Impressum  Copyright © Klaus Piontzik  
German Version 
10  Summary of the fourier analysis
10.1  The longitude position of the extreme values
How already, derived in
the chapter 4, the longitude positions of the
extreme values for the whole field can be shown by an
equation. This equation could be refined in chapter 9.5. Now it would be pointed out to the fact that this equation counts practically to all appearing extreme values of the magnetic field. 

m is an element of the integers (...3,2,1,0,1,2,3...) and λ_{0} = 13,5 degrees of west  
Because the zero point with λ_{0}= 13,5 degree of west longitude and the value of Lundquist and Veis (see chapter 4.4) correspond, seen on a global scale well, so it can be ascertained:  
All
magnetic extreme values stand in relation to the equator axes of a threeaxle ellipsoid 
10.2  Evaluation of the extreme values
If one looks at the earth
virtually from above, namely thus one looks down on the
north pole or the south pole and applies certain circles
of latitude (0, 30, 45, 60 degrees), one receives a
radial coordinate system. Mark of the axes for a threeaxle ellipsoid (the blue cartesian coordinate system with λ_{0} = 13,5 degree of west) and registration of all magnetic extreme values found up to now produces both pictures 10.1 and 10.2. 
The colours in it
signify: Green stands for the basic field ZS, Magenta for
the tesseral field and orange for the appearing extreme
values of the whole field from chapter 2.6. Die Farben darin bedeuten: Grün steht für das Grundfeld ZS, Magenta für das tesserale Feld und orange für die vorkommenden Extrema des Gesamtfeldes aus chapter 2.6. 
North hemisphere  South hemisphere  
The values on the north hemisphere can be accommodated in a narrow zone (7086 degrees of west). Likewise the values on the south hemisphere.  
From the illustration
10.1 arises: Practically all extreme values on the north hemisphere can be accommodated in a narrow zone by 5590 degrees of west or 90125 degrees of east. Merely both minima of the tesseral field form an exception here. From the illustration 10.2 arises: The extreme values on the south hemisphere can be likewise arranged in a narrow zone of 2550 degrees of west or 130155 degrees of east. The exception is formed here by both minima of the basic field ZS. The extreme zone on the north hemisphere is shifted about 3540 degrees compared with the southern extreme zone. 
In the book the
phenomenon of the movement is explained, namely with the
help of the maps of the vertical intensity and the
Inklination. Besides, even the place of the sturgeon source can be localised. 
10.3  Basic fields
Especially interesting in the fourier analysis is that between the tesseral portion of the earth magnetic field and the basic fields a narrow connection exists: Every term in the tesseral portion B_{T} can be shown as a basic field. (see chapter 5) Here some examples to the illustration: 
8,4184·cosλ·sinφ  
8,8172·cosλ·sin2φ  
5,2834·cosλ·sin3φ  
1,6626·cos2λ· sinφ  
0,6739·cos2λ·sin2φ  
1,6343·cos2λ·sin3φ 
As at the examples or in
the equation for B_{T} is to be seen, all
appearing terms of the tesseral part insist of spherical
harmonics how they also appear in the equation of Gauß (chapter 2.7). The tesseral portion of the
earth magnetic field consists of basic fields, i.e. from grid
structures similar to the Hartmanngrid. One can show the magnetic field of the earth from the sum of the tesseral part with the basic field ZS: 
B = 47,2183 + B_{ZS} + B_{T} μT (mükroTesla) 
The consequence from it is: 
The
external magnetic field of the earth can be completely
described by a sum of basic fields (grids) 