The Supermassive Podcast - 20: Firey Worlds
Episode Date: August 27, 2021Izzie and Dr Becky are turning up the heat and exploring the fiery worlds in our solar system. From planets close to the Sun to a distant world of volcanoes and lava. Joining them are planetary scie...ntist Professor David Rothery from the Open University and Professor Alfred McEwen from the University of Arizona, who wants to send a mission to Jupiter’s moon Io. Plus Dr Robert Massey takes on your questions and has his monthly guide to stargazing. This is a Boffin Media production by Izzie Clarke and Richard Hollingham.
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Izzy, do you want to guess at the melting point of rock?
Io has hundreds of volcanoes erupting and it's a smaller world, it's not much bigger than our own moon.
Venus is even hotter than Mercury.
So can we call it a fiery world?
Hello, welcome to the Supermassive Podcast from the Royal Astronomical Society
with me, science journalist Izzy Clark and astrophysicist Dr Becky Smethurst.
Yeah, this month we're doing what the British summer here has not done With me, science journalist Izzy Clark and astrophysicist Dr. Becky Smethurst.
Yeah, this month we're doing what the British summer here has not done and we're turning up the heat, right?
We're exploring the fiery worlds in our solar system from planets close to the sun to distant worlds of fire and lava.
And to help us, we'll be joined by planetary scientist Professor David Rothery from the Open University.
And we'll hear from Professor Alfred McEwan, who wants to send a mission to Jupiter's moon Io.
And you know the drill by now.
Dr. Robert Massey, the Deputy Director of the Royal Astronomical Society, is here too.
So let's get this straight, Robert.
What classifies something, whether that is a planet or an object as fiery? Well I think when you think about this there are a lot of fiery worlds out there and
even before the space age you know we would have been aware of the fact that Mercury the closest
planet to the sun was scorched by virtue of being closer to the sun so during the day the temperature
goes up to 427 degrees Celsius and at night down
to minus 180. So you're simultaneously having a fiery and an icy world. But if you go out to Venus,
the next planet further out and the closest one to the Earth, we often think of Mars as being the
closest, but it's actually Venus. It's the same size of the Earth, but it has a stupendously
thick atmosphere with really high atmospheric pressure at the surface, a big blanket of carbon dioxide.
So the surface temperature is even higher than on Mercury, 470 degrees Celsius, hot enough to melt lead. And we think it might even have active volcanoes too. I definitely think that counts as
a fiery world. And I also like the idea that we should think about the fire, the lava from
volcanoes defining this as well. So Earth in a a sense, could be considered a bit fiery.
Bit fiery she is, just a bit.
And then the exotic moons further out, like Io around Jupiter is the classic example,
which has far more volcanoes than, well, lots of very active volcanoes anyway,
compared with the Earth.
And it's stretched by Jupiter's gravity.
And that generates the melting inside it.
And when it was first seen in the Voyager images, when this stuff was first seen in the Voyager
images, right back in 1979, the classic comment from the researchers was, it looks like a pizza,
because it does. So Izzy's partner, I'm sure you would respect this, looking at this beautiful
pizza image. And these days, even some advanced amateur astronomers can take pictures of that.
You know, they can detect the evidence
for volcanism on its surface,
which says a lot about how amazing
amateur astronomy equipment's become
in the last 50 years.
And as it happens later on,
I'll mention the fact you can see both,
well, all of Venus, Jupiter and Io
in the sky this month too.
Instantly, Io's become my favourite moon.
It looks like a pizza.
Yeah, fine, okay.
I was already my favourite moon, Izzy.
We can debate what sort of pizza.
It was already my favourite.
And I love the fact that we're going to remind people, Robert,
that we can actually see this in the sky.
It's not just, you know, the planets and the stars.
We can see some moons as well after our own moon.
So thank you so much for that, Robert.
We'll be catching up with you later in the show.
Okay, so we have enormous volcanoes in space and
we have hot planets because they're close to the sun. But how much do we really know about these
fiery worlds? I spoke with Professor David Rothery from the Open University and we started with my
favourite pizza moon, Io. Astronomers have revealed that there are more than 150 active volcanoes on this moon and have predicted that there could be up to 400.
Io has hundreds of volcanoes erupting and it's a smaller world.
It's not much bigger than our own moon.
And we didn't really expect small bodies like this to be volcanically active.
But when Voyager 1 flew past Io in 1979, it saw eruption plumes in the same
week that a paper came out in Science saying, hey, there should be tidal heating on Io, it's going to
be molten inside. So that was a remarkable piece of timing. And Io is erupting because it's orbiting
this giant planet Jupiter
with a very big gravity well.
So that's what I was going to ask.
Why is it that Io has so many volcanoes?
