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- Mars.
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The god of war
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and the source of man's
science fictional demise.
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It has fired our imagination
for thousands of years.
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We know the dry, barren
planet was once flowing
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with vast reservoirs of water,
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the sky thick and filled with clouds,
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and the tantalizing possibility of life.
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It is the only other
place in our solar system
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that man might one day call home.
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(exhilarating music)
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We Earthlings have fired
numerous probes and satellites
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towards the red planet,
an invasion of sorts,
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not for conquest but for knowledge.
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What happened to Mars?
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Is there or has there ever
been life on the planet?
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- A fundamental question
that needs to be answered,
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is life as we know it on Earth,
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even the simplest type of
microbial life, unique?
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If we were to go to Mars
and we were to find evidence
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of early microbial life
or maybe even present life
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that somehow survived in the near surface,
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would it be the same as the early life
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that developed on Earth?
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That's a very fundamental question.
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Does life emerge generally in planets
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where the conditions
for life are favorable
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if we find out that they
were favorable on Mars
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or might life take its own unique path
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in different environments
and turn out differently?
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(mellow music)
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- We have bombarded Mars
with satellites and landers,
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but there have been more
failures than successes.
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The Soviets established two Mars orbiters
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while NASA landed two Viking landers
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carrying complex analytical laboratories
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and search for signs of microbial life.
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Their findings were inconclusive.
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Further missions to Mars still
had a high mortality rate,
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but the successes were outstanding,
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with robotic probes operating for years
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beyond their initial missions.
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In fact, Mars is a planet occupied solely
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by robots on the surface
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and satellites peering down from above.
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All these instruments perform admirably
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in their specified fields of endeavor,
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giving us a much clearer
picture of the planet
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and its history.
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The science was following the water,
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what happened and where it is now.
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- Thanks to the specific instrumentation
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on board the mission,
we are able to tell us
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what kind of ice did we find.
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And the result is that there is a mix
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of CO2 ice, or carbon dioxide ice,
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and water ice.
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And it's very important
to characterize it,
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especially for the water
ice, or frozen water,
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because one of the main objective
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of any mission to Mars
is to trace the water
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on Mars in every form.
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Liquid, if possible, solid, water vapor.
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So it's very important to study the ice
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because it's one of reservoirs
of water on the planet.
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- The science was conclusive.
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There was water on Mars.
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There were ancient lakes
and rivers, even an ocean.
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We needed to learn more.
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With the advancement of
analytical technology,
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computer power, and robotics,
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a new rover was constructed.
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Big, complex, and heavy,
it required a new way
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to land on Mars safely.
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Engineers came up with a system
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that couldn't be fully
tested here on Earth.
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It required a lot of
things to happen correctly,
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on time, and in order.
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This was the sky crane
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and the rover, Curiosity,
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was the first to try it out.
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A controlled reentry with heat shield,
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aerobraking with a parachute,
all pretty standard.
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Then a rocket-powered sky
crane drops from the aeroshell
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and gently descends toward the surface,
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spooling out the rover below on cables.
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The rover touches down, cuts the cables,
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and release the sky crane to
fly off and crash harmlessly.
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The Curiosity rover has
been an astounding success,
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traversing the terrain for over 10 years,
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taking samples, drilling,
and studying rock formations,
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zapping samples with a powerful laser,
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and photographing its progress.
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- Now, in the belly of that rover
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is an instrument called SAM.
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It's an instrument suite that has
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a couple different instruments
in it that allow us
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to look at different types of gases.
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It helps us understand
the chemical composition
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of the atmosphere and of
minerals that might be found
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in the rocks and the soils on the surface.
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In particular, it helps us
identify organic molecules
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that might be present.
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- So, the sort of evidence
we're looking for,
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sort of signatures of past life
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that we would be looking for
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would be signature of microbial life.
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So, not realistically
looking for dinosaur bones
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and that kind of thing.
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If life ever existed on Mars,
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we expect it to have been
microbial, microorganisms.
