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It rises in the east and
bathes our planet in light. It
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powers the machinery of nature,
our weather, encourages and
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sustains life on land and at
sea where it warms our oceans
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from pole to pole. When it
sets in the west, it reveals to
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us its many billions of sibling
stars, populating the night
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sky. We study our sun closely,
and like a Rosetta stone, it
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can reveal the secrets of all the stars.
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You cannot study the sun in isolation.
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The influence of its
power throughout the solar
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system it created is
persuasive and dominating.
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The heliosphere is an immense
magnetic bubble extending
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beyond the orbit of Pluto.
It contains the solar wind of
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high and low-speed
energetic particles and
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plasma that originate
at the surface of the sun.
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After traveling for 36 years
and 19 billion kilometers,
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the Voyager 1 spacecraft
has reached the edge of this
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heliosphere.
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Voyager 1 has left the bubble
around the sun and entered
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interstellar space, the space
between stars. There it still
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senses the shock waves emitted
by the sun, which sound like this.
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To understand this source
of power and its influences,
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scientists conduct observations
from the ground and in
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space, where a flotilla of
satellites trains sophisticated
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sensors upon the sun and the
space weather it creates. Space
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weather is the field that
studies how what's going on on
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the sun affects us here on
the earth in our near space
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environment and on the space
environment on other planets.
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The effects of space weather
are so complicated because we
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have to understand what's
going on at the sun as well as all
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that stuff traveling through
interplanetary space, how that
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affects and throughout the
heliosphere, that we need
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an entire fleet of instruments
to look at these various
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effects. It's basically a system
science, so you understand
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one part of it in order to
understand the other part of it,
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and you have to put
that whole puzzle together
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to understand the full
effects of space weather.
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GOES-P is an ongoing series
of Earth observation satellites
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that happen to keep a constant
eye on the sun, monitoring
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this space weather. So the
spacecraft sitting in space, it's
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looking down at the earth
and it stays stationary like this,
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but this solar array out here
moves and tracks the sun, so
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that way it's always looking
at the sun and can take a scan
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every minute. The sun's outer
atmosphere is constantly being
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heated up by the solar
surface, and this causes particles
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from the sun's atmosphere to
stream away constantly. These
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streaming particles, which
are filling our entire solar
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system, are called the solar
wind. Different phenomenon from
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the sun is constantly bombarding
the earth. Although you
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might not know it, the solar
weather affects you every day
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down here as well, not
only just astronauts, it affects
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people on earth. The
latest generation of GOES
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satellite is the GOES-R,
soon to be launched into orbit.
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Other low-air-forbiting
platforms include ESA's micro
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-satellite PROBAT-2, testing
new technology, and PICAR,
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sponsored by CNES, the French space agency.
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Hinode is the Japanese
word for sunrise. It is a joint
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mission between JAXA, NASA
and ESA to study the sun's
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magnetic cycles. Its close-up
study has revealed the complex
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granular textures of the
sun's surface and insights into
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solar flares.
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A solar flare is a huge
release of energy that converts
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the magnetic energy of
the sun into heat, into light, it
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accelerates particles, and
can really heat up the plasma
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in order of minutes to over
60 million Kelvin. For a large
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eruption, the sun produces
a flash of light, which we call
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the solar flare. It also
produces a huge ball of material
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traveling away from the sun
we call coronal mass ejection.
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And both of those phenomena
can accelerate subatomic
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particles, which we call
solar energetic particles.
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These three things together
make up a solar storm.
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To study the solar wind
phenomenon, a group of satellites
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were placed in a unique orbit
between Earth and the sun at
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what is called L1, or
Lagrange Point 1, a point of
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gravitational balance between
the Earth and the sun. The
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Advanced Composition Explorer,
or ACE, observes energetic
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solar particles. Wind studies
radio waves and plasma that
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occur in the solar wind and
in the astromagnetosphere
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and SOHO, the Solar and
Heliospheric Observatory.
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Using SOHO and using technique
called helioseismology, very
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similar to seismology on the
Earth, we're actually able to
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see inside the sun. And so
what we were able to do is see
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the layer of the sun just
below the visible surface that we
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call the convection zone.
And that's where all sorts of
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dynamics are going on. The
inside of the sun is bubbling up
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to the surface. And that's
really where all of the solar
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phenomena that we see is
first developed. And so we were
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able to see underneath the
surface and see these flows of
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solar plasma, see the
formation of sunspots. And this is
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something that's never been
done before. We're actually able
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to see the details inside of a
star. Another high-resolution
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space telescope was TRACE.
