Evaluation of the Inclination of Axis and Elliptic Orbital of the Earth
Abstract
The magnetic field of the earth is practically the same as that of a bar magnet. Magnetic interactions of masses are associated by their shape, distance, direction, position, and type of poles. According to Fleming's rules, directions of the current, motion, and magnetic field in a dynamo or electromotor are different, and the rules are valid in space. Because of the inclination of axis of the earth in stable direction, axis of the sun and the earth are stay in parallel planes in March and September. N (south) and S (north) pole of the earth are bend to the sun in December and June respectively. Elliptic orbital of the earth is close to the sun in March and September, and far in December and June. The distance resulting from the repulsion between the S poles is 21.6poles. According to information above, evaluation of the earth's axial rotation in sun's magnetic field explains stable axial inclinations of the earth. Slightly face-to-face positions of magnetic poles of the earth and the sun in December and June must produce different (stronger) magnetic interactions. Therefore, due to difference of the magnetic interactions and positions, distance between the sun and the earth is variable and gives an elliptic orbital. These suggestions should be evaluated by experimental motions of magnets.
- Publication:
-
APS Division of Plasma Physics Meeting Abstracts
- Pub Date:
- November 2002
- Bibcode:
- 2002APS..DPPCP1012C