The layers of the atmosphere and the magnetic field

	The magnetic field of the earth Lattice structures of the earth magnetic field

Impressum	Copyright © Klaus Piontzik


German Version

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:

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	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:

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:

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=Q·v 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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The Advanced Book: Planetary Systems

The theory, which is developed in this book is based on the remake and expansion of an old idea. It was the idea of a central body, preferably in the shape of a ball, formed around or in concentric layers. Democritus was the first who took this idea with his atomic theory and thereby introduced himself to the atoms as fixed and solid building blocks.
Is the atom used as a wave model, that allows to interpret concentric layers as an expression of a spatial radial oscillator so you reach the current orbital model of atoms.
Now, this book shows that these oscillatory order structures, described by Laplaceâ€™s equation, on earth and their layers are (geologically and atmospherically) implemented. In addition the theory can be applied on concentric systems, which are not spherical but flat, like the solar system with its planets, the rings that have some planets and the moons of planets or also the neighbouring galaxies of the milky way. This principle is applicable on fruits and flowers, such as peach, orange, coconut, dahlia or narcissus.
This allows the conclusion that the theory of a central body as a spatial radial oscillator can be applied also to other spherical phenomena such as spherical galactic nebulae, black holes, or even the universe itself. This in turn suggests that the idea of the central body constitutes a general principle of structuring in this universe as a spatial radial oscillator as well as macroscopic, microscopic and sub microscopic.

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