You're seeing details of the
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coronal loops. In the previous
images from other satellites,
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it would look like it was just
one big loop. And when you're
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actually going to see TRACE,
you can see it's all these
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teeny tiny, finely, they
almost look like threads. And
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there's these teeny tiny
loops. And they're just breaking
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off and reforming and throwing
plasma. Using X-ray and gamma
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ray solar flare imaging, RISI
explores the particle physics
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behind solar flares. Another
event subjecting the solar
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system to bombardment is the
CME, or coronal mass ejection,
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event. A coronal mass
ejection, or CME, is an eruption of
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plasma from the sun that
shoots out into space. And it could
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affect us here at Earth if
that big ball of plasma were to
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hit us. NASA's twin stereo
mission has one spacecraft orbit
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the sun ahead of the Earth
and the other behind, providing
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a stereoscopic view of the
sun to better understand these
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coronal mass ejections
and the energetic particles of
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plasma. Solar energetic
particles are particles of plasma
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that are accelerated at
the flare site from the energy
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that's released in the flare.
And these particles can be
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accelerated up to almost
80% of the speed of light. And a
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coronal mass ejection, when
it's traveling so fast, creates
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a shock. And that can create
solar energetic particles. In
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2009, NASA commenced a new
scientific program called Living
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with a Star.
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The crown jewel of this
program is the Solar Dynamics
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Observatory, or SDO, the
most advanced spacecraft ever
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designed to study the sun
and its dynamic behavior.
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The program's goal is
to develop the scientific
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understanding necessary to
address those aspects of the sun
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that directly affect us here
on Earth. The spacecraft
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provides 16-megapixel
ultra-high-definition imagery of the
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sun in 13 different wavelengths.
From extreme ultraviolet
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frequencies to the helioseismic
and magnetic imager and the
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atmospheric imaging assembly,
each wavelength was selected
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to highlight a particular part
of the sun's atmosphere. The
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results are stunning. They
reveal fine details from the
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solar surface to the upper
reaches of the sun's corona.
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These solar events dwarf
our planet, and the science has
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brought a renewed focus back
to Earth's protective magnetic
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field. We are protected here
on the surface of the Earth
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from solar flares and coronal
mass ejections when they
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impact the Earth due to the
magnetic field of the Earth
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called the magnetosphere,
which deflects the magnetic field
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and the energetic particles,
as well as the atmosphere,
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which absorbs the higher
levels of radiation. Fortunately,
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we are protected here at Earth
from flares and coronal mass
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ejections by the Earth's outer
atmosphere. It absorbs a lot
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of the energy from the
increased light from solar flares,
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but we're also protected by
the magnetic field. You know,
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the Earth has a north pole and
a south pole. Anyone who has
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a compass knows that. But
this magnetic field of the Earth
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also protects us from these
charged particles, the plasma,
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coming from coronal mass
ejections that largely deflects a
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lot of this direct energy. A
coronal mass ejection will
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come and affect the Earth's
magnetic field, and changing and
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hitting the Earth's magnetic
field causes other changes
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on the actual far side away
from the Earth that then
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accelerates more particles
and shoots those particles
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then into the north and south
pole that produce these very
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beautiful waves of green and blue
and red that are just lovely to see.
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The sun is powered by a
process called fusion, and that
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happens at the very core of
the sun, where it is so intense,
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so hot, and so dense that
protons fuse together and create
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helium. And this process fuels
the sun and creates energy.
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As the energy moves outward,
boosted by magnetic fields,
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the temperature drops. Up
until that point, everything makes
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sense in that the hottest
part is in the middle and
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everything gets gradually
cooler as we move away, but then
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something very interesting
starts to happen, which is
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that it starts to get hotter
again. This layer, where the
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temperature begins to
rise again, is called the
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chromosphere. It lies between
the photosphere and the
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corona, which is the hottest
part of the sun's atmosphere.
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To discover how this corona
is powered, another mission
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called IRIS was launched in 2013.
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IRIS carries a single
ultraviolet telescope and imaging
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spectrograph, whose tight
resolution allows it to see
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features as small as 240
kilometers on the sun's surface.
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IRIS's first images showed
a multitude of thin, fibril-like
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structures that have never
been seen before, revealing
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enormous contrasts
in density and
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temperature occurring
throughout the region.
