The Wildest Weather in the Universe Horizon


The Wildest Weather in the Universe

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We all love talking about the weather.

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Is it too hot or is it too cold?

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Is it too wet or too windy?

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It's a national obsession.

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But now scientists have also started looking to the heavens...

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..and wondering what the weather might be like on other planets.

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We are witnessing the birth of extra terrestrial meteorology,

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as technology is allowing astronomers to study the weather

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on other planets like never before.

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Jupiter has these very long-lived storms,

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but Saturn has these very violent storms.

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But, incredibly, today the latest telescopes are enabling astronomers

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to find and study planets beyond our solar system.

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So here we have our image of ROXs 12 b,

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which is pretty amazing to think we are imaging a planet

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400 light years away.

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And our exploration of the universe is revealing alien worlds

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with weather far stranger and more extreme than anyone

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could have ever imagined.

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A lot of the planets that we're studying so far

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are very horrible places.

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You wouldn't want to go there on vacation.

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On these planets you can get the most gigantic storm systems

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ever witnessed by mankind.

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So one side of the planet can be roasting hot while at the same time

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the other side of the planet can be freezing cold.

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On some exoplanets, the temperatures are such that the clouds

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and the rain can be made up of liquid lava droplets.

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We thought we had extreme weather on Earth,

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but it turns out that it's nothing compared to what's out there.

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So instead of having rain which is liquid water droplets like here

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on Earth, it would be raining liquid rubies.

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And the search for the weirdest weather in the universe

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is only just beginning.

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It's a delightfully warm spring morning in Greenwich, London.

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Astronomers of all ages have gathered at the Royal Observatory,

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where they're hoping to witness a rather special event.

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They're waiting to glimpse another world.

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And, unusually for astronomers,

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they've got their telescopes out during the day.

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We're here to see quite a rare astronomical event.

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I'm very excited to see it. I'm just hopeful, as we all are,

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that the clouds don't come along around midday and stay with us.

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It's a chance to get a unique perspective

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of one of our nearest neighbours.

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And to take a closer look,

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astronomer Tom Kerss has set up the Great Equatorial Telescope

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to look at the sun for the first time since 1927.

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Because at exactly 12 minutes past noon,

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the planet Mercury is due to pass in front of the sun.

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So here is Mercury emerging onto the face of the sun,

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looking very beautiful indeed.

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Over the next seven and a half hours or so,

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Mercury will gradually slink across the face of the sun

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as it overtakes us on the inside track in the solar system,

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about 52 million miles away from the Earth right now.

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Ever since we've known about the existence of other planets,

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we've wondered what these mysterious alien worlds might be like.

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Could they be potential homes for life?

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And is there any way of finding out?

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So when wondering whether other planets might be habitable or not,

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the key question we need to ask to begin with is what is the atmosphere

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actually like? What is the climate like?

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What's the weather like? Whether it would be very extreme or whether it

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would be quite pleasant and stable,

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the kind of weather we think is necessary for life.

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So what will the weather be like on Mercury?

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If we look back at the beginning of the Mercury transit we can see

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a really clean bite taken out of the sun.

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And the edge is so clean because Mercury doesn't have any appreciable

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atmosphere to speak of.

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With no real atmosphere, Mercury is effectively a dead and barren world.

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Because Mercury lacks anything that we would call an atmosphere,

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there's essentially no weather on Mercury at all.

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Mercury is unusual in our solar system because all the other planets

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do have atmospheres and so they must also have weather.

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Death Valley, California,

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one of the most extreme and alien environments on Earth.

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Planetary explorer Suzanne Smerkar has come here because it shares

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a surprising similarity to our nearest neighbour, Venus.

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Venus is the brightest object in the night sky and the reason it's so

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bright is because it's covered in thick clouds.

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And when you turn your telescope to it,

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you can see nothing of the surface,

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all you see is this bright reflection coming back at you

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because of the cloud deck that's kept it shrouded in mystery.

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We do know that Venus is similar in size to Earth,

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is a rocky world like our own, and also relatively close to us.

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So what's its climate like?

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We used to think that Venus was much like the Earth,

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maybe 50 degrees hotter because it's that much closer to the sun.

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We thought it had an atmosphere like the Earth,

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we thought it would be cool enough to have oceans.

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We even thought it was covered in steamy hot swamps,

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probably covered with verdant green life.

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But to discover what Venus was really like, we needed to go there.

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At the dawn of the space age, people started to explore.

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It was the Cold War in the '60s,

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and the Soviets and the US were sending spacecraft after spacecraft,

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trying to be the first out there.

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A huge number of spacecraft have been hurled at Venus

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and there were many attempts to get to the surface.

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In the late 1960s, the Russians succeeded.

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The one that finally made it to the surface was Venera 7 in 1967,

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and that probe fell gently through the atmosphere,

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got to the surface and survived for only about two hours.

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Before they died, the Venera probes revealed the true nature

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of Venus's climate.

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Venus has a surface temperature of 462 Celsius,

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which makes it the hottest place in the solar system.

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And the atmospheric pressure on Venus is almost 100 times

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that on the Earth.

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With surface temperatures hot enough to melt lead,

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an oppressive atmosphere of carbon dioxide, and belching clouds

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made of sulphuric acid, Venus is a planetary vision of Hell.

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We knew for the first time that Venus is not a swampy,

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verdant region teeming with life,

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but instead it's a hellish, hot inferno.

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Venus is the hottest planet in the solar system,

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but it's not the closest to the sun.

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Sue has come to Death Valley where the unbearable temperatures

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are created by the same phenomenon at work on Venus.

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We are here today in Death Valley, the hottest place on Earth.

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The temperature today is...

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42 degrees.

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Pretty balmy for Death Valley -

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the hottest recorded temperature is 57 degrees

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so we have it easy today.

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The reason that it is so hot here is that we are at 86m below sea level

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and that means that we have about 86m more atmosphere here

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and that means it's higher pressure and in fact the pressure measurement

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here is 1,016 bars.

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And that extra bit of pressure is really what's giving us

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this intense heat that we are experiencing today.

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It's like adding another layer of insulation or another blanket

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that's holding the heat in.

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And by simply driving uphill,

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Sue can reveal the tremendous insulating power of the atmosphere.

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So now we are at about 1,000m and it's already

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looking greener and a bit cooler up here.

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At Dante's View, almost 2km above the valley floor,

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the temperature is much cooler.

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We're at about 1.7km above the valley floor,

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where we were earlier today, and the temperature is 30 degrees Celsius,

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way cooler than the 42 degrees down there.