Okay, if you distort any solid, you heat it up.
I like to show this to people in lectures
by taking a metal coat hanger, bending it to and fro a few times,
touching it to my lips,
or better still, to a volunteer's lips, and you'll get burnt because where you've bent the metal,
it's hot. Try this at home, people, but be careful. And the interior of Io is being flexed
because it's orbiting this planet with a very strong gravity field, and its orbit has not been
allowed to become circular.
If Io was the only object orbiting Jupiter, it would have been forced into an exactly circular
orbit long ago. But it's a moon called Europa orbiting outside of it, which takes twice as
long to go around Jupiter as Io does. And then there's Ganymede, which takes four times as long
to go around. Now, because it's got this periodic tug, regular repeated tug from Europa and Ganymede, which takes four times as long to go around. Now, because it's got this periodic tug,
regular repeated tug from Europa and Ganymede, keeping the orbit elliptical, that means its
distance from Jupiter is changing all the time. Now, Jupiter's strong gravity is raising tidal
bulges on Io, one on the near side, one on the far side. So Io's shape is distorted from being spherical by the tides, the solid body tides. Because the orbit is constrained to stay very
slightly elliptical because of the presence of Europa and Ganymede in orbital resonance,
Io's distance from Jupiter changes throughout its orbit to heat the interior of Io and that's what's
powering the volcano. It's causing partial melting of the rock inside,
which rises towards the surface and erupts volcanically.
And so these eruptions, you know, is it the same material that we see on Earth?
Is it different?
Like, what is actually coming out of all of these volcanoes?
OK, a lot of it is quite strongly coloured.
So when it was first seen, it was
suggested that, well, we're erupting molten sulphur here. But that turns out not to be the case.
There are infrared measurements of the temperature of what's being erupted, and it's far too hot to
be molten sulphur. It's molten rock. It's probably something called comartii which is high in magnesium but it is molten silicate rock
and there are some very dark fast flowing lava flows on the surface as well as explosive
eruptions powered by expansion of sulfur as a vapor and by expansion of sulfur dioxide as a vapor
to get explosive eruptions you have to have something that will turn to gas and expand violently enough to fragment the rock and drive it out as ash fragments.
Yeah, I mean, it's quite an aggressive moon in terms of all of the processes going on there.
And then we have a few other fiery worlds, and that's because they are close to a fireball that is our sun.
So I'm thinking of Mercury here. Does that classify as a fiery world, would you say?
Well, by day, Mercury is about 430 Celsius. But by night, it's below minus 150 Celsius,
I think. There's no atmosphere to trap the heat, so it cools off very quickly at night. But by day,
yes, absolutely baking hot. It isn't volcanically active, which is a shame but there's a very clear record of volcanic history and all you see on Mercury's surface is lava flow after lava
flow after lava flow of a whole variety of ages mostly between three and four billion years old
but more recent volcanic activity has been explosive. There are holes blasted through
these lavas on Mercury by the force of expanding gas, which has thrown out volcanic ash particles to a range of up to 100 kilometres from the vents,
powered by expanding volatile gases, which is a surprise.
We shouldn't have volatile richness at Mercury.
So that perplexes those of us who are studying Mercury.
Where did it form? How did it form to be able to retain all these volatiles and end up close to the sun
where these volatiles can escape through volcanic processes?
It's a strange old place.
And just finally, looking at beyond our solar system,
we are looking at more and more exoplanets.
Have we seen any form of fiery world beyond our solar system? Do we have the ability
to detect that yet? The way we're going to demonstrate active volcanism on an exoplanet
is a transiting exoplanet that passes in front of its star. That enables us to analyse its
atmospheric gases. Now, if you had a supervolcano eruption,
there you would have an atmosphere loaded with ash,
loaded with sulphur dioxide to such an extent,
but it would affect the atmospheric signal
as it transited across the sun,
seen from a distant observing point.
So we could detect really big catastrophic eruptions
when exoplanets transit their stars.
But we're not going to be detecting infrared radiation from lava flows on exoplanets or anything like that.
It's secondary effects via the atmosphere that we'll be able to see.
That was David Rothery from the Open University.
So, Becky, there was one other planet that we've sort of briefly touched on,
but that's Venus. So as Robert mentioned at the beginning, Venus is even hotter than Mercury.
So can we call it a fiery world? Well, it's certainly hot. And if we were going to go by
the definition of whether it's a hot planet, then yes. It is about 50 degrees hotter than Mercury's
surface just because it has a denser atmosphere
and a really strong greenhouse effect, right? Like Venus is sort of like the warning sign to
all of us on Earth. So by that definition, yes. But I guess the bigger question is whether
it's active volcanically or not, right? So it's not got any plate tectonics like Earth does.
