The northern lights (above) and their lesser-known sibling the southern lights, aurora borealis and aurora australis, respectively, undulate across the skies in hazy green and sometimes red ribbons near Earth’s polar regions. The two phenomena aren’t identical, however, and now researchers think they know why. Aurorae appear as solar wind, a gust of charged particles emitted by the sun, blows across Earth’s magnetic field. Because the charged particles flow along symmetrical lines in Earth’s magnetic field linking the north and south poles, it made sense to assume the atmospheric displays in each hemisphere would mirror each other. Advances in Earth...