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And the reason it's so much cooler up here is that we have

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that 1.7km less air.

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Our pressure is 831 bars, down below it was 1,016.

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So the pressure is much lower.

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We have a lot less atmosphere above us,

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and as a result it's much cooler and much more pleasant up here.

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On Earth, the temperature typically increases

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by about 6.5 degrees Celsius for every kilometre you descend.

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On Venus, with its much deeper atmosphere than Earth,

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this insulating effect is taken to its extreme.

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It is so much hotter on Venus because the pressure is at 92 bars,

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almost 100 times that on the Earth, and the atmosphere is much thicker,

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much denser, and it really holds that heat in,

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making Venus the incredible inferno that it is.

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On top of this, Venus's atmosphere is almost entirely made up

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of the greenhouse gas carbon dioxide.

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And this combines with the intense pressure to make Venus

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the hottest planet in the solar system.

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Our next nearest neighbour couldn't be more different.

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Venus and Mars are like chalk and cheese.

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So Mars is the opposite extreme from Venus.

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It's atmosphere is 1/100th the pressure of Earth's

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and the effect of having that really low atmospheric pressure on Mars

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means that it can't trap any of its heat.

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So Mars is a cold,

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barren desert compared to Earth or to Venus.

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Because of its thin atmosphere,

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Mars is home to some spectacular weather phenomena.

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The rovers sent by NASA revealed that Mars is scoured

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by super-size dust devils,

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reaching up to a kilometre in height.

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But even more impressive are the dust storms,

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which dwarf those on Earth.

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In the thin atmosphere of Mars,

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the dust storms can get to a very high elevation,

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they can get to about 20km above the surface.

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And because most of Mars is a dry, dusty desert,

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these dust storms can cover vast expanses.

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In fact, it seems there is no limit to how far they can spread.

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Every few years an enormous dust storm will grow

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until the entire planet is engulfed.

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Incredibly, storms like these have been shown to envelop

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the whole of Mars for over two months.

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WEATHER REPORT: For England it's a hot and sunny day for all, any mist and fog clearing away quickly...

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Further out in the solar system, the weather gets even wilder.

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It's another fine sunny day in Pasadena,

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home of NASA's Jet Propulsion Laboratory.

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Andrew Ingersoll is the father of extra-terrestrial meteorology.

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He's come to the Deep Space Operations Centre.

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It's mission control for the small fleet of spacecraft that NASA

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has sent to explore the outer reaches of the solar system.

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Andy has worked on all these missions.

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So we've had a whole series of spacecraft

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visiting the giant planets.

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The first big one was Voyager in the '70s,

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which zoomed past all the giant planets.

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Then there was Galileo.

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Then Cassini which has been in orbit around Saturn for ten years.

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And now we have Juno in orbit around Jupiter.

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The spacecraft have given us an unprecedented view of the weather

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on these planets.

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The outer planets are big balls of gas and that makes a huge difference

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in the weather,

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so there's lots of room for weather.

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And because you don't have continents,

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you don't have mountains for the winds to rub against,

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and there's nothing to control the weather the way the continents

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partly control our weather.

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This means these planets have storms on an entirely different scale

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to ours.

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And the most famous storm of all has to be Jupiter's Great Red Spot.

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The Great Red Spot is a huge storm in Jupiter's atmosphere.

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You could put two Earths inside the Red Spot,

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and the winds going around the periphery of the Red Spot

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are about three times the speed of the Earth's jet streams.

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With winds whipping round at about 650km per hour,

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and releasing so much energy that it heats the atmosphere above it

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to around 1,400 degrees Celsius,

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the Red Spot has been raging for as long as we on Earth

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have been able to observe Jupiter.

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Shortly after Galileo built the first telescope,

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people were using these primitive telescopes to look at Jupiter

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and they saw this storm.

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And it's apparently been there ever since, which is remarkable,

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compared with Earth storms.

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The Red Spot has been there for over 350 years and that makes it

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the longest-living storm that we know of.

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Jupiter may have the longest-lasting storm,

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but it's Saturn, the next gas giant,

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that is home to the largest and most powerful storm ever seen

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in the solar system.

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And in 2010, the Cassini spacecraft was there to see it.

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Saturn, of course, is a spectacular sight because of the rings,

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and it's also rather boring as far as the weather is concerned.

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It's a bland thing.

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But every now and then - 20, 30 years -

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Saturn erupts with a giant storm,

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and Cassini was fortunate to be orbiting Saturn at the time

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of one of these eruptions.

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What happened was, on December 5th 2010,

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the radio receiver on Cassini started picking up the radio signal

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of lightning.

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And on the same day the camera saw a little storm up in

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the northern hemisphere of Saturn.

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By January it had developed into a fair-sized thing,

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and then we watched it for six months.

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During that time a huge storm grew and wrapped itself

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around the entire planet, covering 4 billion square kilometres

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until its head caught up with its tail.

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Driven by winds going at around 1,800km per hour, with huge

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lightning flashes 10,000 times stronger than those we get on Earth.

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It's very funny, Jupiter has these very long-lived storms,

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but Saturn has these very violent storms.

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We don't fully understand why there is this difference in the weather

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between Jupiter and Saturn.

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Whether it's duration or size,

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the storms on both these planets dwarf those on Earth.

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However, because they receive far less heat from the sun

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than the Earth does, something else is also powering their weather.

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The weather on Jupiter and Saturn comes from two sources.

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One is the sun, as on Earth,

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and the other is the internal heat left over

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from when the planets formed.

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It's this internal heat trying to escape through

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their deep atmospheres that makes the gas planets so tumultuous.

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This zone dry and sunny throughout the day.

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Later this afternoon there will be more in the way of clouds...

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The storms on the gas planets are certainly

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weirder and wilder than any we have on Earth,

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but when it comes to the clouds and the rain, things get even stranger.

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It's a typical June morning in Southern California...

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..and a local weather phenomenon known as the June gloom makes it

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the perfect day for taking a closer look at the clouds.

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Dr Kevin Baines has a passion for the skies, on Earth and beyond,

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and he's been studying the clouds on the gas planets.

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Coming out of SoCal,

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we're going to make a left turn on alpha

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and taxi over to the run-up area for runway one.

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So on a planet you'll get clouds at different levels,

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depending on the local temperature and the local pressure.

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On Earth, all clouds are made of water.

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So in southern California we have this marine layer.

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What happens is it actually forms over the water.