There's no like heat transfer to the
surface like on earth you know one of the big questions is how venus is actually radiating its
heat away but we have seen young volcanoes lava flows and stuff like that all over the surface
of venus but there's no evidence for the fact that they're still active and they're still active
volcanoes it could be that they're mostly dormant. Although they have just like tantalizing hints that maybe it could be, right? So for example, there was a
detection of an increase in sulfur dioxide in the atmosphere of Venus a few years ago. And that's a
classic indicator, right? Of like volcano was here, right? It's the big volcanic gas. So some planetary
scientists are pretty convinced that it has to be somewhat active,
just again, by this idea of it must be getting rid of its heat somehow, maybe through very low level volcanism. And therefore, you probably would classify it as a fiery world as well as one that
is very, very hot. But there's been no direct evidence yet anyway.
Okay. And Robert, Venus seems to be on the mind of a lot of astronomers at the moment.
I mean, we've had at least three missions announced recently. So what are they hoping to find on Venus?
Well, you're absolutely right. And I think that was partly driven by the potential discovery of
phosphine last autumn that we obviously talked about a lot on the podcast as well. And so there
are now at least six missions under development.
When I was looking at this, I thought, oh, yeah, three or so.
And then I thought, OK, six missions being considered and possibly even the seventh.
But there's six at least at the moment.
And there's a number of partners.
So Rocket Lab, a company in New Zealand, they're thinking about a private mission that would
maybe launch in 2023, drop balloons into the atmosphere with the explicit idea of checking
to see if there's life in the atmosphere of Venus.
The Indian Space Agency, ISRO,
has its Shukrayan-1 mission,
which will launch a year or two after that.
And that will also be looking at the atmosphere
and studying the surface as well
and looking at how the planet interacts with the sun.
There's VERITAS,
which is one of the newly approved missions from NASA,
launching in 2028 or so.
That'll be looking at the geology of Venus and trying to find out whether there was ever water on the planet.
Because one of the ideas is that earlier in the history of the solar system, Venus might have had a much more pleasant surface, that there might have been liquid water and even a large ocean.
There certainly isn't anything like that now.
The Russians want to launch a probe in 2029 with an orbiter and a
lander, which is fantastic. Imagine, there have only been a few landers on Venus because they get
down to the surface. The Russians were very good at this, or the Soviet Union actually in the 1970s.
And those landers shut down within about an hour and a half because it's such a ridiculously
extreme environment. It's not only incredibly hot, but you've got crushing atmospheric pressure
and it rains sulfuric acid. So it's a tough call to get technology to work there.
That might have a balloon added in. Then there's DaVinci Plus, another NASA one that might arrive
the same year. That'll look at the atmosphere, and that's going to drop a probe through the
atmosphere to study the atmosphere and go down to the surface, and also try and understand about
whether there was an ocean. And then finally, the European Space Agency has approved the Envision mission,
which will get there in about 2034 and do similar things,
look again at the atmosphere, look at activity on the surface.
So I'm taking a deep breath after that.
There's a lot of Venus missions going on.
Yeah, there's just so much to look forward to, isn't there?
And I mean, like you said, we haven't had a probe or a lander
since like the 80s with the Soviet Union. So you think about all the questions that we just didn't know to ask back then, that we now are so interested in, you know, I'm really excited to see, you know, what sort of technology and everything will make it onto all these probes and landers that we can, you know, ask all these questions that we're dying to know the answer. But six, I mean, six to Venus and poor Neptune and Uranus people can't even get one.
I'm like, come on.
It always feels like a zero-sum game, doesn't it?
You know, but yeah, we want missions to Neptune as well, obviously.
So it's clear there are so many questions we want answered when it comes to these fiery worlds.
And our next guest is proposing a mission to Io to discover what is actually going on with all of these volcanoes.
Professor Alfred McEwen from the University of Arizona, welcome to the Supermassive podcast.
Now you're working on something called the Io Volcano Observer.
So what is it about volcanoes on Io that we
want to understand? Right. So the Io Volcano Observer or IVO is a mission we did propose
in the last round of the NASA Discovery missions and it will be proposed again in some form.
But it's a mission dedicated to studying Io, the extremely volcanically active moon of Jupiter that's tidally heated and has hundreds of actively erupting volcanoes with high temperature silicate eruptions.
And we want to know more. What makes Io tick? What does this tell us about Io's interior?
What's going on with its unique tectonics and how does that relate to uh to the early earth and
other planets yeah i was just about to ask whether those the tectonics could teach us a lot about
sort of you know anything like mass extinctions on earth that we might think have been driven by
volcanic activity that kind of thing right so they're uh at least four out of five of the
phanerozoic or the last 500 million year mass extinctions on earth are
very precisely correlated in time with the peak eruption of flood lava, such as in Siberia.
