by Annie Sneed
September 16, 2014
from ScientificAmerican Website
Earth's magnetic field is shown in
AND PAUL H. ROBERTS University of California, Los Angeles
Earth's magnetic north and south poles have flip-flopped (Reversals of the Earth's Magnetic Field) many times in our planet's history - most recently, around 780,000 years ago.
The European Space Agency's satellite array dubbed "Swarm" revealed that Earth's magnetic field is weakening 10 times faster than previously thought, decreasing in strength about 5 percent a decade rather than 5 percent a century.
A weakening magnetic field may indicate an impending reversal, which scientists predict could begin in less than 2,000 years.
Magnetic north itself appears to be moving toward Siberia.
Geophysicists do not yet fully understand the process of geomagnetic reversals, but they agree that our planet's field is like a dipole magnet. Earth's center consists of an inner core of solid iron and an outer core of liquid iron, a strong electrical conductor.
The liquid iron in the outer core is buoyant, and as it heats near the inner core, it rises, cools off and then sinks. Earth's rotation twists this moving iron liquid and generates a self-perpetuating magnetic field with north and south poles.
Every so often the flow of liquid iron is disturbed locally and twists part of the field in the opposite direction, weakening it. What triggers these disturbances is unknown.
It seems they are an inevitable consequence of a naturally chaotic system, and geophysicists observe them frequently in computer simulations.
Typically the local reversal peters out after 1,000 years or so, but sometimes the twisting of the field continues to spread and eventually succeeds in reversing the polarity of the entire field.
The flipping takes an average of 5,000 years; it can happen as quickly as 1,000 years or as slowly as 20,000 years.
There is a good chance the weakening magnetic field that the Swarm satellites observed will not lead to a full flip. Indeed, Gary A. Glatzmaier notes that there have been several false starts over geologic history.
The intensity of Earth's magnetic field, though waning, now equals its average strength over millions of years. The field would need to weaken at its current rate for around 2,000 years before the reversal process actually begins.
It is hard to know how a geomagnetic reversal would impact our modern-day civilization, but it is unlikely to spell disaster.
Although the field provides essential protection from the sun's powerful radiation, fossil records reveal no mass extinctions or increased radiation damage during past reversals. A flip could possibly interfere with power grids and communications systems - external magnetic field disturbances have burned out transformers and caused blackouts in the past.
But Glatzmaier is not worried.