This
article is the ninth in a series on NASA High-Performance
Computing
and Communications (HPCC) research teams.
Galileo Galilei,
full-time astronomer, offered this observation about the sun in the 1600s:
"Spots are on the surface of the solar body where they are produced
and also dissolved, some in shorter and others in longer periods. They
are carried around the sun, an important occurrence in itself."
As Galileo
knew better than most, things are not always what they appear to be. The
sun is more than a hot disk on a flat sky. Instead, Galileo found a fiery
ball spinning in space with spots dancing across it.
His subsequent
campaign for a sun orbited by the planets challenged authorities of the
day, and Galileo, who some call "the first scientist," lived
his last years under house arrest.
History may
be repeating itself as another struggle ensues between astrophysicists
who rely on supercomputer simulations to analyze the sun and old-school
astronomers who rest on empirical data alone.
Making
sense of data
The
problem with empirical data is it can only take you so far. Generations
of astronomers vindicated Galileo as they built upon his work. Today,
ground-based telescopes and spacecraft capture the sun's basic make-up
and highly dynamic surface.
Astronomy's
dilemma is that these observations say little about what happens inside
the sun, the source of the energy and magnetism that permeates the solar
system.
Financed
by NASA, HPCC research leader Andrea Malagoli studies mechanisms that
create these forces and motions that pull them through and out of the
sun. "You need to understand the physics behind the observations,"
says Malagoli. The University of Chicago astrophysicist insists that "supercomputer
simulations are the only tool observational people have to make sense
of data and go on to plan new missions."
Malagoli
and his collaborators have confidence in their simulations because they
reproduce observed physical features. These include a granular surface
pattern and variations in temperature and magnetic fields.
Despite these
encouraging results, the research community has long resisted accepting
simulations as scientific discoveries. Resistance to new methods, as we
know, is as old as the scientific method itself and dates back to when
Galileo was collecting the first data on the sun.
"The
problem is when you do simulations, typically you work on well-known equations
and physical principles," Malagoli explains. "You are not developing
any new equation, nor are you deriving rigorous mathematical solutions
to existing equations."
"In
many ways computation is actually closer to an experimental science,"
he adds. "So, the more conservative physics environment is resisting
this approach because they think you're much better off doing some back-of-the-envelope
calculations or some very abstract model that often tells you little about
reality. There is no question that all the recent advances in understanding
solar physics and other parts of astrophysics come from simulations."
The active
sun
Simulating
the sun is no simple matter. Its sheer enormity presents one challenge.
Nearly 110 Earths could line up across its equator and 1.3 million Earths
could fit inside. Complicating things further is that simulations must
treat motions ranging in size from the sun's 1.4 million-kilometer diameter
down to less than one kilometer.
Add all the
physics equations to be solved, and "current supercomputers are almost
like little pocket calculators compared to what you would really need
to accomplish the task," Malagoli says.
To get around
that problem, NASA's HPCC Program supports Malagoli's research team in
developing multiple simulation codes to analyze different aspects of the
sun's behavior, which comes out in two distinct personalities.
One personality
is active, producing sunspots and spectacular outbursts such as
solar flares over an 11-year cycle of boom and bust. The other personality
is quiet, a day-to-day, workhorse production of heat and light.
Playing a
clear role in the active sun is magnetism. X-ray observations show large
magnetic fields accompanying dramatic surface phenomena. Some of these
events inject the solar wind with magnetic and charged particles that
can knock out satellites, and occasionally power grids, when blowing past
Earth.
Observations
stop at the magnetic fields' presence, however, and don't tell how they
are created or how they move to the sun's surface. Understanding these
issues will ultimately contribute to predicting when potentially destructive
events will occur.
In
work destined for coupling with solar weather forecasts, Malagoli's University
of Colorado colleagues Juri Toomre and Nic Brummell are simulating the
large-scale magnetic field involved in the active sun.
They have
been testing the widely held theory that portions of the sun rotating
at varying speeds pump its magnetic field from a big storage area in the
middle. While the basic mechanism has been known for 40 years, the computations
are the only means to study specific effects.
Malagoli,
who hails from the same northern Italian village as opera star Luciano
Pavarotti, likens this solar process to making pasta. "The way you
produce a magnetic field is how you produce noodles. You stretch your
dough," he says. "Stretching and folding creates strong lines
of magnetic field. We haven't gotten the details right. That is where
most of our work comes in and is why we need these big simulations."