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The Pacific Ocean, of course, has a lot of water,

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so during the day it heats up and releases water into the air

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as water vapour. As this water vapour rises,

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it cools then it condenses out as water droplets in the air,

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and when you get millions and millions of water droplets,

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it forms a cloud.

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Clouds will form wherever it gets too cold for water to stay

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as a vapour in the air.

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And if there's enough moisture,

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the cloud droplets grow in size until they are big and heavy enough

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to fall as rain.

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Jupiter and Saturn also have a layer of water clouds.

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If we were to transport ourselves magically to Jupiter or Saturn,

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we could find a water layer like this.

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But other substances form clouds at colder temperatures,

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so above the layer of water clouds,

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higher up in the atmospheres of Jupiter and Saturn,

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there are two more cloud layers.

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As you climb up out of the water layer,

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it gets so cold that first you get ammonia hydrosulphide,

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which is very exotic cloud made of both ammonia

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and sulphur put together,

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and then as you climb up even higher into the atmosphere,

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when it gets down to about minus 130 Celsius,

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there ammonia gas in the atmosphere condenses out and forms clouds.

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So on these planets it doesn't just rain water,

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there could also be a light rain of liquid ammonia.

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Now if you go out to Uranus and Neptune, it is so cold out there,

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about -300 degrees,

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that you even have methane gas come out as clouds.

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And so on Uranus and Neptune, liquid methane could fall from the sky.

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Bizarre as they are, ammonia and methane aren't

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the weirdest rains of all,

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because back on Saturn, in the depths of its atmosphere,

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Kevin believes that an astonishing process is at work that creates

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what could be the strangest rain in the solar system.

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This process can be witnessed an on idyllic summer day in Oxfordshire.

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Inside this unremarkable office building,

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a manufacturing company is replicating the conditions deep

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in Saturn's atmosphere, not to study it, but for industrial purposes.

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Using these massive presses,

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they're turning carbon graphite into something far more valuable...

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..and Kevin has come over from California to see how this process

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can help explain what's happening deep inside Saturn.

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We know that on Saturn there's carbon soot.

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We know that by looking at these dark clouds that we saw with

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our camera onboard the Cassini spacecraft orbiting Saturn,

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and we see the spectroscopic signature of carbon soot there.

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The carbon soot is created by lightning,

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lightning actually zapping methane in the atmosphere.

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Something very strange then happens to the soot as it falls

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through Saturn's atmosphere.

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It is transformed into something remarkable,

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a process that is actually being replicated here.

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What we do, effectively,

0:23:330:23:34

is we take this carbon graphite and mix it with several other materials

0:23:340:23:39

and we assemble what we call a capsule.

0:23:390:23:41

We take that capsule, the graphite material inside it,

0:23:410:23:45

and we place it inside the actual press itself.

0:23:450:23:49

The press is then closed up and the carbon graphite is exposed

0:23:490:23:54

to extreme temperatures and pressures.

0:23:540:23:57

High pressures are generated by these anvils that can press down

0:23:580:24:02

onto the graphite, pressures of around 50,000 atmospheres.

0:24:020:24:06

The graphite's then going to be heated to about 2,000 Celsius -

0:24:060:24:10

that heating happens by large electrical currents.

0:24:100:24:13

This process mimics what's happening inside Saturn.

0:24:140:24:18

We know we have carbon, which is very much like the graphite

0:24:180:24:20

that we just put into the machine over here.

0:24:200:24:23

The carbon soot precipitates or falls through the atmosphere,

0:24:230:24:26

and eventually it will get to the 7,000km level.

0:24:260:24:29

At that point, it will be experiencing the pressures

0:24:290:24:31

and temperatures that we experience in the press over here.

0:24:310:24:35

Inside the press,

0:24:350:24:36

the intense heat and crushing pressure transform the carbon

0:24:360:24:41

from graphite into diamond.

0:24:410:24:43

All right.

0:24:480:24:49

So this may not look like diamonds,

0:24:490:24:51

but we will then take this rubble and process it further

0:24:510:24:54

and we'll extract the diamond.

0:24:540:24:56

Great. So, the diamonds are in there somewhere?

0:24:560:24:58

Somewhere inside this rubble, Kevin, there are diamonds.

0:24:580:25:01

This high-temperature,

0:25:050:25:06

high-pressure process can make a variety of diamonds

0:25:060:25:09

which are used in industry.

0:25:090:25:11

Here we have tiny triangles -

0:25:230:25:25

effectively, these are used for wire drawing dies.

0:25:250:25:28

You get square-shaped diamonds which, in this case,

0:25:280:25:31

are used as single crystal cutting tools.

0:25:310:25:35

These diamonds are yellow because they contain nitrogen.

0:25:350:25:39

So what we were making earlier today, effectively,

0:25:390:25:42

are these diamond grits, tiny little stones of single crystal diamonds,

0:25:420:25:47

normally about 100 microns in size.

0:25:470:25:49

Kevin believes the same thing is happening on Saturn.

0:25:510:25:54

So we really think it's very similar conditions,

0:25:560:25:58

very similar process that's happening.

0:25:580:26:00

At the 7,000km level in Saturn,

0:26:000:26:02

carbon soot will transform itself into diamonds,

0:26:020:26:05

creating a diamond rain.

0:26:050:26:06

As the carbon soot falls from the clouds,

0:26:090:26:12

the extreme temperature and pressure deep in the atmosphere

0:26:120:26:15

turn it into diamonds.

0:26:150:26:17

So inside Saturn we have a huge region of diamond rain.

0:26:200:26:23

Our exploration of the other planets in our solar system has revealed

0:26:280:26:32

weather stranger and more powerful than anything we have here on Earth.

0:26:320:26:36

But what about beyond our solar system?

0:26:390:26:42

What is the weather like in the rest of the universe?

0:26:420:26:46

Some of those showers could be quite heavy. They'll be some dry spells

0:26:500:26:52

in between, but limited brightness and it will be a cool one...

0:26:520:26:56

Perched at the top of Mauna Kea in Hawaii,

0:26:560:26:59

4,000m above sea level, is the Keck Observatory,

0:26:590:27:03

one of the pre-eminent earthbound telescopes for finding planets

0:27:030:27:07

orbiting other stars, known as exoplanets.

0:27:070:27:10

Brendan Bowler has one of the best jobs in the world -

0:27:140:27:18

he's an exoplanet explorer.

0:27:180:27:21

I feel incredibly lucky studying astronomy and contributing

0:27:210:27:24

to exoplanetary science.

