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(eerie electronic music)
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- [Narrator] We have
been observing our home
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for 40 years now; in the last 20 of those
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we have focused intensely on Planet Earth,
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with new technologies and capabilities
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accumulating a massive
data that is now revealing
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a complex and ever-changing living planet.
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(dramatic fusion music)
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(eerie futuristic music)
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They've been watching us from space,
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for the last two decades
in high-resolution detail,
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watching our every move.
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Clouds and aerosols, winds and hurricanes,
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forests and cities, droughts and floods,
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the ocean currents and plankton,
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life in the ocean and on land.
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Land cover.
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Aerosols.
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Chlorophyll concentrations.
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Wave heights.
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Ozone concentrations.
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Atmospheric moisture.
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The human footprint.
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Sea-level change.
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And temperatures and moisture in the soil.
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Now scientists have a
high-definition dataset
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spanning two decades to
study and to learn from.
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- NASA has a fleet of satellites
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that are always measuring Earth.
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They're looking at land, oceans,
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atmospheres, ice, altogether.
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The particular visualization
represents the measurement
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of all life on Earth over 20 years.
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I personally find it mesmerizing.
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You're watching the Earth breathe here.
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The seasons are changing.
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Ice is coming in, and retreating.
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You can see the forests on land in green
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expanding and contracting.
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Can see the deserts moving to the ocean.
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You can see biological deserts
in the centers of the ocean,
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represented by blues and purples.
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And then, as you look further
north in the Atlantic,
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or towards Antarctica, you can
see these greens and yellows.
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Explosion of life in the ocean
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just like on land in
the spring and summer.
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Incredible.
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- What we see for the first time
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is how the oceans and the
land behave at the same time,
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through time, for 20 years.
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We've never had data like these before.
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Half of our photosynthesis
occurs in the oceans
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and the other half on land.
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Having these data to show
both at the same time,
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day after day, month after month,
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year after year for 20 years,
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is a great tool to study life on Earth.
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NASA has observed many aspects
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of the coupled
land-ocean-atmosphere system
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and how they interact.
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For example, we see that with
warmer surface temperatures,
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the growing season is getting longer
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at higher northern latitudes,
and spring is coming earlier.
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With satellite data we're able to map this
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continuously across the Earth's surface
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and across the United
States and across Alaska.
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Before that time, you had to rely
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where you had weather stations,
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and so you had points here, points there,
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but you never had
continuous data like these.
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Using these data, we can
look over very large areas,
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and see regional effects.
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Sometimes these effects are positive,
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and nothing bad has happened.
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It's only with these data
we're able to do this
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over all these areas at the same time,
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and this is made possible
by the use of Earth-viewing
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satellites, which orbit
the Earth day after day,
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month after month, year after year.
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These data are the basis for
saying these things about Earth
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with confidence because we measure them.
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- [Jeremy] The view from
space is opened our eyes
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to so many different things.
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You can see transitions
from La Nina to El Nino,
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represented by huge blooms of
life across the Pacific Ocean
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at the Equator, bigger and
wider than the United States.
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You can see greening of the Arctic.
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You can see earlier
summers, later winters,
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and you can see the emergence
of harmful nuisance algae.
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(aural music)
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- [Narrator] Charting the
carbon-dioxide cycle through
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the atmosphere, land,
and ocean is essential
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to understanding the environmental changes
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that man is driving.
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Higher carbon dioxide, or
CO2, in the Earth's atmosphere
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appears as red and yellow,
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while lower-than-average
CO2 is shown as blue.
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The pulsing of the data is due to
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the day-night cycle of
plant photosynthesis.
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As CO2 is lifted away from the surface,
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it is rapidly spread around the world
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by high-altitude winds.
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CO2 builds up in the
Northern-Hemisphere winter,
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when plants are dormant.
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By summer, photosynthesis
draws massive amounts
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of CO2 out of the atmosphere,
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resulting in lower CO2 throughout
the Northern Hemisphere.
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The growth and decay of
vegetation in the northern lands
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causes the seasonal
change in atmospheric CO2.
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Longterm, however, it is human activity
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that is increasing overall CO2 levels.
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- 2017 was the second-warmest
year ever recorded,
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and the warmest non-El-Nino year.
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That makes five of the warmest years
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ever recorded just since 2010.
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NASA scientists have
taken weather-station data
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from over 6,000 stations,
and we've connected the dots
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to understand how our Earth is changing.
