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- [Narrator] The amazing
Cassini spacecraft
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and its sibling lander
Huygens have now concluded
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their scientific studies,
bringing back years of data
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to be combed through by scientists,
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plotting their next journey
to Saturn and space.
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Now it's time for other planets
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and other spacecraft to shine.
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Juno, piercing the cloak of Jupiter,
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and her distant relative,
New Horizons at the edge
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of the Solar System.
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(dramatic music)
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(catchy piano music)
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After 20 years, the Cassini
project finally comes to an end
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in dramatic style.
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But with one door closing, another opens.
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Now, the enviable task of
having to unravel the data
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Saturn has just laid bare begins.
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And, we have literally
just scratched the surface.
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- I think Cassini has left
us with humankind's presence
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at another planet for 13 years,
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seeing things that we have
never imagined seeing.
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And at the same time, sharing
that with the entire world
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and opening up vistas for
the next sets of missions.
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- [Narrator] One of these
is facing scientists
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when looking at exploring the new frontier
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is leaving it in a better
state than they found it.
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So, eliminating the
problems of space junk,
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or the introduction of
alien microbes is paramount
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in their decision making.
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- And it also helps us satisfy,
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a planetary protection requirement.
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We're protecting the tiny moon, Enceladus
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as well as Titan.
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Both of those have global oceans
underneath their icy crusts
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and just in case there might
be life in those oceans,
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we don't want Cassini to
crash into one of those moons
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once we're out of fuel.
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(ambient piano music)
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- [Narrator] While the main
focus of the Cassini mission
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was to delve into the mysteries
of Saturn and its rings,
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the moons of Saturn proved
most science-worthy.
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And Saturn has many moons, in
fact 62 with confirmed orbits.
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Several are only 50
kilometers in diameter,
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the largest being Titan
which is bigger than Mercury.
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The Huygens module that
traveled aboard Cassini
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also became the first
probe to land on a moon
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other than our own and
transmit data back to Earth.
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- The temperature at the surface of Titan
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is about - 180 degrees, so it's very cold.
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The landscapes of Titan
look a lot like those
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we have on Earth.
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We have rivers, lakes, seas,
almost oceans of methane.
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It rains, it rains methane or
a mix of ethane and methane,
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so there are lots of
meteorological phenomena
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with geophysical phenomena
on Titan that makes you think
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of what happens on Earth.
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But the ingredients are quite different.
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- [Narrator] But it is
Saturn's sixth largest moon
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that excited many scientists,
as it is virtually covered
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by clean ice, and ejected
plumes of water into space.
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- My favorite moon is Enceladus.
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And the reason I'm partial
to Enceladus is it's
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the moon that my team discovered
a water vapor plume at.
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But not only is there liquid
water underneath the surface,
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but there's organic material,
there's a heat source.
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When people get excited
about the potential for life
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elsewhere in the Solar System,
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there are four things that you need.
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You need a heat source,
you need liquid water,
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you need organic material, and
you need those three things
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to be stable over some period of time
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so that life could potentially form.
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At Enceladus, we've got
three, we're not sure
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about the stability over time yet.
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And so based on the Cassini
observations we made
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back in May 2005, we've had lots and lots
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more flybys of Enceladus.
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Now we understand it much better.
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We understand what
organic material is there.
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One of the instruments, the
neutral mass spectrometer
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in a very close flyby through
the plume found some ammonia
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in the plume.
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- First of all, we see moons.
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Then, we start finding out
from the gravity measurements
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and the imaging that there's an ocean,
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and that it's global.
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And then there was some measurements
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by the cosmic dust analyzer that suggested
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there was hot water being
circulated through the rock,
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the silicon dioxide nanoparticles.
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This is just the final step that shows
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that there's molecular
hydrogen being produced
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by these same hydrothermal processes,
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and that molecular hydrogen
has the chemical energy
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to support microbial systems
in the interior ocean.
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- It's really the longevity
of the Cassini mission
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that has allowed us to
put together the pieces
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of the puzzle to really
understand a moon like Enceladus.
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And even this late in
the mission, we continue
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to look at our data to better
understand this ocean world.
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- [Narrator] Collating data is one thing,
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but interpreting and providing a vision
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for future missions is another.
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This is an area for
which the Cassini project
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came up trounced, because
it not only brought together
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free agencies, it provided the
ground for future scientists
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to develop skills that
will provide the basis
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for new projects.