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The light from the chromosphere
is difficult to interpret
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because of the complicated
interaction that the light has
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with the matter. It bounces
around, if you will, many times
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before its final bounce
towards us. This means that that
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interaction between light and
matter needs to be modeled
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in great detail. Due to not
just advances in computational
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power of computers, but in the
computational techniques that
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have been developed by the
IRIS team, we are in a position
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to do this. Data collected
from the IRIS spacecraft has
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shown that the interface
region of the sun is significantly
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more complex than previously
known. Although the corona is
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extremely hot, millions of
degrees, it's at a low density,
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so it doesn't actually take
a lot of energy to heat it to
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that temperature. The
chromosphere, on the other hand, is a
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much higher density, albeit
lower temperature, and there's
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much more energy deposited
in the chromosphere than in the
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corona, so that a tiny
fraction of that energy in the
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chromosphere escaping into
the corona is plenty to power all
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of the processes that we see,
from heating to such extreme
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temperatures to driving the
solar wind that fills the whole
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solar system, impacting all
the planets, including our own.
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We hope to better understand
these fascinating and important
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processes with IRIS.
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This energy streaming
from the sun causes other
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knock-on effects on the
planets of the solar system.
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The northern lights are
particles that are being shot
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into the North Pole and the
South Pole that produce these
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beautiful greens and blues
and reds. They're not direct
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particles from the sun. A
coronal mass ejection will come
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and affect the Earth's
magnetic field, and changing and
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hitting the Earth's magnetic
field causes other changes on
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the actual far side, away
from the Earth, that then
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accelerates more particles
and shoots those particles then
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into the North and South
Pole that produce these very
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beautiful waves of green
and blue and red that are just
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lovely to see. Armed with
more questions about the solar
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wind and energetic particles,
NASA launched a pair of probes
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into Earth orbit. Named
after the famous scientists who
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discovered the radiation belts
surrounding our planet, the
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Van Allen probes were
dispatched to study the radiation
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phenomenon and the magnetic
fields around the Earth in
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greater detail. During the
course of geomagnetic activity,
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disturbances caused by
flares on the sun, by big blobs of
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plasma coming out from
the sun towards the Earth, the
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Earth's magnetic field is
battered and shaken. Some of that
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energy is captured in the
Earth's magnetic field, and
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through a variety of
processes, that energy energizes
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particles in the Earth's
radiation belts up to energies
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that are hazardous to spacecraft
and astronauts. The two
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spacecraft are focused on
the dynamic radiation belts in
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the Earth's inner magnetosphere.
They're the only spacecraft
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that focus on those.
Consequently, they're a critical
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component in the series of
phenomena that link the sun to
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the Earth.
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Solar flares and CMEs
are all driven by magnetic
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reconnection. This is where
the sun turns up the magnetic
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field that's inherent in it,
and then it causes oppositely
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directed magnetic fields to
then annihilate. But you can't
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just get rid of energy, you
have to convert that energy
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and transfer that energy into
other things such as plasma
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motions, accelerating the
plasma, heating up the plasma,
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and also giving out more light.
We are protected here on the
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surface of the Earth from
solar flares and coronal mass
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ejections when they impact
the Earth due to the magnetic
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field of the Earth called the
magnetosphere, which deflects
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the magnetic field and the
energetic particles, as well as
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the atmosphere, which
absorbs the higher levels of
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radiation. But this magnetic
field of the Earth also
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protects us from these charged
particles, the plasma coming
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from coronal mass ejections
that largely deflects a lot of
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this direct energy. The
phenomenon of magnetic reconnection
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is not well understood. So
NASA has launched a multi
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-satellite mission called MMS
to try to unlock the secrets
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of our magnetic field. The
MMS mission is a mission
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consisting of four spacecraft
which will fly in close
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constellation to measure
a process called magnetic
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reconnection. The universe
is full of plasma, and it's full
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of magnetic fields, and all
over the place in the universe
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you have one plasma colliding
with another. An example of
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that is the solar wind coming
in and colliding with Earth's
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magnetosphere. And then the
magnetic energy in the plasma,
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some fraction of that magnetic
energy is converted very
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rapidly into plasma energy.
So you can think of it as
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kind of like a magnetic
explosion. And the reason this is
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important is because these
explosions drive a lot of the
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weather patterns that we see
in the magnetosphere, and so
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what space scientists like
to refer to as space weather.
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And these space weather
phenomena can have impact on our
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everyday lives. It can
actually affect communication
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satellites, the power
grid. So we'd really like to
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00:18:39,440 --> 00:18:42,303
understand how these magnetic
explosions work. We need to
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measure reconnection in more
than one location. We need to
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measure basically how it
varies in space, how it varies
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in all three spatial
dimensions. And that requires a
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tetrahedron. The additional
fantastic benefit that that
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provides is that it will
actually enable us to recognize
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that we are looking with a
reconnecting region much easier
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than a single spacecraft.
