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Gravity Assist Podcast: Jupiter with Jared Espley (1)
Jan. 3, 2018
This illustration depicts NASA's Juno spacecraft soaring over Jupiter’s south pole. Credits: NASA/JPL-CaltechTranscript:
Jim Green: Our solar system is a wondrous place with a single star, our Sun, and everything that orbits around it - planets, moons, asteroids and comets - what do we know about this beautiful solar system we call home? It's part of an even larger cosmos with billions of other solar systems.
Hi, I'm Jim Green, Director of Planetary Science at NASA, and this is Gravity Assist.
With me today is Dr. Jared Espley. He's a planetary scientist at Goddard Space Flight Center, but he's also the program scientist on Juno, one of planetary science's fantastic missions.
Now today, we're gonna talk about the big guy on the block, Jupiter. It's the “800-pound gorilla” of all our planets. Jared, why is it so big? Why did it get the way it is?
Jared Espley: We actually don't know that, Jim. That's, I mean, that's one of the really cool things in science is, you know, we don't know how exactly Jupiter formed and how planets in general formed throughout the universe. And so, that's what Juno mission is designed to do, to try and help us understand how planets form, in general.
I mean, part of the answer, of course, is that gas condensed into solar nebulae to form Jupiter, but exactly under what circumstances that happened and why Jupiter was the largest in our solar system, we just literally don't know.
Jim Green: You know, we think that as the planets were created and Jupiter obtained most of the gasses, that it would have or could have rivaled the Sun at one time in terms of being able to turn on and become another sun since quite a few--I think the large percentage of stars in our galaxy are double stars, so Jupiter perhaps was a failed sun.
Jared Espley: Yeah, that's right. I mean, basically, you just need to get enough mass that you ignite nuclear fusion, of course. And so, Jupiter didn't quite get there, but it's the largest planet in our solar system.
Jim Green: Actually, I think the calculation is it takes about 80 times the mass of Jupiter to get it to the point where it'd become a sun.
Jared Espley: Uh-huh.
Jim Green: You know, one of the most iconic and fascinating features of Jupiter is its Great Red Spot. You know, Juno's really learned a lot about the planet as it's passed over very close, but the red spot, it just passed over this summer. What did we find out?
Jared Espley: Yeah, like you said, we--you know, we've seen a lot of images of the red spot over the years, but Jupiter has all these instruments that are specifically designed to look underneath the clouds of Jupiter. And so, we used those instruments in this specific case to look at the Great Red Spot. And so, what they found in particular with a microwave radiometer, which basically just means that we can see the emissions and the microwave coming from deep down in the atmosphere, that it was warmer underneath the Great Red Spot very deep down, way down into the deep atmosphere, hundreds of kilometers deep.
And so, clearly, there's roots, there's sources of atmosphere turbulence down below, the details of which are being worked out. But, it means that not only is it an iconic storm at the surface but it goes deep down into the atmosphere.
Jim Green: Optical astronomers have been using telescopes to observe Jupiter for several decades and hundreds of years, and they have been observing that the red spot is shrinking. What's been happening? Do we know yet?
Jared Espley: I don't think we really do. Again, that's one of the awesome things about science is always mysteries. Like you say, observationally, we can see clearly at the surface that it's shrinking. Again, we just talked about the roots deep down, whether they've been growing or shrinking. We have no idea because, of course, we just have those measurements from Juno recently.
But, we want to keep tracing that and be able to see the evolution of this gigantic storm over the next decade or so and see how that compares with the past few hundred years.
Jim Green: One of the really exciting instruments on Juno that I really love is the Waves instrument.
Jared Espley: Uh-huh.
Jim Green: And that's an instrument that makes measurements of electromagnetic waves. And we've got a process for which they take those waves that are electromagnetic that are observed by the Waves instrument and convert them into sound, and that's really been a fascinating opportunity for us to, in a new way, listen to the sounds of Jupiter, listen to the sounds of space. What does that tell us?
Jared Espley: So, as you well know, the waves that we typically are recording, these electromagnetic waves are produced by the different energetic particles that are at the different planets, and they produce different types of waves. In some cases, they can be related also to lightning activity. We have whistler waves at Earth. We have these at Jupiter, as well.
So, a lot of these things are the electromagnetic waves. But like you say, the audio version, the sonified version just makes this really eerie space music in some ways.
Jim Green: Yeah. So, let's play a sound clip.
[Sound clip.]
Jupiter as the big guy on the block also seems to have most of the moons. How many moons does Jupiter have?
