MERCURY’S puny magnetic field may be so weak thanks to constant wrangles with the solar wind.
NASA’s Mariner 10 mission detected a magnetic field around our solar system’s innermost planet in 1974, but its cause remained a mystery – until recent measurements suggested that Mercury’s core may be partly molten. As with Earth, these “moving parts†could act like a dynamo, generating electricity and consequently a magnetic field. But that cannot explain why Mercury’s field is so weak, says Karl-Heinz Glassmeier at the Institute for Geophysics and Extraterrestrial Physics at Braunschweig, Germany.
The answer may lie at the magnetopause – the boundary between Mercury’s magnetic field and the solar wind. Glassmeier’s calculations show that strong electric currents generated there would create a secondary magnetic field, which – given the direction of the solar wind – would oppose the polarity of Mercury’s own field, weakening it (Geophysical Research Letters, vol 34, p L22201). This doesn’t happen on Earth as its magnetopause field is too far from the surface to have an effect.
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