0:27:240:27:27

It's humbling, in many ways,

0:27:270:27:28

to be able to contribute and answer some of the questions

0:27:280:27:34

that we've been thinking about as humans for millennia.

0:27:340:27:38

The aim of my job is to find planets orbiting other stars,

0:27:380:27:43

which is a very difficult task to do.

0:27:430:27:45

Planets are both much smaller,

0:27:470:27:49

much lower mass and much fainter than the stars that they orbit,

0:27:490:27:54

so trying to find planets in the glare of their stars

0:27:540:27:58

is very difficult.

0:27:580:28:00

So it's as if we're trying to find a firefly buzzing around a spotlight

0:28:000:28:05

that's 10 billion times brighter than that firefly,

0:28:050:28:08

from a distance of New York all the way to London.

0:28:080:28:11

So how do you find a planet orbiting a distant star,

0:28:150:28:19

let alone study its weather?

0:28:190:28:21

There are two indirect methods that we primarily use to find planets.

0:28:230:28:28

The first is the radial velocity technique.

0:28:280:28:31

Let's say this is the planet and the post is the star that it's orbiting.

0:28:310:28:35

As a planet orbits its star,

0:28:350:28:38

the planet exerts gravitational influence on the host star,

0:28:380:28:42

which causes the host star to wobble.

0:28:420:28:44

We can search for planets by looking for the back and forth wobble

0:28:470:28:50

that planets induce on their host stars.

0:28:500:28:52

And that's exactly how the first exoplanet orbiting a sun-like star

0:28:540:28:58

was discovered, in 1995, changing the face of astronomy for ever.

0:28:580:29:04

And since then, planet hunters have discovered thousands more

0:29:040:29:09

orbiting distant stars.

0:29:090:29:10

But planetary explorers aren't satisfied

0:29:140:29:17

with simply finding planets.

0:29:170:29:20

What we really want to do is to be able to characterise the planet

0:29:200:29:23

in more detail.

0:29:230:29:25

The radial velocity method only tells us about

0:29:250:29:28

the mass of the planet.

0:29:280:29:30

The bigger the wobble, the bigger the mass,

0:29:300:29:33

but luckily there's a second technique for finding planets

0:29:330:29:37

known as the transit method, which reveals a whole lot more.

0:29:370:29:42

The transit method you can think of as a planet crossing between us,

0:29:420:29:46

our line of sight, and the star that it orbits, just like this.

0:29:460:29:51

Now when that crossing event occurs,

0:29:510:29:53

it will cause a dip in the brightness of that host star.

0:29:530:29:57

So we can use that to find planets,

0:29:570:30:00

by searching for periodic dips in the brightness of that star.

0:30:000:30:04

Crucially, the transit method also tells us how big the planet is,

0:30:070:30:12

because the bigger the planet,

0:30:120:30:14

the greater the dip in the light from the star.

0:30:140:30:17

The transit method tells us about the size of the planet,

0:30:180:30:21

while the radial velocity tells us about the mass of the planet,

0:30:210:30:25

so we can use both of those together to measure the density of planets,

0:30:250:30:31

because density is mass over volume.

0:30:310:30:34

And this reveals what the planet is made of.

0:30:340:30:37

Small dense planets are rocky,

0:30:370:30:40

whereas large planets that are not dense are gas giants.

0:30:400:30:45

The first planets discovered were huge gas giants like Jupiter,

0:30:470:30:52

and since then, planet hunters have found all sorts of combinations

0:30:520:30:56

of size and mass, including small, dense planets,

0:30:560:31:01

rocky worlds that could have atmospheres.

0:31:010:31:03

But finding out any more detail about an exoplanet's atmosphere,

0:31:060:31:10

climate and, ultimately, its weather, is extremely difficult.

0:31:100:31:15

But not impossible.

0:31:180:31:20

The key to doing this is the fact that different gases absorb light

0:31:210:31:25

at different wavelengths.

0:31:250:31:27

So we can study the composition of the atmospheres of exoplanets

0:31:300:31:34

by breaking up the light that we receive at Earth

0:31:340:31:37

into its constituent colours.

0:31:370:31:39

This is what we're doing here with the projector which emits

0:31:390:31:41

white light - we're dispersing it with a prism,

0:31:410:31:44

spreading out the light. We can see the various wavelengths and colours

0:31:440:31:48

it's split into.

0:31:480:31:50

If we have a gas intervening between the projector

0:31:500:31:53

and the prism, then the different colours will be blocked out,

0:31:530:31:57

depending on the nature of the gas.

0:31:570:31:59

So what I'm going to do is put a gas in this beam of light

0:31:590:32:03

by burning baking soda, which is sodium bicarbonate.

0:32:030:32:06

So here we have our baking soda.

0:32:080:32:09

We'll drop a little bit of that into the flame.

0:32:110:32:14

And so what we're doing is making the equivalent of an atmosphere

0:32:160:32:20

of sodium atoms in the beam, which is absorbing some of the light.

0:32:200:32:25

What we see on the spectrum is a narrow dark line that comes and goes

0:32:250:32:28

as I drop it in, in the yellow part of the spectrum,

0:32:280:32:31

which corresponds to the wavelength that sodium absorbs.

0:32:310:32:35

Every chemical has its own unique pattern of absorption lines.

0:32:350:32:39

So astronomers can use this information to detect

0:32:420:32:45

the different substances in the atmospheres of planets.

0:32:450:32:49

And that's exactly what Brendan is going to try to do tonight.

0:32:490:32:54

He's pointing the Keck telescope's awesome light gathering power

0:32:540:32:58

at a newly discovered planet.

0:32:580:32:59

I'll be using the Keck telescope to study a planet

0:33:020:33:06

about 400 light years away.

0:33:060:33:08

Its name is ROXs 12 b,

0:33:080:33:11

it has a mass between 10-15 times that of Jupiter,

0:33:110:33:15

and we know it's a gas giant, but we don't know what it's made out of,

0:33:150:33:17

which is the goal of our observations.

0:33:170:33:20

By studying the light that is emitted from this planet,

0:33:200:33:23

we'll be able to learn about the chemical composition and physical

0:33:230:33:26

properties of its atmosphere.

0:33:260:33:28

ROXs 12 is about to rise.

0:33:330:33:35

We have two more minutes.

0:33:350:33:37

It's below the telescope limits, but it is about to go up,

0:33:370:33:40

and then we can slew to it.

0:33:400:33:43

We're trying to look in the infrared,

0:33:430:33:45

to both image the planet and get a spectrum of it.

0:33:450:33:49

When we can get a spectrum of the planet,

0:33:490:33:52

we can learn what's in its atmosphere.

