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Lattice structures of the earth magnetic field
 
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14 - The layers of the atmosphere

14.1 - Evaluation of the extreme distances in the atmosphere for n<21

As by the evaluation for the earth inside the lengths l' (for the atmosphere) are picked out from the table of the distances of the extreme layers ((table in chapter 12.2) and are sorted after size.

 

In memory: The distances l' were won from the following equation:
 
 Formula distances of extrema layers
 
All values are used for n<21 up to a centre distance of 7000 km. This corresponds to a (atmospheric) height of 700 km. Out of this the following table arises:

 

Centre distance n m k
km      
       
6991,974235 11 4 4
       
6989,489849 18 17 12
       
6982,492536 14 5 5
       
6982,090972 5 2 2
       
6977,163231 20 17 13
       
6974,597677 17 6 6
       
6968,255807 20 7 7
       
6960,739283 19 15 12
       
6938,821886 18 18 12
       
6938,432741 19 11 10
       
6931,394797 15 15 10
       
6917,72871 12 12 8
       
6904,770349 18 6 6
       
6898,142822 15 5 5
       
6888,231994 9 9 6
       
6885,92672 12 4 4
       
6866,204466 17 10 9
       
6859,464698 9 3 3
       
6846,251729 19 6 6
       
6841,340061 11 9 7
       
6829,912483 16 5 5
       
6804,587013 13 4 4
       
6804,172188 6 6 4
       
6796,70431 20 6 6
       
6783,318793 6 2 2
       
6782,436594 14 12 9
       
6779,690655 15 9 8
       
6773,908095 17 5
       
6771,524129 19 13 11
       
6771,034958 20 18 13
       
6769,07209 17 15 11
       
6760,482429 10 3 3
       
6755,606221 20 11 10
       
6752,915731 13 10 8
       
6745,118313 17 12 10
       
6740,779379 14 4 4
       
6733,302229 15 11 9
       
6727,352183 18 5 5
       
6689,771048 15 4 4
       
6688,253229 11 3   3
       
6688,218278 19 5 5
       
6674,749063 13 8 7
       
6666,665219 7 2 2
       
6664,012528 16 13 10
       
6657,90373 18 10 9
       
6654,998569 20 5 5
       
6649,655949 20 19 13
       
6648,333478 16 4 4
       
6638,166337 19 16 12
       
6633,883933 12 3 3
       
6614,200568 17 4 4
       
6612,718126 18 14 11
       
6601,072142 17 16 11
       
6597,933215 20 15 12
       
6592,213885 8 2 2
       
6591,907977 13 3 3
       
6585,742391 18 4 4
       
6561,761484 19 4 4
       
6558,809342 14 3 3
       
6546,103523 11 7 6
       
6545,820442 17 17 11
       
6541,736286 9 2 2
       
6541,361614 20 4 4
       
6537,861205 16 9 8
       
6534,421624 14 13 9
       
6532,240499 15 3 3
       
6510,60351 20 13 11
       
6510,584162 16 3 3
       
6505,909824 10 2 2
       
6492,695959 17 3 3
       
6484,622839 19 10 9
       
6479,551554 11 2 2
       
6477,747262 18 3 3
       
6465,125883 19 3 3
       
6459,588513 12 2 2
       
6454,371461 20 3 3
       
6453,386497 14 14 9
       
6444,102959 13 2 2
       
6437,717596 11 10 7
       
6436,871726 18 12 10
       
6431,846936 14 2 2
       
6421,979536 15 2 2
       
6414,918092 19 17 12
       
6413,917146 16 2 2
       
6407,244332 17 2 2
       
6401,658791 18 2 2
       
6396,936261 19 2 2
       
6392,907514 20 2 2
       
6388,26348 9 6 5
       
6386,948305 14 8 7
       
6359,11661 16 11 9
       
6355,758426 n 1 1

 

If one puts down the found distance values of the magnetic layers on a picture of the atmosphere (height<300 km), the following illustration 14.1 arises:
 Magnetic layers of the earth
Illustration 14.1 - Stratifications of the atmosphere and magnetic stratifications for n<21
 
In the areas of the ozone-, D-, E- and F-layer it comes to aggregations respectively compressions of magnetic stratifications. Also well to be seen is that the rooms between ozone-, D-, E- and F-layer belong to the oscillation spectrum.
The values of the magnetic stratification spectrum for n<21 fit in the atmospheric stratifications.
All found distance values establish the maximal possible stratification spectrum for n<21.

