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(suspenseful ethereal music)
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- [Sue] Venus and Earth
are the twin planets.
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We've seen thousands of
exoplanets around other stars
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but Venus is still the
planet most like Earth.
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- [Tony] The surface of Venus
is hot enough to melt lead.
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- [Jonathan] Venus is incredibly hot,
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it has what we call a runaway greenhouse,
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where it's sort of the
extreme state of what happens
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if you let a greenhouse
go completely crazy
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on an Earth-like planet.
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- [Rosaly] Venus is kind of a warning
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that we have to pay
attention to what's happening
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to the atmosphere of the Earth.
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We don't want the Earth
to become evil like Venus.
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(suspenseful ethereal music)
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- Venus and Earth are
actually really similar
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in many, many ways.
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They are almost exactly the same size,
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and they have similar gravity.
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Venus has about 90% of Earth's gravity.
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And we think that they both
formed in a similar part
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of the solar system at about the same time
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from more or less the same materials.
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So they, they really should
have a lot of similarities,
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we see they both have atmospheres,
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they both show the same
types of geologic processes
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on their surfaces with volcanoes
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and tectonic regions,
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which is where the crust is moving around.
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- It's the only planet
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that is likely to be
still geologically active
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in some of the same ways as, as the Earth.
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It has a similar bulk composition.
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It has an atmosphere, a huge atmosphere,
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one of the very few
plants in our atmosphere
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to have a huge atmosphere.
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- [Lori] That thick carbon
dioxide atmosphere acts
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as a greenhouse,
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warming the surface to
hundreds of degrees Fahrenheit,
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and pressures that are
like being about mile deep
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in the ocean.
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At Venus, there's no magnetic field,
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whereas at Earth, there is.
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- [Rosaly] So Venus is kind of
the Earth's evil twin sister.
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It shows how two worlds of
similar size, similar density,
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not that far apart in terms
of distance to the sun,
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evolved very differently.
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- So the real core
question it comes down to
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is what was it in Venus's
and Earth's history
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that made these two similar planets
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take very different paths.
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And then how do we apply that
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to planets beyond our solar system
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and look at how understanding
Venus could help us
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better understand what
exoplanets are like,
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and which ones are the ones
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that could potentially
harbor life like Earth?
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And which ones are those
that are like Venus
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and are very hostile to life?
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- [Mike] We believe that
Earth and Venus formed
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around the same time in our
original circumstellar disc.
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They are probably
geo-chemically very similar
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because they formed very close
to each other in the disc,
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much closer than Earth did
to Mars and from what we know
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about the geo-chemical similarities
between Venus and Earth
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and Earth and Mars,
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certainly we believe that
Earth is more similar to Venus
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than it is to Mars.
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We don't know that much about Venus
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because we haven't sent
enough missions there
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as we have for Mars.
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It does have similar
amounts of carbon dioxide
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in its surface and in its
atmosphere compared to Earth.
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- Venus is, in some
sense, the poster child
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for the greenhouse
effect of carbon dioxide.
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It's a planet that has
much more carbon dioxide
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than the Earth has in its atmosphere.
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And even though it is covered
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by this bright sulfuric acid haze,
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Venus reflects 70-something
percent of the sunlight
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that reaches it, so even
though it's very close,
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it actually doesn't get
nearly as much sunlight
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as you imagine because of that haze.
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Yet it's got this crushingly hot surface.
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And the only way to explain that
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is because of the greenhouse
effect of the carbon dioxide.
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Venus tells us
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that the greenhouse effect
is a real phenomenon.
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- [David] Venus, in many ways,
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is an extreme case of some of
Earth's environmental issues.
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I mean, the most obvious
one being global warming
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and the greenhouse effect,
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which is something we're
all obviously aware of
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here on Earth because the
amount of CO2 has risen
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above 400 parts per million,
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and that is causing global warming
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because of the infrared absorption of CO2.
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And yet here's Venus, the
Earth-sized planet next door
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with an atmosphere that
is almost 100% CO2.
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Venus, as far we can tell,
was a habitable planet
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for some time
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before it went through this
runaway greenhouse transition.
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- Imagine a graph where we have,
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you know, temperature versus CO2.
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And so Earth is in this section over here,
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right, 'cause we have this much CO2.
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So if we want to understand this process,
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Venus offers data up here, right?
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Another set of data points that we can use
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to sort of link how much CO2
do we need before this happens?
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When do we get into a position
where we're really in trouble
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and there's nothing we can do about it
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except move to Mars?
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- [Tony] We don't expect the Earth
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to turn into Venus anytime soon.
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Humankind is putting more
and more carbon dioxide
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into the atmosphere
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as humankind has been doing
now for a few centuries,
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since the Industrial Revolution began.
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We know that the climate
is going to get warmer.
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How warm it will get depends
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on how much carbon dioxide
we put into the atmosphere.
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Humans are not going to be able
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to put enough carbon
dioxide into the atmosphere
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to turn the Earth into Venus.
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- So there's this whole long-term cycle
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where the carbon comes out of volcanoes
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and ends up in the atmosphere
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and then gets pulled out by chemistry
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and made into carbonate rocks,
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which get deposited on the ocean floor
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and then subducted by plate tectonics
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into the interior of the planet
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and ultimately sort of heated and squished
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to the point where the carbon
dioxide is, is released
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and then comes out again in a volcano.
