Earth Magnetic Field: the Dynamo Theory

 

  

Last week I had a conversation with Mike about the magnetic poles. I explained to him that the poles tend to go walkabout. The North magnetic pole moves from North Canada towards Siberia at about 55 – 60 kilometres per year. Then Mike asked: is there a link between the North and South magnetic poles positions?

No but yes. On the “no” side it can be said that over a period of time one pole can be relatively quiet while the other one runs. On the “yes” side the poles are a manifestation of the Earth Magnetic Field, so the cause of their existence and movements is the same.

Many years ago scientists – including Einstein – thought that the totality of the Earth formed a permanent magnet. But since then it was observed that the Earth magnetic field force varied and that its polarity has changed many times in the distant path. A permanent magnet can lose strength over time, but it can’t change polarity. You need something like an electromagnet. And sure enough the Earth outer core, located about 2900 km under the surface, looks like one of those, or rather like a bunch of them loosely coupled together. 

The Dynamo

The outer core is made of highly conductive liquid metal (mainly nickel and iron). It is very hot at the bottom and less hot at the top, which induces convection movements. And it spins around. It all looks like a big dynamo. The current model to explain all this is very aptly named the Dynamo theory.

 

References:

Outer Core: https://www.nationalgeographic.org/encyclopedia/core/

Dynamo theory: https://en.wikipedia.org/wiki/Dynamo_theory




References:


Outer Core: https://www.nationalgeographic.org/encyclopedia/core/

Dynamo theory: https://en.wikipedia.org/wiki/Dynamo_theory


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