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(eerie futuristic music)
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- Orbiters including Mars
Odyssey and Mars Express
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have been hunting down
life as well, from orbit.
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- After 10 years of mission,
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we have achieve a global view of Mars
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and then we know what every
location on the surface,
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if you find some special minerals or not.
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So we have really the global view
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that tell us the history of Mars.
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Mars Express has, for the first time,
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detected methane.
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And also it comes from
pressure in the atmosphere,
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vary from the place to another,
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from a season to another.
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And this discovery, it's been very debated
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in the scientific community
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because, in fact, methane
should not be there
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because it's being
destroyed in the atmosphere
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by the ultraviolet radiation.
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So if methane is there,
there must be a source
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of methane and for the time being,
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the origin of this source
is largely unknown.
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- However, with Curiosity
prowling around Gale Crater,
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it too detected seasonal methane.
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- Now, methane has been found previously
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in the Martian atmosphere by
both Earth-based telescopes
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and space-born orbiters,
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but this is the first time
that we've actually seen
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a sharp increase and decrease
in the abundance of methane
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in the atmosphere in Gale Crater.
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But what this really means
is that present day Mars
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is an active environment.
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- The big question is what
is the origin of this methane
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now being released?
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The two principles areas are first,
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by analogy with the Earth,
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it could be released unproduced initially,
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primarily by biology.
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This would be microbial activity
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acting on certain
chemicals below the surface
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and then producing methane as a byproduct.
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But of course we can't stay with certitude
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that it is biologically produced.
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And so we also consider
geochemical mechanisms
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in which carbon dioxide
is actually combining
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with water and producing methane
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under very high
temperatures and pressures.
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And that methane can then be released
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in the atmosphere separately.
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- Now, at this point we
don't have enough evidence
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to tell us whether or
not the organics refining
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are biological or nonbiological in origin.
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There are several viable
nonbiological explanations,
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including this organic
material could've come down
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from space, from meteorites or comets,
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or organics can be formed
by geological reactions
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in the rock itself.
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Now what's exciting about this discovery
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is it gives us new hope in the search
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for chemical evidence of life.
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We found the organic material.
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Now the next step is trying to figure out
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what its origin is.
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(engine revving)
- Main engine start.
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Ignition and lift off
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of the Atlas V with MAVEN,
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looking for clues about
the evolution of Mars
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through its atmosphere.
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(dramatic music)
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- The latest NASA
orbiter mission is MAVEN.
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Launched in November 2013, it
made orbit 10 months later.
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(relaxing music)
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- MAVEN is the Mars Atmosphere
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and Volatile Evolution Mission.
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Our goal is to study the
role that lost to space
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has played in the history
of the atmosphere.
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Where did the water go?
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Where did the CO2 go
from the early planet?
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These are important
questions to understand
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how Mars went from an
early warm, wet environment
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to the cold, dry environment we see today.
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- There's evidence of
water flowing on Mars
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at one point in time,
perhaps even oceans on Mars.
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And what happened that it's so
barren at this point in time?
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And a key part of that is the atmosphere
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and it's a much thinner
atmosphere than what scientists
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believe it was at one point in time,
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so the stripping away of
that upper atmosphere,
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that's what MAVEN is going after,
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the climate change at Mars.
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- One of these processes
is called sputtering,
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where atoms are knocked
away from the atmosphere
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due to impacts from energetic particles.
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The sun constantly emits
high energy photons.
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When these enter a planet's atmosphere
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it can crash into a molecule,
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knocking loose an electron
and turning it into an ion.
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When this happens in the
presence of a magnetic field,
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the ions are captured and
spin around the field.
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Conveniently, the sun generates
a giant magnetic field
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that is carried by the solar wind.
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As the magnetic field
sweeps past the planet,
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these ions are carried away.
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Depending on where they form,
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other ions will not be carried away
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but will hit the top of the atmosphere.
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These ions crash into other molecules
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and fling atoms everywhere.
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Some of these atoms can be
knocked or sputtered into space
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causing atmospheric loss.
