WEBVTT

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<v Speaker 1>Welcome to Bedtime Astronomy. Explore the wonders of the cosmos

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<v Speaker 1>with our soothing Bedtime Astronomie podcast. Each episode offers a

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<v Speaker 1>gentle journey through the stars, planets, and beyond, perfect for

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<v Speaker 1>unwinding after a long day. Let's travel through the mysteries

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<v Speaker 1>of the universe as you drift off into a peaceful

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<v Speaker 1>slumber under the night sky.

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<v Speaker 2>I want you to take a second and like just

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<v Speaker 2>visualize the most likely place we might finally find alien

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<v Speaker 2>life in our solar system.

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<v Speaker 3>Yeah, that's a big question.

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<v Speaker 2>Right, And you know, if you ask one hundred people

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<v Speaker 2>on the street, the vast majority are going to point

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<v Speaker 2>straight to Mars. Oh.

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<v Speaker 3>Absolutely, the red planet.

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<v Speaker 2>Exactly, Mars. I mean it's right next door. We have

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<v Speaker 2>all these rovers like leaving tire tracks in the dirt everywhere.

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<v Speaker 3>We spend so much time looking at those dried up

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<v Speaker 3>river beds.

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<v Speaker 2>Yeah, just hoping to find, you know, a fossilized microbe

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<v Speaker 2>from billions of years ago. But I want you to

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<v Speaker 2>completely bypass Mars today, gipit entirely. Totally. Forget the red dust,

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<v Speaker 2>forget looking for ghosts of a dead biosphere. We are

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<v Speaker 2>heading much further out into deep space, past the.

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<v Speaker 3>Asteroid belt, straight towards you.

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<v Speaker 2>Straight to the gas giant. But you know, we aren't

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<v Speaker 2>looking at the turbulent atmosphere of Jupiter itself. We are

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<v Speaker 2>locking our sights on one of its icy moons, Europa, Europa,

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<v Speaker 2>and like our mission today is to explore this massive,

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<v Speaker 2>brand new reality check in astrobiology.

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<v Speaker 3>It's a huge shift in how we think.

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<v Speaker 2>It really is because, I mean, we've known for a

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<v Speaker 2>while that Europa hides this global ocean beneath its frozen.

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<v Speaker 3>Shell, right, that's not the new part, no, But.

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<v Speaker 2>The new part is that getting to that water and

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<v Speaker 2>you know, whatever complex chemistry might be swimming around in

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<v Speaker 2>it is going to be a much tougher barrier than

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<v Speaker 2>scientists ever assumed.

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<v Speaker 3>It is arguably the most compelling piece of real estate

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<v Speaker 3>in our entire planetary neighborhood.

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<v Speaker 2>Why is that exactly?

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<v Speaker 3>Primarily because it's not a fossil. It is active right now.

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<v Speaker 3>Like when you look at high resolution images.

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<v Speaker 2>Of Europa once from the Galileo probram yeah.

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<v Speaker 3>The Galileo probe in the nineties, or even the more

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<v Speaker 3>recent stuff from Juno, you immediately notice what is missing exactly.

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<v Speaker 3>You don't see craters. If you look at our own Moon,

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<v Speaker 3>it is absolutely pulverized, just covered in impact craters from

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<v Speaker 3>billions of years of cosmic bombardment with the giant golf ball, right,

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<v Speaker 3>But Europa doesn't have that. You see this brilliant, bright

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<v Speaker 3>white sphere heavily scarred with these incredibly long, dark, sort

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<v Speaker 3>of reddish brown fractures.

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<v Speaker 2>It literally looks like a cracked eggshell floating in the void.

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<v Speaker 3>That's a perfect way to describe it, and the lack

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<v Speaker 3>of craters tells us something vital. The surface is young,

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<v Speaker 3>it is constantly refreshing and renewing itself.

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<v Speaker 2>Because beneath that cracked shell, Europa is hiding a massive

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<v Speaker 2>global ocean of liquid water.

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<v Speaker 3>And not just a subterranean lake either, right.

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<v Speaker 2>Not a slushy aquifer. It is a deep, earning ocean

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<v Speaker 2>that wraps around the entire Moon.

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<v Speaker 3>Which brings us to why astrobiologists are just so obsessed

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<v Speaker 3>with this place. It comes down to what we consider

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<v Speaker 3>the holy trinity for habitable environments.

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<v Speaker 2>The three non negotiable ingredients for life.

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<v Speaker 3>Exactly, if you are looking for life as we know it,

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<v Speaker 3>first you need liquid water, not ice. Now, ice is rigid,

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<v Speaker 3>it traps molecules and not vapor because that's too diffuse.

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<v Speaker 3>You need a liquid medium where molecules can float, interact, bond.

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<v Speaker 2>It's the universal solvent. Right.

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<v Speaker 3>Second, you need the right chemistry. You need the building blocks.

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<v Speaker 2>Like carbon, hydrogen, nitrogen.

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<v Speaker 3>Oxygen, phosphorus, and sulfur. Thechnops elements chnops I always like

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<v Speaker 3>that acronym.

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<v Speaker 2>Yeah, And the assumption is that those elements are present

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<v Speaker 2>on the rocky sea floor of Europa, right.

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<v Speaker 3>That's the running theory.

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<v Speaker 2>Yes, so the water is in direct contact with a

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<v Speaker 2>silicate mantle, meaning the ocean is likely dissolving minerals and salts,

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<v Speaker 2>creating this rich chemical soup.

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<v Speaker 3>That direct contact is so crucial. It's what differentiates Europa

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<v Speaker 3>from a moon like say Gannymat.

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<v Speaker 2>Because Gannymat has an ocean too.

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<v Speaker 3>It does, but Gannymat's ocean is likely sandwiched between two

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<v Speaker 3>layers of impenetrable ice.

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<v Speaker 2>Oh, so it never touches the rock exactly.

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<v Speaker 3>Europa's ocean is interacting with the rock. But that brings

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<v Speaker 3>us to the third crucial ingredient for life, energy and

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<v Speaker 3>energy source. You need something to drive the chemical reactions

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<v Speaker 3>to take those basic elements and force them to assemble

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<v Speaker 3>into complex organic molecules.

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<v Speaker 2>And on Earth, I mean, the vast majority of our

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<v Speaker 2>biosphere relies on the Sun.

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<v Speaker 3>Photosynthesis.

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<v Speaker 2>Plants use the Sun, and then everything else basically eats

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<v Speaker 2>the plants. Yeah, but out in the Jupiter system, the

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<v Speaker 2>Sun is just like a bright star in the sky.

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<v Speaker 3>It's incredibly faint out there.

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<v Speaker 2>The solar radiation is just a fraction of what we

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<v Speaker 2>get here on Earth. So the Sun isn't providing the

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<v Speaker 2>energy for life.

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<v Speaker 3>And it certainly isn't providing the heat to keep a

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<v Speaker 3>global ocean from freezing.

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<v Speaker 2>Solid because space is unimaginably So how does a moon

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<v Speaker 2>floating hundreds of millions of miles away from the Sun

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<v Speaker 2>out in the freezing depths of the outer Solar System

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<v Speaker 2>actually managed to stay liquid?

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<v Speaker 3>Well, if Europa were just floating out there in isolation,

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<v Speaker 3>it would be a solid, inert block of ice all

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<v Speaker 3>the way through to its.

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<v Speaker 2>Core, just a giant ice cube.

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<v Speaker 3>Literally. The surface temperature at europe A's equator never gets

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<v Speaker 3>warmer than about minus two hundred and sixty degrees fahrenheit. Wow,

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<v Speaker 3>And at the Poles it drops down to an agonizing

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<v Speaker 3>minus three hundred and seventy degrees.

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<v Speaker 2>That is just I can't even comprehend that level of cold.

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<v Speaker 3>Any ambient heat from its formation of billions of years

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<v Speaker 3>ago should have radiated away into the vacuum of space

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<v Speaker 3>a long time ago.

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<v Speaker 2>So the heat keeping that ocean liquid has to be

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<v Speaker 2>continually generated from the inside out.

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<v Speaker 3>Exactly. It's the engine keeping Europa alive.

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<v Speaker 2>And that engine is driven entirely by gravity. Like we

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<v Speaker 2>have to picture the sheer, overwhelming gravitational pull of Jupiter.

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<v Speaker 3>Jupiter is a monster. It's three hundred and eighteen times

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<v Speaker 3>more massive than Earth.

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<v Speaker 2>Right, So Jupiter's gravity it completely dictates the physical reality

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<v Speaker 2>of its moons.

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<v Speaker 3>And Europa is caught in this very specific gravitational dance.

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<v Speaker 3>It is in what we call an orbital resonance with

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<v Speaker 3>two of Jupiter's other large moons, Io and Ganymede.

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<v Speaker 2>Orbital resonance, so they are synced up.

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<v Speaker 3>Yes, for every one time Ganymate orbits Jupiter Europa orbits

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<v Speaker 3>twice and Io orbits four times.

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<v Speaker 2>Okay, the four to two to one resonance.

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<v Speaker 3>Right, This laplace resonance forces Europa's orbit to be elliptical

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<v Speaker 3>or oval shaped rather than a perfect circle.

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<v Speaker 2>So the distance between Europa and Jupiter is constantly changing exactly.

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<v Speaker 3>Sometimes Europa swings in relatively close to the gas giant,

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<v Speaker 3>and other times it swings much further out, And.

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<v Speaker 2>That changing distance means a constantly changing gravitational pull.

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<v Speaker 3>Yes, When Europa makes its closest approach to Jupiter, known

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<v Speaker 3>as the parajove, Jupiter's gravity pulls on the Moon with

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<v Speaker 3>immense force.