So that's probably not a coincidence. And it's thought that those eruptions change the
composition of the atmosphere, which in turn changes the composition of the ocean. But anyhow, these are massive eruptions, very high effusion rates, something we've never seen in person.
But that's a good thing. Probably wouldn't survive. Yeah, these are orders of magnitude
bigger eruptions than anything we've observed. But they're happening today on Io.
And there are some features on Io in particular, right, that have grabbed your
attention, piqued your interest? Some of us love all the features on Io, but a couple of favorites,
crowd pleasers are Loki Patera. This is a 200 kilometer wide depression that's full of lava
and it's been described as a lava lake or even a lava sea
and it has periodic sometimes periodic eruptions which might be due to an overturning
crust on a lava lake although loki is the trickster god so we keep reminding ourselves that
it may be fooling us but that's one feature we'd really like to understand. It's the most intense hotspot in terms of heat flow on Io.
Another one is called Pele, after the Hawaiian goddess of volcanology.
And this one has had the biggest plume on Io's equatorial region.
There's been others at higher latitudes that are comparable in size.
But for the IVO mission, we can make
close passes over the equatorial region. So this is one that we could actually fly through and
measure the volcanic gases. And that also has a smaller lava lake with a very high temperature
hotspot. So those are two favorites. Oh, wow. And so that's something I wanted to touch on there.
So you're proposing this mission. So how would you actually try and investigate a lava sea?
You know, no big deal.
Right, so studying Io is challenging.
First of all, it's at Jupiter.
You have to get there.
But then it's also well deep inside Jupiter's giant magnetosphere.
And all that stuff erupting from Io, that gets charged up by the
magnetosphere. So there is a plasma torus full of energetic electrons. So that stuff wears out
your electronics in a hurry. So what we have to do is we're in an elliptical orbit around Jupiter
that's inclined such that we fly lickety split from north to south by Io, get our data in a hurry
and get out of there as fast as possible. So we have a very specific orbital geometry that's
designed to minimize the total ionizing dose, we call it. And so then we have to have, how do we
get the measurements with such a fast flyby and with advances in instrumentation, we can actually do surprisingly well.
Yeah. So is that looking at probes or like what sort of the, what are some of the equipment that
you're hoping to send and to measure? This is quite a hostile environment.
Yes. So we are especially interested in what's happening inside Io. Observing the active volcanism is pretty easy.
We'll take pictures. We have thermal camera. We can measure the temperatures.
And we have to do all that fast, but we can do that. And of course, we have time approaching
and departing to get more global view. And so all that is relatively easy. You have to build and
test the instruments and all that.
But understanding what's inside of Io, that's the hard part.
So we have several tools at our disposal.
One is gravity science.
So it's not a special instrument.
It's just precisely tracking the spacecraft as it flies by Io. In particular, we want to measure the tidal signature.
So Io orbits Jupiter every 42 hours.
the tidal signature. So Io orbits Jupiter every 42 hours, and the surface rises and sinks by as much as 100 meters every day from the extremely strong gravitational tides. It's in an elliptical
orbit around Jupiter, forced by Europa and Ganymede, in fact, with the resonance that they're in.
100 meters is incredible, because if you think about Earth tides is only a couple of meters if we're lucky and that's on the ocean and yet we're
talking about rock here. And so it's 100 meters if Io has a magma ocean where the lithosphere is
detached. If Io is more solid with just interstitial liquid then it's more like 30 meters which is
still pretty high. Still. So that's one of the things we can measure with the gravity signature is, is it big or
small?
That means does it have a magma ocean or does it not?
Another way is with a magnetometer.
So a magma is electrically conducting.
And I mentioned that Jupiter has this giant magnetosphere.
It's also tilted.
So from Io's point of view, it is sweeping north-south
over Io. So this is a giant electromagnetic probing experiment for Io's interior that we get for free.
We just have to bring a magnetometer to measure how the magnetic fields vary as Jupiter's
magnetosphere goes up and down, which depends on the interior conductivity,
which again depends on how much magma there is inside Io. So that's a second method. A third
method is to measure the composition of lavas coming out of Io. We have a mass spectrometer
on the spacecraft that can tell us exactly the elemental composition of everything coming out of Io's plumes.
So what is the status of the IVO mission?
So at the moment, we did extremely well in our last round of discovery.
We were one of the finalists.
We did a phase A study, it's called.
But ultimately, the other ones did well too.
And there were four of them.
And so NASA could only select two and they selected
two Venus missions and that's great because Venus is also deserving of further exploration and it's
also very relevant to understanding Earth and so I can't complain about the Venus missions but
you know we can try again. I think this is interesting because it's not something that
we talk about all that much but the fact that scientists like yourself will have to put in the research and proposals for missions.