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That's a cycle that
takes millions of years
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and it ultimately regulates the carbon
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in Earth's atmosphere, of course,
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recently, we've been perturbing
it with our automobiles
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and smoke stacks and things,
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but that's all probably a
temporary sharp perturbation
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in what is a multi-million-year cycle
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that's been operating
for billions of years.
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Now, compare that to Venus.
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We think that early on Venus
probably had a similar cycle
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because it has volcanoes,
it had volcanoes,
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it's probably been volcanically
active its whole life.
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And it used to, we believe, have an ocean
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which facilitated those
weathering reactions
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that pull carbon dioxide
out of the atmosphere.
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- Part of the issue is that
Venus no longer has an ocean.
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We think it had an ocean
earlier in its history,
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we don't really know when water was lost.
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Having an ocean is an important part
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of pulling carbon dioxide
out of the atmosphere.
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We think that Earth and
Venus have similar amounts
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of carbon dioxide.
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But, on Earth, those are
locked up in carbonate rocks.
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And those carbonate
rocks often are subducted
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back into the interior,
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sequestered, in effect,
by geologic processes.
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- [Martha] So you need an ocean.
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And we hope that we can find evidence
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in early Venus history of sequestering
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of carbon in rocks.
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That's what we look for on Mars,
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that's, a lot of Mars
work has been to look
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for those carbonate rocks on Mars.
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What Venus shows us, without a doubt,
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is that there is a relationship
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between the amount of CO2
you have in an atmosphere
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and the temperature.
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- [Sue] Will the Earth
become 500 degrees Celsius,
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900 degrees Fahrenheit?
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That's really not likely to happen.
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But understanding chemical reactions
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in this very active
atmosphere that Venus has
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is so important for
being able to understand
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how climate change comes about.
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What are the important chemicals,
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what are the important processes?
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So we really have a lot to learn
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from the atmosphere of Venus.
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- [David] For example, acid
rain is a problem here on Earth
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because of sulfur dioxide
from our smoke stacks
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getting into the clouds
and mixing with water
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and making strong acid.
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Well, Venus, again, is sort
of the poster child for,
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for that condition with clouds
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that are basically made
out of purer sulfuric acid,
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and so it's, it's a place
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where we can study this
environmental problem, acid rain,
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in its most extreme manifestation.
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And to give one more example,
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another problem of our own making
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is the problem with the ozone hole
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and the ozone layer being eroded
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by these chemicals,
these chlorofluorocarbons
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that we released into the atmosphere
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where the chlorine gets loose
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because of ultraviolet
light in the stratosphere
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and destroys ozone, which
then becomes a threat
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to life here on the surface of the planet.
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Well, one of the ways we
discovered the ozone layer
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was being eroded on Earth came about
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because we were studying the
upper atmosphere of Venus.
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- [Sue] Venus's atmosphere
is so intriguing.
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We actually found the
ozone hole on the Earth
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because people were studying chemistry
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of what was going on in the atmosphere,
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upper atmosphere of Venus.
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- Some scientists were
trying to understand why,
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why isn't there more ozone on Venus,
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why aren't there more oxygen compounds
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in the high atmosphere of Venus?
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And some other scientists
said, well, you know,
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we've seen these experiments with chlorine
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and chlorine can, can
destroy oxygen compounds.
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And then they came out with a paper
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saying we think it's chlorine
that is destroying ozone
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on Venus.
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Some other scientists saw that paper.
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- And it made them ask
this question, well,
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what's going on in the
upper atmosphere of Earth,
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are there similar types of
chemical reactions going on?
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- And they said, oh, that's interesting,
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what about these, these chlorine compounds
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that we're putting up into
the atmosphere on Earth,
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that, couldn't that, and they
said, uh oh, wait a minute.
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And that helped them
realize what was happening
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and help them sort of sound the alarm.
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- Look at that huge
difference that that made
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in terms of discovering
the ozone hole on the Earth
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and, you know, since
people have taken action
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to actually stop putting those
chemicals into the atmosphere
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that was creating such
a destructive process.
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- And, indeed, that's an
example where we've responded
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in a healthy way to this knowledge
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that we were doing something to our planet
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and have taken measures to fix it.
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And it came about
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partly because we were studying
this neighboring planet
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out of pure curiosity,
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trying to understand the chemistry there.
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- The link between innovation
and expanding our thinking
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is not linear.
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In science and technology,
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you don't plan for that necessarily,
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you don't say, okay, I'm gonna
discover this great thing,
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and I'm gonna start here,
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and I'm gonna, at the end
will be this great discovery.
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That comes from a lot of
tries and a lot of failure.
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And if we don't push at the limits
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of what we can do as a
society, we won't succeed.
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That's the way it works.
257
00:11:17,780 --> 00:11:19,920
That's what we do as scientists.
258
00:11:19,920 --> 00:11:22,060
That's why we sail across the ocean.
259
00:11:22,060 --> 00:11:23,420
That's why we climb the mountain.
260
00:11:23,420 --> 00:11:26,150
And that's why we should go to Venus.
261
00:11:26,145 --> 00:11:29,475
(mellow ethereal music)
19811
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