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In this.
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Growing as we look at how much
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high latitudes in places like
Alaska have warmed since 1950.
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So, across the globe we're
seeing a consistent trend
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towards warming but with
twice as much warming
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across the high latitudes like Alaska.
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(aural music)
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- [Narrator] This rapid increase
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in overall global temperatures
is clearly defined
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when satellite data is added to the model.
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- The ability to expand
your senses into space,
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compress time, watch
visualizations like these,
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see how the ecosystems of
land, ocean, atmosphere,
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ice, all interact, and
then be able to rewind it,
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and watch it again and again,
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it's, yeah, it's amazing.
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(dramatic fusion music)
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(somber aural music)
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- [Narrator] Ask any astronaut.
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When they look down at Earth,
they see a single environment.
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No borders, no plains,
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just a single planet which
we all have to rely on.
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With this data, scientists can check up
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on the health of the plant.
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One primary concern is the Ozone Layer.
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- We know the Montreal
Protocol was a huge success.
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This was signed in late 1980s,
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when scientists and policymakers
from around the world
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gathered together to try
to save the Ozone Layer.
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- The chemicals they regulated persist
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in the atmosphere for many decades.
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They thin the Ozone Layer,
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and they create a seasonal
hole over Antarctica.
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They basically take away
part of our planet's
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natural sunscreen, and
that increases the risk
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of skin cancer and damage to plants.
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- [Narrator] Scientists have
projected the ozone hole
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will disappear almost completely by 2075.
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But several factors
could delay that outcome.
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- There're some industrial compounds
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that did not banned by
the Montreal Protocol,
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but as they enter the atmosphere,
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they will also hurt the Ozone Layer.
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- But the unregulated
compounds have a short lifespan
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in the atmosphere, unlike
the chlorofluorocarbons
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that were originally regulated.
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So they have a short-lived
impact on ozone,
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and we don't think they'll delay recovery
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by more than a few years.
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- We've projected, by 2050 more than half
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of the ozone-depleting
compounds in the atmosphere
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will come from long-lived
substances banned by the protocol.
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- [Narrator] Because these
compounds stay in the air
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for such a long time,
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compared to the unregulated
short-lived compounds,
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they will have a disproportionate
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and lingering impact on ozone.
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Any noncompliance with protocol
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can have significant consequences.
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- The really big uncertainty
in Ozone-Layer recovery
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is climate change.
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There're many naturally-produced
ozone-depleting substances
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that're emitted by the oceans,
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and as the oceans continue
to warm due to climate change
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those emissions will increase,
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and that will further
delay ozone recovery.
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- [Narrator] Scientists
want to understand better
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how climate change will
affect ozone recovery.
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- This is a hard problem.
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As a scientific community,
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we need to work on this major issue.
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We now have a powerful new
tool to simulate atmosphere
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and its interaction with land
and ocean to study this issue,
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and that's what we're going to do.
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- [Narrator] At the top
of the world, however,
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the arctic ice continues to shrink.
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(concerned aural music)
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- Sea ice is the ice that grows
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and melts within the Arctic Ocean.
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It grows in the wintertime
when it gets cold,
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and melts during through the summertime.
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It doesn't raise sea level
but it's very important
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for the global climate system
because the ice is very bright
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and reflective, reflects
a lotta the Sun's energy
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that comes in during the summertime
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and helps keep the Arctic cooler.
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It's like a refrigerator for
the global climate system,
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by keeping the globe cooler
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than it normally would be without sea ice.
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As we lose the ice,
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it's like we're opening
the refrigerator door,
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and not cooling things as
efficiently as we used to.
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- [Narrator] Constant
observation since the '70s
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lets us see a trend.
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- The Arctic sea ice has
been changing quite rapidly.
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We've seen a decline over
35-plus years of our record.
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The last 15 years, particularly,
it's been accelerating.
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So, really, it's become a matter of when,
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not if we lose the Arctic sea ice,
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because we have a lotta
warmth in the Arctic,
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it's gonna continue to warm,
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we're gonna continue to melt sea ice.
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There's uncertainty as to
exactly when that will happen,
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but sometime in the
not-too-distant future,
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faster than we used to
think, the Arctic Ocean
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will be substantially
ice-free by the end of summer.
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Arctic sea ice is not the only place
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we're seeing big changes.
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We're also seeing big
changes in Greenland,
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which is the big massive
ice on top of the continent,
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and we're seeing more and more melt,
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we're seeing ice calving off as icebergs.