And obviously, Io is so interesting.
Everything that we've discussed already is just like, yes, let's go.
Let's find out more.
So what is that next step?
It depends on when NASA releases an announcement of opportunity for a new mission, either New Frontiers or Discovery.
Right now, we anticipate something like 2023 for that, which means we really need to get going.
They'll announce it well in advance, and we really need to get going in 2022.
So that's only next year.
There are other missions going to the Jupiter system that can get some
remote observations, so that's good. The Europeans are interested in Io as well, but Europe could
have a standalone mission at some point in the future or make some extra contribution to a NASA
mission, such as we'd really love to have a probe. We release and impacts into Io with a seismometer
because the seismic signal from Io has got to be spectacular,
and it only needs to survive in one Ionian day, 42 hours,
to get the total signature of that.
And it can have a heat flow probe as well for conducted heat flow.
So we have lots of ideas. What really happens remains to be seen.
We wish you the best of luck. I'm sure all the listeners will agree with that. And thank you so
much for joining us as well. That was Professor Alfred McEwan from the University of Arizona.
This is the Supermassive podcast from the Royal Astronomical Society
with me, astrophysicist Dr Becky Smethurst and science journalist Izzy Clark.
This month we're exploring the hottest worlds in our solar system
and we're not the only one with questions.
We've got a whole pile of questions from listeners
so thanks as ever for sending them in.
Robert Lewis on Twitter asks,
Am I right in saying that the majority of exoplanets
that we have discovered are hot Jupiters?
What is special about our solar system
that means we don't have actual Jupiter and Saturn closer to the sun?
So perhaps let's start with what is a hot Jupiter?
Well, a hot Jupiter is exactly what it implies.
It's a big, massive planet close into its star.
And a good example is one of the very first one that was discovered. Actually,
there was a weird pulsar planet discovered a couple of years before that. But 51 Pegasi b,
the defining exoplanet discovery in 1995, co-discovered by Didier Queloz, is actually
in the UK, in the University of Cambridge. And he worked with Michel Mayor,
they found this object, it goes around its star every 4.2 days. Now, if you think about something
like Mercury, it takes 88 days to go around the sun, our sun. And so the fast orbit is because
it's much, much closer, it's just 8 million kilometres from the star's surface, or about
six times closer in the Mercury. So it gets heated to at least a thousand degrees
Celsius. And that's before you consider any atmospheric effects or anything else. This is
the kind of heat you have if you're that close to the star. So that is certainly hot Jupiter.
And it turns out, think about Lewis's question, a lot of the planets we found are like that,
but that's partly because they're easier to detect. I'm not sure, by the way, if it's still
true the majority. It certainly was the case initially. But it's partly because they're easier to detect. I'm not sure, by the way, if it's still true. The majority certainly was the case initially.
But it's partly because they're easier to see because if you detect them because they move in front of the star, what's called a transit where they block out a bit of the light, then a big planet that's doing that very often, it's more likely you're going to be able to detect that.
And also if they're Jupiter-sized, they've got a big gravitational pull.
And also, if they're Jupiter-sized, they've got a big gravitational pull.
One of the other methods of detecting a planet is that the planet goes around the star and pulls it back and forth.
And we measure that by looking at the change in the wavelength of the light, the Doppler shift.
It goes back and forth as the planet goes around. So bigger planets, that's easier to see.
And that's why certainly a lot of the earliest discoveries were like this and why it's much, much harder to find things like Earth-like worlds,
because Earth as a smaller gravitational pool is likely to be further away
if you want it in a place where it might be habitable.
So that's a lot of the effect.
Now, the final thing he did ask about why we don't have that scenario in our solar system.
That's a really interesting question.
There is a lot of argument.
The planets like these hot Jupiters we think migrated in,
that they started out further out and then
they interacted with either other planets in their system or with the kind of residual planetary
disks that these things form from and ended up much closer to their star. So why that didn't
happen in the solar system is a really intriguing question. Maybe the solar system is slightly
special that we don't have that kind of setup. And it's the sort of thing to really explore with
an exoplanetary specialist as there is a lot of argument about this and whether or not, you know,
some people also say these planets might have formed much closer into their star, but the
favored view I think is that they formed further out and were likely to migrate in.
Yeah, I heard that it was because of the interaction of Jupiter and Saturn. Like this
is the leading hypothesis, right? That if hadn't existed then jupiter would have
migrated inwards completely unchecked but saturn essentially pulled it back again into its current
orbit and so i mean you could say if you wanted to that saturn is the whole reason that earth is
still here and that is reason number 732 why saturn is my favorite planet or are we saying that Saturn is just holding Jupiter back? No. No.