0:33:520:33:54

Direct imaging of distant planets like this

0:33:560:33:59

is at the very cutting edge of astronomy.

0:33:590:34:03

It's incredibly difficult to image planets,

0:34:030:34:06

but for the most massive planets, like ROXs 12 b,

0:34:060:34:09

it emits enough light that we can actually detect the photons,

0:34:090:34:13

so we can see the planet and take pictures of the planet.

0:34:130:34:17

And for this, we need our very best telescopes.

0:34:170:34:20

Keck is the biggest telescope in the world,

0:34:210:34:25

so we need the size of the mirror, which is ten metres in diameter,

0:34:250:34:28

to gather enough photons.

0:34:280:34:30

Incredibly, the Keck telescope also compensates for interference

0:34:310:34:36

from our own atmosphere.

0:34:360:34:38

Stars twinkle because of turbulence in the Earth's atmosphere.

0:34:400:34:44

We don't like that twinkling, we want it to stop,

0:34:440:34:47

so we use adaptive optics to actively compensate, in real time,

0:34:470:34:51

thousands of times per second, for that turbulence.

0:34:510:34:55

It's as if we're putting these big telescopes that we have

0:34:550:34:57

on the ground in space.

0:34:570:34:59

So far, only a handful of planets have ever been

0:35:020:35:05

directly imaged like this.

0:35:050:35:07

Martha, what are the coordinates?

0:35:070:35:09

16, 26, 28.1.

0:35:090:35:12

Can you go to ROXs 12 and the moon and look how it looks in the tracks?

0:35:140:35:18

Yeah.

0:35:180:35:19

That's it finished, and we're ready.

0:35:190:35:22

This is our sixth attempt to get this target.

0:35:220:35:25

We've been weathered out, we've had instrument issues,

0:35:250:35:29

and we think we're finally going to get it tonight.

0:35:290:35:32

OK, so I think we have the target centred up

0:35:340:35:37

in the field of view here.

0:35:370:35:40

I think we can start...

0:35:400:35:42

exposing.

0:35:420:35:43

So, here we have our image of ROXs 12 b.

0:35:530:35:56

So this is an infrared image of this planet,

0:35:560:36:00

which is pretty amazing to think that we are imaging a planet

0:36:000:36:04

400 light years away.

0:36:040:36:05

ROXs 12 b is one of only 15 exoplanets

0:36:070:36:11

to have ever been directly imaged.

0:36:110:36:14

And, incredibly, the faint light captured in this picture

0:36:160:36:20

will reveal the secrets of ROXs 12 b's atmosphere,

0:36:200:36:24

the first step towards understanding its weather.

0:36:240:36:28

We're looking at the infrared light from this planet.

0:36:280:36:30

This is light that's emitted in the interior of the planet

0:36:300:36:33

and passed through its atmosphere, and whatever chemicals, molecules,

0:36:330:36:38

atoms are in the atmosphere,

0:36:380:36:39

will induce absorption features in the spectrum,

0:36:390:36:43

and that's what we're looking for.

0:36:430:36:45

So here we can actually get a spectrum in real-time,

0:36:450:36:48

and let's go ahead and do it.

0:36:480:36:49

So here's our spectrum of ROXs 12 b in the infrared.

0:36:510:36:56

What we're looking for are absorption features

0:36:560:36:59

from carbon monoxide, CO.

0:36:590:37:00

So we can see these two dips here in the spectrum,

0:37:030:37:06

which correspond to the wavelengths where CO absorbs,

0:37:060:37:09

and that means that this planet really does have carbon monoxide

0:37:090:37:12

in its atmosphere.

0:37:120:37:13

The spectrum also revealed that this exoplanet has water vapour,

0:37:150:37:18

iron hydride, vanadium oxide, potassium and sodium

0:37:180:37:23

in its atmosphere - fairly typical for an exoplanet.

0:37:230:37:26

So by studying the light from exoplanets

0:37:270:37:30

hundreds of light years away,

0:37:300:37:32

astronomers are able to detect what's in their atmosphere...

0:37:320:37:35

..a key ingredient that goes into creating their weather.

0:37:390:37:42

Later today, a mixture of brighter spells

0:37:500:37:52

and showers for the majority...

0:37:520:37:55

As well as being able to detect the gases in a planet's atmosphere,

0:37:550:37:59

scientists can also use the infrared light to work out

0:37:590:38:02

just how hot a planet is.

0:38:020:38:04

It's a blustery day in California

0:38:080:38:11

and exoplanet meteorologist Heather Knutson

0:38:110:38:14

is visiting Santa Monica Pier.

0:38:140:38:16

So the main thing that determines the temperature of a planet

0:38:180:38:21

is the distance that it is from its host star.

0:38:210:38:24

Planets that are really close in are going to be boiling hot.

0:38:240:38:26

Planets that are further away will be a little bit cooler

0:38:260:38:29

by comparison.

0:38:290:38:31

Most of the exoplanets discovered so far are close to their stars,

0:38:310:38:35

so scientists expected them to be hot,

0:38:350:38:39

but they didn't know how hot.

0:38:390:38:41

So we can actually go and measure the temperature of these planets

0:38:410:38:43

by measuring their brightness in infrared light.

0:38:430:38:46

Hotter things are going to glow more brightly in infrared wavelengths,

0:38:460:38:49

cooler things are going to be a little bit dimmer and fainter.

0:38:490:38:53

So probably the hottest planet that we know of is a planet

0:38:550:38:58

called WASP-33 b.

0:38:580:38:59

WASP-33 b is the hottest planet discovered so far

0:39:010:39:05

in the entire universe.

0:39:050:39:08

It's a gas giant, four and a half times the size of Jupiter.

0:39:080:39:12

Its atmosphere is a scorching 3,200 Celsius.

0:39:120:39:17

So this planet is hot for two reasons -

0:39:190:39:21

one is it's very close to its host star.

0:39:210:39:23

The other is it orbits a star that is bigger and hotter than the sun.

0:39:230:39:28

Both those things together combine to make this

0:39:280:39:30

one of the hottest planets we've discovered.

0:39:300:39:33

Planets like WASP-33 b are nicknamed Hot Jupiters,

0:39:350:39:40

and they don't just have extreme temperatures...

0:39:400:39:42

..because being close to their star has another important effect

0:39:440:39:47

on the weather.

0:39:470:39:50

So all planets spin on their axis, just like I am now.

0:39:500:39:54

The Earth spins once every 24 hours,

0:39:540:39:56

but not all planets spin at the same speed.