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<v Speaker 2>It literally stretches the Moon, doesn't it.

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<v Speaker 3>It does. The solid rock of the mantle and the

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<v Speaker 3>thick ice shell actually bulge outward toward Jupiter by as

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<v Speaker 3>much as thirty meters.

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<v Speaker 2>It's like one hundred feet solid rock and ice bulging

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<v Speaker 2>up one hundred feet right.

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<v Speaker 3>And then as Europa swings further away in its orbit,

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<v Speaker 3>reaching up a jove, that gravitational grip relaxes.

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<v Speaker 2>And the moon shape settles back down exactly. So an

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<v Speaker 2>entire planetary body is being physically stretched and compressed one

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<v Speaker 2>hundred feet up and one hundred feet down every single orbit.

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<v Speaker 3>Which takes about three and a half earthdays.

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<v Speaker 2>That is insane. Just think about the mechanical stress of that.

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<v Speaker 2>I mean, it's like, okay, if you take a thick

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<v Speaker 2>metal paper clip, Okay, and you just hold it, nothing happens. Yeah,

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<v Speaker 2>But if you start bending it back and forth rapidly

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<v Speaker 2>and repeatedly.

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<v Speaker 3>The metal right at the bend gets hot.

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<v Speaker 2>Right, you can actually burn your fingers on it. The

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<v Speaker 2>friction of the metallic crystalline structure grinding against itself generates internal.

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<v Speaker 3>Heat that translates perfectly to a planetary scale.

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<v Speaker 2>So Jupiter is basically bending Europa like a paper clip.

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<v Speaker 3>The continuous squeezing and stretching is bending that planetary paper clip.

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<v Speaker 3>The massive amounts of rock deep in the Moon's silicate

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<v Speaker 3>mantle are grinding against each other, and.

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<v Speaker 2>The layers of deep ice are flexing too.

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<v Speaker 3>Yes, all of that incredible internal friction generates an enormous

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<v Speaker 3>amount of thermal energy deep within the Moon's interior tidal heating,

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<v Speaker 3>exactly tidal heating. It is a ceaseless, powerful geologic engine.

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<v Speaker 2>So this immense heat is radiating outward from the rocky core.

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<v Speaker 2>It hits the bottom of the frozen crust, melting it

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<v Speaker 2>from the.

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<v Speaker 3>Inside out, creating this massive, warm global ocean hidden in

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<v Speaker 3>the dark.

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<v Speaker 2>Right, the ocean exists in this state of tension. Its

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<v Speaker 2>sandwiched between the hot, volcanically active rocky seafloor below and

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<v Speaker 2>the frozen ice shell above. Yes, but wait, I have

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<v Speaker 2>to push back here. If there is so much heat

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<v Speaker 2>being generated inside this moon, enough to melt a volume

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<v Speaker 2>of water twice the size of all of Earth's oceans combined,

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<v Speaker 2>why doesn't the heat just melt the rest of the ice.

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<v Speaker 3>That's a great question.

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<v Speaker 2>Why is the outside still frozen solid? It seems like

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<v Speaker 2>it should.

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<v Speaker 3>Just be a water world because you are witnessing a

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<v Speaker 3>stalemate between two extreme thermodynamic forces.

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<v Speaker 2>Okay, stalemate.

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<v Speaker 3>You have the intense, constant tidal heating pushing up from

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<v Speaker 3>the seafloor, but you also have the brutal, unforgiving cold

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<v Speaker 3>of deep space pressing down from above.

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<v Speaker 2>Right, The minus two hundred and sixty.

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<v Speaker 3>Degrees thorodynamics dictates that heat will always move to where

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<v Speaker 3>it is cold. The thermal energy from the ocean is

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<v Speaker 3>constantly trying to bleed away into the vacuum of space.

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<v Speaker 2>And as a result, the outermost layer of the water freezes.

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<v Speaker 3>Creating the thick ice shell.

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<v Speaker 2>And once that ice forms, it changes the dynamic Right.

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<v Speaker 2>Because ice is a remarkably good insulator.

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<v Speaker 3>It acts as planetary armour. The ice shell traps the

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<v Speaker 3>remaining heat inside, preventing the rest of the ocean from

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<v Speaker 3>freezing solid. Wow, it is a delicate equilibrium. The ice

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<v Speaker 3>shell is estimated to be anywhere from ten to fifteen

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<v Speaker 3>miles thick fifteen miles, perhaps even thicker in certain regions,

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<v Speaker 3>depending on the localized heat flow from the mantle.

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<v Speaker 2>So we have this incredible, potentially life bearing ocean, complete

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<v Speaker 2>with the care, chemistry, and the energy needed to sustain

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<v Speaker 2>a biosphere. Yes, but it is locked inside a planetary

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<v Speaker 2>vault with walls made of miles thick rock hard.

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<v Speaker 3>Ice, which creates an absolute nightmare for planetary scientists and engineers.

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<v Speaker 2>I can imagine, how do you sample an ocean you

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<v Speaker 2>can't reach. We don't have the technology to pack a

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<v Speaker 2>fifteen mile long drill onto a rocket, No, we definitely don't,

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<v Speaker 2>and then fly it to Jupiter, land it softly on

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<v Speaker 2>the ice, and power it for years as it grinds

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<v Speaker 2>through cryogenic ice. That's just science fiction.

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<v Speaker 3>Completely, which is exactly why the scientific community has spent

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<v Speaker 3>the last few decades clinging to the dream of the shortcut.

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<v Speaker 2>The shortcut. Okay, let's unpack this. What was the assumption here?

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<v Speaker 3>The shortcut was a highly optimistic yet theoretically grounded assumption

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<v Speaker 3>about the mechanics of the ice shell, hoping.

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<v Speaker 2>We wouldn't need a gargantuan drilling operation. Right.

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<v Speaker 3>The hope was that the ocean was actively doing the

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<v Speaker 3>hard work for us, that the ocean might be migrating

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<v Speaker 3>up to meet us.

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<v Speaker 2>Because we're looking at a surface covered in thousands of

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<v Speaker 2>miles of caaotic fractures, ridges.

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<v Speaker 3>And bands, the shell is clearly active.

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<v Speaker 2>So the theory was that deep ocean water could travel

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<v Speaker 2>upward through narrow vertical fractures in.

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<v Speaker 3>The ice geological features known as dikes, yes.

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<v Speaker 2>And that this pressurized water would pool in shallow reservoirs

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<v Speaker 2>much closer to the surface, like maybe just a few

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<v Speaker 2>dozen meters down.

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<v Speaker 3>That was the dream. The scientific framework for this is cry.

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<v Speaker 2>Volcanism ice vulcanism.

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<v Speaker 3>Exactly to conceptualize it, scientists naturally look at the geologic

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<v Speaker 3>processes we understand.

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<v Speaker 2>Best traditional vulcanism.

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<v Speaker 3>Here on Earth, right beneath our feet, we have incredibly hot,

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<v Speaker 3>pressurized molten rock magma moving through the lithosphere.

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<v Speaker 2>And when this magma encounters weak points, faults or tectonic

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<v Speaker 2>fractures in the Earth's crust.

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<v Speaker 3>The immense lithostatic pressure forces it upward. Sometimes it erupts

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<v Speaker 3>explosively on the surface as.

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<v Speaker 2>Lava, or it pools in shallow magma chambers just below

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<v Speaker 2>the crust, creating geothermal anomalies.

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<v Speaker 3>Exactly, cry vulcanism takes that entire Earth based plumbing system

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<v Speaker 3>and applies it to an ice world.

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<v Speaker 2>So instead of molten silicate rock moving through a rocky

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<v Speaker 2>granite crust, you have liquid water moving through cracks in

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<v Speaker 2>a solid water ice crust.

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<v Speaker 3>Yes, the deep ocean is highly pressurized by the weight

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<v Speaker 3>of the.

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<v Speaker 2>Ice above it, the ice shell flexes, a crack opens

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<v Speaker 2>up at the bottom, and that pressure squeezes the liquid

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<v Speaker 2>water up into the fracture.

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<v Speaker 3>That was the prevailing model for a long time. If

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<v Speaker 3>cryovulcanism operates on Europa with the same fundamental mechanics as

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<v Speaker 3>vulcanism on Earth, you would expect these vertical dikes to

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<v Speaker 3>act as natural.

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<v Speaker 2>Pipelines, continuously ferrying deep, mineral rich ocean water up into

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<v Speaker 2>shallow pockets just beneath the surface.

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<v Speaker 3>Or even erupting onto the surface to create the smooth,

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<v Speaker 3>renewed planes we see in the orbital imagery.

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<v Speaker 2>I mean, this would be the ultimate game changer for exploration.

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<v Speaker 2>If this shortcut exists, future space missions wouldn'tne a fifteen

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<v Speaker 2>mile drill.

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<v Speaker 3>They could simply use ground penetrating radar from orbit to

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<v Speaker 3>map out these shallow pockets.

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<v Speaker 2>Right then, you land a relatively small, simple probe equipped

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<v Speaker 2>with like a thermal melt probe.

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<v Speaker 3>You melt through maybe ten, twenty or fifty feet of ice.

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<v Speaker 2>And suddenly you are sampling the deep ocean. You're tasting

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<v Speaker 2>the exact chemical environment where life might be thriving without

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<v Speaker 2>having to breach the primary fifteen mile vault.

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<v Speaker 3>It was an incredibly elegant solution to an impossible engineering problem. Look, but,

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<v Speaker 3>as we often find in planetary science, mapping the mechanics

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<v Speaker 3>of one planet directly onto another is fraught with peril.

