Earth's crust have all become molten. | 0:45:07 | 0:45:12 | |
It's amazing - you can really feel the temperature from the lava lake | 0:45:12 | 0:45:16 | |
all the way up here. It's really very hot. | 0:45:16 | 0:45:19 | |
It's 1,000 degrees melting the Earth's crust down there, | 0:45:21 | 0:45:24 | |
so it's no surprise. | 0:45:24 | 0:45:26 | |
And it's these substances that are thought to make up the clouds | 0:45:28 | 0:45:32 | |
on some exoplanets. | 0:45:32 | 0:45:34 | |
There's a planet called 55 Cancri e | 0:45:35 | 0:45:38 | |
that we think is rocky because of its density, | 0:45:38 | 0:45:40 | |
but it orbits very close to its parent star and is tidally locked, | 0:45:40 | 0:45:44 | |
so temperatures on the day side should be high enough to melt the rock, | 0:45:44 | 0:45:48 | |
making it a lava planet. | 0:45:48 | 0:45:50 | |
55 Cancri e is a lava planet. | 0:45:54 | 0:45:57 | |
While its night side will be relatively cool and solid rock, | 0:45:57 | 0:46:01 | |
its day side is an ocean of permanently molten lava. | 0:46:01 | 0:46:06 | |
On the day side, the temperatures go over 2,500 degrees. | 0:46:06 | 0:46:11 | |
This is hot enough to vaporise the rock at the surface. | 0:46:11 | 0:46:15 | |
This can then be lifted into the atmosphere and condensed | 0:46:15 | 0:46:19 | |
to form clouds of liquid lava droplets that then can be | 0:46:19 | 0:46:22 | |
transported to colder parts of the planet, | 0:46:22 | 0:46:25 | |
where they will rain down as pebbles on the surface. | 0:46:25 | 0:46:28 | |
So on some planets, it rains rock | 0:46:34 | 0:46:37 | |
rather than water like it does here in Hawaii. | 0:46:37 | 0:46:39 | |
Back on the ground on Kilauea, | 0:46:50 | 0:46:52 | |
Hannah has an example of what rock rain might be like. | 0:46:52 | 0:46:55 | |
Right here was the site of a massive eruption. | 0:47:00 | 0:47:03 | |
All along this fissure, | 0:47:03 | 0:47:05 | |
fountains of lava shot into the air nearly 100m high. | 0:47:05 | 0:47:10 | |
The liquid lava droplets then cooled and solidified in the air | 0:47:10 | 0:47:14 | |
before raining down onto the surface as these tiny pebbles, | 0:47:14 | 0:47:19 | |
and sometimes we get these perfect little droplets called Pele's tears. | 0:47:19 | 0:47:23 | |
This is what we think the rain might be like an planets like 55 Cancri e. | 0:47:25 | 0:47:29 | |
But perhaps the strangest rain in the entire universe has been discovered | 0:47:40 | 0:47:45 | |
on a giant gas planet which orbits a star hundreds of light years away. | 0:47:45 | 0:47:50 | |
We've been able to study the exoplanet WASP-12b | 0:47:53 | 0:47:57 | |
and the way that it scatters light suggests that there are clouds | 0:47:57 | 0:48:00 | |
high up in the atmosphere. | 0:48:00 | 0:48:02 | |
At this part of the atmosphere, the temperature is around 2,000 degrees, | 0:48:02 | 0:48:06 | |
so the most likely substance forming these clouds | 0:48:06 | 0:48:09 | |
is an aluminium oxide called corundum, | 0:48:09 | 0:48:11 | |
which forms the basis of rubies. | 0:48:11 | 0:48:14 | |
So instead of having rain which is liquid water droplets | 0:48:14 | 0:48:18 | |
like here on Earth, it would be raining rubies. | 0:48:18 | 0:48:21 | |
We are only just witnessing the birth of exoplanet meteorology. | 0:48:28 | 0:48:32 | |
But so far, what astronomers have discovered on exoplanets | 0:48:32 | 0:48:37 | |
is even more extreme and bizarre than anything anyone had imagined. | 0:48:37 | 0:48:42 | |
Compared to what's out there, | 0:48:49 | 0:48:51 | |
the most extreme weather on Earth - our hurricanes and tornadoes, | 0:48:51 | 0:48:55 | |
our rain and our snow - all seem pretty mild. | 0:48:55 | 0:48:59 | |
Our climate and weather is actually very hospitable. | 0:48:59 | 0:49:02 | |
The Earth is a nice place and that's all because of the weather. | 0:49:02 | 0:49:07 | |