0:39:560:39:59

There are some planets which we're discovering which are very,

0:39:590:40:02

very close to their stars.

0:40:020:40:04

They're so close that the star tugs on the planet as it spins around

0:40:040:40:08

on its axis, and the tugging of that star actually slows

0:40:080:40:12

the planet's rotation down,

0:40:120:40:15

keeps slowing it down and keeps slowing it down until the planet

0:40:150:40:18

rotates at exactly the same speed that it orbits.

0:40:180:40:23

So the same side of the planet always faces towards the star,

0:40:230:40:26

just like I'm always facing the centre of this ride here.

0:40:260:40:28

We call this tidal locking,

0:40:300:40:32

and it means the planet has a permanent day side

0:40:320:40:35

and a permanent night side.

0:40:350:40:37

And being tidally locked has a dramatic impact.

0:40:380:40:41

So whenever you have one part of a planet that's hot and another part

0:40:430:40:46

that's cold, the natural result is that you get a wind moving

0:40:460:40:50

from one part to another.

0:40:500:40:51

Here at the beach during the day the land heats up but the sea stays

0:40:520:40:56

relatively cold, and so you get this nice wind moving from the ocean

0:40:560:40:59

towards the land that's trying to even out the temperatures.

0:40:590:41:02

So when we first discovered these very close-in planets,

0:41:020:41:05

we realised they were probably close enough to be tidally locked.

0:41:050:41:09

And one of the very first things we wanted to know is what that meant

0:41:090:41:11

for the planet's atmosphere.

0:41:110:41:13

Did it mean these planets had a boiling hot day side

0:41:130:41:16

and a freezing cold night side?

0:41:160:41:18

Or were there winds in the atmosphere that were able to carry

0:41:180:41:20

some of that heat around to the night side?

0:41:200:41:23

To find out, Heather mapped the temperature on a Hot Jupiter...

0:41:250:41:29

..which scientists think is blue in colour.

0:41:320:41:35

The particular planet we decided to look at was a Hot Jupiter

0:41:350:41:39

called HD 189733.

0:41:390:41:41

That's kind of a mouthful, but I can tell you that this is actually

0:41:410:41:44

my favourite Hot Jupiter, this was one of the very first planets

0:41:440:41:47

that I looked at when I was a grad student.

0:41:470:41:49

By looking at it in infrared,

0:41:490:41:51

Heather was able to measure its temperature.

0:41:510:41:53

So this is the map we made.

0:41:550:41:56

So the colour tells you the temperature of different parts

0:41:560:41:59

of the atmosphere. So here on the day side things are relatively hot,

0:41:590:42:03

so the day side is about 900 degrees Centigrade.

0:42:030:42:07

Here, on the edges, that's the night side,

0:42:070:42:10

and that's a relatively cool part of the atmosphere,

0:42:100:42:12

it's only 700 degrees Centigrade, which is still really hot.

0:42:120:42:16

That difference is actually much smaller than we expected,

0:42:160:42:19

and the fact it's so small suggested to us that this planet must have

0:42:190:42:22

strong winds circulating through its atmosphere and carrying that hot air

0:42:220:42:26

from the day side around to the night side.

0:42:260:42:29

Incredibly, these winds have now been measured directly,

0:42:310:42:36

and it turns out that HD 189733 b is home

0:42:360:42:41

to the fastest winds in the universe

0:42:410:42:44

which rage around it at about 8,700km per hour,

0:42:440:42:50

seven times the speed of sound,

0:42:500:42:52

and 20 times faster than the fastest winds ever experienced on Earth.

0:42:520:42:57

Showers, some of them of sleet and snow.

0:42:590:43:02

Elsewhere fewer showers and here the showers will be of rain...

0:43:020:43:08

It's a beautiful tropical morning on the Big Island in Hawaii.

0:43:080:43:11

Exoplanet expert Hannah Wakeford is taking to the skies

0:43:140:43:18

to explore another bizarre effect the extreme heat on exoplanets

0:43:180:43:22

has on their weather.

0:43:220:43:23

The strangest thing about exoplanets is the clouds and the rain -

0:43:270:43:30

they're nothing like we have here on Earth.

0:43:300:43:33

Spectroscopy has revealed that exoplanets have clouds,

0:43:330:43:37

and also what these clouds might be made of.

0:43:370:43:40

We know that exoplanets have clouds.

0:43:400:43:42

If we have a planet that we know should be gaseous because of

0:43:420:43:44

its density but we don't detect any spectral signatures from that gas,

0:43:440:43:48

then we think there must be clouds in the way which are blocking that

0:43:480:43:51

light and obscuring our view.

0:43:510:43:54

And sometimes we can detect signatures directly from

0:43:540:43:56

those clouds by the way that they scatter or reflect the light.

0:43:560:43:59

But these aren't clouds we'd recognise.

0:44:030:44:06

A lot of the exoplanets that we've been able to follow up are very hot,

0:44:090:44:12

over 1,000 degrees,

0:44:120:44:14

so we know that water can't exist as a liquid at those temperatures,

0:44:140:44:17

so they're not going to be clouds like we have here on Earth.

0:44:170:44:20

Woo, we're in a cloud!

0:44:220:44:24

So, on some exoplanets,

0:44:260:44:27

the clouds will be made of far more exotic substances.

0:44:270:44:31

The temperatures are such that substances that we think of

0:44:330:44:36

as solids on Earth can actually exist as liquids or gas

0:44:360:44:39

in exoplanet atmospheres.

0:44:390:44:41

We can get a glimpse of this on Earth in volcanoes,

0:44:430:44:46

where temperatures can reach over 1,000 degrees Celsius.

0:44:460:44:50

Down there is the crater of Pu'u 'O'o,

0:44:520:44:55

and you can see the lava bubbling away.

0:44:550:44:59

The temperature of this lava lake is around 1,000 degrees

0:44:590:45:02

and all of the rock has melted.

0:45:020:45:04

The metals and minerals and the silicates that make up

0:45:040:45:07

the Earth's crust have all become molten.

0:45:070:45:12

It's amazing - you can really feel the temperature from the lava lake

0:45:120:45:16

all the way up here. It's really very hot.

0:45:160:45:19

It's 1,000 degrees melting the Earth's crust down there,

0:45:210:45:24

so it's no surprise.

0:45:240:45:26

And it's these substances that are thought to make up the clouds

0:45:280:45:32

on some exoplanets.