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<v Speaker 2>I mean, wait, ice and liquid water are fundamentally different

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<v Speaker 2>materials from solid rock and molten lava.

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<v Speaker 3>Completely different.

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<v Speaker 2>Can we really assume they behave the same way under pressure?

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<v Speaker 3>No, we can't. They possess completely different thermodynamic properties, different densities,

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<v Speaker 3>and they transfer heat in entirely different ways.

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<v Speaker 2>And this is where the dream of the shortcut collides

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<v Speaker 2>with a massive, sobering reality check.

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<v Speaker 3>A major twenty twenty six study has completely dismantled the

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<v Speaker 3>system yeah.

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<v Speaker 2>Led by lejendro Oshaw, a planetary scientist at the Rutger

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<v Speaker 2>School of Arts and Sciences.

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<v Speaker 3>They finally ran the brutal, unfiltered physics on this concept.

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<v Speaker 2>Because they didn't want to rely on Earth based analogies anymore.

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<v Speaker 2>They wanted to know exactly what happens when liquid water

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<v Speaker 2>tries to force its way through deep.

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<v Speaker 3>Space ice, and their methodology was focused entirely on the

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<v Speaker 3>journey itself. The core question they tackled was whether liquid

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<v Speaker 3>water could realistically rise from Europa's deep, highly pressurized ocean,

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00:14:29.360 --> 00:14:32.480
<v Speaker 3>travel vertically through narrow fractures in the ice shell, and

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<v Speaker 3>reach the shallow subsurface without freezing solid along the way.

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<v Speaker 2>And to answer a question like that, you can't just

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<v Speaker 2>rely on telescope observations. You have to build the environment

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<v Speaker 2>in a computer.

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<v Speaker 3>They utilized advanced computational fluid dynamics to simulate the localized

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<v Speaker 3>physics of this upward journey, modeling.

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00:14:49.879 --> 00:14:52.840
<v Speaker 2>The pressure, the temperature gradient of the ice shell, the

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00:14:52.879 --> 00:14:54.799
<v Speaker 2>specific heat capacity of the water.

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<v Speaker 3>And the geometry of the fractures.

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<v Speaker 2>And in doing so they exposed a critical flaw in

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<v Speaker 2>the older models, the models that it generated so much optimism.

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<v Speaker 3>Yes, the previous models relied heavily on a mathematical simplification.

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<v Speaker 3>They treated the rising water as if it moved in

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<v Speaker 3>a laminar flow.

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<v Speaker 2>Laminar flow. Okay, let's make sure we have a vivid

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<v Speaker 2>picture of this, because it is the lynchpin of the

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<v Speaker 2>old theory. It is Laminar flow is smooth, It's highly orderly,

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<v Speaker 2>like if you turn on your kitchen fauce. It just

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<v Speaker 2>a tiny bit and the water glides out in this

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<v Speaker 2>perfect clear glass like cylinder where all the water molecules

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<v Speaker 2>are moving perfectly parallel to.

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<v Speaker 3>One another with no class currents or mixing.

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00:15:34.120 --> 00:15:35.840
<v Speaker 2>Right. That is laminar flow.

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<v Speaker 3>The old models effectively assumed that water from the deep

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<v Speaker 3>ocean would behave like that faucet. It would gently and

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<v Speaker 3>smoothly slide up these fractures.

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<v Speaker 2>In the ice, which sounds nice in theory.

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<v Speaker 3>In a laminar flow regime, the water maintains its thermal

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<v Speaker 3>energy relatively well because the fluid isn't mixing, so only

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<v Speaker 3>the very.

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<v Speaker 2>Outer layer of the water touches the freezing ice walls exactly.

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<v Speaker 3>It acts as an insulating buffer for the warmer water

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<v Speaker 3>in the center of the flow.

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00:16:02.559 --> 00:16:05.919
<v Speaker 2>But Ojcha's team realized there was a fundamental physics element

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<v Speaker 2>missing from those assumptions.

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00:16:07.279 --> 00:16:10.720
<v Speaker 3>Applying laminar flow to a highly pressurized extrusion event on

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<v Speaker 3>an active moon was a mathematically convenient, but physically impossible assumption.

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<v Speaker 2>Because space isn't to controlled laboratory. You can't expect millions

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00:16:19.840 --> 00:16:23.000
<v Speaker 2>of gallons of pressurized water to flow up a jagged,

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00:16:23.080 --> 00:16:26.600
<v Speaker 2>dynamic freezing pipe in a smooth straight line.

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<v Speaker 3>The older models were completely ignoring the chaotic, unpredictable nature

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<v Speaker 3>of fluid dynamics.

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<v Speaker 2>They were ignoring turbulence.

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<v Speaker 3>Purbulence dictates the reality of the flow. When you factor

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<v Speaker 3>in the intense pressures at the bottom of the ocean,

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<v Speaker 3>the narrow, jagged constraints of these tectonic fractures, and the

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00:16:43.679 --> 00:16:46.759
<v Speaker 3>immense vertical distance the water must traverse.

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<v Speaker 2>A gentle laminar stream is physically impossible.

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<v Speaker 3>The fluid dynamics simulations proved that the water wouldn't rise peacefully.

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<v Speaker 3>It would be injected into the fracture at high velocity,

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<v Speaker 3>resulting in violently turbulent flow.

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<v Speaker 2>And if the water is turbulent, the molecules aren't moving

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<v Speaker 2>in a straight parallel line anymore. The fluid is tearing

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<v Speaker 2>itself apart.

356
00:17:06.240 --> 00:17:09.160
<v Speaker 3>It is moving left and right, surging up and dropping down.

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00:17:09.319 --> 00:17:13.960
<v Speaker 2>It is swirling aggressively, creating massive eddies and vortices inside

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<v Speaker 2>the crack.

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00:17:14.640 --> 00:17:18.440
<v Speaker 3>Picture a raging whitewater river violently rushing through a narrow,

360
00:17:18.559 --> 00:17:22.000
<v Speaker 3>jagged slot canyon. Oh wow, Yeah, the water is crashing

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00:17:22.039 --> 00:17:25.640
<v Speaker 3>against the rock walls, folding over on itself, constantly churning

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00:17:25.680 --> 00:17:26.200
<v Speaker 3>and mixing.

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00:17:26.319 --> 00:17:29.599
<v Speaker 2>Now take that chaotic energy and place it inside a

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<v Speaker 2>vertical crack in Europa's ice shell.

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00:17:32.880 --> 00:17:36.599
<v Speaker 3>You have a churning, swirling mass of liquid water violently

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00:17:36.640 --> 00:17:39.480
<v Speaker 3>scraping and mixing against the walls of the fracture, and.

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00:17:39.720 --> 00:17:43.119
<v Speaker 2>We have to focus on the thermal reality of those walls.

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00:17:43.799 --> 00:17:46.400
<v Speaker 2>This isn't a rocky canyon in Arizona.

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00:17:45.880 --> 00:17:48.640
<v Speaker 3>No, And it isn't the relatively warm ice you'd find

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<v Speaker 3>in an Earth glacier either.

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00:17:50.279 --> 00:17:53.000
<v Speaker 2>This is deep space ice. As you move up through

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<v Speaker 2>the shell, the temperature of the ice drops precipitously, plunging

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<v Speaker 2>down toward that surface temperature of minus two hundred and

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<v Speaker 2>sixty degrees fair.

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<v Speaker 3>It is a cryogenic environment which triggers the fatal mechanism

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<v Speaker 3>that destroys the shortcut right catastrophic heat loss.

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<v Speaker 2>Yes.

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00:18:08.240 --> 00:18:11.240
<v Speaker 3>In our earlier laminar flow example, the water in the

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00:18:11.279 --> 00:18:14.440
<v Speaker 3>center was insulated, but in a turbulent flow there.

380
00:18:14.319 --> 00:18:16.519
<v Speaker 2>Is no center because it's constantly mixing.

381
00:18:16.920 --> 00:18:20.200
<v Speaker 3>The swirling motion constantly takes the relatively warm water from

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00:18:20.240 --> 00:18:23.359
<v Speaker 3>the interior of the crack and violently throws it outward,

383
00:18:23.440 --> 00:18:26.279
<v Speaker 3>smashing it directly against the freezing cryogenic walls.

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00:18:26.400 --> 00:18:29.599
<v Speaker 2>So the water rapidly surrenders its thermal energy into the

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00:18:29.599 --> 00:18:30.279
<v Speaker 2>surrounding ice.

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00:18:30.599 --> 00:18:34.279
<v Speaker 3>The rate of heat transfer is staggering, far faster than

387
00:18:34.319 --> 00:18:37.079
<v Speaker 3>any of the older simplified models had accounted for.

388
00:18:37.440 --> 00:18:41.720
<v Speaker 2>The water is rushing up, furiously, churning and rapidly harringing

389
00:18:41.799 --> 00:18:45.000
<v Speaker 2>its heat into the walls of the fracture. It cools

390
00:18:45.119 --> 00:18:48.599
<v Speaker 2>down at a phenomenal rate as it climbs towards the surface.

391
00:18:48.359 --> 00:18:52.039
<v Speaker 3>And this rapid cooling in a chaotic environment leads to

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00:18:52.119 --> 00:18:55.680
<v Speaker 3>a state of matter that dictates the final outcome super

393
00:18:55.720 --> 00:19:00.240
<v Speaker 3>cooling super cooling. It is a fascinating thermodynamic.

394
00:18:59.400 --> 00:19:01.920
<v Speaker 2>State because, as we generally assume that the instant water

395
00:19:01.960 --> 00:19:06.039
<v Speaker 2>reaches thirty two degrees fahrenheit or zero degree celsius. It

396
00:19:06.119 --> 00:19:08.440
<v Speaker 2>immediately transitions into a solid state.