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As this process continues
over billions of years,
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Mars' atmosphere has disappeared
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and along with it, the water.
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How much water has Mars lost this way?
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- We use the world's
three majors telescopes
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for infrared astronomy.
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From the ground we could
actually take a snapshot
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of the whole hemisphere of
the planet on a single night.
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- Water naturally carries a heavy isotope
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of hydrogen deuterium,
which remains trapped
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in the water cycle while normal
hydrogen is lost to space.
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Detecting the amount
of deuterium enrichment
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tells us how much water has been lost.
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- Now we know that Mars'
water is much more enriched
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than terrestrial ocean water
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in the heavy form of
water, the deuterated form.
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Immediately that permits us to
estimate the amount of water
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Mars has lost since it was young.
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- So in the ancient past,
when you have some indications
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that water was flowing on the surface,
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but how much water was there?
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Talking about oceans, I'm
talking about small rivers,
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little rain.
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So these definitions of how
much water was on the planet,
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it was very undefined.
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- A major question has been
how much water did Mars
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actually have when it was young
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and how did it lose that water?
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- The findings indicate that
only 13% of an ancient ocean
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remains on the planet today,
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now stored in the polar ice caps.
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87% of this ocean has been lost to space.
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This means that early Mars
would have looked much different
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than it does today, with
a significant portion
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of its surface covered by water.
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- So the really interesting question is
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could it form a sea or an ocean?
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And indeed, it would.
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In the northern plains, which
is a relatively flat region,
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but depressed from the rest of the planet,
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it would form an ocean
that was approximately
263
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20% of the planet's surface area.
264
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And so that is a respectable ocean.
265
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- This ocean had a maximum
depth of around 5,000 feet
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or around one mile deep.
267
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It's deep, not as deep as the
deepest points of our oceans,
268
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but comparable to average
depth of the Mediterranean Sea.
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- By combining Martian
topography with a new estimate
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for water loss, the researchers
were able to simulate
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Mars's ancient ocean
and its escape to space.
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As Mars lost its atmosphere
over billions of years,
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it lost the pressure and heat
needed to keep water liquid,
274
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causing the ocean to shrink
and recede northward.
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The remaining water eventually condensed
276
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and froze over the north and south poles,
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giving Mars the ice
caps that we see today.
278
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- We now know that Mars was wet
279
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for a much longer time
than we thought before.
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Curiosity shows it was
wet for 1.5 billion years,
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already much longer than
the period of time needed
282
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for life to develop on Earth.
283
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And now we see that Mars must've been wet
284
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for a period even longer.
285
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- It's fascinating that
we can learn so much
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about 4.5 billion years ago
with measurement taken right now
287
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and ultimately we can conclude this idea
288
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of a ocean covering 20% of the planet,
289
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which opens the idea of habitability
290
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and the evolution of life on the planet.
291
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- Building on this knowledge,
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scientists are developing the
next series of robotic probes
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to be sent to Mars in the coming years.
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This time, NASA is
building on its successes,
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utilizing hardware and systems
that they know will work.
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- We've been to Mars before
297
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with the JPL, Lockheed Martin team.
298
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We've been to the surface
of Mars before successfully
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with Phoenix.
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We know how to operate the arm.
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The surface operations are
much, much simpler than Phoenix
302
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and we're putting two
instruments on the surface
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and then we're leaving them there
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with no ground-in-the-loop interaction.
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Repetitive weekly up
link, down link sessions.
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We're just made to do this mission.
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- The InSight mission is a
geophysical mission to Mars.
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It's gonna go to Mars
and take its vital signs.
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It's gonna take its heartbeat,
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the seismic activity of the planet.
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- So we're gonna be doing
that using a seismometer,
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a very high precision seismometer.
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Using techniques that have
been well-developed on Earth
314
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to get the understanding of
the crust, mantle, and core,
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and sort of the
relationship between those.
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- Gonna take its temperature by measuring
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the thermal gradient of the surface,
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which tells how much heat is coming out.
