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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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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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- 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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- 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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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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- 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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- 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?
245
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- The findings indicate that
only 13% of an ancient ocean
246
00:12:39,141 --> 00:12:41,020
remains on the planet today,
247
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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
250
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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?
254
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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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00:13:04,702 --> 00:13:06,501
but depressed from the rest of the planet,
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it would form an ocean
that was approximately
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20% of the planet's surface area.
259
00:13:13,263 --> 00:13:15,862
And so that is a respectable ocean.
260
00:13:15,863 --> 00:13:19,342
- This ocean had a maximum
depth of around 5,000 feet
261
00:13:19,343 --> 00:13:21,062
or around one mile deep.
262
00:13:21,063 --> 00:13:24,141
It's deep, not as deep as the
deepest points of our oceans,
263
00:13:24,142 --> 00:13:27,382
but comparable to average
depth of the Mediterranean Sea.
264
00:13:28,423 --> 00:13:31,382
- By combining Martian
topography with a new estimate
265
00:13:31,383 --> 00:13:34,302
for water loss, the researchers
were able to simulate
266
00:13:34,303 --> 00:13:38,623
Mars's ancient ocean
and its escape to space.
267
00:13:38,624 --> 00:13:41,743
As Mars lost its atmosphere
over billions of years,
268
00:13:41,744 --> 00:13:45,102
it lost the pressure and heat
needed to keep water liquid,
269
00:13:45,103 --> 00:13:48,382
causing the ocean to shrink
and recede northward.
270
00:13:48,383 --> 00:13:50,743
The remaining water eventually condensed
271
00:13:50,744 --> 00:13:53,222
and froze over the north and south poles,
272
00:13:53,223 --> 00:13:56,222
giving Mars the ice
caps that we see today.
273
00:13:56,223 --> 00:14:00,263
- We now know that Mars was wet
274
00:14:00,264 --> 00:14:03,463
for a much longer time
than we thought before.
275
00:14:03,464 --> 00:14:06,664
Curiosity shows it was
wet for 1.5 billion years,
276
00:14:06,665 --> 00:14:09,664
already much longer than
the period of time needed
277
00:14:09,665 --> 00:14:11,464
for life to develop on Earth.
278
00:14:11,465 --> 00:14:14,023
And now we see that Mars must've been wet
279
00:14:14,024 --> 00:14:15,624
for a period even longer.
280
00:14:15,625 --> 00:14:17,503
- It's fascinating that
we can learn so much
281
00:14:17,504 --> 00:14:21,064
about 4.5 billion years ago
with measurement taken right now
282
00:14:21,065 --> 00:14:23,303
and ultimately we can conclude this idea
283
00:14:23,304 --> 00:14:25,823
of a ocean covering 20% of the planet,
284
00:14:25,824 --> 00:14:27,984
which opens the idea of habitability
285
00:14:27,985 --> 00:14:29,985
and the evolution of life on the planet.
286
00:14:32,745 --> 00:14:34,183
- Building on this knowledge,
287
00:14:34,184 --> 00:14:37,464
scientists are developing the
next series of robotic probes
288
00:14:37,465 --> 00:14:40,143
to be sent to Mars in the coming years.
289
00:14:40,144 --> 00:14:43,265
This time, NASA is
building on its successes,
290
00:14:43,266 --> 00:14:47,465
utilizing hardware and systems
that they know will work.
291
00:14:47,466 --> 00:14:49,824
- We've been to Mars before
292
00:14:49,825 --> 00:14:52,024
with the JPL, Lockheed Martin team.
293
00:14:52,025 --> 00:14:54,584
We've been to the surface
of Mars before successfully
294
00:14:54,585 --> 00:14:55,745
with Phoenix.
295
00:14:55,746 --> 00:14:57,985
We know how to operate the arm.
296
00:14:57,986 --> 00:15:01,345
The surface operations are
much, much simpler than Phoenix
297
00:15:01,346 --> 00:15:03,425
and we're putting two
instruments on the surface
298
00:15:03,426 --> 00:15:04,785
and then we're leaving them there
299
00:15:04,786 --> 00:15:07,745
with no ground-in-the-loop interaction.
300
00:15:07,746 --> 00:15:11,384
Repetitive weekly up
link, down link sessions.
301
00:15:11,385 --> 00:15:13,305
We're just made to do this mission.
302
00:15:14,626 --> 00:15:17,626
- The InSight mission is a
geophysical mission to Mars.
303
00:15:17,627 --> 00:15:20,305
It's gonna go to Mars
and take its vital signs.