397
00:19:08.880 --> 00:19:12.359
<v Speaker 3>Right, But the phase change from liquid to solid requires

398
00:19:12.359 --> 00:19:15.599
<v Speaker 3>a starting point, a nucleation site for the ice crystals

399
00:19:15.640 --> 00:19:16.359
<v Speaker 3>to begin forming.

400
00:19:16.440 --> 00:19:17.920
<v Speaker 2>And if it doesn't have one, if.

401
00:19:17.799 --> 00:19:21.359
<v Speaker 3>The water cools down rapidly enough, it can actually drop

402
00:19:21.400 --> 00:19:24.640
<v Speaker 3>below its standard freezing temperature and temporarily remain in a

403
00:19:24.640 --> 00:19:25.279
<v Speaker 3>liquid state.

404
00:19:25.559 --> 00:19:28.480
<v Speaker 2>This is super cooled liquid. We see this on Earth

405
00:19:28.559 --> 00:19:31.599
<v Speaker 2>under very specific conditions. Right. They like, if you leave

406
00:19:31.680 --> 00:19:34.559
<v Speaker 2>a perfectly sealed bottle of highly purified water in the

407
00:19:34.599 --> 00:19:37.359
<v Speaker 2>freezer just a little too long, you can pull it

408
00:19:37.359 --> 00:19:40.200
<v Speaker 2>out and it still looks completely liquid. It might be

409
00:19:40.240 --> 00:19:44.359
<v Speaker 2>like twenty five degrees fahrenheit, but it's flowing. However, the

410
00:19:44.440 --> 00:19:47.279
<v Speaker 2>moment you flick the bottle with your finger or twist

411
00:19:47.319 --> 00:19:49.160
<v Speaker 2>the cap and release the pressure.

412
00:19:48.880 --> 00:19:50.599
<v Speaker 3>You introduce a mechanical disturbance.

413
00:19:50.839 --> 00:19:54.839
<v Speaker 2>You provide a nucleation point, and the entire bottle flashes

414
00:19:54.880 --> 00:19:57.039
<v Speaker 2>into solid ice right in front of your eyes in

415
00:19:57.079 --> 00:19:58.279
<v Speaker 2>a matter of seconds.

416
00:19:58.519 --> 00:20:01.960
<v Speaker 3>The water in that bottle is is thermode dynamically unstable.

417
00:20:02.119 --> 00:20:04.680
<v Speaker 3>It desperately wants to freeze. It just needs a trigger.

418
00:20:04.839 --> 00:20:08.680
<v Speaker 2>Now apply that to Europa. The turbulent water rushing up

419
00:20:08.720 --> 00:20:12.400
<v Speaker 2>the fracture becomes deeply super cooled by the constant contact

420
00:20:12.400 --> 00:20:14.000
<v Speaker 2>with the cryogenic walls.

421
00:20:13.680 --> 00:20:18.440
<v Speaker 3>And in that violently churning, highly pressurized environment, there is

422
00:20:18.480 --> 00:20:21.920
<v Speaker 3>no shortage of mechanical disturbances or nucleation sites.

423
00:20:22.160 --> 00:20:25.720
<v Speaker 2>The ice walls themselves provide infinite points for crystallization to begin.

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00:20:25.920 --> 00:20:28.319
<v Speaker 3>So the supercooled water starts to flash freeze.

425
00:20:28.359 --> 00:20:31.119
<v Speaker 2>But because it's moving so violently, it doesn't freeze into

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00:20:31.160 --> 00:20:33.799
<v Speaker 2>a single smooth sheet of solid ice from the outside in.

427
00:20:34.240 --> 00:20:37.160
<v Speaker 3>It forms something entirely different. It forms frizil ice.

428
00:20:37.400 --> 00:20:39.200
<v Speaker 2>For zil ice, that's a specific term.

429
00:20:39.279 --> 00:20:42.240
<v Speaker 3>Yes, frazil ice is the nail in the coffin for

430
00:20:42.319 --> 00:20:44.599
<v Speaker 3>the cryovulcanism theory on Europa.

431
00:20:44.640 --> 00:20:45.480
<v Speaker 2>What exactly is it?

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00:20:45.599 --> 00:20:50.279
<v Speaker 3>When this highly agitated supercooled fluid begins to freeze, it

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00:20:50.359 --> 00:20:55.119
<v Speaker 3>instantly forms billions of tiny needle like microscopic ice crystals

434
00:20:55.359 --> 00:20:57.640
<v Speaker 3>suspended directly within the liquid column.

435
00:20:57.799 --> 00:21:01.640
<v Speaker 2>So it stops being a fluid and turn into a thick, gritty,

436
00:21:01.839 --> 00:21:04.319
<v Speaker 2>abrasive slush exactly.

437
00:21:03.880 --> 00:21:07.799
<v Speaker 3>The consistency of slush. And as the turbulent flow continues

438
00:21:07.839 --> 00:21:10.359
<v Speaker 3>to bleed heat into the walls, more and more of

439
00:21:10.400 --> 00:21:13.680
<v Speaker 3>these frizil ice crystals precipitate out of the liquid, so.

440
00:21:13.680 --> 00:21:15.880
<v Speaker 2>The concentration of ice crystal sky rockets.

441
00:21:16.079 --> 00:21:19.640
<v Speaker 3>They begin to clump and stick together, increasing the viscosity

442
00:21:19.640 --> 00:21:22.960
<v Speaker 3>of the fluid. More importantly, they aggressively stick to the

443
00:21:23.000 --> 00:21:25.960
<v Speaker 3>incredibly cold, jagged walls of the fracture.

444
00:21:26.079 --> 00:21:29.240
<v Speaker 2>They start to accumulate. They're actively paving the inside of

445
00:21:29.240 --> 00:21:32.440
<v Speaker 2>the crack with sticky slush, narrowing the pathway by the second.

446
00:21:32.559 --> 00:21:35.319
<v Speaker 3>It's like trying to pump rapidly set in concrete through

447
00:21:35.319 --> 00:21:35.799
<v Speaker 3>a pipe.

448
00:21:35.839 --> 00:21:37.759
<v Speaker 2>The more it flows, the thicker it gets, until it

449
00:21:37.839 --> 00:21:38.640
<v Speaker 2>chokes itself out.

450
00:21:38.759 --> 00:21:41.880
<v Speaker 3>The timeline generated by Oshaw's computer simulations is the most

451
00:21:41.880 --> 00:21:43.119
<v Speaker 3>sobering aspect of the.

452
00:21:43.039 --> 00:21:44.960
<v Speaker 2>Study because of how fast this happens.

453
00:21:45.079 --> 00:21:48.200
<v Speaker 3>Given the rapid turbulence driven heat loss and the explosive

454
00:21:48.240 --> 00:21:52.480
<v Speaker 3>formation of Frazil ice, these vertical dikes simply cannot sustain flow.

455
00:21:52.880 --> 00:21:55.680
<v Speaker 2>The models demonstrated that these narrow cracks wouldn't stay open

456
00:21:55.720 --> 00:21:57.839
<v Speaker 2>for years or months or even weeks.

457
00:21:57.920 --> 00:22:01.720
<v Speaker 3>They would violently freeze shut within a matter of mere hours.

458
00:22:01.759 --> 00:22:05.400
<v Speaker 2>Hours a massive Techti fracture rips open at the bottom

459
00:22:05.400 --> 00:22:09.160
<v Speaker 2>of the ice shell. The pressurized liquid ocean rushes in,

460
00:22:09.480 --> 00:22:10.799
<v Speaker 2>hoping to find a path.

461
00:22:10.559 --> 00:22:12.799
<v Speaker 3>To the surface, it immediately becomes turbulent.

462
00:22:13.119 --> 00:22:16.400
<v Speaker 2>It's super cools. The Frazil ice forms a dense slush,

463
00:22:16.480 --> 00:22:19.839
<v Speaker 2>and within a few hours the entire fracture cements itself shut.

464
00:22:19.960 --> 00:22:22.119
<v Speaker 3>The fluid never even gets close to the surface.

465
00:22:22.440 --> 00:22:25.799
<v Speaker 2>Nature essentially slams the vault door shut the moment the

466
00:22:25.799 --> 00:22:26.960
<v Speaker 2>ocean tries to escape.

467
00:22:27.279 --> 00:22:31.039
<v Speaker 3>The physics of the environment make the process brutally self defeating.

468
00:22:31.680 --> 00:22:34.519
<v Speaker 3>The very act of the pressurized water forcing its way

469
00:22:34.599 --> 00:22:38.599
<v Speaker 3>upward generates the fluid turbulence that rapidly seals its own

470
00:22:38.640 --> 00:22:39.480
<v Speaker 3>exit pathway.

471
00:22:39.839 --> 00:22:43.400
<v Speaker 2>The mechanics of the ice shell actively prevent cryovulcanism from

472
00:22:43.440 --> 00:22:45.759
<v Speaker 2>functioning the way vulcanism functions.

473
00:22:45.359 --> 00:22:46.359
<v Speaker 3>On Earth exactly.

474
00:22:46.519 --> 00:22:48.880
<v Speaker 2>Okay, but I have a question. Looking at the scale

475
00:22:48.920 --> 00:22:53.039
<v Speaker 2>of Europa, a moon subjected to the immense gravitational torture

476
00:22:53.079 --> 00:22:55.160
<v Speaker 2>of Jupiter. Couldn't we just assume the.

477
00:22:55.160 --> 00:22:57.160
<v Speaker 3>Cracks are bigger, You mean, wider fractures?

