Dolores Beasley

Headquarters, Washington, DC

March 30, 2000

(Phone: 202/358-1753)

Susan Hendrix

Goddard Space Flight Center, Greenbelt, MD

(Phone: 301/286-7745)

RELEASE: 00-50

Like blood pulsing in an artery, newly discovered currents of gas beat deep
inside the
Sun, speeding and slackening every 16 months.

The solar “heartbeat” throbs in the same region of the Sun suspected of
driving the
11-year cycle of solar eruptions, during which the Sun goes from stormy to quiet
and back
again. Scientists are hopeful that this pulse can help them unravel the origin
and operation
of the solar cycle.

The discovery comes from an international team pooling observations from
the
Michelson Doppler Imager (MDI) instrument on the Solar and Heliospheric
Observatory
(SOHO) spacecraft and from a worldwide chain of ground stations called the
Global
Oscillation Network Group (GONG). Dr. Rachel Howe of the National Science
Foundation’s
National Solar Observatory in Tucson, AZ, and her colleagues announce their
results in the
March 31 issue of the journal Science.

“We are excited to see the first evidence of changes close to the location
of the solar
dynamo, the region that generates the Sun’s large-scale magnetic field and is
believed to
drive the solar cycle,” says lead author Howe. “It’s very surprising to find
that the changes
have such a short period — 16 months or so rather than the 11 years of the
solar cycle.”

Eruptions on the Sun are believed to result from the buildup and rapid
release of stress
in solar magnetic fields. Just as a twisted rubber band can break suddenly, the
solar
magnetic field under stress “breaks” to a new, lower-energy configuration,
releasing
tremendous energy. The frequency and intensity of these eruptions rises to a
peak over an
11-year cycle, and scientists believe the cycle is also tied to magnetic
activity.

To explain the solar cycle, theorists visualize a dynamo inside the Sun,
where movement
of electrically charged gas generates a magnetic field. Because magnetic fields
are

produced by moving electric charges, relative motions between neighboring layers
of
electrified gas supposedly drive the dynamo. As the years pass, so the theory
goes, the
magnetic field becomes too strong for the gas to hold. As a result, the magnetic
field breaks
out to the solar surface, creating active regions with sunspots and magnetic
explosions. The
changes now observed are at the right depth for a dynamo.

The flows of gas under study occur about 140,000 miles beneath the visible
surface, or
almost a third of the way down to the center of the Sun. Here is the supposed
dynamo
region (tachocline), where the turbulent outer region, the convective zone,
meets the orderly
interior, or radiative zone. The speed of the gas in this “dynamo” region
changes abruptly.
Near the equator the outer gas travels around the Sun’s axis of rotation faster
than the inner
gas. The difference in speed between the two layers gradually diminishes as
latitude
increases, until at the polar regions, the situation is reversed, with the inner
gas rotating
faster than the outer gas.

The news from SOHO and GONG is that the contrast in speed between layers
above
and below the supposed dynamo region can change by 20 percent in six months.
When the
lower gas speeds up, the upper gas slows down, and vice versa. In observations
spanning
four and a half years, from May 1995 to November 1999, these alternations in
speed
occurred three times. They indicate a heartbeat of the Sun at one pulse per 15
to 16 months
in equatorial regions, and perhaps faster at higher latitudes.

Scientists are able to probe the solar interior by analyzing ripples on the
Sun’s surface
produced by sound waves reverberating through the Sun. Analysis of solar sound
waves is
the science of helioseismology, and it opened the Sun’s gaseous interior to
investigation in
much the same way as seismologists learned to explore the Earth’s rocky interior
with
earthquake waves.

The Science report also raises the question of whether there may be a link
between the
deep changes and another remarkable phenomenon seen by helioseismologists nearer
the
surface. At depths down to 37,000 miles, bands of gas parallel to the equator
move slightly
faster or slower than the average speed for their solar latitudes. Although the
effect is
subtle, it is very persistent, and the scientists see the bands of fast and slow
gas gradually
moving from high latitudes toward the equator as the years go by. A similar
“equator-ward”
shift has long been observed in the locations of sunspots, as the solar cycle
approaches its
maximum of activity.

SOHO is a project of international cooperation between the European Space
Agency
and NASA. GONG is an international project led by the U.S. National Science
Foundation,
with the participation of twenty nations.

More information and images are available on the Internet at:
http://pao.gsfc.nasa.gov/gsfc/spacesci/sunearth/sunearth.htm#pulse