304
00:15:20,306 --> 00:15:22,105
It's gonna take its heartbeat,
305
00:15:22,106 --> 00:15:24,705
the seismic activity of the planet.
306
00:15:24,706 --> 00:15:27,385
- So we're gonna be doing
that using a seismometer,
307
00:15:27,386 --> 00:15:29,505
a very high precision seismometer.
308
00:15:29,506 --> 00:15:32,066
Using techniques that have
been well-developed on Earth
309
00:15:32,067 --> 00:15:35,746
to get the understanding of
the crust, mantle, and core,
310
00:15:35,747 --> 00:15:38,025
and sort of the
relationship between those.
311
00:15:38,026 --> 00:15:39,705
- Gonna take its temperature by measuring
312
00:15:39,706 --> 00:15:41,105
the thermal gradient of the surface,
313
00:15:41,106 --> 00:15:42,585
which tells how much heat is coming out.
314
00:15:42,586 --> 00:15:46,305
And we also have a heat
flow probe called HP Cubed
315
00:15:46,306 --> 00:15:48,185
and what that does is
it's gonna basically take
316
00:15:48,186 --> 00:15:50,786
the temperature of Mars
and from that it'll be able
317
00:15:50,787 --> 00:15:52,747
to understand what the thermal flex is
318
00:15:52,748 --> 00:15:54,826
over the course of a full Martian year.
319
00:15:54,827 --> 00:15:57,586
- And it's gonna sort
of measure its reflexes
320
00:15:57,587 --> 00:16:00,146
by looking at how the rotation wobbles
321
00:16:00,147 --> 00:16:03,627
with the tiled effects of the sun.
322
00:16:03,628 --> 00:16:06,306
- Our final experiment is called RISE
323
00:16:06,307 --> 00:16:08,627
and that's going to be looking at the,
324
00:16:08,628 --> 00:16:11,427
basically the wobble of
Mars to help understand
325
00:16:11,428 --> 00:16:14,668
what the core size may be in composition.
326
00:16:16,907 --> 00:16:19,427
- The European Space
Agency is also well along
327
00:16:19,428 --> 00:16:23,106
with ExoMars, a rover with
advanced drilling capability
328
00:16:23,107 --> 00:16:25,506
due to be launched by 2018.
329
00:16:25,507 --> 00:16:28,186
Its principle goal, to drill down deep
330
00:16:28,187 --> 00:16:30,588
in search of microorganisms.
331
00:16:37,388 --> 00:16:41,307
- What is new with ExoMars,
with the rover in particular,
332
00:16:41,308 --> 00:16:43,027
is what we call the mobility.
333
00:16:43,028 --> 00:16:46,147
Mobility, not only
horizontal, but also vertical.
334
00:16:46,148 --> 00:16:48,307
This is a particular thing that we have
335
00:16:48,308 --> 00:16:52,587
on board ExoMars mission,
so we will be able to sample
336
00:16:52,588 --> 00:16:54,947
material from below the surface
337
00:16:54,948 --> 00:16:56,868
that is quite important to understand
338
00:16:56,869 --> 00:17:01,147
if there is any sign of a
past life activity on Mars.
339
00:17:01,148 --> 00:17:03,348
- We will be looking, for the first time,
340
00:17:03,349 --> 00:17:04,828
in the third dimension,
341
00:17:04,829 --> 00:17:07,269
the third dimension being depth.
342
00:17:07,270 --> 00:17:10,669
And we think that is where
we have the highest chance
343
00:17:10,670 --> 00:17:13,148
of making an interesting discovery
344
00:17:13,149 --> 00:17:17,870
regarding the presence of
organic molecules in Mars.
345
00:17:26,350 --> 00:17:28,469
- It's a whole planet out there
346
00:17:28,470 --> 00:17:30,508
with a complicated history.
347
00:17:30,509 --> 00:17:34,629
It's that history is a story
that's stored in the rocks
348
00:17:34,630 --> 00:17:37,028
and our job is to figure out that story
349
00:17:37,029 --> 00:17:38,989
and what that story of that planet
350
00:17:38,990 --> 00:17:41,509
tells us about this
planet that we live on.
351
00:17:41,510 --> 00:17:44,709
- So where Curiosity takes
rocks and grinds them up
352
00:17:44,710 --> 00:17:46,949
into powder and looks at
their bulk constituents,
353
00:17:46,950 --> 00:17:50,309
what this mission would need
to do is be able to look
354
00:17:50,310 --> 00:17:53,430
in a microscopic level
and examine the rocks
355
00:17:53,431 --> 00:17:55,670
for these very tiny and detailed messages
356
00:17:55,671 --> 00:17:57,109
that they would be sending to us
357
00:17:57,110 --> 00:17:59,350
about the past life that
could've lived there.