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- The number of Ph.Ds we've
put through the system,
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they are going to be the
educators of the next generations.
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We've put out 3,000-plus
peer reviewed papers.
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Hundreds of Ph.Ds, thousands
of peer-reviewed papers,
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the scientific legacy is huge.
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The engineering legacy
of using every ounce
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of engineering capability
to exploit a system,
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I think is, again, will be built upon.
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And I can't ignore the
international cooperation.
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This, we had 19 nations
contributing hardware
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to this mission.
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We've got over 26 nations now
contributing scientifically.
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And despite whatever else is going on,
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this really has been an
amazing collaboration
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across the world.
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- [Narrator] The mighty
Jupiter is the current target
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under the microscope with the
Juno mission in full swing.
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The story of our Solar
System is linked to Jupiter
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as it is believed that it
was the first planet formed.
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So if we can understand
how, we can begin to unravel
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the origins of our Solar System,
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and thus, how the Earth came about.
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Juno must work in a very harsh environment
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to tease out the answers
from the gas giant.
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- When you go to a place
as hazardous as Jupiter,
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we put a lot of time through
the whole development process
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in trying to design a
spacecraft% that will operate
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in the high radiation
fields, magnetic environment,
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spacecraft charging environment,
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everything that you
deal with with Jupiter.
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And I have to say, the spacecraft
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has been performing admirably.
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- [Narrator] Jupiter's
radiation belts pose
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one of the biggest problems
faced by Juno's scientists.
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They exist within the
enormous magnetic field
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that surrounds Jupiter.
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With its magnetosphere trapping
of accelerating particles,
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it produces intense belts of radiation
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similar to Earth's Van Allen Belts,
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but thousands of times stronger.
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- Juno just flew by
Jupiter for the first time
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with all the science instruments
on and it was spectacular.
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The spacecraft performed flawlessly.
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The instruments all
worked exactly as planned,
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and the data is amazing.
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We're looking deep into Jupiter,
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we're learning about the
secrets that it's holding,
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but we're also getting a lot
of surprises about the aurora,
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about the atmosphere, how it works.
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I mean, it's just incredible.
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- [Narrator] The flybys
which followed showed
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that the massive amounts
of energy swirling
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over Jupiter's polar regions were creating
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the giant planet's powerful auroras,
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but not in ways the researchers expected.
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What puzzled the researchers
was the fact that despite
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the magnitude of these
potentials at Jupiter,
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they are observed only sometimes,
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and are not the source of
the most intense auroras
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as they are on Earth.
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- Juno had its camera, Juno came on.
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During the flyby we got the first pictures
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of Jupiter's poles, the
north and south pole.
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They were amazing, a lot of surprises.
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It didn't look like we
thought, doesn't look much
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like Saturn's pole.
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Jupiter's poles are
covered in these cyclones,
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like anticyclone storms,
some of them half the size
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of the Earth or bigger.
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And we're puzzled as to
how they could be formed
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and stable in that configuration.
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And the north pole doesn't
look like the south pole.
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And so we're questioning,
the scientists are really
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questioning whether this
is a dynamic system,
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and are we seeing just one stage,
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and over the next year we're
gonna watch it disappear?
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Or is this a stable configuration,
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and that these storms are
circulating around each other?
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- [Narrator] While the polar
activity appears unique
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to our Solar System, the
engineers are looking
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below its shell for answers.
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- The new science results
from Juno really are our
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first look, close-up,
at how Jupiter works.
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And so for the first time,
we're looking inside of Jupiter
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into the interior, and what we're seeing
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is that it doesn't work at
all like we had predicted.
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Almost every model that
has the interior motion,
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how the magnetic field, the gravity field,
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how the deep atmosphere
works, it's all different.
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- [Narrator] Like most
scientific undertakings,
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they result in more questions
being asked than answered.
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- So Juno's original
objectives really were
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to understand how Jupiter formed.
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And that would help us
understand how planets
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in general form, and how the
whole Solar System was made.
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What we're finding is that
actually we didn't understand
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giant planet dynamics very well,
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the whole atmosphere or
the interior structure.
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- What we've seen so far is
exciting, no question about that
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but it's like a puzzle.
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And we're putting the pieces
of the puzzle together,
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and it's exciting but we don't
have the whole picture yet.
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- [Narrator] And one of those puzzles
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is the so-called Great Red Spot.
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And while its presence in
a turbulent gaseous planet
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is not unusual, the scale is.
