Credits: data from Craig DeForest, SwRI
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Ever since the 1950s discovery of the solar wind – the constant flow
of charged particles from the sun – there’s been a stark disconnect
between this outpouring and the sun itself. As it approaches Earth, the
solar wind is gusty and turbulent. But near the sun where it originates,
this wind is structured in distinct rays, much like a child’s simple
drawing of the sun. The details of the transition from defined rays in
the corona, the sun’s upper atmosphere, to the solar wind have been,
until now, a mystery.
Using NASA’s Solar Terrestrial Relations Observatory, or STEREO,
scientists have for the first time imaged the edge of the sun and
described that transition, where the solar wind starts. Defining the
details of this boundary helps us learn more about our solar
neighborhood, which is bathed throughout by solar material – a space
environment that we must understand to safely explore beyond our planet.
A paper on the findings was published in The Astrophysical Journal on Sept. 1, 2016.
“Now we have a global picture of solar wind evolution,” said
Nicholeen Viall, a co-author of the paper and a solar scientist at
NASA’s Goddard Space Flight Center in Greenbelt, Maryland. “This is
really going to change our understanding of how the space environment
develops.”
Both near Earth and far past Pluto, our space environment is
dominated by activity on the sun. The sun and its atmosphere are made of
plasma – a mix of positively and negatively charged particles which
have separated at extremely high temperatures, that both carries and
travels along magnetic field lines. Material from the corona streams out
into space, filling the solar system with the solar wind.
But scientists found that as the plasma travels further away from the
sun, things change: The sun begins to lose magnetic control, forming
the boundary that defines the outer corona – the very edge of the sun.
“As you go farther from the sun, the magnetic field strength drops
faster than the pressure of the material does,” said Craig DeForest,
lead author of the paper and a solar physicist at the Southwest Research
Institute in Boulder, Colorado. “Eventually, the material starts to act
more like a gas, and less like a magnetically structured plasma.”
The breakup of the rays is similar to the way water shoots out from a
squirt gun. First, the water is a smooth and unified stream, but it
eventually breaks up into droplets, then smaller drops and eventually a
fine, misty spray. The images in this study capture the plasma at the
same stage where a stream of water gradually disintegrates into
droplets.
Credits: NASA's Goddard Space Flight Center/Lisa Poje
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Before this study, scientists hypothesized that magnetic forces were
instrumental to shaping the edge of the corona. However, the effect has
never previously been observed because the images are so challenging to
process. Twenty million miles from the sun, the solar wind plasma is
tenuous, and contains free-floating electrons which scatter sunlight.
This means they can be seen, but they are very faint and require careful
processing.
In order to resolve the transition zone, scientists had to separate
the faint features of the solar wind from the background noise and light
sources over 100 times brighter: the background stars, stray light from
the sun itself and even dust in the inner solar system. In a way, these
images were hiding in plain sight.
Credits: data from Craig DeForest, SwRI
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Images of the corona fading into the solar wind are crucial pieces of
the puzzle to understanding the whole sun, from its core to the edge of
the heliosphere, the region of the sun’s vast influence. With a global
perspective, scientists can better understand the large-scale physics at
this critical region, which affect not only our planet, but also the
entire solar system.
Such observations from the STEREO mission – which launched in 2006 –
also help inform the next generation of sun-watchers. In 2018, NASA is
scheduled to launch the Solar Probe Plus mission, which will fly into
the sun’s corona, collecting more valuable information on the origin and
evolution of the solar wind.
STEREO is the third mission in NASA Heliophysics Division’s Solar
Terrestrial Probes program, which is managed by Goddard for the Science
Mission Directorate, in Washington, D.C.
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