Abstract
The Earth’s magnetic field is shaped roughly as a magnetic dipole, with the poles currently located proximate to the planet’s geographic poles. At the equator of the magnetic field, the magnetic field strength at the planet’s surface is 3.05 × 10−5 T, with global magnetic dipole moment of 7.91 × 1015 T m3.
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The author wishes to acknowledge Richard B. Cathcart for correcting the English and for offering useful advices and suggestions.
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Bolonkin, A.A. (2015). Artificial Magnetic Field for Venus. In: Badescu, V., Zacny, K. (eds) Inner Solar System. Springer, Cham. https://doi.org/10.1007/978-3-319-19569-8_17
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DOI: https://doi.org/10.1007/978-3-319-19569-8_17
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