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We're seeing big masses of ice loss
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over the last several years.
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That means that that ice
is going into the ocean,
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that's raising sea level.
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That's gonna have big
impacts down the road
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as we continue to lose more
and more ice from Greenland.
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(concerned aural music)
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- [Narrator] Ancient air
bubbles trapped in ice
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enable us to step back in
time, and see what Earth's
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atmosphere and climate were
like in the distant past.
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Today we stand on the
threshold of a new geologic era
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which some term the
Anthropocene, where the climate
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is very different to the
one our ancestors knew.
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- We can see that a warmer world means
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that there's an impact
for warming temperatures
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in the Arctic, melting sea ice.
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That sea ice leads to
larger sea-level rise.
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NASA scientists are on
the ground, in airplanes,
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and using our satellite data
to understand how what starts
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in the Arctic doesn't
exactly stay in the Arctic.
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(dramatic fusion music)
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- [Narrator] The hope is
that all this data collection
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will mean that real-world
problems can be reassessed
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and new angles explored.
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A case in point: dolphin
and whale stranding.
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Could this accumulated satellite data
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help address the problem?
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Cape Cod in the US State of Massachusetts
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is home to one of the most
frequent marine-mammal
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stranding sites in the world.
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- If we can get there quickly,
and provide supportive care,
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they have a much better
prognoses in terms of survival.
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- [Narrator] Scientists
know very little about why
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these mammals strand, and only a quick
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and efficient response in
these events will save lives.
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Katie Muir works on the frontline,
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and has fine-tuned rescue efforts.
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- If we can develop an
algorithm that pieces together
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the different variables that
may be causing mass strandings
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or driving mass strandings,
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then we have the ability
to then prevent them.
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We can have teams that
are out on the shore
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looking for animals in those hotspots,
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knowing that all those
variables have come together
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and this is a likely point in time
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where we're likely to see it.
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But we can also have
teams ready to respond
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so that if they do strand,
we're there that much faster,
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and more animals will survive the event.
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- [Narrator] Marine biologists from
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the US Bureau of Ocean Energy Management
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were also looking at this problem.
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- For the large proportion
of these strandings,
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the animals are across the
ages, in pretty good health,
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and there's no really immediate evidence
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as to why they actually strand.
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- [Narrator] One possibility
is geomagnetic perception:
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the ability to navigate
using Earth's magnetic field,
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which is believed to be
used by marine mammals.
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Could changes in the magnetic
field confuse the animal?
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Geomagnetic pulses or storms
can be caused by space weather.
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- Geomagnetic perception
is one of the theories.
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I thought: "Well, hmm, if a
magnetometer can pick it up,
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"maybe the animals
actually can pick it up."
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- [Narrator] Dr. Reeb consulted with NASA
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at the Goddard Space Flight Center.
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- [Scientist] The coolest
thing was that we realized
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that nobody had really
taken a cold hard data
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science analysis look at the problems.
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- What we're trying to look at here
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was if there was a potential
driver or relationship
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or correlation between the
occurrence of mass strandings
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and any solar activity.
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- The data that we have
correlated, or analyzed so far
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is information about the
local geomagnetic conditions.
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We have long data records
from geophysical observatories
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of the local geomagnetic-field variations
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and marine-mammal stranding.
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- [Narrator] Their
analysis was inconclusive.
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They needed more data from
other environmental conditions.
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- Easy-fix correlation
between a geomagnetic pulse
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and, ooh, a stranding, doesn't
seem to be very evident,
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but what it does show is that
there are multiple variables
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involved in this equation and
that the geomagnetic storms
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could just be one very small
part of it, significant still.
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But, it looks like there
are multiple oceanographic
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and environmental elements.
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- [Narrator] With more data in hand,
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it was time to expand the team.
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They recruited statisticians
and the expertise
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of NASA Earth-science data analyst
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and oceanographer Erdem Karakoylu.
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- A dataset, no matter
its shape or content,
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always has a story to tell.
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Trying to figure out how
different data are connected,
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I think, require a wide
diversity of skills
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and background knowledge.
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- For example, I'll be explaining
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how a mass stranding occurs
and how we respond to try
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and understand why I'm presenting
the data in a certain way,
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and my colleagues from
NASA will look at me,
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and ask questions that
wouldn't think to ask
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because I take for
granted my understanding,
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and they're coming at it
from a totally new angle
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with no background.