358
00:17:59,351 --> 00:18:01,509
- This that I'm holding up here
359
00:18:01,510 --> 00:18:03,790
is a classic biosignature from the Earth,
360
00:18:03,791 --> 00:18:04,870
it's a fossil.
361
00:18:04,871 --> 00:18:07,109
We're not actually
expecting to see a fossil
362
00:18:07,110 --> 00:18:09,589
of shells or other components,
363
00:18:09,590 --> 00:18:12,870
but what we want to be able to see are,
364
00:18:12,871 --> 00:18:14,309
with this instrumentation,
365
00:18:14,310 --> 00:18:17,510
are the fine-scale layering
that one might see in a rock,
366
00:18:17,511 --> 00:18:20,471
in which we can see dark
and light-toned layers.
367
00:18:20,472 --> 00:18:23,272
And those dark and light tone
layers are telling a story.
368
00:18:30,311 --> 00:18:33,550
- When will NASA send astronauts to Mars?
369
00:18:33,551 --> 00:18:35,471
- Five, four, three,
370
00:18:35,472 --> 00:18:37,191
two, one.
371
00:18:38,792 --> 00:18:41,550
And lift off at dawn.
372
00:18:41,551 --> 00:18:43,071
The dawn of Orion
373
00:18:43,072 --> 00:18:46,311
and a new era of American
space exploration.
374
00:18:47,831 --> 00:18:49,030
- The first test flight
375
00:18:49,031 --> 00:18:51,351
of the Orion crew capsule is complete,
376
00:18:51,352 --> 00:18:54,831
the hardware and systems are
ready for mass production.
377
00:18:54,832 --> 00:18:57,432
The components, the
engineering, the manufacturing,
378
00:18:57,433 --> 00:18:59,792
are all underway with NASA looking back
379
00:18:59,793 --> 00:19:01,272
to what worked in the past
380
00:19:01,273 --> 00:19:03,353
and utilizing it for the future.
381
00:19:10,633 --> 00:19:11,911
- Fire.
382
00:19:11,912 --> 00:19:14,031
- The solid rocket booster technology
383
00:19:14,032 --> 00:19:15,432
straight from the space shuttle
384
00:19:15,433 --> 00:19:17,552
has been extended and tested.
385
00:19:19,952 --> 00:19:22,872
NASA's new Space Launch System, or SLS,
386
00:19:22,873 --> 00:19:24,591
is coming closer to fruition,
387
00:19:24,592 --> 00:19:26,992
reusing the space shuttle's main engines
388
00:19:26,993 --> 00:19:28,832
as the new system's work horses,
389
00:19:28,833 --> 00:19:30,673
saving billions of dollars
390
00:19:30,674 --> 00:19:33,113
and years in research and development.
391
00:20:00,393 --> 00:20:02,473
The Europeans are teaming up with NASA
392
00:20:02,474 --> 00:20:04,754
to provide the service model for Orion,
393
00:20:04,755 --> 00:20:08,314
allowing for long duration,
deep space flights.
394
00:20:15,314 --> 00:20:18,233
Autonomous Martian landing
systems are well advanced
395
00:20:18,234 --> 00:20:19,393
and being tested.
396
00:20:19,394 --> 00:20:21,833
Software and hardware are fully integrated
397
00:20:21,834 --> 00:20:25,193
for both manned and
unmanned Martian landings
398
00:20:25,194 --> 00:20:27,355
and when they get there.
399
00:20:28,154 --> 00:20:29,393
- Desert RAT stands for
400
00:20:29,394 --> 00:20:31,713
Desert Research and Technology studies.
401
00:20:31,714 --> 00:20:34,634
This is a group of
engineers and scientists.
402
00:20:34,635 --> 00:20:37,233
- We're looking to test out new concepts,
403
00:20:37,234 --> 00:20:40,514
procedures, equipment,
like rover concepts,
404
00:20:40,515 --> 00:20:42,114
to see how they work in
the field environment.
405
00:20:42,115 --> 00:20:44,394
- So the team tests these technologies
406
00:20:44,395 --> 00:20:47,075
to make sure that in future
human space flight missions
407
00:20:47,076 --> 00:20:49,514
we'll be able to do
science as best as we can.
408
00:20:49,515 --> 00:20:51,475
That's something that NASA's never done,
409
00:20:51,476 --> 00:20:54,075
two human rovers at the same time.