We've got warm temperatures - not too hot, not too cold. | 0:49:07 | 0:49:10 | |
It's a great place. | 0:49:10 | 0:49:11 | |
Ultimately, the planet hunters of the world are hoping to find one thing - | 0:49:13 | 0:49:17 | |
another Earth. | 0:49:17 | 0:49:19 | |
A small, rocky planet with a thin blue line encircling it. | 0:49:20 | 0:49:24 | |
A planet with a nice climate, | 0:49:24 | 0:49:27 | |
a climate that could be hospitable to life. | 0:49:27 | 0:49:29 | |
What we're really looking for is rocky terrestrial-type planets | 0:49:31 | 0:49:35 | |
with an atmosphere around them which is habitable. | 0:49:35 | 0:49:38 | |
We'd like that planet to be at the right temperature to have liquid water, | 0:49:40 | 0:49:43 | |
so that means being at just the right distance from your stars | 0:49:43 | 0:49:47 | |
and having exactly the right kind of atmosphere. | 0:49:47 | 0:49:51 | |
But so far, astronomers have mainly found planets | 0:49:51 | 0:49:54 | |
with extreme environments - | 0:49:54 | 0:49:56 | |
planets with ruby rain or lava clouds. | 0:49:56 | 0:50:00 | |
So the planets that we've found so far aren't particularly nice places to go. | 0:50:00 | 0:50:04 | |
They're not somewhere you would put on your vacation list any time soon. | 0:50:04 | 0:50:08 | |
Because at the moment, it's easier to both find and study | 0:50:08 | 0:50:11 | |
the bigger planets... | 0:50:11 | 0:50:13 | |
When you're looking at other stars, | 0:50:13 | 0:50:14 | |
it's easy to find the large planets like Jupiter and Saturn, | 0:50:14 | 0:50:19 | |
where you don't have the right kind of atmosphere. | 0:50:19 | 0:50:22 | |
..or ones that are close to their stars. | 0:50:22 | 0:50:24 | |
Our surveys are really good at finding planets that are very close | 0:50:24 | 0:50:27 | |
to their stars, which means mostly the planets that we've discovered | 0:50:27 | 0:50:30 | |
are much too hot to host life as we know it on Earth. | 0:50:30 | 0:50:34 | |
Just over 20 years ago, astronomers began finding exoplanets. | 0:50:34 | 0:50:39 | |
The first were giant Hot Jupiters orbiting close to their stars, | 0:50:39 | 0:50:43 | |
because they were the easiest to spot. | 0:50:43 | 0:50:46 | |
And now hundreds of smaller rocky planets have also been found, | 0:50:46 | 0:50:50 | |
but most of these are still larger than Earth | 0:50:50 | 0:50:53 | |
and still too close to their stars. | 0:50:53 | 0:50:55 | |
But the search for another Earth is still in its infancy. | 0:50:58 | 0:51:02 | |
Dr Brice Demory is a planet hunter | 0:51:05 | 0:51:09 | |
and he may have found the promised land of planetary exploration - | 0:51:09 | 0:51:13 | |
a planet that could have warm, mild weather, | 0:51:13 | 0:51:16 | |
weather just like a lovely summer evening in Cambridge. | 0:51:16 | 0:51:19 | |
So we are looking for rocky planets | 0:51:21 | 0:51:23 | |
similar to the Earth in size and located at the right distance from its star. | 0:51:23 | 0:51:28 | |
It is a bit like cooking a marshmallow - | 0:51:28 | 0:51:30 | |
If the marshmallow is too close to the fire, then it will burn, | 0:51:30 | 0:51:33 | |
if it is too far away, it will never cook. | 0:51:33 | 0:51:35 | |
So we want the planet to be at the distance that is just right | 0:51:35 | 0:51:39 | |
for habitable conditions to happen. | 0:51:39 | 0:51:41 | |
We have just found three Earth-sized planets that are orbiting | 0:51:42 | 0:51:46 | |
a very cool star called Trappist-1, | 0:51:46 | 0:51:49 | |
and these planets are remarkable. | 0:51:49 | 0:51:51 | |
The first one is located here and receives about four times the level | 0:51:51 | 0:51:55 | |
of radiation that the Earth does. | 0:51:55 | 0:51:58 | |
The second one, look at it here, | 0:51:58 | 0:52:00 | |
receives twice the level of radiation that the Earth does. | 0:52:00 | 0:52:04 | |