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The red spot covers an area
twice as large as Earth.
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- [Scott] And we're gonna go
right over the Great Red Spot,
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and that's really gonna be the first time
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that we get a close look at
that and to see what it's like
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underneath the top surface layer.
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I mean, how deep are the roots of that.
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That's a 300 year old storm.
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A lot of scientists believe that the roots
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must be very deep.
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When we go over with our
microwave radiometer,
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we're gonna see, is it the
same as the zones and belts,
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or is it very different,
and nobody really knows.
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(grandiose music)
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(dramatic music)
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- [Narrator] But it's
not just Jupiter's poles
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that hold the greatest interest
for the Juno investigators.
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They are also intrigued
by the weather pattern
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that is unique to this planet
yet familiar in other ways.
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Studying the atmospheric
dynamics helps understand
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other planets' atmospheres.
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- So when we look at Jupiter,
we see a lot of structure
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that looks very similar to the Earth.
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We can see storms, we see
cyclones, we see anticyclones.
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And these sort of storms
and weather systems
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that we see on Earth are very similar
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and are happening on Jupiter.
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Fluid mechanics is hopefully
the same everywhere
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in the universe.
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But Jupiter and Earth are very different.
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Jupiter's much bigger
and rotates a lot faster.
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They're made of different material
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and Jupiter's much
further away from the Sun
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than the Earth is.
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The quasi biennial oscillation
or the QBO on Earth
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is an equatorial phenomenon
in the stratosphere
250
00:14:39,790 --> 00:14:41,810
where the winds are changing direction
251
00:14:41,810 --> 00:14:43,560
approximately every two years.
252
00:14:43,560 --> 00:14:47,450
Depending on which phase the
QBO is in, eastward or westward
253
00:14:47,450 --> 00:14:49,470
the temperature signal
corresponds to that,
254
00:14:49,470 --> 00:14:51,620
so it's warmer in the eastwards phase,
255
00:14:51,620 --> 00:14:53,760
and cooler in the westward phase.
256
00:14:53,760 --> 00:14:55,855
It's been shown that it
could actually be a barrier
257
00:14:55,855 --> 00:14:59,410
to transport of aerosols
across the equator.
258
00:14:59,410 --> 00:15:02,250
And has been linked to the
frequency in the formation
259
00:15:02,250 --> 00:15:05,400
of hurricanes in the Atlantic
and the Pacific Ocean.
260
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The long term scales on
Earth's climate is something
261
00:15:08,640 --> 00:15:11,130
that we're very interested
in and how that applies
262
00:15:11,130 --> 00:15:13,451
to other planets'
atmospheres is really why
263
00:15:13,451 --> 00:15:16,220
we're studying Earth and Jupiter.
264
00:15:16,220 --> 00:15:19,040
The quasi quadrennial oscillation
in Jupiter's stratosphere
265
00:15:19,040 --> 00:15:21,866
is the temperature signal
that we see in the equator.
266
00:15:21,866 --> 00:15:24,940
We see the temperature
get warmer and cooler
267
00:15:24,940 --> 00:15:27,060
approximately every four Earth years.
268
00:15:27,060 --> 00:15:29,789
We used a general circulation
model where we focused
269
00:15:29,789 --> 00:15:32,640
on simulating the effects
of small-scale waves
270
00:15:32,640 --> 00:15:35,679
produced from convection in
Jupiter's equatorial region
271
00:15:35,679 --> 00:15:38,070
to simulate the QQL.
272
00:15:38,070 --> 00:15:40,500
The waves propagate
outwards from the clouds
273
00:15:40,500 --> 00:15:44,020
and force the winds in the
stratosphere to change direction
274
00:15:44,020 --> 00:15:46,334
going from eastward to
westward approximately
275
00:15:46,334 --> 00:15:48,280
every four years.
276
00:15:48,280 --> 00:15:51,490
Our model is able to reproduce
the behavior of the QQL,
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00:15:51,490 --> 00:15:53,890
but was also able to
reproduce temperatures
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00:15:53,890 --> 00:15:55,066
from the observations.
279
00:15:55,066 --> 00:15:58,000
And both of those together
give us a lot of confidence
280
00:15:58,000 --> 00:16:01,313
that our model is very accurate
in what's driving the QQL.
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00:16:02,580 --> 00:16:04,330
The outer planet serve as a laboratory
282
00:16:04,330 --> 00:16:06,446
for understanding atmospheric physics
283
00:16:06,446 --> 00:16:08,670
under very different conditions
284
00:16:08,670 --> 00:16:10,150
that are present on the Earth.
