Abstract
The Earth's main magnetic field changes slowly over a period of years, and also exhibits regular daily changes with both solar and lunar components, and magnetic storms. Studies of these changes can be used as a probe into the Earth's interior, the upper atmosphere and the oceans. -Author
Cite
CITATION STYLE
APA
Winch, D. E. (1989). The Earth’s magnetic field. Journal & Proceedings - Royal Society of New South Wales, 122(1–2), 1–9. https://doi.org/10.1029/00eo00131
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