Wednesday, October 2, 2013
Earth’s Core Spin Variation
It is an explanation, yet I do not particularly trust it. It is a little too glib and ignores polarity reversal and generally presumes the magnetic dynamo model which also looks good on first glance. Let us simply understand it as speculative theory in want of an alternative speculative theory. There is plenty of that going around in the world of empirical science.
What they really mean here is that the magnetic effect postulated is sufficient to cause balanced acceleration in east west directions. This is a worthy conjecture that now needs to somehow be confirmed.
All good stuff and may help. My alternative conjecture allows us to use a conductive shell of liquid carbon as our field generator and reduce the mass that needs to move for crustal movement generally and allows easy pole reversal. As evidence we have the pole reversals, the non-homogenous magnetic surface field and the kimberlitic pipes evidencing carbon jets cutting to the surface at high velocity.
New research shows Earth’s core spins in opposite directions
According to new research from UK and Swiss scientists, the core of our planet is more complicated than we thought, with layers rotating in different directions, and it all may solve a mystery about the Earth's magnetic field that's persisted for over 300 years.
The Earth's core is separated into two different layers. At the centre is the solid inner core, which is surrounded by the liquid outer core — both made up of a mixture of nickel and iron. Scientists figured out the structure of the two layers decades ago, based on watching seismic waves from earthquakes passing through the planet, and they also discovered that it is circulations in the hot, liquid metal of the outer core that generate the Earth's magnetic field.
There are some things about the core that have remained a mystery, though. A study from 2005 revealed that, although the inner core rotates in the same direction as the surface, it actually rotates slightly faster than the surface. That strange result joins another curious finding, from back in 1692,when astronomer Edmond Halley (of Halley's Comet fame) discovered that the Earth's magnetic field 'drifts' towards the west by a few degrees every decade.
A new study has finally offered an explanation for these two mysteries, tying everything together at last.
It started with researchers not only confirming that the inner core rotates faster than the surface, but also finding that the outer core rotates in the opposite direction. To find out what's going on, they used the Monte Rose supercomputer to run a simulation that was roughly 100 times more accurate than any previous model of the Earth's core. The simulation revealed that it's the Earth's magnetic field that's causing the layers of the core to spin like they do. It's providing an extra little push to the inner core, driving the added spin towards the east, while at the same time an equal and opposite reaction to that push is causing the 'backward' spin of the outer core towards the west.
The added bonus from their simulation is that it solved Halley's mystery as well. Since the outer core slowly rotates towards the west, the circulations within the liquid metal also rotate in that direction, and the magnetic field 'drifts' along with them.
The researchers are hoping that all of this will help scientists to better understand the behaviour of the core, and thus the planet's magnetic field.