478
00:22:57.519 --> 00:23:01.400
<v Speaker 2>Yeah, if a narrow pipe freezes shut in hours, what

479
00:23:01.480 --> 00:23:05.000
<v Speaker 2>if the fracture is a massive gaping chasm in the ice.

480
00:23:05.559 --> 00:23:07.759
<v Speaker 2>Surely a massive fracture could survive the cold.

481
00:23:07.920 --> 00:23:10.359
<v Speaker 3>It's the logical next step in the hypothesis.

482
00:23:10.559 --> 00:23:14.440
<v Speaker 2>Right, If the pathways wide enough, wouldn't sheer volume allow

483
00:23:14.480 --> 00:23:16.640
<v Speaker 2>at least some of the water in the center to

484
00:23:16.640 --> 00:23:19.720
<v Speaker 2>survive the journey and pool near the surface before the

485
00:23:19.839 --> 00:23:21.119
<v Speaker 2>edge is managed to freeze.

486
00:23:21.279 --> 00:23:25.160
<v Speaker 3>Oshaw's team rigorously tested that exact scenario. They adjusted the

487
00:23:25.200 --> 00:23:28.920
<v Speaker 3>simulations to account for significantly wider fractures, pushing the boundaries

488
00:23:28.960 --> 00:23:32.160
<v Speaker 3>of what is geologically plausible for the ice shell. The

489
00:23:32.200 --> 00:23:36.240
<v Speaker 3>results were incredibly stubborn. Even under the most idealized generous

490
00:23:36.279 --> 00:23:39.839
<v Speaker 3>conditions maximizing the width of the fractures, the upward migration

491
00:23:40.000 --> 00:23:40.720
<v Speaker 3>still fails.

492
00:23:40.799 --> 00:23:44.079
<v Speaker 2>Wait, really, why does scaling up the width fail to

493
00:23:44.119 --> 00:23:45.359
<v Speaker 2>solve the thermal problem?

494
00:23:45.559 --> 00:23:48.839
<v Speaker 3>Because fluid turbulence does not scale linearly in a way

495
00:23:48.839 --> 00:23:49.799
<v Speaker 3>that protects the heat.

496
00:23:50.039 --> 00:23:51.240
<v Speaker 2>Okay, unpack that for me.

497
00:23:51.480 --> 00:23:54.880
<v Speaker 3>Yes, a much wider fracture possesses a greater volume of water,

498
00:23:55.400 --> 00:23:58.720
<v Speaker 3>and technically it takes slightly longer to freeze completely shut

499
00:23:58.759 --> 00:24:01.759
<v Speaker 3>compared to a narrow crack. Makes sense, But the chaotic

500
00:24:01.880 --> 00:24:05.680
<v Speaker 3>energy of the turbulence scales up alongside the volume. The

501
00:24:05.759 --> 00:24:09.079
<v Speaker 3>violent mixing continues to throw the interior heat against the

502
00:24:09.119 --> 00:24:10.119
<v Speaker 3>cryogenic walls.

503
00:24:10.319 --> 00:24:13.240
<v Speaker 2>Ah, so it's just mixing even more aggressively.

504
00:24:12.920 --> 00:24:16.640
<v Speaker 3>To successfully transport enough liquid water to the upper crust

505
00:24:16.920 --> 00:24:19.880
<v Speaker 3>to carve out the vast geological features we observe on

506
00:24:19.920 --> 00:24:24.440
<v Speaker 3>the surface, the massive lenticularate, the sprawling chaotic terrain, the

507
00:24:24.480 --> 00:24:27.119
<v Speaker 3>fractures would need to be unrealistically massive.

508
00:24:27.279 --> 00:24:30.519
<v Speaker 2>They would require a width or a frequency that simply

509
00:24:30.640 --> 00:24:34.640
<v Speaker 2>defies the structural integrity and the physical limits of Europa's

510
00:24:34.680 --> 00:24:37.480
<v Speaker 2>ice shell exactly. It's like a battle of thermal mass

511
00:24:37.559 --> 00:24:41.319
<v Speaker 2>versus environmental hostility. Like if you take a standard garden hose,

512
00:24:41.440 --> 00:24:43.640
<v Speaker 2>fill it with warm water and snak it through a

513
00:24:43.640 --> 00:24:47.759
<v Speaker 2>frozen snowbank while violently shaking it, the water freezes almost instantly.

514
00:24:48.119 --> 00:24:50.960
<v Speaker 2>If you upgrade to a massive, high volume fire hose

515
00:24:50.960 --> 00:24:53.559
<v Speaker 2>and do the same thing, the sheer volume means more

516
00:24:53.599 --> 00:24:56.519
<v Speaker 2>water gets through initially, But if the walls of that

517
00:24:56.559 --> 00:24:59.160
<v Speaker 2>fire hose are minus two hundred degrees and the water

518
00:24:59.240 --> 00:25:02.319
<v Speaker 2>inside is churned violently, that fire hose is still going

519
00:25:02.359 --> 00:25:04.880
<v Speaker 2>to freeze solid before the water can establish a sustained

520
00:25:04.880 --> 00:25:05.680
<v Speaker 2>long term flow.

521
00:25:05.839 --> 00:25:09.920
<v Speaker 3>The cyogenic environment is just too overwhelming. The thermodynamic reality

522
00:25:10.000 --> 00:25:11.640
<v Speaker 3>is absolute.

523
00:25:11.039 --> 00:25:13.559
<v Speaker 2>So no matter how much water you pump, the cold

524
00:25:13.599 --> 00:25:16.119
<v Speaker 2>walls and the chaotic slow are going to freeze its

525
00:25:16.160 --> 00:25:18.160
<v Speaker 2>solid before it reaches the other end.

526
00:25:18.519 --> 00:25:21.559
<v Speaker 3>The ice shell is too thick, the ambient temperature is

527
00:25:21.599 --> 00:25:24.599
<v Speaker 3>too low, and the fluid dynamics are too chaotic for

528
00:25:24.680 --> 00:25:28.200
<v Speaker 3>any localized volume of deep ocean water to punch its

529
00:25:28.240 --> 00:25:30.799
<v Speaker 3>way through to the surface without surrendering all of its

530
00:25:30.839 --> 00:25:33.039
<v Speaker 3>heat and freezing solid in the attempt.

531
00:25:33.200 --> 00:25:36.759
<v Speaker 2>This realization forces us into a very uncomfortable corner regarding

532
00:25:36.799 --> 00:25:40.680
<v Speaker 2>our maps of Europa. It does because planetary geologists have

533
00:25:40.720 --> 00:25:45.240
<v Speaker 2>spent decades analyzing the images from the Galilee emission. We

534
00:25:45.279 --> 00:25:49.000
<v Speaker 2>see vast regions of chaotic terrain where the ice looks

535
00:25:49.000 --> 00:25:52.319
<v Speaker 2>like it has been shattered, melted, and refrozen into massive,

536
00:25:52.440 --> 00:25:53.359
<v Speaker 2>jagged blocks.

537
00:25:53.480 --> 00:25:56.119
<v Speaker 3>We see these features that unequivocally look like they are

538
00:25:56.200 --> 00:25:59.119
<v Speaker 3>formed by liquid water interacting with the shallow crust.

539
00:25:59.279 --> 00:26:03.119
<v Speaker 2>In fact, based on radar and gravitational data, many scientists

540
00:26:03.160 --> 00:26:05.359
<v Speaker 2>are heavily invested in the idea that there are distinct

541
00:26:05.519 --> 00:26:08.119
<v Speaker 2>shallow lenses of liquid water trapped in the ice just

542
00:26:08.160 --> 00:26:11.240
<v Speaker 2>below the surface right now. Yes, But if OSHA's physics

543
00:26:11.240 --> 00:26:14.759
<v Speaker 2>are correct and the deep ocean absolutely cannot make the

544
00:26:14.839 --> 00:26:18.680
<v Speaker 2>vertical journey, where did that shallow water come from?

545
00:26:18.880 --> 00:26:22.039
<v Speaker 3>This leads to the most critical and perhaps most disappointing

546
00:26:22.119 --> 00:26:26.839
<v Speaker 3>astrobiological consequence of the study, the concept of the false hope.

547
00:26:26.880 --> 00:26:29.359
<v Speaker 2>The false hope of shallow reservoirs.

548
00:26:29.519 --> 00:26:32.400
<v Speaker 3>If we identify pockets of liquid water residing in the

549
00:26:32.440 --> 00:26:36.480
<v Speaker 3>shallow subsurface of Europa, the physics dictate that they almost

550
00:26:36.519 --> 00:26:39.599
<v Speaker 3>certainly did not originate from the deep global ocean.

551
00:26:39.720 --> 00:26:41.640
<v Speaker 2>If they didn't migrate up from the bottom, the only

552
00:26:41.720 --> 00:26:45.039
<v Speaker 2>logical conclusion is that they were generated right there inside

553
00:26:45.079 --> 00:26:46.200
<v Speaker 2>the upper layers of the crust.

554
00:26:46.440 --> 00:26:49.640
<v Speaker 3>Precisely the conclusion we are forced to draw. The alternative

555
00:26:49.640 --> 00:26:53.720
<v Speaker 3>origin mechanism is localized heating and melting, occurring entirely within

556
00:26:53.759 --> 00:26:56.039
<v Speaker 3>the confined matrix of the ice shell itself.

557
00:26:56.079 --> 00:26:58.599
<v Speaker 2>But how do you generate enough thermal energy to melt

558
00:26:58.759 --> 00:27:03.319
<v Speaker 2>massive pockets of liquid water entirely within a cryogenic ice shell,

559
00:27:03.799 --> 00:27:06.079
<v Speaker 2>completely isolated from the hot, rocky core.