Those planets are probably too hot to be habitable. | 0:52:04 | 0:52:08 | |
The third one is the most interesting one. | 0:52:08 | 0:52:10 | |
We're not exactly sure of its location right now, | 0:52:10 | 0:52:13 | |
but we believe it is located just here, | 0:52:13 | 0:52:16 | |
where it would receive about the same level of radiation | 0:52:16 | 0:52:19 | |
as the Earth does. | 0:52:19 | 0:52:22 | |
So this is our best candidate to date for habitability prospects. | 0:52:22 | 0:52:25 | |
Could this planet really be another Earth? | 0:52:27 | 0:52:31 | |
As ever, this will depend on its atmosphere. | 0:52:31 | 0:52:33 | |
The atmosphere dramatically affects the habitability of a planet. | 0:52:35 | 0:52:39 | |
In the solar system, Venus, | 0:52:39 | 0:52:41 | |
the Earth and Mars are all within a very close habitable zone, | 0:52:41 | 0:52:45 | |
but the atmosphere of Venus and Mars make them completely un-habitable. | 0:52:45 | 0:52:49 | |
Even if this planet has the right type of atmosphere, | 0:52:52 | 0:52:55 | |
it could still be very different to Earth. | 0:52:55 | 0:52:59 | |
These three planets are tidally locked to their star, | 0:52:59 | 0:53:01 | |
meaning that they show permanent day side that would too hot for | 0:53:01 | 0:53:04 | |
habitability and a permanent night side that would be too cold, | 0:53:04 | 0:53:08 | |
while still having hospitable temperatures between the two. | 0:53:08 | 0:53:12 | |
It is a bit like this marshmallow - | 0:53:12 | 0:53:13 | |
if I put it in the fire and I don't rotate it, | 0:53:13 | 0:53:16 | |
one side will be completely burnt while the other will be uncooked. | 0:53:16 | 0:53:21 | |
But in the middle, it would be just right. | 0:53:21 | 0:53:23 | |
These planets could have a barren, frozen wasteland on the night side, | 0:53:24 | 0:53:28 | |
a baking inferno on their day side and yet have a temperate | 0:53:28 | 0:53:33 | |
and yet have a potentially habitable strip down the middle | 0:53:33 | 0:53:36 | |
where it is permanent twilight. | 0:53:36 | 0:53:38 | |
But if you have a thick atmosphere surrounding this planet | 0:53:43 | 0:53:46 | |
then all the heat coming from the star on the day side | 0:53:46 | 0:53:49 | |
will recirculate to the night side, | 0:53:49 | 0:53:51 | |
making the day side cooler and the night side warmer. | 0:53:51 | 0:53:54 | |
To really know if any of these planets could be habitable, | 0:53:57 | 0:54:00 | |
we need to study their atmospheres. | 0:54:00 | 0:54:03 | |
But they are too small for even our best telescopes. | 0:54:04 | 0:54:08 | |
So the atmospheres in small planets actually are very thin. | 0:54:12 | 0:54:16 | |
So it is very difficult to detect them, | 0:54:16 | 0:54:18 | |
even with the state-of-the-art telescopes that we have today. | 0:54:18 | 0:54:21 | |
We have reached the limits of our current technology, | 0:54:23 | 0:54:27 | |
but NASA is building a new space telescope called the James Webb, | 0:54:27 | 0:54:32 | |
which will enable us to study the atmospheres of exoplanets | 0:54:32 | 0:54:36 | |
in far more detail than is possible today. | 0:54:36 | 0:54:39 | |
It will have far greater light-gathering abilities | 0:54:39 | 0:54:42 | |
than its predecessor, the Hubble Space Telescope. | 0:54:42 | 0:54:45 | |
James Webb will have a mirror diameter of 6.5m, | 0:54:45 | 0:54:50 | |
which compared to the 2.4m of Hubble means that James Webb | 0:54:50 | 0:54:55 | |
will collect seven times more photons than Hubble does, | 0:54:55 | 0:54:59 | |
which means it will have more signal to study these planets. | 0:54:59 | 0:55:02 | |
The James Webb will also be able to look at a far greater range | 0:55:03 | 0:55:07 | |
of wavelengths. | 0:55:07 | 0:55:08 | |
So the James Webb will have the possibility to go | 0:55:08 | 0:55:11 | |