285
00:16:10,150 --> 00:16:12,818
Understanding how their
atmospheres change and evolve
286
00:16:12,818 --> 00:16:15,100
and their climates, can give us insight
287
00:16:15,100 --> 00:16:17,123
into any planetary atmosphere.
288
00:16:18,450 --> 00:16:19,890
- [Narrator] Juno has studied the planet
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00:16:19,890 --> 00:16:22,090
with a suite of tools, revealing much
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00:16:22,090 --> 00:16:24,733
that was previously
hidden to the human eye.
291
00:16:24,733 --> 00:16:29,160
- We have an infrared
instrument on Juno called JIRAM,
292
00:16:29,160 --> 00:16:32,600
and it was designed,
and built, and delivered
293
00:16:32,600 --> 00:16:34,661
by the Italian Space Agency.
294
00:16:34,661 --> 00:16:37,856
And this instrument makes
thermal maps of Jupiter,
295
00:16:37,856 --> 00:16:41,284
so the images are showing
you what's warm, hot, cold
296
00:16:41,284 --> 00:16:44,410
on Jupiter, and one of the
things you can see right away
297
00:16:44,410 --> 00:16:46,581
is the center of some of
these hurricane-like storms
298
00:16:46,581 --> 00:16:49,310
are cooler than the surrounding area.
299
00:16:49,310 --> 00:16:51,370
And sometimes you go over a warm spot.
300
00:16:51,370 --> 00:16:52,804
And we went over one that was very small
301
00:16:52,804 --> 00:16:55,260
but seems hotter than
those surrounding area,
302
00:16:55,260 --> 00:16:58,140
and that's very similar to what
the Galileo probe went into
303
00:16:58,140 --> 00:16:59,573
back in 1995.
304
00:17:00,760 --> 00:17:04,140
- The Juno mission is unique,
because it's the first time
305
00:17:04,140 --> 00:17:06,610
that we've ever gone in a polar orbit,
306
00:17:06,610 --> 00:17:09,031
which goes from pole to
pole over the north pole
307
00:17:09,031 --> 00:17:13,560
through periapsis, and
under the south pole.
308
00:17:13,560 --> 00:17:15,257
All the other missions we've done,
309
00:17:15,257 --> 00:17:18,050
and all the observations
we've made from Earth
310
00:17:18,050 --> 00:17:19,596
were made from the equator.
311
00:17:19,596 --> 00:17:22,580
And you don't see the poles very well
312
00:17:22,580 --> 00:17:24,015
if you're sitting on the equator.
313
00:17:24,015 --> 00:17:27,840
This is the first time we get
the first, clear unobstructed
314
00:17:27,840 --> 00:17:29,519
view of what the aurora looks like
315
00:17:29,519 --> 00:17:32,000
and what the polar phenomena looks like.
316
00:17:32,000 --> 00:17:34,140
And at the same time, we're flying through
317
00:17:34,140 --> 00:17:36,416
the magnetosphere right above the aurora
318
00:17:36,416 --> 00:17:40,003
so we can sample, in situ,
the charged particles
319
00:17:40,003 --> 00:17:43,057
that are precipitating
down magnetic field lines,
320
00:17:43,057 --> 00:17:46,723
the guys that are exciting
the emissions that we see.
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00:17:48,258 --> 00:17:50,675
(dark music)
322
00:18:02,330 --> 00:18:04,100
- [Narrator] Juno, like
its sister Cassini,
323
00:18:04,100 --> 00:18:06,350
has a used by date when the craft runs out
324
00:18:06,350 --> 00:18:08,340
of maneuvering fuel.
325
00:18:08,340 --> 00:18:10,530
This may occur during its 12th orbit
326
00:18:10,530 --> 00:18:12,960
at the end of its prime and mission.
327
00:18:12,960 --> 00:18:15,370
However, now some mean
to extend the mission
328
00:18:15,370 --> 00:18:17,390
if there are sufficient reserves.
329
00:18:17,390 --> 00:18:19,523
In that case, the
de-orbit would occur later
330
00:18:19,523 --> 00:18:21,990
on the 34th orbit as part
331
00:18:21,990 --> 00:18:24,723
of the planetary
protection policy of NASA.