0:45:320:45:34

There's a planet called 55 Cancri e

0:45:350:45:38

that we think is rocky because of its density,

0:45:380:45:40

but it orbits very close to its parent star and is tidally locked,

0:45:400:45:44

so temperatures on the day side should be high enough to melt the rock,

0:45:440:45:48

making it a lava planet.

0:45:480:45:50

55 Cancri e is a lava planet.

0:45:540:45:57

While its night side will be relatively cool and solid rock,

0:45:570:46:01

its day side is an ocean of permanently molten lava.

0:46:010:46:06

On the day side, the temperatures go over 2,500 degrees.

0:46:060:46:11

This is hot enough to vaporise the rock at the surface.

0:46:110:46:15

This can then be lifted into the atmosphere and condensed

0:46:150:46:19

to form clouds of liquid lava droplets that then can be

0:46:190:46:22

transported to colder parts of the planet,

0:46:220:46:25

where they will rain down as pebbles on the surface.

0:46:250:46:28

So on some planets, it rains rock

0:46:340:46:37

rather than water like it does here in Hawaii.

0:46:370:46:39

Back on the ground on Kilauea,

0:46:500:46:52

Hannah has an example of what rock rain might be like.

0:46:520:46:55

Right here was the site of a massive eruption.

0:47:000:47:03

All along this fissure,

0:47:030:47:05

fountains of lava shot into the air nearly 100m high.

0:47:050:47:10

The liquid lava droplets then cooled and solidified in the air

0:47:100:47:14

before raining down onto the surface as these tiny pebbles,

0:47:140:47:19

and sometimes we get these perfect little droplets called Pele's tears.

0:47:190:47:23

This is what we think the rain might be like an planets like 55 Cancri e.

0:47:250:47:29

But perhaps the strangest rain in the entire universe has been discovered

0:47:400:47:45

on a giant gas planet which orbits a star hundreds of light years away.

0:47:450:47:50

We've been able to study the exoplanet WASP-12b

0:47:530:47:57

and the way that it scatters light suggests that there are clouds

0:47:570:48:00

high up in the atmosphere.

0:48:000:48:02

At this part of the atmosphere, the temperature is around 2,000 degrees,

0:48:020:48:06

so the most likely substance forming these clouds

0:48:060:48:09

is an aluminium oxide called corundum,

0:48:090:48:11

which forms the basis of rubies.

0:48:110:48:14

So instead of having rain which is liquid water droplets

0:48:140:48:18

like here on Earth, it would be raining rubies.

0:48:180:48:21

We are only just witnessing the birth of exoplanet meteorology.

0:48:280:48:32

But so far, what astronomers have discovered on exoplanets

0:48:320:48:37

is even more extreme and bizarre than anything anyone had imagined.

0:48:370:48:42

Compared to what's out there,

0:48:490:48:51

the most extreme weather on Earth - our hurricanes and tornadoes,

0:48:510:48:55

our rain and our snow - all seem pretty mild.

0:48:550:48:59

Our climate and weather is actually very hospitable.

0:48:590:49:02

The Earth is a nice place and that's all because of the weather.

0:49:020:49:07

We've got warm temperatures - not too hot, not too cold.

0:49:070:49:10

It's a great place.

0:49:100:49:11

Ultimately, the planet hunters of the world are hoping to find one thing -

0:49:130:49:17

another Earth.

0:49:170:49:19

A small, rocky planet with a thin blue line encircling it.

0:49:200:49:24

A planet with a nice climate,

0:49:240:49:27

a climate that could be hospitable to life.

0:49:270:49:29

What we're really looking for is rocky terrestrial-type planets

0:49:310:49:35

with an atmosphere around them which is habitable.

0:49:350:49:38

We'd like that planet to be at the right temperature to have liquid water,

0:49:400:49:43

so that means being at just the right distance from your stars

0:49:430:49:47

and having exactly the right kind of atmosphere.

0:49:470:49:51

But so far, astronomers have mainly found planets

0:49:510:49:54

with extreme environments -

0:49:540:49:56

planets with ruby rain or lava clouds.

0:49:560:50:00

So the planets that we've found so far aren't particularly nice places to go.

0:50:000:50:04

They're not somewhere you would put on your vacation list any time soon.

0:50:040:50:08

Because at the moment, it's easier to both find and study

0:50:080:50:11

the bigger planets...

0:50:110:50:13

When you're looking at other stars,

0:50:130:50:14

it's easy to find the large planets like Jupiter and Saturn,

0:50:140:50:19

where you don't have the right kind of atmosphere.

0:50:190:50:22

..or ones that are close to their stars.

0:50:220:50:24

Our surveys are really good at finding planets that are very close

0:50:240:50:27

to their stars, which means mostly the planets that we've discovered

0:50:270:50:30

are much too hot to host life as we know it on Earth.

0:50:300:50:34

Just over 20 years ago, astronomers began finding exoplanets.

0:50:340:50:39

The first were giant Hot Jupiters orbiting close to their stars,

0:50:390:50:43

because they were the easiest to spot.

0:50:430:50:46

And now hundreds of smaller rocky planets have also been found,

0:50:460:50:50

but most of these are still larger than Earth

0:50:500:50:53

and still too close to their stars.

0:50:530:50:55

But the search for another Earth is still in its infancy.

0:50:580:51:02

Dr Brice Demory is a planet hunter

0:51:050:51:09

and he may have found the promised land of planetary exploration -

0:51:090:51:13

a planet that could have warm, mild weather,

0:51:130:51:16

weather just like a lovely summer evening in Cambridge.

0:51:160:51:19

So we are looking for rocky planets

0:51:210:51:23

similar to the Earth in size and located at the right distance from its star.

0:51:230:51:28

It is a bit like cooking a marshmallow -

0:51:280:51:30

If the marshmallow is too close to the fire, then it will burn,

0:51:300:51:33

if it is too far away, it will never cook.

0:51:330:51:35

So we want the planet to be at the distance that is just right

0:51:350:51:39

for habitable conditions to happen.

0:51:390:51:41

We have just found three Earth-sized planets that are orbiting

0:51:420:51:46

a very cool star called Trappist-1,

0:51:460:51:49

and these planets are remarkable.

0:51:490:51:51

The first one is located here and receives about four times the level

0:51:510:51:55

of radiation that the Earth does.

0:51:550:51:58

The second one, look at it here,

0:51:580:52:00

receives twice the level of radiation that the Earth does.

0:52:000:52:04

Those planets are probably too hot to be habitable.

0:52:040:52:08

The third one is the most interesting one.