410
00:20:54,076 --> 00:20:55,795
So we're really trying to develop
411
00:20:55,796 --> 00:20:58,275
how do you use these
assets at the same time?
412
00:20:58,276 --> 00:21:00,554
And interesting things that
you might not think about
413
00:21:00,555 --> 00:21:02,394
are your communications.
414
00:21:02,395 --> 00:21:04,914
So you potentially have
four astronauts talking
415
00:21:04,915 --> 00:21:06,834
all at the same time to Mission Control
416
00:21:06,835 --> 00:21:08,675
or science communication backroom.
417
00:21:08,676 --> 00:21:10,594
- It's just like planning
a real mission, say
418
00:21:10,595 --> 00:21:13,114
like you kind of think about
Apollo missions.
419
00:21:13,115 --> 00:21:14,475
You had the astronauts on the moon
420
00:21:14,476 --> 00:21:16,515
and you had people, Mission Control,
421
00:21:16,516 --> 00:21:18,515
but there was a science
backroom you didn't hear about
422
00:21:18,516 --> 00:21:22,476
but the astronauts were
getting information from them.
423
00:21:22,477 --> 00:21:25,315
- Arizona has a very good climate
424
00:21:25,316 --> 00:21:27,356
for these types of analog studies.
425
00:21:27,357 --> 00:21:29,915
You have pretty much open
plains and you have a lot
426
00:21:29,916 --> 00:21:31,796
of geological features that are analogous
427
00:21:31,797 --> 00:21:34,357
to places on the moon and on Mars.
428
00:21:42,437 --> 00:21:45,715
- Long-term space voyages are
being replicated on the ground
429
00:21:45,716 --> 00:21:48,436
and in orbit with the ISS.
430
00:21:48,437 --> 00:21:50,756
Surface habitats, power systems,
431
00:21:50,757 --> 00:21:53,036
food and oxygen supply manufacturing,
432
00:21:53,037 --> 00:21:55,397
are also on the drawing board.
433
00:21:59,078 --> 00:22:00,997
- The human flight
component would like to see
434
00:22:00,998 --> 00:22:04,116
an experiment where resources
on the surfaces of Mars
435
00:22:04,117 --> 00:22:06,357
from the rocks or the
atmosphere could be used
436
00:22:06,358 --> 00:22:08,916
to generate fuel or other parts
437
00:22:08,917 --> 00:22:12,677
that would enable future exploration
438
00:22:12,678 --> 00:22:15,677
in cutting the tie, so to speak, to Earth.
439
00:22:15,678 --> 00:22:17,236
So you wouldn't necessarily have to bring
440
00:22:17,237 --> 00:22:17,998
everything with you.
441
00:22:17,999 --> 00:22:19,997
You can actually
manufacture it on the planet
442
00:22:19,998 --> 00:22:22,477
and that's a really exciting
additional component
443
00:22:22,478 --> 00:22:25,316
that we've been exploring and analyzing
444
00:22:25,317 --> 00:22:26,917
in this work.
445
00:22:29,639 --> 00:22:32,837
- NASA isn't the only one
with its eye on this prize.
446
00:22:32,838 --> 00:22:36,278
ESA and now the Indian
Space Research Organization
447
00:22:36,279 --> 00:22:38,517
have a spacecraft orbiting Mars
448
00:22:38,518 --> 00:22:40,999
and they did it on their first attempt.
449
00:22:42,238 --> 00:22:44,957
Private enterprise is
hard at work as well.
450
00:22:44,958 --> 00:22:48,278
Mars 500, Mars One, The Mars Society,
451
00:22:48,279 --> 00:22:51,638
Mars Foundation, and the Mars
Initiative, to name a few.
452
00:22:51,639 --> 00:22:54,278
And they have volunteers lining up already
453
00:22:54,279 --> 00:22:56,398
for a one-way trip to Mars.
454
00:22:58,238 --> 00:23:01,037
It is inevitable that
we will set foot on Mars
455
00:23:01,038 --> 00:23:02,517
in the very near future.
456
00:23:02,518 --> 00:23:05,440
We will stay and learn her secrets.
457
00:23:08,000 --> 00:23:09,279
Perhaps in the future
458
00:23:09,280 --> 00:23:11,759
we will be able to alter
the atmospheric density
459
00:23:11,760 --> 00:23:14,118
through terraforming and return Mars
460
00:23:14,119 --> 00:23:15,958
to the world that it once was,
461
00:23:15,959 --> 00:23:20,679
awash with oceans and
rivers, clouds and rain.
462
00:23:20,680 --> 00:23:23,839
Maybe some of us could call it home.
36765
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