Jared Espley: We think it has dozens, 50, 60 moons, but it has four major satellites, the Galilean satellites that were discovered by Galileo hundreds of years ago. And those moons are particularly interesting to us because they are full worlds in their own right and really interesting features - oceans, ice, tenuous atmospheres. And so, they're really fascinating moons.
Jim Green: Yeah, they're huge. I think Europa, which is the smallest of the four, is just a little smaller than our own moon. And then Ganymede is the largest moon in the solar system, plus it has its own magnetic field.
Jared Espley: Yep.
This image of Jupiter’s iconic Great Red Spot was created by citizen scientist Björn Jónsson using data from the JunoCam imager on NASA’s Juno spacecraft. Credits: NASA/JPL-Caltech/SwRI/MSSS/Björn JónssonJim Green: How cool is that?
Jared Espley: Yep, they're real worlds in their own right.
Jim Green: One of the things that the moons do, of course, is, as they orbit the planet, is they really connect to the magnetic field of Jupiter, and that produces all kinds of effects. What are some of those things?
Jared Espley: Yeah, it's really neat how the magnetic field does that connection between the moons and Jupiter itself, like you said, because one of the main things that we think is happening is that material from some of the moons, Io in particular, is being lofted into space. Giant volcanoes on the moon are blowing material into space. It becomes ionized, loses an electron and then gets entrained in the magnetic field and driven back into Jupiter then. So, there's a literal physical connection between a moon, volcanoes blowing stuff into Jupiter. And when that happens, then it produces the aurora that we can see at Jupiter, those northern and southern lights. And so, it's just an awesome connection between geology, space physics and Jupiter itself.
Jim Green: Jupiter's magnetic field is really quite different than the ones that we're used to around some of the other planets, but it also gives us an opportunity to study where the magnetic field is generated. What are we learning about Jupiter's magnetic field?
Jared Espley: Yeah, so Juno as a mission, like I've said, is designed to look inside of Jupiter, and one of those ways is through the magnetic field, like you mentioned. And so, with our instruments on board Juno, we are learning that the magnetic field at Jupiter is even more complex than we thought originally. It's got this global planetary magnetic field that we knew something about to begin with. But, it looks like there's even more structure going on there. So, there may or may not be multiple places where the magnetic field's originating, something deep inside and something maybe a little closer to the surface. We're starting to just disentangle that now.
Jim Green: Perhaps that is related to the core of Jupiter, and Juno is designed through its gravity measurement to make some of those measurements. What are we finding out about the size of Jupiter's core?
Jared Espley: Yeah, exactly, the two--the gravity and the magnetic fields are ways to probe that deep interior. And so, working together, they're starting to revise the classic picture that we've always had in our mind where we thought there might be a dense rocky core in the center surrounded by really, really condensed hydrogen and helium and a metallic layer because it's under so much material--or so much pressure and then the lighter layers above that of gas.
And so, the gravity measurements are starting to really kind of upend this classical view, and it looks like it may just be more well mixed down there. There may not be the classic rocky core that we thought. But, honestly, there's a lot of controversy, discussion going on right now within the science team, which is what you want. You want to have scientists arguing because that's what's fun.
Jim Green: You know, we're gonna be talking to Linda Spilker (project scientist for NASA’s Cassini mission at Saturn) about some of the gravity measurements being made at Jupiter and finding out about cores from another sister planet, which is Saturn. So, indeed, we're really heading towards, I think, a tremendous understanding of these giant planets.
One of the things that Jupiter's got that is just absolutely spectacular are the beautiful cloud structures. What is Juno finding out about these?
Jared Espley: Yeah, so we have, like I said, a lot of interest to look inside, but we also happen to have this instrument, the JunoCam instrument, that's creating these amazing pieces of data and art at the same time. And so, some of those images are just beautiful to look at, but some of them are really revealing new science. And a lot of that's in the polar regions because we're getting really good imagery at the polar regions that we didn't have before. And we're starting to see all these storms, these vortices that are swirling around the polar regions, and so the JunoCam's really starting to tease out how the polar atmosphere is working.
Jim Green: How come we didn't see these before? Is this something new?
Jared Espley: It is because almost all of our imagery either comes directly from Earth, of course, where we have the Hubble Space Telescope or even the backyard telescopes that the listeners might have where you can look at Jupiter. But there, you're able to see the side view of Jupiter, and it's almost impossible to see the top view unless you happen to have a spacecraft there flying directly over that top view, which we do.
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