I didn't say that.
Well, Lewis, I hope that answered your question.
Becky Francois asks,
is there a limit to the amount of heat a rocky planet can withstand,
whether it be from tidal friction, greenhouse atmosphere or proximity?
Yeah, this was a great question.
I actually had to look this one up because I didn't know.
And I started with what the hottest rocky exoplanet is that we know of.
It's Kepler-70b.
Well, there is a bit of concession about whether it does exist or not,
but we're pretty sure it does. It orbits around its star in five hours and 45 minutes.
Wow, okay.
So it has an estimated surface temperature of 7,000 Kelvin.
Oh my gosh.
And we know it's rocky
because it's only about half the size of the Earth as well.
So we think it's actually very likely
that it's like a core remnant of something
that was once a gas giant
that's essentially had its atmosphere boiled off,
perhaps if its star went
through a red giant phase or something like that and swelled up but at 7 000 kelvin right
i mean even if it is a core you've not got solid rock anymore you've got something that's
completely and utterly liquid you've got magma you've got lava right because izzy do you want
to guess at the melting point of rock i mean i wouldn't know robert you want to guess at the melting point of rock? I mean, I wouldn't know.
Robert, do you want to guess a number around about what it is?
Well, I admit I did check some of this out,
but it depends what the rock's made of, doesn't it?
But I think some of it melts at about 1,000 degrees and then some of it melts at 2,000.
Yeah, so it's somewhere between about 900 and about 1,600 Kelvin.
So it's pretty high.
So you're definitely in the
realm of completely melted rock right so at these extreme temperatures of 7 000 kelvin you actually
have to start thinking about evaporation of rock of liquid rock which is incredible to think about
right it's hot enough that there's enough energy for the rock to overcome the
gravitational energy binding the planet together like that's how hot we're talking so i actually
found a paper way back from 2013 that was called catastrophic evaporation of rocky planets which
is one of the greatest titles of a paper i've ever seen in my entire life
and they modeled this happening with a planet that was just a little bit heavier than Mercury.
It's about 10%-ish of the mass of the Earth.
And with a temperature of only 2,000 Kelvin, not 7,000 Kelvin.
And they worked out that it would take just less than about 10 billion years for that rocky planet to fully evaporate.
Now, obviously, Kepler-70b is about half the mass
of earth and it's about 7 000 kelvin so it would probably take a little bit longer than 10 billion
years despite that larger temperature um and i mean 10 billion years you're getting towards sort
of current age of the universe right of 14 billion years so it's much more likely that like a star
would die off and disperse all of the materials
before a rocky planet could fully evaporate due to proximity i didn't really look into greenhouse
gases but obviously if you're that close to a star you're obviously going to be undergoing
tidal friction as well francoise so i mean i think that question is yes theoretically if you gave it
long enough and you put it close enough, you could have an evaporating
rock planet.
I sort of think about this hot
blob going around the star
or something with some
wonderful long trail.
I imagine it a little bit like, you know
the videos of water
on the International Space Station?
Yeah, yeah, yeah.
That's what I'm picturing, just like wobbling around in stuff oh my gosh well i mean thanks
for the deep dive becky that's great you're welcome i had a great fun prepping that one
all right robert next question is for you from john white who asks would it be possible for a
rocky planet in a close orbit to have one half molten and one half
with a solid surface because it's tidally locked so let's start with what does it mean if something
is tidally locked well tidally locked is the best example of something being tidally locked is our
own moon it means that the where one body is orbiting another that they it always keeps the
same face to it so it's still rotating round but it's doing that over the length of its orbit.
So the moon does spin.
It's just that it takes as long to spin as it does to go around the Earth.
So we always see the same face.
And that does happen with a lot of systems.
I think Pluto and Charon, the moon of Pluto, do that.
Some of the moons of the giant planets do it as well.
So it's not an unusual thing.
And the sun has that effect, I believe, to a lesser extent on Mercury as well.
There's partial effects going on there.
We definitely are going to be seeing that with some planets around other stars.
So that's what John's referring to there.
Now, as for, I was just thinking about Becky's answer,
but as for what it would mean if one side was molten and the other wasn't, I think it probably depends a lot on the type of planet.
If it had, and whether or not that atmosphere would survive, if it was hot enough for it to be cooked like that, I guess we could assume it's so hot there's probably very little of an original atmosphere left that you're talking about material gassing off the surface.
If it's fairly small, I find it hard to believe believe a lot that heat wouldn't be being transferred round.
But it is a really intriguing thought,
the idea that you might go round to the night side
and there would be this super cold place,
like on Mercury,
despite the rock facing its star being superheated.