560
00:27:06.400 --> 00:27:09.400
<v Speaker 3>We return to the primary engine, tidal heating from Jupiter.

561
00:27:09.640 --> 00:27:13.319
<v Speaker 3>The gravitational squeezing and stretching from Jupiter doesn't just affect

562
00:27:13.359 --> 00:27:17.039
<v Speaker 3>the rocky mantle, it flexes the entire fifteen mile thick

563
00:27:17.079 --> 00:27:17.680
<v Speaker 3>ice shell.

564
00:27:18.079 --> 00:27:21.319
<v Speaker 2>As the Moon orbits. The ice is subjected to immense

565
00:27:21.400 --> 00:27:25.319
<v Speaker 2>tectonic stress. It bends, it shears, and it grinds against

566
00:27:25.359 --> 00:27:27.039
<v Speaker 2>itself along massive fault.

567
00:27:26.759 --> 00:27:30.559
<v Speaker 3>Lines, and in certain concentrated areas, perhaps where the ice

568
00:27:30.640 --> 00:27:34.880
<v Speaker 3>is structurally deformed, the mechanical friction of the ice aggressively

569
00:27:34.920 --> 00:27:39.599
<v Speaker 3>grinding against itself sheer heating can generate enough localized thermal

570
00:27:39.720 --> 00:27:43.000
<v Speaker 3>energy to literally melt the surrounding ice in situ.

571
00:27:43.200 --> 00:27:45.880
<v Speaker 2>So the mechanical friction melts the ice right where it sits.

572
00:27:46.240 --> 00:27:49.000
<v Speaker 2>It's like it's the planetary equivalent of vigorously rubbing your

573
00:27:49.000 --> 00:27:50.599
<v Speaker 2>hands together when you're out in the cold.

574
00:27:50.680 --> 00:27:51.680
<v Speaker 3>That's exactly what it is.

575
00:27:51.799 --> 00:27:54.599
<v Speaker 2>The friction generates a small pocket of heat right between

576
00:27:54.599 --> 00:27:57.839
<v Speaker 2>your palms, entirely independent of your body's core temperature. Right

577
00:27:58.079 --> 00:28:01.519
<v Speaker 2>so youru rope's crust is constantly rubbing together, generating enough

578
00:28:01.519 --> 00:28:04.880
<v Speaker 2>friction to melt localized pockets of slush and liquid water

579
00:28:05.240 --> 00:28:06.799
<v Speaker 2>miles above the actual ocean.

580
00:28:07.160 --> 00:28:11.279
<v Speaker 3>It creates a shallow, isolated reservoir of liquid and to

581
00:28:11.359 --> 00:28:14.559
<v Speaker 3>a remote sensing instrument like a radar sander looking down

582
00:28:14.599 --> 00:28:17.839
<v Speaker 3>from a spacecraft in orbit, a pocket of liquid water

583
00:28:18.000 --> 00:28:20.440
<v Speaker 3>simply registers as a pocket of liquid water.

584
00:28:20.839 --> 00:28:24.039
<v Speaker 2>But the distinction between those two origins is an absolute

585
00:28:24.039 --> 00:28:27.559
<v Speaker 2>heartbreak for anyone designing a mission to find life. It

586
00:28:27.640 --> 00:28:30.039
<v Speaker 2>completely changes the value of the target.

587
00:28:30.160 --> 00:28:33.359
<v Speaker 3>It alters the astrobiological potential of that water from a

588
00:28:33.400 --> 00:28:35.759
<v Speaker 3>prime target to a virtually sterile puddle.

589
00:28:35.960 --> 00:28:40.559
<v Speaker 2>Because if we go back to the holy trinity of life, water, chemistry,

590
00:28:40.599 --> 00:28:44.880
<v Speaker 2>and energy, we know life needs the complex, nutrient rich

591
00:28:44.960 --> 00:28:47.799
<v Speaker 2>chemistry that is only happening down in the deep ocean,

592
00:28:48.160 --> 00:28:51.720
<v Speaker 2>where the water is actively dissolving minerals from the rocky seafloor.

593
00:28:52.000 --> 00:28:54.039
<v Speaker 3>That is where the hydrothermal vents would be. That is

594
00:28:54.079 --> 00:28:56.039
<v Speaker 3>where the organic building blocks are churning.

595
00:28:56.359 --> 00:28:59.000
<v Speaker 2>If a space probe samples a shallow puddle that just

596
00:28:59.119 --> 00:29:03.079
<v Speaker 2>melted locally, it's completely disconnected from the deep ocean environment.

597
00:29:03.559 --> 00:29:07.759
<v Speaker 2>If a future multi billion dollar space probe lands on Europa,

598
00:29:07.960 --> 00:29:10.359
<v Speaker 2>manages to melt its way through fifty feet of ice

599
00:29:10.759 --> 00:29:14.559
<v Speaker 2>and successfully samples one of these shallow reservoirs, and it

600
00:29:14.599 --> 00:29:17.440
<v Speaker 2>turns out that reservoir was just created by mechanical friction

601
00:29:18.000 --> 00:29:21.039
<v Speaker 2>melting a block of pure sterile ice, it is.

602
00:29:21.000 --> 00:29:24.960
<v Speaker 3>Completely disconnected from the biosphere. The scientific return would be

603
00:29:25.079 --> 00:29:26.319
<v Speaker 3>profoundly limited.

604
00:29:26.480 --> 00:29:29.319
<v Speaker 2>It won't tell us what's happening in Europa's most intriguing,

605
00:29:29.680 --> 00:29:31.400
<v Speaker 2>potentially life bearing zone.

606
00:29:31.440 --> 00:29:34.319
<v Speaker 3>It would be akin to a marine biologist attempting to

607
00:29:34.359 --> 00:29:38.839
<v Speaker 3>study the bizarre complex hydrothermal vent ecosystems of the Mariana

608
00:29:38.920 --> 00:29:42.799
<v Speaker 3>Trench by analyzing a puddle of melted snow sitting on

609
00:29:42.880 --> 00:29:44.519
<v Speaker 3>top of a glacier in Greenland.

610
00:29:44.839 --> 00:29:48.400
<v Speaker 2>Wow. Yeah, physically they are both liquid water, yes.

611
00:29:48.480 --> 00:29:52.160
<v Speaker 3>But one is a rich, dynamic chemical ecosystem and the

612
00:29:52.200 --> 00:29:53.880
<v Speaker 3>other is just melted precipitation.

613
00:29:54.079 --> 00:29:58.119
<v Speaker 2>A shallow reservoir on Europa, if formed entirely by localized

614
00:29:58.160 --> 00:30:01.240
<v Speaker 2>sheer heating within the crust, tell us absolutely nothing about

615
00:30:01.240 --> 00:30:04.359
<v Speaker 2>the chemical conditions, the potential habitability, or the presence of

616
00:30:04.440 --> 00:30:05.440
<v Speaker 2>life in the deep ocean.

617
00:30:05.720 --> 00:30:08.680
<v Speaker 3>It's a brutal bait and switch. We spend decades hoping

618
00:30:08.720 --> 00:30:12.119
<v Speaker 3>these shallow pockets were a convenient window into the deep ocean, but.

619
00:30:12.160 --> 00:30:15.920
<v Speaker 2>This research suggests they are just a mirror reflecting only

620
00:30:15.960 --> 00:30:19.920
<v Speaker 2>the isolated, frozen, sterile reality of the crust itself.

621
00:30:20.119 --> 00:30:23.720
<v Speaker 3>While it is undeniably a sobering realization for our immediate

622
00:30:23.759 --> 00:30:27.240
<v Speaker 3>exploration goals, it is also a vital timely piece of

623
00:30:27.319 --> 00:30:28.559
<v Speaker 3>scientific course.

624
00:30:28.319 --> 00:30:31.480
<v Speaker 2>Correction because this discovery isn't just theoretical, is it.

625
00:30:31.839 --> 00:30:35.319
<v Speaker 3>No, This theoretical modeling isn't just an academic exercise confined

626
00:30:35.319 --> 00:30:39.440
<v Speaker 3>to a university server. This new understanding of fluid dynamics

627
00:30:39.440 --> 00:30:44.440
<v Speaker 3>and Frazil ice has immediate massive implications for billions of

628
00:30:44.480 --> 00:30:47.240
<v Speaker 3>dollars of space hardware currently flying through the void of

629
00:30:47.279 --> 00:30:48.079
<v Speaker 3>the Solar System.

630
00:30:48.400 --> 00:30:51.119
<v Speaker 2>We're looking at the incoming fleet. The stakes here are

631
00:30:51.200 --> 00:30:54.599
<v Speaker 2>incredibly high because we have two flagship missions already launched,

632
00:30:54.640 --> 00:30:56.359
<v Speaker 2>already on their way to the Jupiter.

633
00:30:56.079 --> 00:30:59.319
<v Speaker 3>System, and they were designed, funded, and built based largely

634
00:30:59.359 --> 00:31:03.279
<v Speaker 3>on the older, more optimistic assumptions about Europa's ice shell.

635
00:31:03.359 --> 00:31:05.640
<v Speaker 2>Let's break down the timeline. First, we have the European

636
00:31:05.680 --> 00:31:06.440
<v Speaker 2>Space Agency.

637
00:31:06.480 --> 00:31:10.400
<v Speaker 3>The European Space Agency launched the Jupiter Icy Moons Explorer

638
00:31:10.680 --> 00:31:14.160
<v Speaker 3>universally known as jew IC in April of twenty twenty three.

639
00:31:14.400 --> 00:31:15.720
<v Speaker 2>Okay, so that's already out there.