319
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And we also have a heat
flow probe called HP Cubed
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and what that does is
it's gonna basically take
321
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the temperature of Mars
and from that it'll be able
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to understand what the thermal flex is
323
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over the course of a full Martian year.
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- And it's gonna sort
of measure its reflexes
325
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by looking at how the rotation wobbles
326
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with the tiled effects of the sun.
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- Our final experiment is called RISE
328
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and that's going to be looking at the,
329
00:16:08,560 --> 00:16:11,360
basically the wobble of
Mars to help understand
330
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what the core size may be in composition.
331
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- The European Space
Agency is also well along
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with ExoMars, a rover with
advanced drilling capability
333
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due to be launched by 2018.
334
00:16:25,439 --> 00:16:28,119
Its principle goal, to drill down deep
335
00:16:28,119 --> 00:16:30,519
in search of microorganisms.
336
00:16:30,519 --> 00:16:32,839
(uplifting music)
337
00:16:37,319 --> 00:16:41,239
- What is new with ExoMars,
with the rover in particular,
338
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is what we call the mobility.
339
00:16:42,959 --> 00:16:46,079
Mobility, not only
horizontal, but also vertical.
340
00:16:46,079 --> 00:16:48,239
This is a particular thing that we have
341
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on board ExoMars mission,
so we will be able to sample
342
00:16:52,519 --> 00:16:54,879
material from below the surface
343
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that is quite important to understand
344
00:16:56,800 --> 00:17:01,079
if there is any sign of a
past life activity on Mars.
345
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- We will be looking, for the first time,
346
00:17:03,280 --> 00:17:04,759
in the third dimension,
347
00:17:04,759 --> 00:17:07,200
the third dimension being depth.
348
00:17:07,200 --> 00:17:10,600
And we think that is where
we have the highest chance
349
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of making an interesting discovery
350
00:17:13,079 --> 00:17:17,800
regarding the presence of
organic molecules in Mars.
351
00:17:26,280 --> 00:17:28,400
- It's a whole planet out there
352
00:17:28,400 --> 00:17:30,439
with a complicated history.
353
00:17:30,439 --> 00:17:34,560
It's that history is a story
that's stored in the rocks
354
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and our job is to figure out that story
355
00:17:36,959 --> 00:17:38,920
and what that story of that planet
356
00:17:38,920 --> 00:17:41,439
tells us about this
planet that we live on.
357
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- So where Curiosity takes
rocks and grinds them up
358
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into powder and looks at
their bulk constituents,
359
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what this mission would need
to do is be able to look
360
00:17:50,239 --> 00:17:53,360
in a microscopic level
and examine the rocks
361
00:17:53,360 --> 00:17:55,600
for these very tiny and detailed messages
362
00:17:55,600 --> 00:17:57,039
that they would be sending to us
363
00:17:57,039 --> 00:17:59,280
about the past life that
could've lived there.
364
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- This that I'm holding up here
365
00:18:01,439 --> 00:18:03,720
is a classic biosignature from the Earth,
366
00:18:03,720 --> 00:18:04,800
it's a fossil.
367
00:18:04,800 --> 00:18:07,039
We're not actually
expecting to see a fossil
368
00:18:07,039 --> 00:18:09,519
of shells or other components,
369
00:18:09,519 --> 00:18:12,800
but what we want to be able to see are,
370
00:18:12,800 --> 00:18:14,239
with this instrumentation,
371
00:18:14,239 --> 00:18:17,439
are the fine-scale layering
that one might see in a rock,
372
00:18:17,439 --> 00:18:20,400
in which we can see dark
and light-toned layers.
373
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And those dark and light tone
layers are telling a story.
374
00:18:23,200 --> 00:18:25,479
(exhilarating music)
375
00:18:30,239 --> 00:18:33,479
- When will NASA send astronauts to Mars?
376
00:18:33,479 --> 00:18:35,400
- Five, four, three,
377
00:18:35,400 --> 00:18:37,119
two, one.
378
00:18:38,720 --> 00:18:41,479
And lift off at dawn.
