15. Ionosphere Dansk

 

In the ionosphere we find the so-called Ionospheric dynamo.

In the northern hemisphere a huge electric current, the so-called “ring current”, moves anticlockwise, and conversely at the southern hemisphere it moves clockwise.

 

According to this theory space will contract in the centre of an extended mass.

It must be assumed that four billion of years ago there was only one large extended mass of ions which covered both the northern and southern thermosphere. Immediately after their creation the Coriolis Force began separating the mass into 2 parts, one moving clockwise and one moving anticlockwise.

 

 

What we really see here can be thought of as two hurricanes of particles. The Coriolis Force powers the process and the force of gravity keeps the mass together.

 

This phenomenon takes place on the side of the earth experiencing daytime.

Ions move to higher attitudes during daytime, this ion movement occurs in a circulating pattern.

 

It must be expected that the low pressure must be weaker in the centre of these 'hurricanes', similar to what we see in a hurricane closer to earth. Here is also an opportunity to test the validity of this theory.

  

 

 

 

Copyright © 2006 - 2007 Bjarne Lorenzen www.science27.com