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 Study:
Earth's magnetic field is changing
Observing fluid motions in core could help
scientists predict future changes
By Jeremy Hsu
Source: www.msnbc.msn.com/id/26273268/
The
innermost part of the earth. The outer core extends
from 2500 to 3500 miles below the earth's surface
and is liquid metal. The inner core is the central
500 miles and is solid metal.
Something beneath the surface is changing Earth's
protective magnetic field, which may leave satellites
and other space assets vulnerable to high-energy
radiation.
The gradual weakening of the overall magnetic
field can take hundreds and even thousands of
years. But smaller, more rapid fluctuations within
months may leave satellites unprotected and catch
scientists off guard, new research finds.
A new model uses satellite data from the past
nine years to show how sudden fluid motions within
the Earth's core can alter the magnetic envelope
around our planet. This represents the first
time that researchers have been able to detect
such rapid magnetic field changes taking place
over just a few months.
"There are these changes in the South Atlantic,
an area where the magnetic field has the smallest
envelope at one third [of what is] normal," said
Mioara Mandea, a geophysicist at the GFZ German
Research Center for Geosciences in Potsdam, Germany.
Even before the newly detected changes, the
South Atlantic Anomaly represented a weak spot
in the magnetic field — a dent in Earth's
protective bubble
Bubble bobble
The Earth's magnetic field extends about 36,000
miles into space, generated from the spinning
effect of the electrically-conductive core
that acts something like a giant electromagnet.
The field creates a tear-drop shaped bubble
that has constantly shielded life on Earth
against much of the high-energy radiation flowing
from the sun.
The last major change in the field took place
some 780,000 years ago during a magnetic reversal,
although such reversals seem to occur more often
on average. A flip in the north and south poles
typically involves a weakening in the magnetic
field, followed by a period of rapid recovery
and reorganization of opposite polarity.
Some studies in recent years have suggested
the next reversal might be imminent, but the
jury is out on that question.
Measuring interactions between the magnetic
field and the molten iron core 1,864 miles down
has proven difficult in the past, but the constant
observations of satellites such as CHAMP and
Orsted have begun to bring the picture into focus.
Electric storm
Mandea worked with Nils Olsen, a geophysicist
at the University of Copenhagen in Denmark,
to create a model of the fluid core that fits
with the magnetic field changes detected by
the satellites.
However, the rapid weakening of the magnetic
field in the South Atlantic Anomaly region could
signal future troubles for such satellites. Radiation
storms from the sun could fry electronic equipment
on satellites that suddenly lacked the protective
cover of a rapidly changing magnetic field.
"For satellites, this could be a problem," Mandea
told SPACE.com. "If there are magnetic storms
and high-energy particles coming from the sun,
the satellites could be affected and their connections
could be lost."
The constant radiation bombardment from the
sun blows with the solar wind to Earth, where
it flows against and around the magnetic field.
The effect creates the tear-drop shaped magnetosphere
bubble, but even the powerful field cannot keep
out all the high-energy particles.
Topsy-turvy history
A large sunspot set off a major radiation storm
in 2006 that temporarily blinded some sun-watching
satellites. Astronauts on the International
Space Station retreated to a protected area
as a precaution to avoid unnecessary radiation
exposure.
The Earth's overall magnetic field has weakened
at least 10 percent over the past 150 years,
which could also point to an upcoming field reversal.
Mandea and Olsen hope to continue refining their
model with updated observations, and perhaps
to eventually help predict future changes in
the Earth's magnetic field.
The study was detailed in the May online edition
of the journal Nature Geoscience.
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