much further in infrared than what Hubble is able to do today, | 0:55:11 | 0:55:16 | |
which means that it will give us the ability to probe for many more | 0:55:16 | 0:55:20 | |
chemical compounds than what we are able to do with Hubble. | 0:55:20 | 0:55:23 | |
When James Webb launches in 2018, | 0:55:24 | 0:55:28 | |
astronomers are going to be able to study Earth-sized planets | 0:55:28 | 0:55:32 | |
and discover if they are potentially habitable. | 0:55:32 | 0:55:35 | |
I'm convinced that we will find a habitable planet maybe in the next | 0:55:37 | 0:55:41 | |
five or ten years. | 0:55:41 | 0:55:42 | |
There are so many planets in our galaxy, | 0:55:42 | 0:55:45 | |
and this is the result of the last 20 years of planet hunting, | 0:55:45 | 0:55:48 | |
that based on sheer probability we will definitely find | 0:55:48 | 0:55:51 | |
at least another habitable planet. | 0:55:51 | 0:55:54 | |
But, for the time being, our planet remains unique. | 0:55:57 | 0:56:01 | |
Our exploration of other worlds so far suggests that it is a fairly rare | 0:56:01 | 0:56:06 | |
combination of factors that make our climate and weather so hospitable. | 0:56:06 | 0:56:10 | |
What makes the Earth so perfect for life is that first off it is rocky. | 0:56:11 | 0:56:16 | |
It has also got an atmosphere around it. | 0:56:16 | 0:56:18 | |
And our atmosphere is just right. | 0:56:18 | 0:56:21 | |
The size and the mass of our atmosphere is critical. | 0:56:21 | 0:56:23 | |
And, in addition, the composition of the atmosphere is just right. | 0:56:28 | 0:56:31 | |
Carbon dioxide and water in our atmosphere gives us just the right | 0:56:33 | 0:56:37 | |
greenhouse effect. | 0:56:37 | 0:56:38 | |
Venus has too much greenhouse effect. | 0:56:38 | 0:56:41 | |
Mars doesn't have enough. | 0:56:41 | 0:56:43 | |
We're also the right distance from our star. | 0:56:43 | 0:56:47 | |
We're just far enough away from the sun that we are not too hot, | 0:56:47 | 0:56:51 | |
but we're close enough that we're not too cold. | 0:56:51 | 0:56:54 | |
The temperature is perfect for water to exist in all three conditions | 0:56:54 | 0:56:58 | |
and that is so vital for life to have developed | 0:56:58 | 0:57:01 | |
and evolved on this planet. | 0:57:01 | 0:57:03 | |
And the Earth even spins in the right way. | 0:57:03 | 0:57:07 | |
So the other thing that makes Earth such a great place to live | 0:57:07 | 0:57:10 | |
is that it spins on its axis every 24 hours, | 0:57:10 | 0:57:14 | |
so the day and night temperatures never get super extreme. | 0:57:14 | 0:57:18 | |
So our planet has the right unique combination of things to make it | 0:57:18 | 0:57:23 | |
just the right place for life to have developed and maintained itself | 0:57:23 | 0:57:27 | |
for billions of years. | 0:57:27 | 0:57:28 | |
For thousands of years, we've gazed up at the night sky, | 0:57:32 | 0:57:36 | |
wondering what other planets might be like. | 0:57:36 | 0:57:38 | |
Astronomers began by studying our own solar system. | 0:57:40 | 0:57:44 | |
Now they are exploring the wider universe and can even study | 0:57:44 | 0:57:48 | |
the weather on planets hundreds of light years away. | 0:57:48 | 0:57:51 | |
They have discovered climates and weather stranger than fiction - | 0:57:53 | 0:57:58 | |
alien worlds with extreme temperatures, | 0:57:58 | 0:58:01 | |
bizarre clouds and even ruby rain. | 0:58:01 | 0:58:04 | |
But they've yet to find another planet like Earth, | 0:58:08 | 0:58:12 | |
with weather that is suitable for life, | 0:58:12 | 0:58:15 | |
that's not too hot or too cold. | 0:58:15 | 0:58:17 | |
So, for the time being, | 0:58:19 | 0:58:20 | |
it looks like a warm and pleasant day on Earth with a gentle breeze | 0:58:20 | 0:58:25 | |
and a slight risk of rain | 0:58:25 | 0:58:26 | |
might actually be the weirdest weather of them all. | 0:58:26 | 0:58:29 |