The ideal situation is that we
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would like the four spacecraft
to kind of be surrounding
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this region where the
explosion is happening. So the
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separation of the spacecraft
is about 10 to 100 kilometers,
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which may seem like a long
distance. But in terms of the
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magnetosphere, which is
absolutely huge, this is really a
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00:19:20,330 --> 00:19:23,340
microscopic region that we're
trying to cover. MMS has in a
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nutshell two orbital phases
which are designed to study
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reconnection. On the day
side, basically you have a
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situation where the solar
wind is just constantly running
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into Earth's magnetic field.
And this is really great for
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MMS because we know that
at some point MMS is going to
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encounter this region. And
our hope is that since this
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process is always happening,
we're going to get lucky and
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actually fly right through
the magnetic explosion as it's
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happening. Now on the night
side, the situation is a little
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bit different. So what happens
is you have a more gradual
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buildup of magnetic
energy in the tail. And these
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reconnection processes, these
magnetic explosions, can just
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sort of pop off randomly.
We don't really know when it's
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going to happen or where
it's going to happen in the tail.
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We need to understand both of
those if we want to understand
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how the magnetosphere
works. And we believe that both of
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those scenarios are also
very important for other
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applications, such as on
the Sun, in the solar wind, in
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planetary magnetospheres,
and in many astrophysical objects,
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as well as in the laboratory.
We hope that it's going to
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allow us to improve our models
so that we can put the right
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physics in it and actually make
predictions about where and
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when reconnection is going
to happen. The magnetic
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explosions will help us make
our space weather models more
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predictively powerful. The
instruments that are actually
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going to be measuring the
particles in space are collecting
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00:20:40,900 --> 00:20:44,105
them much more rapidly at a
much higher cadence than they
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00:20:44,117 --> 00:20:47,500
have on previous missions,
about a factor of 100. So whereas
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00:20:47,500 --> 00:20:51,091
it would take a previous
generation particle instrument
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00:20:51,103 --> 00:20:54,900
about three or four seconds
to build up a whole picture of
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00:20:54,900 --> 00:20:59,037
the sky, it's going to take
MMS about 30 milliseconds.
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So it really is sort of
game-changing technology.
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The current two dozen or
so operating satellites will be
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enhanced with new missions
under development. The Japanese
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00:21:14,800 --> 00:21:18,594
Space Agency will be
launching their next solar physics
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00:21:18,606 --> 00:21:22,140
satellite, Solar-C. The
Indian Space Agency will be
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00:21:22,140 --> 00:21:26,315
launching Aditya to study the
Sun's coronal mass ejections
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00:21:26,327 --> 00:21:30,160
and magnetic field structures.
The Deep Space Climate
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00:21:30,160 --> 00:21:33,657
Observatory will maintain
real-time solar wind monitoring
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00:21:33,669 --> 00:21:37,360
capabilities critical to the
accuracy and lead time of space
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00:21:37,360 --> 00:21:41,813
weather alerts and forecasts.
The European Space Agency's
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00:21:41,825 --> 00:21:46,520
Solar Orbiter will be launched
in 2018 and fly closer to the
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Sun than the planet
Mercury to study how the
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00:21:49,179 --> 00:21:51,660
Sun creates and
controls its heliosphere.
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00:21:54,980 --> 00:21:58,618
Also planned for a 2018 launch
is NASA's Solar Probe Plus.
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It will approach the Sun more
closely than any other probe
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00:22:02,280 --> 00:22:06,980
before, just 3.8 million miles
from the surface of the star.
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Scientists have long wanted
to send a probe through the
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00:22:13,885 --> 00:22:17,080
Sun's outer atmosphere. The
spacecraft will be exposed to
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00:22:17,080 --> 00:22:22,172
temperatures approaching
1,370 degrees Celsius. Together
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they will continue to monitor,
study and discover the
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secrets of this nuclear anvil
that supplies us with light and life.
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Aside from the science, the
images captured reveal to us
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the beauty and power of
this, our nearest star in all its
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grandeur.
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00:22:59,880 --> 00:23:00,829
NASA Jet Propulsion
Laboratory, California Institute of
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00:23:00,841 --> 00:23:01,820
Technology California
Institute of Technology California
335
00:23:01,820 --> 00:23:07,980
Institute
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00:23:07,980 --> 00:23:07,980
of Technology
32049
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