And I think you probably need to ask
a sort of geologist about how efficiently
that heat would transfer
through the system.
Maybe as well if it didn't.
Again, I don't know whether this would apply or not, but whether it had a molten interior
or not like the Earth does, because that would presumably efficiently transfer some of the
heat as well.
So it's a very intriguing science fiction idea, I think.
The idea that you build some sort of base in the twilight area where it's just about a clement temperature. Of course, there's little details
like actually getting to the star in this planet in the first place, but, you know, nice idea.
And there are examples thinking about, you know, Becky's description. There is the idea that some
of the hot Jupiter planets, if they're around long enough, might have their atmosphere stripped
away completely and be left in that sort of situation hot Jupiter planets, if they're around long enough, might have their atmosphere stripped away completely
and be left in that sort of situation.
So they start off as a very hot Jupiter-type planet
and end up as a hot rocky one.
But yeah, it's an intriguing thing to look for,
just about that planet that's just on the threshold like that.
Yeah, and I swear, from some of the questions we get in from listeners,
we're basically building a back catalogue for sci-fi book ideas.
I'm just like, yep, making a note of that one.
I think we both support and ruin sci-fi sometimes,
don't we?
Oops.
Okay, well, thanks for clearing that one up.
And so, Becky, one more question for you.
Will the James Webb Space Telescope
or one of the proposed future space telescopes
allow us to detect volcanic
activity on exoplanets i mean yeah we really hope so anyways what people have got their fingers
crossed for so we're talking before about how volcanism gives off you know a lot of telltale
gases right we've already spoken about sulfur dioxide which reacts with water in atmospheres
to give you sulfuric acid which is not great But you've also got carbon dioxide and methane as well that's produced by volcanic activity. And all of these gases leave
an imprint on the starlight that passes through the atmosphere of the planet, you know, while it
passes in front of its star. And a lot of those imprints are in the infrared part of the spectrum
where the James Webb Space Telescope is sensitive as well. James Webb is also big enough to be able to
collect enough of that light and isolate it from the overall starlight as well,
the little bit that's just passed through the atmosphere. So technically, yes, but then you've
got to think of sort of like whether any volcanic eruption has spewed out enough gas for it to leave a big enough signal
on the light for us to be able to detect it. So we have the capability to do it, but I guess it
comes down a little bit to a numbers game as well. Like, is the eruption strong enough? Is the planet
passing in front of its star from our perspective at the right time, just after the eruption, for us
to see that before it breaks down into things like sulfuric acid so bit of a game of
chance but we're very hopeful that we will spot this and this is one of the main goals of the sort
of the james webb space telescope sort of exoplanet science as well yeah i cannot wait for james webb
space telescope i just want it ready no offense hubble but you know come on hubble's back though
which is good but yeah james webb is supposed to be
october i think it's been pushed to december now because of the issues with the um the arianne
rocket that it was going to be launched on um but i'm fingers crossed it's definitely going to
happen in 2021 um and i can't decide whether i'd love to be one of the people that's at the launch
site who've been working on this for the past 20 years of their life or if i'd want to be as far
away from as possible i was going to add is there there are a couple of other exoplanet missions that would be trying
to do this kind of thing too, whether or not they're able to, but you know, like CHEOPS
is already operating, trying to look at atmospheres of exoplanets.
And there's the PLATO mission, which will be looking for rocky planets.
I don't know, probably does come to notice exactly what Becky's describing about how
big a signature it is, but part of their job is
to try and look at
the atmospheres of
these things for the
first time which is
which is an amazing
thing is it I mean
imagine the idea we
didn't even I'm old
enough I don't I
remember when I'm not
even sure if you two
are old enough that
you remember when
there were no
exoplanets but I
definitely am well I
don't remember but I
know that it was
something like Jurassic
Park was released in
1993 no exoplanets Toy Story 1995 one exoplanet and that's But I know that it was something like Jurassic Park was released in 1993.
No exoplanets.
Toy Story, 1995, one exoplanet.
And that's the marker I use in my head.
It's like, well, pre-Jurassic Park, no.
Pre-Jurassic Toy Story, yes.
Of course that's your scale.
Of course that's your scale.
All right, well, actually some really brilliant questions this month.
So thanks, everyone.
And if you want to send in a question, do so please we love them so you can email podcast at ras.ac.uk or tweet at royal astro sock so robert what are some of the things that we can see in the night sky this month it's
funny this is a great time actually to be out looking at the night sky because the weather
you know isn't too cold typically although i admit august has been a slightly disappointing month so far in terms of temperatures understated of the year but i'm
waiting for the clear night to see the persons and it never came i think i got lucky we were camping
in dorseter last week and we actually had a really dark sky there a fabulous view and it was fairly
clear and i had a lot of sunny weather as well probably something about the coast but what i was
really struck by the beautiful thing you do, you get in that setting.