379
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The dawn of Orion
380
00:18:43,000 --> 00:18:46,239
and a new era of American
space exploration.
381
00:18:47,759 --> 00:18:48,959
- The first test flight
382
00:18:48,959 --> 00:18:51,280
of the Orion crew capsule is complete,
383
00:18:51,280 --> 00:18:54,759
the hardware and systems are
ready for mass production.
384
00:18:54,759 --> 00:18:57,360
The components, the
engineering, the manufacturing,
385
00:18:57,360 --> 00:18:59,720
are all underway with NASA looking back
386
00:18:59,720 --> 00:19:01,200
to what worked in the past
387
00:19:01,200 --> 00:19:03,280
and utilizing it for the future.
388
00:19:10,560 --> 00:19:11,839
- Fire.
389
00:19:11,839 --> 00:19:13,959
- The solid rocket booster technology
390
00:19:13,959 --> 00:19:15,360
straight from the space shuttle
391
00:19:15,360 --> 00:19:17,479
has been extended and tested.
392
00:19:19,879 --> 00:19:22,800
NASA's new Space Launch System, or SLS,
393
00:19:22,800 --> 00:19:24,519
is coming closer to fruition,
394
00:19:24,519 --> 00:19:26,920
reusing the space shuttle's main engines
395
00:19:26,920 --> 00:19:28,759
as the new system's work horses,
396
00:19:28,759 --> 00:19:30,600
saving billions of dollars
397
00:19:30,600 --> 00:19:33,039
and years in research and development.
398
00:19:48,280 --> 00:19:51,000
(suspenseful music)
399
00:20:00,319 --> 00:20:02,400
The Europeans are teaming up with NASA
400
00:20:02,400 --> 00:20:04,680
to provide the service model for Orion,
401
00:20:04,680 --> 00:20:08,239
allowing for long duration,
deep space flights.
402
00:20:15,239 --> 00:20:18,159
Autonomous Martian landing
systems are well advanced
403
00:20:18,159 --> 00:20:19,319
and being tested.
404
00:20:19,319 --> 00:20:21,759
Software and hardware are fully integrated
405
00:20:21,759 --> 00:20:25,119
for both manned and
unmanned Martian landings
406
00:20:25,119 --> 00:20:27,280
and when they get there.
407
00:20:28,079 --> 00:20:29,319
- Desert RAT stands for
408
00:20:29,319 --> 00:20:31,639
Desert Research and Technology studies.
409
00:20:31,639 --> 00:20:34,560
This is a group of
engineers and scientists.
410
00:20:34,560 --> 00:20:37,159
- We're looking to test out new concepts,
411
00:20:37,159 --> 00:20:40,439
procedures, equipment,
like rover concepts,
412
00:20:40,439 --> 00:20:42,039
to see how they work in
the field environment.
413
00:20:42,039 --> 00:20:44,319
- So the team tests these technologies
414
00:20:44,319 --> 00:20:47,000
to make sure that in future
human space flight missions
415
00:20:47,000 --> 00:20:49,439
we'll be able to do
science as best as we can.
416
00:20:49,439 --> 00:20:51,400
That's something that NASA's never done,
417
00:20:51,400 --> 00:20:54,000
two human rovers at the same time.
418
00:20:54,000 --> 00:20:55,720
So we're really trying to develop
419
00:20:55,720 --> 00:20:58,200
how do you use these
assets at the same time?
420
00:20:58,200 --> 00:21:00,479
And interesting things that
you might not think about
421
00:21:00,479 --> 00:21:02,319
are your communications.
422
00:21:02,319 --> 00:21:04,839
So you potentially have
four astronauts talking
423
00:21:04,839 --> 00:21:06,759
all at the same time to Mission Control
424
00:21:06,759 --> 00:21:08,600
or science communication backroom.
425
00:21:08,600 --> 00:21:10,519
- It's just like planning
a real mission, say
426
00:21:10,519 --> 00:21:13,039
like you kind of think about
Apollo missions (mumbles).