The quiet
sun
In the last
few years, observational tools have gotten powerful enough to find the
quiet sun generating magnetic fields of its own. While the amounts are
much smaller, these fields seem to be important in getting heat out of
the sun so it can supply, either directly or indirectly, all the Earth's
energy.
Simulations
are piecing together the elements of this story. The sun creates energy
by fusing hydrogen protons within its searing core (approximately 14 million
degrees Celsius). Radiation transports the energy to the next, cooler
region. About two-thirds of the way to the surface, the physics changes
and radiation cannot move all the energy anymore.
Matter
throughout the sun is plasma, a very hot gas of freely floating protons
and electrons. The plasma in the star's upper third must start boiling,
or convecting, to carry energy. "That is why the sun is so
interesting, because you deal with so many different issues, depending
on what layer you're studying," Malagoli says.
Like a wider
telescope mirror, a faster computer can see a bigger portion of
a celestial object or focus its resolution on smaller details. Because
there are trade-offs in the complexity of physics one can simulate, Malagoli's
team pursues both options.
The University
of Minnesota's Paul Woodward and David Porter simulate convection throughout
the sun's outer ring, techniques they have applied to studying other stars,
including red giants. At the University of Chicago, Fausto Cattaneo and
Anshu Dubey's simulations take on a smaller chunk to determine how and
where these motions produce magnetic fields -- the well-known solar
dynamo phenomenon.
"By
using a big enough computer, we can set up a system we believe roughly
reproduces working processes responsible for generating magnetic fields,"
says Cattaneo, an astrophysicist originally from Rome.
Cattaneo
and Dubey's latest calculation considers a region about 50,000 kilometers
across and 6,000 kilometers deep. It represents the plasma as a box of
fluid divided into 134 million smaller boxes. The supercomputer solves
the physics equations in each box and advances the solutions 100,000 steps
in time.
With all
that number-crunching, three hours of simulated solar time consumes three
weeks of NASA HPCC's 512-processor CRAY T3E at Goddard Space Flight Center.
Running at 50 billion mathematical operations per second, it generates
more than four trillion bytes of data, an output equal to three million
books.
Ten times
the size of the team's first NASA-supported simulations in 1993, "this
is probably the largest simulation to date in studying magnetic fields,"
Malagoli says. "That's why it is important to go through all these
performance milestones with HPCC."
The simulation
begins with the fluid not moving. As if turning up a stove burner, heat
from below starts boiling the fluid. The surface becomes a meeting place
for rising, hot fluid and sinking, cooler fluid.
One reason
the simulation takes so long is that it must continue until the convective
motions repeat themselves. After all, the sun has been doing that for
millions of years! 
Magnetic
fields arise because the simulated fluid mimics the plasma's ability to
conduct electricity. "It is a certainty that churning a highly conductive
fluid will generate a magnetic field," Cattaneo says. Alleys of cooler,
sinking fluid concentrate the magnetic fields, which flail around like
spaghetti.
As it follows
these dynamics, the simulation begins to resolve the paradox of the sun's
atmosphere being nearly one million degrees hotter than its surface. "There's
something really bizarre going on. It is not conduction or radiation because
they move energy down a gradient. You cannot convince heat to go the wrong
way!" Cattaneo says.
"We're
finding that it's all this evolving of magnetic fields that keeps bumping
heat into the atmosphere, and that's why it's so hot," he explains.
"The total contribution to this emission doesn't just come from the
active regions; it comes from magnetic fields all over the surface of
the sun."
One step
ahead
The
phenomena probed by the quiet sun calculation are beyond observations'
limits, both physical (even spacecraft cannot see below 100 kilometers
or so) and temporal (convection's magnetic fields last only five minutes).
"I challenge
you to find someone who by hand can find a solution of the equations that
resembles anything like that," Malagoli stresses.
Simulations
keeping ahead of observations also can contribute to future missions,
as Cattaneo describes. "You design an instrument to measure things
you believe are important. To know what to measure, you have to have some
idea of what is going on," he says. "That understanding comes
from setting up simulations. If you have no idea what you're looking for,
chances are you're not going to find it."
Cementing
the relationship between observation and simulation, this HPCC team's
results are serving as reference models for planning NASA's Solar-B, a
spacecraft slated for launch in 2003.
"As
long as there are missions, you will need HPCC," Malagoli says. 

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