0:52:080:52:10

We're not exactly sure of its location right now,

0:52:100:52:13

but we believe it is located just here,

0:52:130:52:16

where it would receive about the same level of radiation

0:52:160:52:19

as the Earth does.

0:52:190:52:22

So this is our best candidate to date for habitability prospects.

0:52:220:52:25

Could this planet really be another Earth?

0:52:270:52:31

As ever, this will depend on its atmosphere.

0:52:310:52:33

The atmosphere dramatically affects the habitability of a planet.

0:52:350:52:39

In the solar system, Venus,

0:52:390:52:41

the Earth and Mars are all within a very close habitable zone,

0:52:410:52:45

but the atmosphere of Venus and Mars make them completely un-habitable.

0:52:450:52:49

Even if this planet has the right type of atmosphere,

0:52:520:52:55

it could still be very different to Earth.

0:52:550:52:59

These three planets are tidally locked to their star,

0:52:590:53:01

meaning that they show permanent day side that would too hot for

0:53:010:53:04

habitability and a permanent night side that would be too cold,

0:53:040:53:08

while still having hospitable temperatures between the two.

0:53:080:53:12

It is a bit like this marshmallow -

0:53:120:53:13

if I put it in the fire and I don't rotate it,

0:53:130:53:16

one side will be completely burnt while the other will be uncooked.

0:53:160:53:21

But in the middle, it would be just right.

0:53:210:53:23

These planets could have a barren, frozen wasteland on the night side,

0:53:240:53:28

a baking inferno on their day side and yet have a temperate

0:53:280:53:33

and yet have a potentially habitable strip down the middle

0:53:330:53:36

where it is permanent twilight.

0:53:360:53:38

But if you have a thick atmosphere surrounding this planet

0:53:430:53:46

then all the heat coming from the star on the day side

0:53:460:53:49

will recirculate to the night side,

0:53:490:53:51

making the day side cooler and the night side warmer.

0:53:510:53:54

To really know if any of these planets could be habitable,

0:53:570:54:00

we need to study their atmospheres.

0:54:000:54:03

But they are too small for even our best telescopes.

0:54:040:54:08

So the atmospheres in small planets actually are very thin.

0:54:120:54:16

So it is very difficult to detect them,

0:54:160:54:18

even with the state-of-the-art telescopes that we have today.

0:54:180:54:21

We have reached the limits of our current technology,

0:54:230:54:27

but NASA is building a new space telescope called the James Webb,

0:54:270:54:32

which will enable us to study the atmospheres of exoplanets

0:54:320:54:36

in far more detail than is possible today.

0:54:360:54:39

It will have far greater light-gathering abilities

0:54:390:54:42

than its predecessor, the Hubble Space Telescope.

0:54:420:54:45

James Webb will have a mirror diameter of 6.5m,

0:54:450:54:50

which compared to the 2.4m of Hubble means that James Webb

0:54:500:54:55

will collect seven times more photons than Hubble does,

0:54:550:54:59

which means it will have more signal to study these planets.

0:54:590:55:02

The James Webb will also be able to look at a far greater range

0:55:030:55:07

of wavelengths.

0:55:070:55:08

So the James Webb will have the possibility to go

0:55:080:55:11

much further in infrared than what Hubble is able to do today,

0:55:110:55:16

which means that it will give us the ability to probe for many more

0:55:160:55:20

chemical compounds than what we are able to do with Hubble.

0:55:200:55:23

When James Webb launches in 2018,

0:55:240:55:28

astronomers are going to be able to study Earth-sized planets

0:55:280:55:32

and discover if they are potentially habitable.

0:55:320:55:35

I'm convinced that we will find a habitable planet maybe in the next

0:55:370:55:41

five or ten years.

0:55:410:55:42

There are so many planets in our galaxy,

0:55:420:55:45

and this is the result of the last 20 years of planet hunting,

0:55:450:55:48

that based on sheer probability we will definitely find

0:55:480:55:51

at least another habitable planet.

0:55:510:55:54

But, for the time being, our planet remains unique.

0:55:570:56:01

Our exploration of other worlds so far suggests that it is a fairly rare

0:56:010:56:06

combination of factors that make our climate and weather so hospitable.

0:56:060:56:10

What makes the Earth so perfect for life is that first off it is rocky.

0:56:110:56:16

It has also got an atmosphere around it.

0:56:160:56:18

And our atmosphere is just right.

0:56:180:56:21

The size and the mass of our atmosphere is critical.

0:56:210:56:23

And, in addition, the composition of the atmosphere is just right.

0:56:280:56:31

Carbon dioxide and water in our atmosphere gives us just the right

0:56:330:56:37

greenhouse effect.

0:56:370:56:38

Venus has too much greenhouse effect.

0:56:380:56:41

Mars doesn't have enough.

0:56:410:56:43

We're also the right distance from our star.

0:56:430:56:47

We're just far enough away from the sun that we are not too hot,

0:56:470:56:51

but we're close enough that we're not too cold.

0:56:510:56:54

The temperature is perfect for water to exist in all three conditions

0:56:540:56:58

and that is so vital for life to have developed

0:56:580:57:01

and evolved on this planet.

0:57:010:57:03

And the Earth even spins in the right way.

0:57:030:57:07

So the other thing that makes Earth such a great place to live

0:57:070:57:10

is that it spins on its axis every 24 hours,

0:57:100:57:14

so the day and night temperatures never get super extreme.

0:57:140:57:18

So our planet has the right unique combination of things to make it

0:57:180:57:23

just the right place for life to have developed and maintained itself

0:57:230:57:27

for billions of years.

0:57:270:57:28

For thousands of years, we've gazed up at the night sky,

0:57:320:57:36

wondering what other planets might be like.

0:57:360:57:38

Astronomers began by studying our own solar system.

0:57:400:57:44

Now they are exploring the wider universe and can even study

0:57:440:57:48

the weather on planets hundreds of light years away.

0:57:480:57:51

They have discovered climates and weather stranger than fiction -

0:57:530:57:58

alien worlds with extreme temperatures,

0:57:580:58:01

bizarre clouds and even ruby rain.

0:58:010:58:04

But they've yet to find another planet like Earth,

0:58:080:58:12

with weather that is suitable for life,

0:58:120:58:15

that's not too hot or too cold.

0:58:150:58:17

So, for the time being,

0:58:190:58:20

it looks like a warm and pleasant day on Earth with a gentle breeze

0:58:200:58:25

and a slight risk of rain

0:58:250:58:26

might actually be the weirdest weather of them all.

0:58:260:58:29

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