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- [Narrator] These datasets
may reveal a pattern,
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allowing scientists to
predict the likelihood
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and location of mass
stranding before it happens.
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- We've really sort of
slowly peeled the first layer
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of this onion back, and I
think that there's so many
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more layers that still need
to be addressed and looked it.
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I hope that we can actually
find additional collaborators,
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additional funding partners
to really bring all the data
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that's really available
to really give this
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the study and the
scrutiny that it deserves.
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- We are also going other
make all these datasets
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available to the entire
scientific community
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so that we can utilize the
entire scientific community,
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attack, and a new
approach to this problem.
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- I think that there will be other things
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to take and run with, get new
ideas, maybe add more data.
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I'm hoping also there will be a model
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for how projects can then be
opened to the wider public.
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(emotional music)
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- The ability to release animals
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after they've stranded is tremendous.
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When we do that, that's the
best feeling in the world
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after all of that hard work.
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- Those questions that seem unanswerable,
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if you give them time
and support and effort
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and put people on them,
we can do amazing things.
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(emotional piano music)
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(dramatic fusion music)
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- [Narrator] Data from satellites reveals
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the interconnection
between air, sea, and land.
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This is a visualization of three aerosols:
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dust, smoke, and sea salt.
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The CALIPSO-Satellite data reveals in 3D
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how dust from the arid Sahara Desert
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is lifted by the winds
each year, and transported
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nearly 5,000 kilometers
across the Atlantic Ocean.
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(pensive music)
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Some of it settles in the Amazon Basin,
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the largest rainforest on the planet.
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Sahara dust contains phosphorus,
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an important nutrient for plants.
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CALIPSO shows that, on average,
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182 million tons of dust
leaves Africa each year.
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When the Sahel was dry, the dust transport
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to the Amazon in the
next year would increase;
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when it was wet, dust
transport would decrease.
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We can now track global
precipitation, wind currents,
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cloud cover, and ocean temperature.
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Satellites have detected
a shift in phytoplankton
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populations across the planet's
five great ocean basins,
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showing the expansion of biological desert
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where little life thrives.
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Diatoms are one of the most abundant types
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of marine phytoplankton, but
a new 15-year-long NASA study
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reveals global populations have declined.
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Diatoms, like all
phytoplankton, have chlorophyll,
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the same photosynthesizing
pigment as plants.
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They occupy the surface of the ocean,
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where they harvest light from the Sun.
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In large numbers, diatoms
form colorful swirling blooms
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that can be seen from space.
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According to the study,
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significant decreases in
populations, shown here in red,
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are mainly in the Northern Hemisphere.
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- Diatoms rely on nutrients
such as nitrate, silicate,
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and iron to reach the surface
layer where they live.
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What the study shows is
that the availability
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of these nutrients has changed
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due to the Wave Cycle
within the water column.
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- [Narrator] Diatoms occupy
the surface area of the ocean
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called the Mixed Layer.
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Nutrients collect on the ocean floor,
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and are cycled up to this layer.
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00:21:30,370 --> 00:21:32,630
Various physical forces
can cause the depth
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00:21:32,630 --> 00:21:34,800
of the mixed layer to become shallower
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so that fewer nutrients reach the diatoms.
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Without these, their populations decline.
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This map shows areas on the globe
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where the depth of the
Mixed Layer shallowed.
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- It's hard to pinpoint exactly
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why these change have happen.
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Things like wind, circulation,
and temperature can affect
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the way these nutrients are
brought to the surface layer.
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We hope a longer study
can yield more information
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00:22:00,410 --> 00:22:02,990
on whether these changes are, in fact,
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a trend or variability.
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00:22:05,760 --> 00:22:10,010
(majestic orchestral fusion music)
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- [Narrator] Next-generation satellites
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are reaching orbit now to
continue this important work.
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They will collect data,
maintain observation continuity,
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00:23:01,930 --> 00:23:03,400
and allow scientists to track
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00:23:03,400 --> 00:23:04,950
the changes in our environment.
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They can then model dynamic simulations
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00:23:08,370 --> 00:23:11,310
to better understand this unique planet
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00:23:11,310 --> 00:23:15,005
and the myriad of
lifeforms that rely on it.
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00:23:15,005 --> 00:23:19,255
(majestic orchestral fusion music)
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00:23:37,070 --> 00:23:40,403
(dramatic fusion music)
34993
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