332
00:18:39,022 --> 00:18:40,940
Its fact-finding mission
is leading the way
333
00:18:40,940 --> 00:18:43,780
for the one to come, the Europa Clipper,
334
00:18:43,780 --> 00:18:47,080
a mission in the design phase
to look closely at Europa,
335
00:18:47,080 --> 00:18:48,780
the moon with a hidden ocean,
336
00:18:48,780 --> 00:18:52,597
and the possible location for
life to evolve beyond Earth.
337
00:19:00,151 --> 00:19:02,901
(dramatic music)
338
00:19:11,911 --> 00:19:14,911
(suspenseful music)
339
00:19:26,040 --> 00:19:28,364
The blue haze of Pluto's
atmosphere, possibly
340
00:19:28,364 --> 00:19:33,100
a hydrocarbon smog, seen
from 200,000 kilometers away
341
00:19:33,100 --> 00:19:36,840
by NASA's departing New
Horizons spacecraft.
342
00:19:36,840 --> 00:19:38,960
A few years ago, the dwarf planet Pluto
343
00:19:38,960 --> 00:19:42,040
and its five known moons
were just small dots
344
00:19:42,040 --> 00:19:44,317
in the outer reaches of our Solar System.
345
00:19:50,340 --> 00:19:51,970
- One of the important
things you should understand
346
00:19:51,970 --> 00:19:54,240
about Pluto is the real
scale of it compared
347
00:19:54,240 --> 00:19:55,730
to the rest of the Solar System.
348
00:19:55,730 --> 00:19:57,420
So we come here to the
beach to really convey
349
00:19:57,420 --> 00:19:59,970
that scale and distance.
350
00:19:59,970 --> 00:20:03,457
So, if I draw the Sun as
a 30 centimeter circle,
351
00:20:03,457 --> 00:20:06,650
then we'd have to walk
about 35 steps this way
352
00:20:06,650 --> 00:20:10,180
in order to draw the Earth
in the same type of scale.
353
00:20:10,180 --> 00:20:13,723
So we're walking the equivalent
of 150 million kilometers,
354
00:20:13,723 --> 00:20:16,082
which we call one astronomical unit.
355
00:20:16,082 --> 00:20:20,550
Normally, Pluto orbits at
about 40 astronomical units
356
00:20:20,550 --> 00:20:22,910
from the Sun, but it's actually
quite an elliptical orbit
357
00:20:22,910 --> 00:20:26,843
so it changes between about
30 and 50 astronomical units.
358
00:20:27,800 --> 00:20:28,970
But, back to the Earth.
359
00:20:28,970 --> 00:20:31,458
So the Sun is over
there at 30 centimeters,
360
00:20:31,458 --> 00:20:34,110
which means that the Earth
should be about here,
361
00:20:34,110 --> 00:20:37,160
about three millimeters,
something like this.
362
00:20:37,160 --> 00:20:39,420
If we were to draw
Pluto on the same scale,
363
00:20:39,420 --> 00:20:41,970
it should be 0.3 millimeters,
364
00:20:41,970 --> 00:20:43,880
and it should be one
kilometer down the beach,
365
00:20:43,880 --> 00:20:45,913
so I'm going to draw it.
366
00:20:48,370 --> 00:20:51,300
Now obviously, I can't draw
something that's 0.3 millimeters
367
00:20:51,300 --> 00:20:53,150
so I have to draw Pluto a bit bigger.
368
00:20:54,030 --> 00:20:57,790
If this is Pluto, then its
largest moon is Charon,
369
00:20:57,790 --> 00:20:59,650
which is about half its size.
370
00:20:59,650 --> 00:21:02,780
But Pluto has four other moons, Styx, Nyx,
371
00:21:02,780 --> 00:21:04,950
Kerberos and Hydra.
372
00:21:04,950 --> 00:21:07,170
So there's a lot going on
around the Pluto system.
373
00:21:07,170 --> 00:21:09,143
It's not just a cold, dead, icy rock.
374
00:21:12,399 --> 00:21:14,982
(upbeat music)
375
00:21:21,300 --> 00:21:24,030
- [Narrator] The spacecraft
spent 16 months sending its data
376
00:21:24,030 --> 00:21:25,110
back to Earth.
377
00:21:25,110 --> 00:21:28,302
And scientists and non-scientists
alike have been enthralled
378
00:21:28,302 --> 00:21:29,743
by what it has revealed.