427
00:21:13,039 --> 00:21:14,400
You had the astronauts on the moon
428
00:21:14,400 --> 00:21:16,439
and you had people, Mission Control,
429
00:21:16,439 --> 00:21:18,439
but there was a science
backroom you didn't hear about
430
00:21:18,439 --> 00:21:22,400
but the astronauts were
getting information from them.
431
00:21:22,400 --> 00:21:25,239
- Arizona has a very good climate
432
00:21:25,239 --> 00:21:27,280
for these types of analog studies.
433
00:21:27,280 --> 00:21:29,839
You have pretty much open
plains and you have a lot
434
00:21:29,839 --> 00:21:31,720
of geological features that are analogous
435
00:21:31,720 --> 00:21:34,280
to places on the moon and on Mars.
436
00:21:34,280 --> 00:21:37,079
(relaxing upbeat music)
437
00:21:42,360 --> 00:21:45,639
- Long-term space voyages are
being replicated on the ground
438
00:21:45,639 --> 00:21:48,360
and in orbit with the ISS.
439
00:21:48,360 --> 00:21:50,680
Surface habitats, power systems,
440
00:21:50,680 --> 00:21:52,959
food and oxygen supply manufacturing,
441
00:21:52,959 --> 00:21:55,319
are also on the drawing board.
442
00:21:59,000 --> 00:22:00,920
- The human flight
component would like to see
443
00:22:00,920 --> 00:22:04,039
an experiment where resources
on the surfaces of Mars
444
00:22:04,039 --> 00:22:06,280
from the rocks or the
atmosphere could be used
445
00:22:06,280 --> 00:22:08,839
to generate fuel or other parts
446
00:22:08,839 --> 00:22:12,600
that would enable future exploration
447
00:22:12,600 --> 00:22:15,600
in cutting the tie, so to speak, to Earth.
448
00:22:15,600 --> 00:22:17,159
So you wouldn't necessarily have to bring
449
00:22:17,159 --> 00:22:17,920
everything with you.
450
00:22:17,920 --> 00:22:19,920
You can actually
manufacture it on the planet
451
00:22:19,920 --> 00:22:22,400
and that's a really exciting
additional component
452
00:22:22,400 --> 00:22:25,239
that we've been exploring and analyzing
453
00:22:25,239 --> 00:22:26,839
in this work.
454
00:22:29,560 --> 00:22:32,759
- NASA isn't the only one
with its eye on this prize.
455
00:22:32,759 --> 00:22:36,200
ESA and now the Indian
Space Research Organization
456
00:22:36,200 --> 00:22:38,439
have a spacecraft orbiting Mars
457
00:22:38,439 --> 00:22:40,920
and they did it on their first attempt.
458
00:22:42,159 --> 00:22:44,879
Private enterprise is
hard at work as well.
459
00:22:44,879 --> 00:22:48,200
Mars 500, Mars One, The Mars Society,
460
00:22:48,200 --> 00:22:51,560
Mars Foundation, and the Mars
Initiative, to name a few.
461
00:22:51,560 --> 00:22:54,200
And they have volunteers lining up already
462
00:22:54,200 --> 00:22:56,319
for a one-way trip to Mars.
463
00:22:58,159 --> 00:23:00,959
It is inevitable that
we will set foot on Mars
464
00:23:00,959 --> 00:23:02,439
in the very near future.
465
00:23:02,439 --> 00:23:05,360
We will stay and learn her secrets.
466
00:23:07,920 --> 00:23:09,200
Perhaps in the future
467
00:23:09,200 --> 00:23:11,680
we will be able to alter
the atmospheric density
468
00:23:11,680 --> 00:23:14,039
through terraforming and return Mars
469
00:23:14,039 --> 00:23:15,879
to the world that it once was,
470
00:23:15,879 --> 00:23:20,600
awash with oceans and
rivers, clouds and rain.
471
00:23:20,600 --> 00:23:23,759
Maybe some of us could call it home.
472
00:23:23,759 --> 00:23:26,079
(relaxing nature music)
37387
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