640
00:31:15.839 --> 00:31:19.440
<v Speaker 3>It is currently executing a complex looping trajectory through the

641
00:31:19.440 --> 00:31:21.920
<v Speaker 3>inner Solar System to build up speed, and it is

642
00:31:21.960 --> 00:31:24.799
<v Speaker 3>scheduled to finally arrive in the Jupiter System in July

643
00:31:24.920 --> 00:31:25.960
<v Speaker 3>of twenty thirty one.

644
00:31:26.039 --> 00:31:30.079
<v Speaker 2>And right on its heels we have NASA's massive contribution

645
00:31:30.160 --> 00:31:33.440
<v Speaker 2>to the effort the Europa Clipper. It launched recently in

646
00:31:33.480 --> 00:31:36.440
<v Speaker 2>October of twenty twenty four. It is taking a more

647
00:31:36.440 --> 00:31:40.359
<v Speaker 2>direct gravitational trajectory and is slated to arrive at Jupiter

648
00:31:40.400 --> 00:31:43.680
<v Speaker 2>ahead of Juicy in April of twenty thirty.

649
00:31:43.799 --> 00:31:47.839
<v Speaker 3>These are monumental engineering achievements. The Europa Clipper, for example,

650
00:31:47.960 --> 00:31:50.799
<v Speaker 3>is the largest spacecraft NASA has ever developed for a

651
00:31:50.839 --> 00:31:54.039
<v Speaker 3>planetary mission. It's huge, It will enter a highly elliptical

652
00:31:54.119 --> 00:31:57.079
<v Speaker 3>orbit around Jupiter designed to sweep past Europa and make

653
00:31:57.119 --> 00:32:00.680
<v Speaker 3>forty nine incredibly close low altitude flyby, and.

654
00:32:00.640 --> 00:32:04.519
<v Speaker 2>It carries a massive payload of nine highly sophisticated scientific

655
00:32:04.640 --> 00:32:08.839
<v Speaker 2>instruments designed to map the Moon's surface, composition, and interior

656
00:32:08.839 --> 00:32:10.960
<v Speaker 2>structure in unprecedented detail.

657
00:32:11.039 --> 00:32:13.079
<v Speaker 3>And one of the most critical instruments on that Tale

658
00:32:13.079 --> 00:32:16.079
<v Speaker 3>of the Reason instrument, which stands for radar for Europa

659
00:32:16.079 --> 00:32:19.559
<v Speaker 3>Assessment and sounding ocean to near surface, is directly impacted

660
00:32:19.559 --> 00:32:20.599
<v Speaker 3>by ocha's research.

661
00:32:21.039 --> 00:32:26.160
<v Speaker 2>This is a powerful ice penetrating radar. Its primary directive

662
00:32:26.240 --> 00:32:28.880
<v Speaker 2>is to fire radio waves down into the ice shell,

663
00:32:29.319 --> 00:32:32.160
<v Speaker 2>measure how those waves bounce back and map out the

664
00:32:32.200 --> 00:32:33.079
<v Speaker 2>internal structure.

665
00:32:33.519 --> 00:32:37.640
<v Speaker 3>It is specifically hunting for the dielectric signature of liquid water.

666
00:32:38.200 --> 00:32:41.440
<v Speaker 3>It is looking for those shallow reservoirs.

667
00:32:40.960 --> 00:32:44.960
<v Speaker 2>Without the sobering reality check provided by the fluid dynamics modeling.

668
00:32:45.480 --> 00:32:49.000
<v Speaker 2>Consider the scenario when Clipper arrives and powers up that radar.

669
00:32:49.119 --> 00:32:52.799
<v Speaker 3>The potential for a massive false positive is glaring right.

670
00:32:53.000 --> 00:32:56.720
<v Speaker 2>Clipper conducts its low altitude flybys, the radar pings the

671
00:32:56.799 --> 00:32:59.240
<v Speaker 2>upper layers of the ice shell, and the data lights up.

672
00:32:59.319 --> 00:33:02.160
<v Speaker 3>The radar waves hit a boundary transition from solid iceed

673
00:33:02.160 --> 00:33:03.920
<v Speaker 3>to liquid water and bounce back.

674
00:33:04.319 --> 00:33:06.920
<v Speaker 2>The science teams back at the jet propulsion laboratory look

675
00:33:06.920 --> 00:33:09.640
<v Speaker 2>at the telemetry. They see a massive pocket of liquid

676
00:33:09.640 --> 00:33:12.400
<v Speaker 2>water just a few miles down, and they celebrate. They

677
00:33:12.440 --> 00:33:14.319
<v Speaker 2>announce to the world that they have found it.

678
00:33:14.359 --> 00:33:17.039
<v Speaker 3>They'd think the deep ocean is venting upward, just like

679
00:33:17.079 --> 00:33:19.759
<v Speaker 3>the old cryo vulcanism models predicted.

680
00:33:19.400 --> 00:33:20.279
<v Speaker 2>But they would be wrong.

681
00:33:20.599 --> 00:33:23.599
<v Speaker 3>They would look at a localized, sheer, melted pocket of

682
00:33:23.640 --> 00:33:28.599
<v Speaker 3>sterile water and fundamentally misinterpret it as a direct, active

683
00:33:28.839 --> 00:33:31.599
<v Speaker 3>chemical window into the deep global ocean.

684
00:33:31.839 --> 00:33:35.279
<v Speaker 2>And the danger of that misinterpretation extends far beyond a

685
00:33:35.319 --> 00:33:36.400
<v Speaker 2>single press conference.

686
00:33:36.920 --> 00:33:40.839
<v Speaker 3>It dictates the future of space exploration for decades. They

687
00:33:40.960 --> 00:33:44.960
<v Speaker 3>might use that flawed interpretation to lobby for fund and

688
00:33:45.079 --> 00:33:50.599
<v Speaker 3>design a subsequent astronomically expensive lander mission targeted directly at

689
00:33:50.599 --> 00:33:52.279
<v Speaker 3>that specific reservoir.

690
00:33:51.839 --> 00:33:54.599
<v Speaker 2>Fully believing they're about to drill down and sample the

691
00:33:54.640 --> 00:33:55.880
<v Speaker 2>habitable zone.

692
00:33:55.640 --> 00:33:57.960
<v Speaker 3>A lander mission that would take another twenty years to

693
00:33:58.039 --> 00:33:58.759
<v Speaker 3>build and fly.

694
00:33:59.039 --> 00:34:01.799
<v Speaker 2>They would finally land on the ice, deploy a thermal drill,

695
00:34:02.079 --> 00:34:04.480
<v Speaker 2>melt their way down to the water, activate their mass

696
00:34:04.480 --> 00:34:06.839
<v Speaker 2>spectrometers to look for complex organic.

697
00:34:06.640 --> 00:34:08.880
<v Speaker 3>Molecules, and find absolutely nothing.

698
00:34:08.880 --> 00:34:11.280
<v Speaker 2>Sterile, isolated, friction, melted water.

699
00:34:11.480 --> 00:34:15.239
<v Speaker 3>It would be a catastrophic generational waste of time, engineering,

700
00:34:15.280 --> 00:34:16.320
<v Speaker 3>and scientific funding.

701
00:34:16.679 --> 00:34:21.480
<v Speaker 2>This highlights why theoretical modeling, simulation, and constantly challenging our

702
00:34:21.480 --> 00:34:26.480
<v Speaker 2>own assumptions are the bedrock of planetary science. Oscha's research

703
00:34:26.559 --> 00:34:30.280
<v Speaker 2>acts as a preemptive, critical guidebook for the scientists who

704
00:34:30.280 --> 00:34:32.920
<v Speaker 2>will be analyzing the data from Clipper and JUC.

705
00:34:33.320 --> 00:34:36.960
<v Speaker 3>It shatters the easy dream, but it sharpens the actual science.

706
00:34:37.079 --> 00:34:39.559
<v Speaker 3>It forces the teams to be far more rigorous in

707
00:34:39.599 --> 00:34:40.440
<v Speaker 3>their analysis.

708
00:34:40.519 --> 00:34:43.760
<v Speaker 2>When Clipper and je arrive in the early twenty thirties

709
00:34:43.960 --> 00:34:47.440
<v Speaker 2>and start beaming back petabytes of radar and gravitational data,

710
00:34:47.960 --> 00:34:51.079
<v Speaker 2>the mission scientists now possess a crucial piece of the puzzle.

711
00:34:51.320 --> 00:34:53.800
<v Speaker 3>They know that the ice shell is a much more formidable,

712
00:34:54.000 --> 00:34:57.400
<v Speaker 3>actively defensive barrier than they ever assumed, so the.

713
00:34:57.440 --> 00:35:00.000
<v Speaker 2>Data won't trick them into a false sense of victory.

714
00:35:00.000 --> 00:35:02.480
<v Speaker 3>We will know to treat any evidence of shallow liquid

715
00:35:02.480 --> 00:35:05.360
<v Speaker 3>water with extreme skepticism regarding its origin.

716
00:35:05.559 --> 00:35:08.400
<v Speaker 2>It completely redefines the parameters of the search. If they

717
00:35:08.400 --> 00:35:10.880
<v Speaker 2>find a shallow pocket, they can't just assume its ocean water.

718
00:35:10.960 --> 00:35:14.320
<v Speaker 3>They have to analyze the surrounding geologic context. Is there

719
00:35:14.360 --> 00:35:17.679
<v Speaker 3>evidence of massive sheer faulting nearby that could explain it

720
00:35:17.719 --> 00:35:19.079
<v Speaker 3>as localized melt?

721
00:35:19.360 --> 00:35:21.480
<v Speaker 2>They will know they either have to calibrate their instruments

722
00:35:21.519 --> 00:35:24.679
<v Speaker 2>to look much much deeper, trying to penetrate the full

723
00:35:24.760 --> 00:35:25.880
<v Speaker 2>fifteen miles.