379
00:21:31,630 --> 00:21:33,210
- If you go in closer to the surface,
380
00:21:33,210 --> 00:21:35,930
you can see this type of
really diverse terrain.
381
00:21:35,930 --> 00:21:38,890
So you have a very bright
region, these are flat plains,
382
00:21:38,890 --> 00:21:40,750
not entirely sure how they formed yet,
383
00:21:40,750 --> 00:21:42,716
but there's a couple of leading theories.
384
00:21:42,716 --> 00:21:45,010
There's a huge range of mountains.
385
00:21:45,010 --> 00:21:47,560
There's all kinds of
different aged surfaces,
386
00:21:47,560 --> 00:21:49,200
some of them have lots of craters,
387
00:21:49,200 --> 00:21:52,070
some of them have very few
which means they're younger.
388
00:21:52,070 --> 00:21:54,210
If you look at a lot of detail at some
389
00:21:54,210 --> 00:21:56,230
of the mountainous
regions, you can see that
390
00:21:56,230 --> 00:21:59,600
they are a few kilometers
high but made of water-ice,
391
00:21:59,600 --> 00:22:02,480
I mean, on Pluto it's
so cold that water-ice
392
00:22:02,480 --> 00:22:04,800
is the hardest thing, it's more like rock.
393
00:22:04,800 --> 00:22:07,900
And so, the stuff that
forms the softer material
394
00:22:07,900 --> 00:22:10,430
is actually nitrogen ice.
395
00:22:10,430 --> 00:22:13,260
- [Narrator] Water-ice on
Earth is close to zero degrees,
396
00:22:13,260 --> 00:22:17,929
but on Pluto, it's minus
230 degrees Celsius.
397
00:22:17,929 --> 00:22:22,380
And as a glacier of nitrogen-ice,
called Sputnik Planitia,
398
00:22:22,380 --> 00:22:24,880
thought to be under a million years old.
399
00:22:24,880 --> 00:22:27,040
This is young by planetary standards.
400
00:22:27,040 --> 00:22:30,410
And no one knows yet how
it formed or is renewed.
401
00:22:30,410 --> 00:22:31,800
- One of the really fascinating things
402
00:22:31,800 --> 00:22:34,800
is some of the surface
coloration you can see
403
00:22:34,800 --> 00:22:36,090
in these images actually shows
404
00:22:36,090 --> 00:22:39,420
that there are these
compounds called tholins
405
00:22:39,420 --> 00:22:42,440
which are a combination of elements,
406
00:22:42,440 --> 00:22:46,010
but they're related to
pre-biotic molecules.
407
00:22:46,010 --> 00:22:48,796
So they're kind of relevant
to pre-biotic chemistry.
408
00:22:48,796 --> 00:22:50,910
And I think the fact
that they have been able
409
00:22:50,910 --> 00:22:53,940
to form on planetary surfaces very far out
410
00:22:53,940 --> 00:22:56,610
in the Solar System at
very cold temperatures
411
00:22:56,610 --> 00:22:58,980
really has implications
for a lot of places.
412
00:22:58,980 --> 00:23:02,686
I mean, if you can imagine for
star systems outside our own
413
00:23:02,686 --> 00:23:06,630
where the star may be dim and
the planets are quite faraway,
414
00:23:06,630 --> 00:23:08,640
it's interesting to know
that there are molecules
415
00:23:08,640 --> 00:23:13,260
that could be involved in
supplying biotic material
416
00:23:13,260 --> 00:23:17,280
to processes that may one day lead to life
417
00:23:17,280 --> 00:23:19,402
or be involved in life
or something like that.
418
00:23:19,402 --> 00:23:22,210
They're actually forming
way out in the Solar System
419
00:23:22,210 --> 00:23:23,660
where no one really expected.
420
00:23:24,860 --> 00:23:27,699
- [Narrator] Pluto is
unlike anything seen before.
421
00:23:27,699 --> 00:23:30,760
But the six gigabytes
of New Horizons images
422
00:23:30,760 --> 00:23:33,061
and scientific measurements
are giving scientists
423
00:23:33,061 --> 00:23:36,440
mysteries to unravel for years to come.
424
00:23:36,440 --> 00:23:39,030
In the meantime, asleep for the moment,
425
00:23:39,030 --> 00:23:41,750
the probe travels deeper into the unknown
426
00:23:41,750 --> 00:23:44,573
soon to awaken at its next destination.
427
00:23:48,830 --> 00:23:51,497
(ominous music)
35357
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