 

 

14.2 - Evaluation of the averages

As by the evaluation for the earth inside, the lengths l' for the atmosphere were picked out from the table of the distances of the extreme layers and were sorted after size.

92 values exist on a distance of 636 km. This corresponds to a cut of 6.9 km per value.

All distances with lower difference than the cut value are looked here. As to be seen, one can summarise these distances to areas. The distances which lie in an area, have been marked in the table in the same colour. The average won from it, respectively the converted height, can be found in both right columns of the table.

It is worth:
Height = average distance - 6371 km

6,371 km is the middle earth radius as used in the astronomy and geophysics.

 

Centre distance Difference Average distance Height
      Atmosphere
km km km km
       
6991,974235      
  2,48 6990,732 619,732
6989,489849      
  7,00    
6982,492536      
  0,40    
6982,090972      
  4,93    
6977,163231   6976,920 605,920
  2,57    
6974,597677      
  6,34    
6968,255807      
  7,52    
6960,739283      
  21,92    
6938,821886      
  0,39 6938,627 567,627
6938,432741      
  7,04    
6931,394797      
  13,67    
6917,72871      
  12,96    
6904,770349      
  6,63 6901,456 530,456
6898,142822      
  9,91    
6888,231994      
  2,31 6887,079 516,079
6885,92672      
  19,72    
6866,204466      
  6,74 6862,834 491,835
6859,464698      
  13,21    
6846,251729      
  4,91 6843,795 472,796
6841,340061      
  11,43    
6829,912483      
  25,33    
6804,587013      
  0,41 6804,379 433,380
6804,172188      
  7,47    
6796,70431      
  13,39    
6783,318793      
  0,88    
6782,436594      
  2,75    
6779,690655      
  5,78    
6773,908095   6775,855 404,855
  2,38    
6771,524129      
  0,49    
6771,034958      
  1,96    
6769,07209      
  8,59    
6760,482429      
  4,88    
6755,606221   6756,334 385,335
  2,69    
6752,915731      
  7,80    
6745,118313      
  4,34 6742,948 371,949
6740,779379      
  7,48    
6733,302229      
  5,95 6730,327 359,327
6727,352183      
  37,58    
6689,771048      
  1,52    
6688,253229   6688,747 317,748
  0,03    
6688,218278      
  13,47    
6674,749063      
  8,08    
6666,665219      
  2,65    
6664,012528      
  6,11    
6657,90373      
  2,91 6656,928 285,928
6654,998569      
  5,34    
6649,655949      
  1,32    
6648,333478      
  10,17    
6638,166337      
  4,28 6636,025 265,025
6633,883933      
  19,68    
6614,200568      
  1,48 6613,459 242,459
6612,718126      
  11,65    
6601,072142      
  3,14    
6597,933215      
  5,72    
6592,213885   6593,773 222,774
  0,31    
6591,907977      
  6,17    
6585,742391      
  23,98    
6561,761484      
  2,95 6560,285 189,285
6558,809342      
  12,71    
6546,103523      
  0,28    
6545,820442      
  4,08    
6541,736286      
  0,37    
6541,361614   6539,935 168,935
  3,50    
6537,861205      
  3,44    
6534,421624      
  2,18    
6532,240499      
  21,64    
6510,60351      
  0,02    
6510,584162   6509,032 138,032
  4,67    
6505,909824      
  13,21    
6492,695959      
  8,07    
6484,622839      
  5,07    
6479,551554   6480,640 109,641
  1,80    
6477,747262      
  12,62    
6465,125883      
  5,54    
6459,588513      
  5,22 6458,118 87,118
6454,371461      
  0,98    
6453,386497      
  9,28    
6444,102959      
  6,39    
6437,717596      
  0,85 6437,634 66,635
6436,871726      
  5,02    
6431,846936      
  9,87    
6421,979536      
  7,06    
6414,918092      
  1,00    
6413,917146      
  6,67    
6407,244332      
  5,59    
6401,658791   6400,349 29,349
  4,72    
6396,936261      
  4,03    
6392,907514      
  4,64    
6388,26348      
  1,32    
6386,948305      
  27,83    
6359,11661      
  3,36    
6355,758426      

 

If one puts down the found averages for the magnetic extreme layers on a picture of the atmosphere (height <300 km), the following illustration 14.2 arises:
 Average distances of the magnetic layers
Illustration 14.2 - Stratifications of the atmosphere and average layers
 
The averages virtually show the areas in which it comes to aggregations of magnetic stratifications.
All values of the average spectrum fit in the atmospheric stratifications.
Also well to be seen is, that the rooms between D-, E- and F-layer likewise belong to the oscillation spectrum,
i.e. the complete atmosphere shows an oscillation phenomenon.