724
00:35:25.760 --> 00:35:30.079
<v Speaker 3>Or they have to look for incredibly rare catastrophic geological anomalies,

725
00:35:30.239 --> 00:35:35.239
<v Speaker 3>perhaps massive impact basins where a comet punched a temporary

726
00:35:35.320 --> 00:35:37.280
<v Speaker 3>hole through the Brazil ice barrier.

727
00:35:37.519 --> 00:35:40.760
<v Speaker 2>It forces the scientific community to be much smarter and

728
00:35:40.840 --> 00:35:43.840
<v Speaker 2>much more discerning about the data they are about to collect.

729
00:35:44.000 --> 00:35:46.559
<v Speaker 3>Science is just as much about closing doors as it

730
00:35:46.599 --> 00:35:49.920
<v Speaker 3>is about opening them. Proving that a specific pathway is

731
00:35:49.960 --> 00:35:53.360
<v Speaker 3>physically impossible is a highly valuable scientific return.

732
00:35:53.599 --> 00:35:57.320
<v Speaker 2>It prevents the entire field of astrobiology from wandering down

733
00:35:57.360 --> 00:36:00.000
<v Speaker 2>a theoretical blind alley for the next twenty years.

734
00:36:00.039 --> 00:36:00.920
<v Speaker 3>Exactly so.

735
00:36:00.960 --> 00:36:04.320
<v Speaker 2>Synthesizing this entire reality check, we began with a vision

736
00:36:04.320 --> 00:36:08.519
<v Speaker 2>of Europa that was deeply appealing. We pictured an accessible oasis,

737
00:36:09.039 --> 00:36:13.760
<v Speaker 2>a dynamic, cracked icy shell that was constantly bleeding its deep, warm,

738
00:36:14.079 --> 00:36:17.280
<v Speaker 2>potentially life filled ocean out towards the surface.

739
00:36:17.000 --> 00:36:19.480
<v Speaker 3>Offering up its secrets for us to easily scoop up.

740
00:36:19.519 --> 00:36:21.639
<v Speaker 2>We banked entirely on the dream of the shortcut.

741
00:36:21.840 --> 00:36:25.760
<v Speaker 3>We relied heavily on terrestrial analogies. Assuming that the mechanics

742
00:36:25.760 --> 00:36:28.639
<v Speaker 3>of magma and rock would neatly translate to water and

743
00:36:28.679 --> 00:36:29.599
<v Speaker 3>cryogenic ice.

744
00:36:29.840 --> 00:36:32.960
<v Speaker 2>We envisioned a complex plumbing system of dikes and fractures

745
00:36:33.320 --> 00:36:34.880
<v Speaker 2>driven by the pressure of the ocean.

746
00:36:34.920 --> 00:36:38.920
<v Speaker 3>But then the brutal, unforgiving reality of computational fluid dynamics

747
00:36:39.000 --> 00:36:39.480
<v Speaker 3>was applied.

748
00:36:39.719 --> 00:36:42.159
<v Speaker 2>The researchers at Rutgers pulled back the curtain on the

749
00:36:42.159 --> 00:36:45.320
<v Speaker 2>actual mechanics of an alien moon. We were forced to

750
00:36:45.360 --> 00:36:50.400
<v Speaker 2>abandon the calm, orderly, mathematically convenient assumption of laminar flow

751
00:36:50.880 --> 00:36:55.079
<v Speaker 2>and plunge into the chaotic, violent, and thermally destructive reality

752
00:36:55.079 --> 00:36:56.559
<v Speaker 2>of high velocity turbulence.

753
00:36:56.880 --> 00:37:00.360
<v Speaker 3>We saw how that fluid turbulence aggressively strips the thermal

754
00:37:00.440 --> 00:37:03.639
<v Speaker 3>energy away from the water, violently transferring the heat into

755
00:37:03.679 --> 00:37:06.000
<v Speaker 3>the cryogenic walls of the tenttonic fractures.

756
00:37:06.280 --> 00:37:09.039
<v Speaker 2>We witness the rapid onset of supercooling, and.

757
00:37:08.960 --> 00:37:12.199
<v Speaker 3>We saw the fatal mechanism the super cooled water flashing

758
00:37:12.239 --> 00:37:15.000
<v Speaker 3>into billions of needles of brazil ice.

759
00:37:15.199 --> 00:37:19.639
<v Speaker 2>Instantly creating a highly viscous, gritty slush that aggressively adheres

760
00:37:19.639 --> 00:37:22.880
<v Speaker 2>to the walls, cementing the massive fractures shut within a

761
00:37:22.920 --> 00:37:23.679
<v Speaker 2>matter of hours.

762
00:37:23.960 --> 00:37:28.119
<v Speaker 3>It is nature's own impenetrable failsafe mechanism. The very act

763
00:37:28.159 --> 00:37:30.880
<v Speaker 3>of the pressurized ocean trying to violently force its way

764
00:37:30.920 --> 00:37:34.320
<v Speaker 3>to the surface generates the exact chaotic conditions that seal

765
00:37:34.360 --> 00:37:35.159
<v Speaker 3>its own fate.

766
00:37:35.440 --> 00:37:40.079
<v Speaker 2>The vault actively locks itself, and because of that physical reality,

767
00:37:40.400 --> 00:37:43.000
<v Speaker 2>the shallow reservoirs we are hunting for with the upcoming

768
00:37:43.079 --> 00:37:46.639
<v Speaker 2>radar instruments on Clipper and Jewsies are likely just phantoms.

769
00:37:46.639 --> 00:37:51.280
<v Speaker 3>They are localized milk pockets generated by tantonic friction, entirely

770
00:37:51.320 --> 00:37:55.039
<v Speaker 3>disconnected from the rich, complex habitable zone of the deep ocean.

771
00:37:55.159 --> 00:37:59.320
<v Speaker 2>The barrier remains intact and the ocean remains profoundly isolated.

772
00:37:58.840 --> 00:38:01.639
<v Speaker 3>Which leaves us with a linger r'aring immensely daunting thought

773
00:38:01.679 --> 00:38:04.639
<v Speaker 3>for the future of astrobiology and human engineering. What's that

774
00:38:04.920 --> 00:38:09.079
<v Speaker 3>We now understand precisely how formidable Europa's ice shell truly is.

775
00:38:09.800 --> 00:38:12.159
<v Speaker 3>It is not a passive layer of frozen water. It

776
00:38:12.239 --> 00:38:15.960
<v Speaker 3>is an active, self sealing, dynamic armoor that brutally shuts

777
00:38:16.000 --> 00:38:20.880
<v Speaker 3>down even nature's own immense gravitational and thermodynamic forces attempting

778
00:38:20.880 --> 00:38:22.199
<v Speaker 3>to push water to the surface.

779
00:38:22.480 --> 00:38:27.239
<v Speaker 2>If an entire pressurized ocean, driven by the relentless grinding

780
00:38:27.320 --> 00:38:30.320
<v Speaker 2>tidal forces of the largest planet in our Solar system,

781
00:38:30.800 --> 00:38:35.039
<v Speaker 2>cannot physically punch a hole through that cryogenic.

782
00:38:34.519 --> 00:38:38.920
<v Speaker 3>Armor, If nature cannot break the vault, what kind of radical,

783
00:38:39.000 --> 00:38:44.039
<v Speaker 3>out of the box, entirely unprecedented engineering will humanity eventually

784
00:38:44.079 --> 00:38:47.440
<v Speaker 3>need to invent to pierce that armor ourselves?

785
00:38:47.760 --> 00:38:50.800
<v Speaker 2>That is a staggering thought. If we are truly committed

786
00:38:50.840 --> 00:38:53.480
<v Speaker 2>to touching that dark ocean below, we can no longer

787
00:38:53.519 --> 00:38:55.400
<v Speaker 2>rely on the hope of a natural shortcut.

788
00:38:55.559 --> 00:38:57.400
<v Speaker 3>We cannot waste for the ocean to come to us.

789
00:38:57.400 --> 00:38:58.840
<v Speaker 3>We are going to have to figure out how to

790
00:38:58.840 --> 00:39:00.639
<v Speaker 3>break the planetary vault ourselves.

791
00:39:00.760 --> 00:39:03.039
<v Speaker 2>It forces us to ask just how badly we want

792
00:39:03.079 --> 00:39:04.960
<v Speaker 2>to know what is swimming in the dark down there.

793
00:39:05.159 --> 00:39:07.280
<v Speaker 2>When we started, we wanted to find an easy path

794
00:39:07.320 --> 00:39:09.800
<v Speaker 2>to alien life. We thought Europa was going to cooperate.

795
00:39:09.840 --> 00:39:11.559
<v Speaker 3>We thought we could just skim the surface and find

796
00:39:11.559 --> 00:39:12.039
<v Speaker 3>the answers.

797
00:39:12.079 --> 00:39:16.079
<v Speaker 2>But Europa is fiercely protective of its environment. The diagnostic

798
00:39:16.159 --> 00:39:19.599
<v Speaker 2>landscape here isn't just murky. It is actively sealed under

799
00:39:19.639 --> 00:39:22.880
<v Speaker 2>fifteen miles of the hardest, coldest, most defensive ice in

800
00:39:22.920 --> 00:39:25.119
<v Speaker 2>the Solar System. The shortcut is closed.

801
00:39:25.400 --> 00:39:28.440
<v Speaker 3>The real, grueling work of exploration is just beginning.

802
00:39:28.719 --> 00:39:32.239
<v Speaker 2>Keep looking up and keep questioning what you think you know.