Even in the UK, you can go out and you can see the Milky Way stretched across the sky.
Absolutely fantastic.
I didn't have any cameras with me or anything like that.
I just soaked it in and watched the Percy and Meech's shower at the same time.
But it's still a really good time to be looking at that because the advantage is that although it's moving more into the evening sky and won't be there all night as it was the skies are a bit darker so we have properly dark night skies in
august particularly and the further on the month you go the better uh and into september and the
dust lanes all the wonderful details stand out so what i would really encourage people to do if
you're going on a holiday like that you know staycations everybody's sitting there thinking
oh you know just about managed to do some camping or something like that but if you get even one or two clear nights take a pair of
binoculars with you and soak up the view and you can see quite a lot of little things you can see
this wonderful asterism i love i mean look it up on some charts called the coat hanger which is
between the stars vega and alto about halfway between the two in the triangle uh and the wild
duck cluster another beautiful little little sprinkling of stars lower down.
And if you have a small telescope, even better.
I mean, I don't know if taking that to a campsite is more complicated,
but if you do have one, then you can see just a whole load of things
in that central plane of our galaxy.
It's a fantastic time to look at it.
But pertinent to today's stuff, Venus is also getting a bit easier to spot as well,
and it will improve as the year goes on it's been
not been very easy so far it's been very very low down but as we move into september it should get
it's a bit better place it'll be a bit higher in the sky after sunset over in the northwest and
then moving around to the west as the position of the sunset changes as the year goes on and on the
10th of september you've got the crescent moon near it another always a fantastic photo op it's
just yes exactly we're not going to say what becky've got the crescent moon near it. Always a fantastic photo op. We're not going to say what Becky's
definition of crescent moon is.
But she might.
Fantastic photo op. And also
we have got both Saturn and
Jupiter low down in the south
as well. They're not going to get that high this
year. They're just still stuck down in the lower
part of the ecliptic. But if you have
part of the zodiac, the constellation of Zem, if you
have a nice clear southern horizon, they're very very easy to spot if you have a clear sky
and jupiter stands out because there's a it's much brighter than any star but secondly there's just
nothing else around it you can't mistake it um so get a pair of binoculars and look at that if you
don't have a telescope and you can see the four little points of light that galileo discovered as
recognized as moons the jupiter and that will include io the closest one into jupiter and you can see the four little points of light that Galileo discovered as recognised as moons to Jupiter and that will include Io, the closest one into Jupiter and
you have to watch it over a few nights because obviously it depends on exactly where they are.
The closest one is Io and if you look at that little tiny point of light you can just imagine
the pizza moon and those maybe 400 volcanoes. And another really interesting thing that perhaps you guys can explain is the
fact that we've been able to see behind a black hole recently what is going on there
i always say there was this new study do you remember the um interstellar the film where they
they beautifully rendered that black hole and it and it has this accretion disc around it right
which is the material that's spiraling around the black hole that eventually become part of it
and in the film the light from that is bent around the black hole so you almost see this ring of
light around the black hole and it's light that comes from behind it so i'm saying basically this
new study is like a little tick next to that interstellar rendering of a black hole and people
always get confused this idea of behind a black hole because they think of a black hole as a hole but it's not right they
were once 3d objects you know and we consider the event horizon as a three-dimensional sphere
so what this is like saying is say i got in a little spacecraft i'm imagining that yeah trundled
off to behind the moon and i just like off i go right behind the moon playing a game of hide and
seek right you can't see me because i'm behind the moon imagine if i took a torch and was sort
of just like flashing light periodically and the moon's gravity was strong enough so that the path
of that light was no longer straight it got curved around so you could still see it on earth this is
essentially what they've detected they've detected light from the part of the accretion disc that
from our perspective you know say if you imagine it like the rings of saturn is behind the black hole
that's been bent by the huge gravity around it so that we can actually see it and they can actually
tell where it comes from because that accretion disc is moving so depending where it comes from
and how close it goes to the black hole it gets a different doppler shift as well a gravitational
red shift or a different uh red shift so it's really cool they've seen it in x-rays
which also makes it sound extra cool like x-rays shifted to see behind a black hole right and it
was just a really cool study that came out and it and basically it um confirmed something that
einstein's theory of general relativity predicted you know way back 100 years ago when you hear
when you hear stuff like that you just think god space is
so cool like you're just like why why do you think i became an astrophysicist busy i'm just like
yeah man okay i can get behind that it's so good
right well i think that's it for this month we've covered the fiery worlds so next month it's all
about the icy ones.
Yeah, and don't forget
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