 

 

14.3 - Evaluation of the distances in the atmosphere

If one takes the borders of the atmospheric layers and looks for oscillation distances which lie nearby, the following table occours:


Layer Height centre
distance
elected n m k
             
Ozon 30 6401 6401,658 18 2 2
Ozon 50 6421 6421,979 15 2 2
             
D 60 6431 6431,846 14 2 2
D 70 6441 6444,102 13 2 2
             
E 100 6471 6477,747 18 3 3
E     6479,551 11 2 2
E            
E 140 6511 6510,603 20 13 11
E     6510,584 16 3 3
E     6505,909 10 2 2
             
F 180 6551 6558,809 14 3 3
F     6546,103 11 7 6
F     6545,820 17 17 11
F     6541,736 9 2 2
F            
F 300 6671 6674,749 13 8 7
F     6666,665 7 2 2

 

As is to be seen, oscillations with m=2 and k=2 near the atmospheric borders appear as increased.. Putting the values for m and k in the equation for l' delivers:
 Formula for the atmospheric layers

 

If one uses successively the values 1,2.3 ... for n in the above equation, the following table arises:

 

n centre
distance
Height
     
1 31778,792 25407
2 11621,041 5250
3 8280,127 1909
4 7365,952 994,9
5 6982,090 611,1
6 6783,318 412,3
7 6666,665 295,6
8 6592,213 221,2
9 6541,736 170,7
10 6505,909 134,9
11 6479,551 108,5
12 6459,588 88,5
13 6444,102 73,1
14 6431,846 60,8
15 6421,979 50,9
16 6413,917 42,9
17 6407,244 36,2
18 6401,658 30,6
19 6396,936 25,9
20 6392,907 21,9

 

If one puts down the calculated values of the magnetic layers on a picture of the atmosphere (height<300 km), the following picture arises:
 Calculated values and the layers of the atmosphere
Illustration 14.3 - Stratifications of the atmosphere and calculated magnetic layers for 6<n<20

 

 

14.4 - Result

The following result can be derived from the previous considerations:

 


An oscillation structure forms the base of the layer construction of the atmosphere

This oscillation structure stands in relation to the magnetic oscillation spectrum

i.e. the layer distances, referred to the centre of the earth, are directly deducible from the magnetic distances

 

For 6<n<20 count to the atmospheric layers up to 300-km height:

 Formula for the atmospheric layers

 

Because the ozone-, D-, E and F-layer establish the electrically conducting layers of the atmosphere, that implies the magnetic extreme layers supply the basis for this conductivity.
The magnetic field is afflicted by light variations, is so not quite constant. However, this would have to be enough to induce a suitable electrical field. Is called:
A part of the electric earth field is induced by the magnetic earth field.
 
Because the magnetic oscillation structure stands in relation to the bowl construction of the earth and also to the stratifications of the atmosphere, the consequence is all together that the layers of the atmosphere show no pure surface phenomenon of this planet, but above the magnetic field, are connected with the inside of the earth. And from it results, that climate and weather of the earth are connected with the magnetic field.
 
The natural water- and air transports on the earth and in the atmosphere show also electric charge transports. And a moved electric charge finds out (experiences) in a magnetic field a force, the Lorentz force (F=Qv x B). With east-west or west-east current this leads to a force which points radial down or upwards.
The intensity of the grid fields amounts to about 14-16% of the complete intensity. Locally seen may be these very small forces, but because they are effective everywhere on the earth, they would have some influence on the global air/clouds/water currents.
The connections described here are not taken into consideration in all present weather or climate models at all.
 
It would be still considered which influence probably a change of the earth magnetic field on the atmosphere and their processes would have. There is here a certain probability, that the changes in climate of the last years, are induced partly by the likewise changing magnetic field.
 
Because certain layers of the atmosphere are connected with frequency, so to electromagnetic activities, there can be thought an electromagnetic emitter system with which a certain bowl, directly with certain frequency, is moved into oscillation.
And today this already happens. As an example the US-American Haarp project which is treated in the
chapter 19 in detail is to be mentioned here.

 

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